OBSERVATIONAL DATA OF THE SCIENTIFIC-RESEARCH DRIFTING STATION OF 1950-1951, VOLS. I-III.

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• Publication Date: October 10, 1957
• Content Type: REPORT

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STAT
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ASTIA Document No. AD 117140
AMERICAN METEOROLOGICAL SOCIETY
3 Joy Street
Boston, Mass.
Translation of
STAT
OBSERVATIONAL DATA OF THE SCIENTIFIC-RESEARCH DRIFTING
STATION OF 1950-1951, Vols. I-III.
EDITOR, M. M. SOMOV
[Materialy nabliudenii nauchno-issledovatel'skoi drei-
fuiushchei stantsii 1950/51 goda, red. M. M. Samov,
Leningrad, lzd. 'Morskoi Transport,' 1954-1955]
VOLUM! III
SECTION 9
This translation has been made by the American
Meteorological Society under contract AF 19(604)-
1936, through the support and sponsorship of the
GEOPHYSICS RESEARCH DIRECTORATE ?
AIR FORCE CAMBRIDGE RESEARCH CENTER
AIR RESEARCH AND DEVELOPMENT COMMAND
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Department- of Defense, their contractors, and other
government agencies should be directed to-the:
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DOCUMENT SERVICE CENTER,
-- 'DAYTON 2,,OHIO
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All Other persons and organizations should 'a? pply to the:
U. S.. DEPARTMENT OF COMMERCE
OFFICE OF TECHNICAL SERVICES,
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?
-4,7=
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ASTIA Document No. AD 117140
AMERICAN METEOROLOGICAL SOCIETY
3 Joy Street
Boston, Mass.
Translation of
OBSERVATIONAL DATA OF THE SCIENTIFIC-RESEARCH DRIFTING
STATION OF 1950-1951, Vois. I-Ill.
EDITOR, M. M. SOMOV
50-Yr 2014/0
[Materialy nabliudenii nauchno-issledovatel'skoi drei-
fuiushchei stantsii 1950/51 goda, red. M. M. Somov,
Leningrad, lzd. Morskoi Transport,' 1954-1955]
VOLUME III
SECTION 9
This translation has been made by the American
Meteorological Society under contract AF 19(604)-
1936, through the support and sponsorship of the
GEOPHYSICS RESEARCH DIRECTORATE
AIR FORCE CAMBRIDGE RESEARCH CENTER
AIR RESEARCH AND DEVELOPMENT COMMAND
1/17: CIA-RDP81-01043R002600210003-3
cs)e
,
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4011101111?
1
PREFACE
The source material for these translations was submitted to the
U. S. Delegation attending the CSAGI Arctic Conference in Stockholm,
May 22-25, 1956 and loaned for the purpose of these translations by
the National Academy of Sciences, U. S. National Committee for the
International. Geophysical Year.
It is felt that the translated articles have a timely appropriate-
ness in view of the IGY plans for the occupation of Arctic Ocean Drift
Stations. They are offered in rough draft in order to insure their
speedy distribution to all concerned with the Arctic operations. It
will be noted that consecutive pagination was not attempted in yield-
ing to the most expeditious means of translating and reproducing the
material. Each translated article has its own number sequence.
The tables and appendices for the most part retain the page numbers
of the original text.
Articles 1, 2, and 3 of Volume I translated by Mr. E. R. Hope
have been made available to the American Meteorological Society
through the kind cooperation of the Department of Defence, Ottawa,
Canada, in the interest of promoting Arctic research.
. The assistance of the National Academy of Sciences, USNC-
IGY, in the preparation of the translated text for reproduction is
also gratefully acknowledged.
a
t,
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I, I
TABLE OF CONTENTS
VOLUME I
Section 1. - AD 117132
Introduction. Translator David Kraus
"The drift of the scientific research station of 1950-1951,"
M. M. Somov. Translator David Kraus
OCEANOGRAPHY
Article 1 - "Organization of the oceanographic work."
M. M. Nikitin. Translator E. R. Hope
Article 2 - "Depth soundings." Z. M. Gudkovich.
Translator E. R. Hope
Article 3 - "Water-temperature observations and collection
of samples for chemical analysis. " Z. M. Gudkovich.
Translator E. R. Hope
Article 4 - "Determining the chemical composition of the
sea water. " M. M. Somov and A. A. Musina.
Translator David Kraus
Section 2 - AD 117133
Article 5 - "Results of a preliminary analysis of the deep-
water hydrological observations." Z. M. Gudkovich.
Translator David Kraus
Section 3 - AD 117134
Article 6 - "Observations of currents. " M. M. Nikitin.
Translator David Kraus
Section 4 - AD 117135
Article 7 - "Hydrobiological work." K. A. Brodskii and M. M.
Nikitin. Translator David Kra.us
Article 8 - "Results of the study of bottom deposits. " N. A.
Belov. Translator David Kraus
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VOLUME II
Section 5 - AD 117136
ICE SCIENCE
Article 1 - "Visual observations of the state of the drifting
ice cover." G. N. Iakovlev. Translator David
Kraus
Article 2 - "Study of the morphology of the ice cover by sur-
veying." G. N. Iakovlev. Translator David Kraus
Section 6 - AD 117137
Article 3 - "Physical-mechanical properties and thickness of
the ice cover. " I. G. Petrov. Translator David
Kraus
Section 7 - AD 117138
Article 4 - "The thermal regime of the ice cover. " G. N.
Iakovlev. Translator David Kraus
ASTRONOMY
Article 5 - "Astronomical observations. !' N. A. Miliaev.
Translator David Kraus
VOLUME III
Section 8 - AD 117139
AERO-METEOROLOGY
Article 1 - "Meteorological observations." K. I. Chukanin.
Translator David Kraus
Section 9 - AD 117140
Article 2 - "Aerological observations. " E. G. Kanaki and
V. E. Blagodarov. Translator David Kraus
Article 3 - "Wind observations by damper vane." M. M.
Nikitin. Translator David Kraus
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AEROLOGICAL OBSERVATIONS
by
V. G. Kanaki and
V. E. Blagodarov
Source:
Materialy nabliudenii nauchno-issledovateliska dreltuiUshchel
stantsii 1950/51 goda, ed. M. M. Somov, Leningrad., Izd. 'Morska
Transport' 1954. pp. 218-228 and Appendix, pp. 229-495.
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ORGANIZATION OF TIE WORK
Aerological observations on the ice of the Central Arctic were
first undertaken on a large scale at the Scientific-Research Drifting
Station of 1950/51. The experience of the High-Latitude Aerial Ekpedi-
tions of 1948 and 1949 was used widely in planning these observations.
The work program of the aerologists at the drifting station
included the following:
1) Daily release of two radiosondes;
2) Pilot-balloon observations of the radiosondes from one point;
3) Releases of radiosondes in series, four sondes per day (by
special order of the Arctic Institute).
The work was to have been carried out by two aerologists. Later,
on the spot, one more observer was added to the group. Thus, the aero-
logical group consisted of three members, P. F. Zaichikay, V. G. Kanaki
and V. E. Blagodarov. This made it possible. to expand the program some-
what, particularly to organize systematic base-line observations of the
radiosondes and even to give help to other groups.
- Much attention was devoted to the organization of the physical
labor program. Daily watches were maintained from the first. The man
on duty had the following tasks: preparation and release of two radio-
sondes, processing of the data and conduct of the meteorological obser-
vations during the other 5bservatiop7 intervals. The assistant to the
man on duty produced the hydrogen, filled the radiosonde balloons and
made the theodolite observations from the first base point. The third
aerologist made the theodolite observations from the second base point,
did the housekeeping for the group, kept a general camp watch, helped
other groups and saw to the replenishment of household supplies and
equipment for the group.
The aerological equipment of the drifting station was prepared
at. the Arctic Institute and in its Experimental Workshops. Consider-
able assistance was given by the Central Aerological Observatory (CAO)*
where all instruments were tested in a very short time, and from which
improved radiosonde balloons No. 150 were procured.
*TsentralInaia aerologicheskaia observatoria (TsA0).
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The Aerostat Workshops of the CAO prepared 5-m3 gas containers
for the hydrogen; they were made of four-ply percale; wind shelters
were also prepared there. The Ekperimental Workshops of the Arctic
Institute prepared gas generators of the ordinary Kanaki-Ledokhovich
type and portable "XL" radiosonde laboratories.
The aerological group of the drifting station had the. following
equipment:
1)
2)
3)
4)
5)
6)
7)
8)
9)
10)
11)
12)
13)
14)
15)
16)
17)
18)
19)
20)
21)
comb radiosondes
balloons, No, 150
balloons, No. 100
aerologic . theodolites
gas generators
gas containers
wind shelters
"Kapah-2" tents
duralumin radio masts
field telephones
electric inflaters for the radiosondes
"KUB-4" radio receivers
"BAS-80" batteries
11BNS-100" batteries
radiosonde field laboratories
locksmith's tools
spare radio tubes
"5NKN-45" storage batteries
ferrosilicon
caustic soda
ammonium chloride
420 sets
200 items
250 It
2
2 sets
3 items
1 item
1
2 items
2 ft
1 item
1
40 items
16 "
2
1 set
4 sets
3 items
1.6 tons
3.0 tons
5 kg
On 15 April 1950 the aerologists finished their preparatory work
and began observations. The "Kapsh-2" tent was set up as living and
work quarters for the three-man crew, the aerological and meteorological
equipment was kept there. The KUB-4 receiver Was set up on the bench
below the skylight. The gadiosondil signals were received and the
radiosonde data processed there. The aerological and meteorological
area could be seen easily from the skylight, as could the place where
the radiosondes were released, which made it possible to detect the
moment of release. The bench with the portable KL aerological labora-
tory, used to prepare the radiosondes for release, was placed next to
the.work table. Besides, there was a bench for meteorological appara-
tus and three folding cots in the tent. No more than two men could
work in the tent at one time, since there was so little free space.
An area 75 m north of the tent was outfitted, hydrogen was pro-
duced there and used to fill the radiosonde balloons. A. wind shelter
3.5 m in circumference was set up for this purpose; it consisted of a
piece of material 3 x 12 m with nine duralumin rods spaced equally.
Fish netting was pulled over this shelter as a roof to prevent the
1
-3-,
accidental escape of a balloon. Two hydrogen-filled gas containers were
placed-inside the shelter. The balloons were filled there. During
period of operations, the shelter had to be moved three times, because
the waste products of the gas production dirtied the snow and caused
deep pools to form.
Twenty meters to the south of the spot where the balloons were
filled a stake with the electric inflater attached. was frozen into the
Ice to hold the balloon before its release.
Two 7-in duralumin masts with 20.,m antennas were erected near the
tent; they were used to receive time and radiosonde signals. The recep-
tion of radiosonde signals by the KUB4 receiver was always good and,
as a rule, they were received as long as the radio transmitter func-
tioned.- The radio receiver was fed by "BAS-80" and "BNS-100" batteries.
Hydrogen production is the most laborious task of the aerologists.
Therefore, special attention was paid this matter in providing the
equipment, and some innovations were made in the method of obtaining the
hydrogen. First of all, the aerological group was provided with con-
tainers for storing the gas. These containers made it possible to
store gas enough for 4-5 radiosonde ascents, thanks to which a whole day
could be spent in carrying out this time-consuming operation. Fig. 1
shows the filling of a gas container from the gas generator.
The hydrogen was transferred from the gas containers into the
radiosonde balloons by a diaphragm pump (from a rubber liferaft)
specially adapted for this work. A nozzle with a flange was attached
to the suction end of the pump.- A hose, connected with the gas con-
tainer, was attached to this nozzle. The second (forcing) hose was
hooked. up to the balloon. It took 10 to 15 minutes to fill a balloon.
In the gas generator used at the drifting station, the intensity
of the reaction was regulated by changing the dose of ferrosilicon,
gradually feeding it in (as needed) from a special tank connected to
the tank of the gas-generator by a durite hose 45 mm in diameter. Sea
water was used for gas generation, and in the summer, water from fresh
pools. In both cases, 5-6 liters of hot water were poured in to start
the reaction. The salinity of the water did not seem to affect the
process. The weather conditions, however, exerted a great influence
on the process and the intensity of the reaction. For example, with
low temperatures and winds with drifting snow, the tank of the gas
generator had to be protected from the wind by a special shield (Fig. 2)
or covered with insulating material, otherwise the reaction would not
begin immediately and it would be very weak. When the process was too
Intense, however, the gas generator was cooled by covering it with snow.
Chemicals of home manufacture were used to produce the hydrogen;
their quality was good enough, although they had been at the Cape
Schmidt polar station for about two years, The ferrosilicon, however,
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was somewhat damp and had frozen together in a solid lump. Much time
and labor had to be expended in drying it and breaking it up. The
caustic soda (in standard 300 kg lots) was also in solid form. As a
consequence, the aerologist whose duty it was to produce the hydrogen
spent at least half his day breaking up the chemicals.
Despite the effort required by this process, during the whole
drift we always had enough hydrogen and. we had it in time.
The aerological observations were carried out from 15 April
through 19 October 1950.. Fran the beginning of operations to 1 September
they were made twice a day (at 0400 and 1600 hours Moscow time), from
1 September on they were made only once a day (0400 hours), due to a
shortage of chemicals. In all, 313 radiosondes were released, for which
222 observations were made by theodolite (25 of these were base-line
observations). After the data were processed and examined carefully,
the following were selected for publication:
radiosonde observations - 291
theodolite observations - 212
The mean height of ascent of the radiosondes was 18.6 km. The
maximum, height reached was 32.8 km. on 23 May. Two hundred eighty
radiosondes reached the stratosphere,
height of more than 10 km - 275 radiosondes
15
-263
20
r 148
30
r 2
Table 1 gives data of the distribution of the radiosonde ascents:
the length of time signals were received, height reached and the month
of release.
Table 1
Length of time signals were received and height of ascent
of the radiosondes
Whole
Apr. May June July Aug. Sept.Oct. perf.od
'
Mean length of signal
reception (min.)
61
71
74
82
70
73
47
71
Mean height of ascent (km)
15.2
19.4
20.0
22.4
18.2
17.7
13.5
18.6
Maximum height of ascent (km)
26.4
32.8
27.7
28.9
25.0
23.5
18..8
32.8
?
Minimum height of ascent (km)
6.9
5.0
8.7
10.8
6.o
6.4
7.4
5.0
Number of observations
28
58
53
59
51
27
15
291
- 5 -
All observations were carried
instructions and directions. Below
changes in method. The data on the
Appendix.
out in conformity with the assigned
we give an account of the various
processed material are given in the
Tilb RADIOSONDE WORK
A control check on the radiosondes was made before the expedition
set out, in January of 1950 at the CAO. The results of checking the
temperature recorders were entered in the specification sheet* Lfor
each instrumeng and, in case they did not check out with the factory
specifications, the latter were corrected. The pressure recorder was
checked at positive and negative temperatures. New specification sheets
for the pressure recorder were made on the basis of the data from this
check at the CAO.
Before being prepared for release the instruments were examined
carefully and those whose condition seemed doubtful were not used. The
instruments were made ready 3-4 hours before release.
The portable "KL" laboratory was used to check the electrical
systems of the instruments. The radio transmitter and the feeding
source were mounted as suggested by V. G. Kanaki. This differs from
the ordinary method in that the radio transmitter is not placed inside
the radiosonde, but is packed together with its batteries and attached
to the casing of the balloon before its release. The transmitter tubes
keep the batteries warm, preventing them from freezing.
The radio transmitter was tuned by the thermocouple of the field
laboratory or by "mikro" radio tubes. It was fed by 3-5 anode and
1 filament battery, which were drenched with a saturated solution of
ammonium chloride with 25% alcohol added. The drenching lasted for
1-2 hours before release, and the batteries together with the radio
transmitter were taken out to the release area 10 minutes before
release time.
The instruments were "exposed" only before the release and at
the release area. Attempts to "expose" the instruments in the tent
failed because of the differences in the air temperatare and the dif-
ferent inertia of the instruments (the temperature recorder of the
radiosonde and the psychrometer). In taking down the initial position
of the recording pens in the specially equipped. box with a ventilator
the readings of the radiosonde and the mercury thermometer did not
coincide; this was due to the causes mentioned above and to the inade-
quacy of the ventilator.
*In Russian the word here is "certificate," perhaps this is prefel'abla
to "specification sheet." (Tr. note)
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The instruments were "exposed" on the area before release on a
stake frozen into the ice to which the ventilator and two hooks for
the radiosonde and psychrometer were attached at a height of 2 m above
sea level.
In individual cases the radiosondes were "exposed" along with the
psychrometer shelter as a control and calibration of the readings made
during the basic "exposure" on the electric inflater as against the
readings of the instruments in the psychrometer shelter. In ordinary
work, the humidity instruments were taken out onto the release area an
hour to an hour-and-sAialf before release. The readings of the initial
position of the recording pens at the release site were entered in the
appropriate columns of the radiosonde sheet. The results of the
"exposure" made in the tent or at the psychrometer shelter were entered
in the blank titled "Exposure and place".
Humidity at a temperature higher than -5?C* was determined by
the aspiration psychrometer, at a temperature below -5?C by the
hygrometer. Pressure was measured by a mercury inspector's barometer**
which was kept in the tent. Wind was measured by the Tret'idkov wind
gauge*** set up on the meteorological area. The data on atmospheric
phenomena and cloudiness at the moment of release were entered in the
pilot-balloon log (with subsequent transfer onto the radiosonde sheet).
*All temperatures are in ?C (Tr. note).
**Inspector's barometer. A barometer carried by an inspector of a
meteorological network to a station to check the accuracy of the
barometers at that station. An inspector's barometer is an instrument
intermediate between a normal working barometer for a given meteoro-
logical region and a stationary barometer. Before the inspector makes
his trip the instrument correction of the inspector's barometer is
made by comparing it with a normal working barometer. A second com-
parison with the normal working barometer is made after the inspector
returns. The inspector's barometer must be portable, durable and
accurate. These requirements are satisfied by the Wild-Turretini
barometer used at stations in the USSR (Tr. note). Source: Meteoro-
logicheskii slover'l Khromov and Mamontoval p. 153.
***Tret'iakov wind gauge. A portable instrument for determining the
velocity and direction of the wind under field conditions. The wind
velocity is measured by the deflection of a freely suspended metal
plate having a spoon-shaped form. The direction of the wind is deter-
mined by a special vane included in the construction of the instrument.
The scale for this wind gauge was obtained experimentally from deter-
minations in an aerodynamic tube (Tr. note). Source: Meteorolog-
icheskii slover'l Khramov and Mamontova, p. 283,
7
The radiosonde balloons were hung about, over the gas burner or
the kerogaz,* before filling and were rotated constantly for half an
hour. The heating pi.ovided add-Itional vulcanization. The preparation
made the balloons elastic and insured a great height of ascent.
After the radio receiver had been tuned in on the transmitter wave
band, the radiosondes were released on a signal from the aerologist on
duty at the tent window. On days when the wind. was light, the balloons
were towed with the wind for take-off. During high winds, by way of
experiment, the P. F. Zaidhikov method was sometimes used. The equip-
ment necessary for this was prepared on the spot by station mechanic
M. S. Komarov. The radiosonde was hung so that it could slide easily
along the cable. The cable was stretched out with the wind at a height
of 1.5 in, one end of it was firmly fixed to a stake frozen into the ice,
the other end to a duralumin mast through an automatic release mechanism.
The balloon, under the influence of the wind, would pull the instrument
along the cable; in the process the ring would strike the automatic
release and the cable would be detached from the mast, which, because
of the rubber guy lines, would be cast in the direction opposite that
In which the instrument was moving, and the radiosonde, breaking free
of the cable, would continue in flight.
The signals were received (Fig. 3) by one of the aerologists
through a speaker or, in case reception were poor, by earphones.
Besides the temperature, pressure and. humidity signals, signals were
received of the speed of rotation of the propeller. For this purpose,
the time of the beginning and end of all control humidity signals were
entered on a separate form. These observations were conducted to study
atmospheric turbulence.
The data on the ascent of the radiosonde up to 5 km were worked up
very soon after the signals were received, since the information had to
be included in the LyeatheE7-telegram. The remaining information was
processed at the Arctic Institute after the expedition had returned.
The pressure data were processed according to the specifications
of the CAO. The correction for layer thickness was determined by slide
rule from the formula:
Htih av.
273
where H is the layer thickness and tav is the average temperature of
the layer.
*Kerogaz. A kerosene heating device on the order of a noiseless primus
stove (Tr. note).
0
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Temperature observations were processed according to the factory
specification sheets, with account taken of the corrections made at
the time of the instrument check at the CAO. The dew-point temperature
was determined by nomogram.
THEODOLITE OBSERVATIONS OF TBE RADIOSONDES
The pibal theodolite on the first base point, fixed on a tripod,
was located at the release area for radiosondes. Before an observation
was made, the theodolite's position with respect to the level was
checked, as well as its orientation. The theodolite was lined up with
a surveyor's stake, which first was a peg frozen into the ice on the
meridional line to the north of the instrument. Beginning 19 May, the
theodolite of the second base point located in the same direction,
served as the surveyor's mark. Since the floe gradually turned, a
correction factor had to be introduced to account for the change in
the azimuth of the stake, which increased fram 0? (15 April) to 34?
(20 October).
The azimuth was determined by the North Star and. by the sun. In
the first case the telescope of the theodolite, oriented with zero on
the surveyor's stake, was fixed on the North Star and readings were
made by the horizontal circle of the theodolite. The difference between
the readings with the theodolite directed on the stake (3600) and on tLe
North Star was taken as the azimuth of the stake. In the second in-
stance, the azimuth was determined by the familiar formula:
sin A
cosP 'sin tial
sin Z
combined
Since the zero of the theodolite was always directed on the stake,
the difference 360?-A gave the azimuth of the stake according to the
sun.
The pilot-balloon observations were processed in the usual manner,
whereby the heights were determined by the mean vertical velocity of
the radiosonde.
By the time the base was laid out (19 May), the floe had already
turned 5?. In order to preserve the initial position of the theodolite
at the first point of the base, the place for the second theodolite of
the base was selected exactly in the direction of the stake (peg),
whose azimuth at that time was 5?. The dimensions of the floe did not
permit us to lay out a base line of more than 600 m.
- 9 -
The length of the base was measured twice with a steel tape:
First measurement - 600.o8 m
- 600,90 m
_ Average length of base line - 600.50 m
A pibal theodolite on a tripod. was set at the second base point
as well as the first. Both points were connected by field telephones.
To synchronize the readings from the tent by a line connected to the
telephone line, signals of 2-3 sec duration were sent every minute.
This was attained by use of a contact on the timing gear of an alarm
clock and the sound mechanism. This device was prepared at the drifting
station.
The base observations were taken only on days without fog and low
cloud cover.
Second
As the floe turned, the azimuth of the base changed correspond-
ingly. The processing was done with a Molchanov circle* according to
the instructions of the Hydrometeorological Service. The base line
observations were processed using a 25-cm slide rule.
The small length of the base line did not permit us to process
the prolonged observations to the end, since angles B and B' often
were smaller than
The expedition's observational data were completely processed,
checked and prepared for publication at the Arctic Institute by N. V.
Basieva, L. I. Vorontsova, L. P. KUritsynal N. V. Shiposh under the
general direction and with the aid of I. M. Dolgin, Candidate in
Geographical Sciences, and Junior Scientific Colleague T. V. Nikolaeva.
In conclusion let us note a number of organizational and metho-
dological inadequacies which could not but have had an effect on the
work progress and the quality of the individual observations. These
inadequacies include, first of all, the lack of general standard
*Molchanov circle. An instrument for constructing the horizontal pro-
jection of the path of a pilot balloon, to a certain scale, by angles
plotted during theodolite observations of the balloon. The direction
and speed of the wind aloft is then determined from the projection.
The Molchanov circle consists of a wooden board with a diagram glued
to it, of a movable celluloid disk that turns about the center and of
a movable celluloid ruler. Designed by P. A. Molchanov (Tr. note).
Source:. Meteorologicheskii slovarl, Marmot?' and Mamontova, p. 190.
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Declassified in Part - Sanitized Copy Approved for Release ? 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
-10-
aerological field equipment. Therefore, in preparing for the expedi-
tion ordinary station instruments were selected and to a certain degree
adapted to the specifications of work on an ice floe. A number of
instruments and objects of secondary equipment were invented or re-
designed. As a consequence, the aerological equipment of the drifting
station was quite diverse, which doubtless complicated the work in a
number of cases. Some pieces of equipment, as was found when the work
was processed, were not thought out well enough. In particular, the
wind shelter proved unsatisfactory, since in autumn much snow entered
it during the ground blows, and covered the hydrogen gas containers.
In the future, instead of shelters a large Danish-type tent with a wide
entrance should be used.
The initial positions of the recording pens of the instruments,
"exposure' in the tent, were not recorded, although instructions had
been given to do this, because the temperature measurement and the tak-
ing of the position of the recording pens lost all physical sense in
view of the large temperature gradients. In individual cases and when
the instruments were exposed to air on sunny still days even the use
of the electric inflater with a flow of air 5-6 m/sec did not guarantee
reliable enough initial data. This is to be explained by the large
contrasts between the temperatures of the air and the inflater that
had been warmed in the sun.
In the future it will be necessary to work out a device for ex-
posing the apparatus both in the tent and in the open air. Thermostats
and the necessary shading together with good ventilating apparatus may
serve this purpose.
The shortness of the base line and the crude nature of its equip-
ment may be considered a real disadvantage for pilot-balloon observa-
tions. For example, in assembling the equipment, the contact watches
for the transmission of time signals were forgotten. The apparatus to
replace the watches was made at the station from an ordinary alarm clock
and was not very reliable, and often the convergence of the base alti-
tudes was poor.
The work was complicated a great deal by the fact that the caustic
soda, moulded in solid 300-kg masses, was contained in iron barrels,
Under the work conditions at the drifting station it is quite necessary
to have caustic soda either in pulverized form sealed in 2-3 kg tin
cans, or, still better, in flake form.
Finally, neither the method of observations nor the suitability
of this or that piece of equipment needs special comment.
A preliminary examination and analysis of the data makes it
possible to draw certain conclusions as to the stratification of the
atmosphere in the central part of the Arctic Basin. Below we give a
space-time graph of isopleths, constructed on the basis of the data
of the morning radiosonde ascents (Fig. 4). One hundred sixty seven
?,1
11
ascents for the period from 15 April through 19 October were used in
constructing this graph; all radiosondes reached the tropopause and in
most cases sounded the stratosphere up to 20-25 km.
The isopleth graph clearly shows the existence of an inversion
layer in the lower troposphere. As a rule this layer lies between the
heights 0.5 and 2.5-3.0 km. At the same time, a seasonal character of
the inversions was discovered. Thus, the deepest inversion was observed
in the middle of July. This was connected, with the transport northward
of warm Pacific-Ocean air, arriving from the American continent. The
inversion occurred as a result of the cooling of the lower layer of air
because of the expenditure of heat on the intensive thawing of the snow
and ice cover. In the inversion layer the growth of temperature with
height reached 10?C at the 3.5 km level. The maximum air temperature
(10-11?C) in that layer was noted at 1.0-1.5 km, The ice-adjacent layer
of air, in moving northward, became 8-90 cooler than the higher layers.
At the same time, at a height of 3.5 km, the zero isotherm held
steady, during the remaining time it appeared only episodicarly (in the
second ten days of June and then during all of August). In October,
with the arrival of polar night and the increase in radiation, the
winter inversions were observed, which can also be seen clearly on the
Isopleth graph.
Fig. 5 shows a graph of temperature distribution with height for
15 October. The deep inversion in the layer from the ice surface to a
height of 1 km can be explained by the great loss of heat from the low-
lying layer due to night radiation. In the 0-0,5 km layer, the negative
temperature gradient amounted to 2.56?C per 100 m, while the absolute
rise in temperature reached 12.8?C.
The trend of the isopleths above the inversion layer, for the whole
period investigated, almost exactly followed the variations of the
tropopause; the vertical temperature gradient of the layer from 4 km to
the tropopause sharply departed from its mean value, which was 0.56?C.
This indicates the connection between the thermal regime of the upper
troposphere and the height of the tropopause.
The height of the tropopause fluctuates on an average around the
9.8 km level, dropping sometimes to 7.0 km (30 June-1 July) and rising
to 12.0 km (5-15 July, during the invasion of warm masses of Pacific
Ocean air).
In the spring period, when cyclonic activity is strongly developed,
frequent fluctuations in the height of the tropopause are to be observed,
For example, between 23 June and 2 ally the height of the tropopause
dropped sharply from 11 km to 7 km, while in the succeeding days it again
rose to 12 km. This amplitude of variation of the height of the tropo-
pause, the greatest for the whole period, was caused by an abrupt change
In the air currents in the troposphere,
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Declassified in Part - Sanitized Copy Approved for Release ? 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
12
From the data given it is evident that the mean height of the
tropopause in the central part of the Arctic Basin has approximately
the same values as in the temperate latitudes. Proceeding from this
we may conclude that warm air masses, embracing the whole troposphere,
penetrate into the central Arctic. The transport of warm air into the
high latitudes leads to frontogenesis in these regions. In his time
B. L. Dzerdzeevskii noted this and it was confirmed by observations of
the aerial expeditions of 1948, 1949 and 1950.
During the whole period of operations of the drifting station,
the temperature of the tropopause varied within the limits -39.4? and
-64.2?C. The lowest temperature values were observed in April and
October, while the highest values occurred in the warm season of the
year. Fram this we can conclude that the temperature of the tropopause
has a seasonal character. The layer of the stratosphere above the
tropopause has great temperature fluctuations.
The following detailed study and analysis of the data from radio-
sonde ascents combined with the study of the synoptic characteristics
of the atmospheric processes makes it possible to broaden our knowledge
of the dynamics and transformation of air masses of the Arctic Basin.
Figure 1:
Figure 2:
Figure 3:
Figure 4:
- 13 -
Figure Captions
Filling a gas container with hydrogen.
A radiosonde balloon in the wind shelter.
Preparing a radiosonde for release and reception of
signals in the tent.
Graph of isopleths, accarding to morning radiosonde
ascents.
x-axis (bottom, reading left to right): April,
May, June, July, August, September, October
Figure 5: Distribution of temperature in the troposphere accord-
ing to the morning radiosonde ascent of 15 October 1950.
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Declassified in Part - Sanitized Copy Approved for Release ? 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
-111.-
APPENDIX
Explanation of the tables
Radiosonde observations were conducted at 011.001 and 1600 hours
Moscow time.
For the majority of the radiosondes, the observations were con-
ducted. by theodolite (base or from one point), and by this the direc-
tion and velocity of the wind aloft were determined.
The release time of the radiosondes, mean local solar time, is
given in four ciphers in the tables, of which the first two indicate
the hour, the last two, the minute.
The heights of the clouds was determined. by the moment "it becomes
hazy" by the theodolite observation; they are expressed in geopotential
decameters above sea level.
The results of the aerological radiosonde ascents are given in
table form, where the meteorological data are given, computed by
height stages for the main isobaric surfaces and. for the individual
levels and expressed in geopotential kilometers above sea level.
The upper and lower boundaries of the inversions and isotherms,
the boundaries of the segments with decreased gradient, and also the
height of the lower boundary of the tlopopause are referred to particu-
lar levels.
The table contains the following data: Date, release time of the
radiosonde, coordinates, cloudiness, height of the clouds; pressure,
temperature, vertical temperature gradient, relative and specific
humidity, wind velocity and direction (data obtained from the base
observations are given in heavy type), and vertical velocity of the
radiosondes are given by heights.
The values of the gradients and the vertical velocities are given
in the line corresponding to the height of the upper boundary of the
layer for which the computations were made. Heights given in paren-
theses mean that such data are not accurate for the beginning or the
end of the particular point. The temperature and humidity data given
In parentheses were taken from interpolated curve segments. Discon-
tinuities in the wind data (direction or velocity) are marked with an
asterisk.
The organization of the aerological observations (radiosonde
ascents, pilot balloon observations) and their processing were carried
out in compliance with the "Instructions to the hydrameteorological
stations and posts" (Nastavlenie gidrametorologicheskim stantsiiam i
postam), Pub, Gidrcmeteoizdat, 4th fd? Parts I, II, and III, 1944,
1945, 1947.
-15-
CONVENTIONAL SYMBOLS
? height in geopotential kilometers -7X-- wet snow
B atmospheric pressure in nib ? rain (eh? light)
t temperature in degrees A granular snow ( light)
vertical temperature gradient 4 snow shower
U relative humidity of the air
q specific humidity in grams per
kg of air
d wind direction in degrees
^ wind direction in m per sec
W vertical velocity of the radio-
sonde in m per min
-;?.- snow (-,.K? light)
,
4 o, drizzle 0 light)
==... fog with charges
? sea fog
ground-level fog
=== unbroken fog
fog with gaps (sky visible)
glaze
4; low drifting snow
x14 surface snowstorm
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Declassified in Part - Sanitized Copy Approved for Release ? 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
;-Plietl'-',HailoAtieinte-.?ra3ro.riwiepa'CB0110
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Declassified in Part - Sanitized Copy Approved for Release ? 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
, ? 4 V,4*:.4.'i?
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Declassified in Part - Sanitized Copy Approved for Release . 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
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Declassified in Part - Sanitized Copy Approved for Release ? 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
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Puc. 5. Pacnpene.rtene TemnepaTypm B Tpono e p e
no rpetinemy noirbemy pamo3o1rna 15 oicrsp5pB 1950 r.
j. 70ENDIX
See tr2_nslated text for colurnn head-
ings 7..n1 F..3ditional. notes.
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1
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YCJI0BHUE 0603HALIEHH51
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S
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RADio .50r0E. 0135 ER V477045
PA114030H,LtOBblE HA6J1101tEliMi
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5.0
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281
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10.0
241
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340
1.06
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0.00
14.0
132
__48.7
--0.10
323
1.87
800
--17.3
15.0
113
__47.7
--0.10
2.0
787
--17.3
0.00
15.77
100
-47.0
2.1
776
--17.3
0.00
16.0
96
--46.7
--0.10
2.5
736
--18.5
0.30
17.0
84
-45.2
--0.15
319
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H
B
t
7
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d
V
W
H
B
t
7
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.
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W
17.32
81
--44.2
--0.31
3.98
600
--26.4
0.55
311
5
18.0
73
--44.2
0.00
5.0
520
--33.0
0.65
302
4
19.0
62
--44.2
0.00
5.26
500
--34.3
297
4
20.0
53
--44.2
0.00
254
6.0
450
--39.8
0.68
300
3
6.78
400
--45.2
306
3
307
7.0
387
--47.0
0.72
306
4
18.4 1343 cp . 76?19' A = 192'27'
8.0
333
--52.1
0.51
306
7
8.68
300
--55.6
313
7
0/0 Ci
(8.74)
298
--56.0
0.53
313
7
287
9.0
285
--
--
312
8
0.0
026
--22.6
93
292
3
10.0
245
--
--
310
8
0.19
000
--21.3
--0.68
327
5
11.0
210
--51.5
--
311
7
248
0.5
960
--18.8
--0.81
342
5
11.29
200
--51.0
305
6
0.6
947
--18.0
--0.80
334
4
12.0
180
--49.3
--0.22
290
3
0.98
900
--18.0
0.00
320
5
13.0
155
--47.3
--0.20
259
3
240
1.41
850
--18.0
0.00
309
5
14.0
133
--45.8
--0.15
232
4
1.5
839
--18.2
309
5
15.0
114
--44.4
--0.14
191
3
1.87
800
--18.6
309
5
15.85
100
--42.9
199
5
2.0
787
--18.8
0.14
313
5
16.0
97
--42.6
--0.18
202
5
2.5
735
--19.3
0.10
313
6
17.0
85
--41.5
--0.11
183
4
236
2.7
715
--19.5
0.10
316
5
18.0
75
--40.9
--0.06
177
4
2.85
700
--20.3
318
4
19.0
65
--40.5
--0.04
174
4
3.0
685
--21.0
0.50
321
4
332
20.0
55
--40.5
0.00
165
4
302
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Hpoaamic. npuiwycemulz
H
B
t
1
Uq
d
VWIH
B
t
7
U
q
d
V
W
20.7
21.0
22.0
22.8
0.0
0.17
0.2
0.5
0.88
0.94
1.0
1.2
1.36
1.5
1.8
2.0
2.5
2.8
3.0
50
48
40
35
19.4
026
.000
997
956
908
900
893
870
850
833
800
779
729
700
681
--40.5
--39.5
--38.8
--38.8
0149
--30.8
--26.2
--24.4
--18.7
--16.6
--16.6
--16.6
--16.6
--16.7
--16.8
--17.4
--17.8
--19.0
--20.0
--20.7
0.00
--0.33
--0.07
0.00
cp = 76?19'
2/0
--3.20
--1.90
--0.55
0.00
0.00
0.07
0.20
0.24
0.34
Ci
87
k.=
168
169
161
192?29'
292
--
--
249
266
268
270
271
268
271
279
277
272
271
271
5
5
3
2
--
--
5
'4
4
5
5
4
4
4
4
6
5
5
1
304
i
310
3.93
4.0
5.0
5.24
6.0
6.78
7.0
8.0
8.64
8.72
9.0
9.52
10.0
11.0
11.27
12.0
13.0
14.0
15.0
1 15.77
1 16.0
17.0
18.0
600
595
519
500
449
400
386
332
300
297
283
262
242
209
200
178
153
131
113
100
96
83
72
--25.6
--26.2
--33.3
--35.0
--39.7
--45.4
--47.2
--53.0
--56.2
--56.4
--56.4
--56.4
--55.7
--53.3
--52.8
--51.5
--49.4
--48.2
--46.4
--45.0
--44.6
--43.7
--43.0
0.55
0.71
0.64
0.75
0.58
0.47
0.00
0.00
--0.15
--0.24
--0.18
--0.21
--0.12
--0.18
--0.18
--0.09
--0.07
272
272
271
5
5
5
293
270
226
226
938
252
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Irpoaoitatc. npumacettuR
B
U
q
d
V
W
d1V
20.4 0139 y = 76?17' X = 192?32'
8.0
340
--48.0
0.63
244
7/0 Ci, Cs
8.8
9.0
300
290
--52.5
--53.0
0.50
0.0
030
-29.3
96
292
1
9.9
253
--53.0
0.00
0.21
. 000
-20.3
-4.29
347
4
10.0
250
--52.8
-0.20
175
0.5
963
-17.1
-1.10
346
3
11.0
214
--50.5
-0.23
164
0.65
943
-16.2
--0.60
343
2
11.44
200
--49.4
1.0
900
--16.2
0.00
028
2
12.0
184
--48.2
--0.23
1.45
850
-16.2
003
I
13.0
158
--45.9
--0.23
1.5
843
-16.2
0.00
003
1
13.82
140
--45.6
--0.04
; 164
1.84
807
--16.2
0.00
321
1
1.9
800
-16.4
306
1
21.4 0155 q) ==.: 76?17' X = 192?35'
2.0
789
-16.8
0.38
293
I
2.5
738
--18.4
0.32
307
1
0;0
2.88
700
-19.6
0.0
030
--30.8
96
313
9
3.0
689
--20.0
0.32
303
0.21
000
4.01
600
--25.I
0.50
0.5
960
5.0
523
.2-28.9
0.38
0.97
900
5.31
500
-31.4
1.0
897
6.0
454
-35.7
0.68
280
1.4
850
6.87
400
-40.7
1.5
839
7.0
393
--41.7
0.60
1.85
SOO
--17.8
2.0
784
--18.6
17podoxic. npu.AoNceuuA
H
B
t
1
U
q
d
VWIIHB
t
7
U
q
d
V
NV
19.0
62
-42.4
--0.06
4.0
597
--27.3
0.58
246
4
200
20.0
53
--42.4
0.00
5.0
519
--32.1
0.48
274
5
20.3
50
-42.4
5.27
500
--33.1
283
6
21.0
46
-42.4
0.00
252
6.0
450
-37.1
0.50
301
9
6.83
400
--42.1
301
13
194
19.4 1359 op .--: 76?18' k === 192931'
7.0
390
-43.4
0.63
299
14
8.0
336
--48.0
0.46
303
19
0/0 Ci
8.73
300
--52.1
298
18
198
0.0
029
-22.4
96
292
2
9.0
287
--53.1
0.51
296
17
0.1
014
--22.6
0.20
__
__
9.17
280
--54.1
0.59
296
17
0.2
000
-22.3
-0.30
282
3
9.89
251
--54.1
0.00
294
14
0.5
961
--19.4
286
4
10.0
246
-53.7
--0.36
294
12
210
0.55
955
--19.2
--0.89
277
. 3
11.0
212
-50.5
--0.32
294
5
0.99
900
--19.2
0.00
283
4
11.33
200
--49.7
293
4
1.43
850
-19.2
285
3
12.0
182
--48.2
-0.23
275
2
206
1.5
841
-19.2
0.00
289
3
13.0
157
--45.4
--0.28
293
2
1.87
SOO
--19.2
283
2
14.0
134
-43.4
-0.20
277
1
200
2.0
786
--19.2
0.00
287
2
15.0
116
-41.8
-0.16
214
1
2.3
755
--19.2
0.00
283
3
16.0
100
--40.4
-0.14
154
2
200
2.5
735
--19.7
0.25
280
4
250
;17.0
86
-39.1
-0.13
113
3
2.85
700
-20.8
279
4
18.0
74
--38.4
-0.07
123
3
3.0
686
--21.5
0.36
277
3
19.0
62
-37.5
-0.09
154
4
3.97
600
-27.2
246
4
19.65
55
--37.4
--0.02
210
0
CD
0
CD
(/)
(/)
CD
0.
-0
CD
(I)
CD
CD
0.0
0
73
73
73
CD
CD
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73
01
0
0
4?1
0
Bj
q d V
W H
2.5
2.85
3.0
3.98
5.0
5.27
6.0
6.79-
7.0
7.2
733
700
685
600
519
500
449
400
388
376
--20.1
--21.7
--22.5
--27.0
--32.5
--34.2
--39.2
--44.2
--44.9
--45.6
0.30
0.48
0.46
0.54
0.67
0.57
0.35
22.4 0155 q) ==.: 76?17' --= 192?36'
8/0 Ci, Cs
0.0 031 --28.7 87 315 3
0.22 000 -24.0 -2.14 353 5
0.46 967 -17.1 --2.88 358 5
0.5 962 -17.1 355 6
1.0 900 --17.1 0.00 343 5
1.3 866 --17.1 0.00 334 5
1.44 850 -17.3 330 5
1.5 843 --17.4 0.15 330 5
1.88 800 --18.5
320
314
2.0
2.5
2.86
3.0
4.0
5.0
5.3
6.0
6.86
6.9
0.0
0.2
0.24
0.5
1.0
1.03
1.17
1.45
1.5
787
735
700
687
600
522
500
452
400
398
--18.9
--20.2
--21.1
--21.3
--25.1
--30.5
--32.2
--36.7
--43.2
--44.5
apoa0.4.71C. tipll./10,71CellUR
7 U ql d V
0.30
0.26
0.22
0.38
0.54
0.62
0.87
22.4 1352 q) === 76?17' 192?36'
8/0 Ci, Cs
034
-20.4
94
0.6
338
2
005
--18.7
-0.85
94
0.7
001
5
000
-18.7
94
0.8
002
5
965
-18.7
0.00
95
0.8
003
6
903
--18.7
0.00
96
0.8
026
4
900
--18.7
96
0.8
099
4
883
-18.7
0.00
96
0.9
013
4
850
-19.1
97
0.8
001
5
845
-19.2
0.15
97
0.8
358
5
w
329
3.50
?
17poaawc. npattooKeHust
H
B
t
7
U
q
d
V
WIH
B
t
1 T
UqdV
W
1.9
800
--19.g
97
0.8
343
4
16.0
97
-45.5
-0.18
2.0
789
-19.9
0.14
97
0.8
338
4
17.0
82
--45.5
0.00
265
2.5
737
--20.7
0.16
96
0.8
323
3
2.88
700
--21.5
95
0.8
310
5
23.4 0149 q) ... 76?17' A=192?35'
3.0
689
--21.7
0.20
95
0.8
297
6
316
4.01
600
--26.8
0.50
93
0.5
306
8
7/0 Ci, Cs
5.0
523
-32.4
0.57
91
275
7
0.0
039
-26.9
0
5.31
500
--34.5
91
273
8
0.2
009
-20.4
--3.25
6.0
453
--38.8
0.64
90
273
10
0.27
000
--19.8
6.85
400
-43.5
88
303
18
371
0.5
970
--18.0
-0.80
060
2
7.0
391
--43.9
0.51
88
305
21
0.8
933
--16.2
-0.60
060
4
8.0
337
--48.2
0.43
87
314
35
1.0
908
--16.2
0.00
057
4
8.75
300
--53.2
86
1.07
900
--16.2
051
5
9.0
288
--55.5
0.73
85
1.34
869
--16.2
0.00
029
8
9.32
274
-55.6
0.34
85
1.5
850
--16.4
0.12
028
6
10.0
246
--56.6
0.00
84
344
1.95
800
--16.8
029
3
11.0
211
--52.8
--0.38
82
2.0
794
--16.9
0.10
029
3
11.33
200
--51.8
2.5
744
--17.3
0.08
236
1
12.0
180
--51.1
--0.17
268
2.66
728
--17.5
0.12
266
1
13.0
155
--50.2
-0.09
2.94
700
--18.3
304
2
14.0
133
-49.2
--0.10
3.0
695
--18.5
0.29
297
2
15.0
15.85
115
100
-47.3
-45.6
-0.19
4.0
4.09
608
600
--21.7
--22.0
0.32
278
270
3
3
385
-:-
50-Yr 2014/01/17 : CIA-RDP81-01043R002600210003-3
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
ullf.M?V`
lip 0a011.71C. npultametua
H
B
t
1
U
q
d
V
W 11
H
B
t
1
UqdV
VV
5.0
530
-25.8
0.41
308
4
0.9
923
--16.8
-0.65
081
4
5.4
500
--27.2
325
4
1.0
911
--16.8
0.00
088
4
6.0
461
--28.9
0.31
332
6
1.09
900
--16.8
096
4
2
7.0
400
-33.5
0.46
334
10
1.5
854
--16.8
0.00
105
8.0
347
--40.0
0.65
332
10
440
1.53
850
--16.8
109
2
2
8.98
300
--46.4
0.65
329
22
1.8
819
--16.8
0.00
146
10.0
256
--54.5
0.79
324
26
1.97
800
--17.7
168
2
10.42
240
--57.3
0.67
325
25
2.0
797
--17.8
0.50
171
2
11.0
219
-57.3
0.00
326
23
2.5
746
-19.2
0.28
216
2
11.1
215
--57.3
0.00
325
22
2.97
700
--20.4
242
2
11.57
200
--56.3
324
19
3.0
697
--20.5
0.26
244
3
330
12.0
188
--54.4
-0.32
323
16
3.56
647
--22.5
0.36
276
4
13.0
160
--52.0
--0.24
317
12
4.0
609
-23.3
0.18
306
5
14.0
137
--51.0
--0.10
312
12
4.1
600
--23.4
0.10
314
5
6
15.0
117
-50.4
-0.06
506
4.8
543
--24.1
345
5.0
530
--25.8
0.85
347
7
5.41
500
349
7
23.4 1404 cp--=76?17' k ----.- 192?34'
6.0
460
0.84
347
9
310
10/0 Ci, Cs
6.97
400
--41.8
330
8
0.0
042
--19.8
86
135
1
7.0
397
--42.0
0.78
0.62
330
336
9
11
0.2
012
--21.1
0.65
106
3
8.0
343
-48.2
339
16
250
0.29
000
--20.8
099
4
8.83
300
--55.0
0.80
340
16
0.5
973
--19.4
--0.57
086
5
9.0
292
--56.2
1
6.85
256
--60.0
0.45
10.0
250
--60.0
0.00
10.73
223
--60.0
0.00
11.0
214
--58.4
--0.59
11.44
200
--55.0
12.0
183
--53.5
--0.49
13.0
156
--50.7
--0.28
14.0
134
--50.0
--0.07
15,0
116
--49.4
--0.06
15.95
100
--47.9
16.0
99
--47.8
--0.16
17.0
85
--46.8
--0.10
18.0
74
--45.9
--0.09
19.0
64
--45.3
--0.06
90.0
55
--44.6
--0.07
334
334
330
332
328
320
314
313
310
299
299
287
288
298
24.4 0149 p =76?17' X = 192?34'
135 1
80 Ci, Cs
? 0.0
043
--24.8
99
0.2
014
--20.2
-2.30
0.3
000
--I8.2
0.5
973
--16.5
--1.23
21
22
15
13
11
8
5
6
6
5
4
6
5
4
180 4
188 4
247
290
316
17poaonote. npunoycetuut
1-1
U
q d IV IW
1.0
911
--14.6
190
5
1.05
905
--14.5
-0.36
191
5
1.09
900
--14.5
192
5
1.5
854
--14.5
0.00
202
2
1.53
850
--14.5
204
2
1.86
814
--14.5
0.00
242
2
1.99
800
--15.0
0.38
265
2
2.5
747
--16.5
0.29
270
2
293
3.0
700
--17.7
0.24
4.0
612
--19.1
0.14
4.15
600
--19.6
t?D
5.0
534
--25.2
0.61
5.47
500
--28.0
6.0
463
--32.0
0.68
329
7.0
404
--38.4
0.64
7.06
400
--39.0
8.0
348
--46.3
0.79
8.96
300
--53.4
9.0
10.0
298
254
--53.6
--58.6
0.73
0.50
308
10.6
230
--61.7
0.52
10.88
221
--61.7
0.00
11.0
217
--61.1
-0.50
247
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
IV W
11.5 200
12.0 185
13.0 158
14.0 135
15.0 116
16.0 100
16.2 97
--57.9
--54.3
--52.6
--51.9
--50.9
--48.7
--48.4
--0.68
--0.17
--0.07
--0.10
--0.22
--0.15
24.4 1356 1) = 76?17' X= 192?32'
1010 Cs (590)
0.0 043 --18.5 84 135
0.1 029 --18.7 0.20 137
0.9 015 --18.3 --0.40 153
0.31 000 --17.5 162
0.5 975 -16.7 --0.53 156
0.8 937 --15.5 --0.40 169
1.0 913 --15.5 0.00
1.11 900 -15.5
1.5 855 --15.5 0.00 145
1.54 850 __15.5 142
1.9 810 --15.5 0.00
1.99 800 -15.8
1
2
3
2
3
2
1
1
2
1
1
1
228
233
-------
"Otral**50,404-,-
H B
2.5
3.0
4.0
4.15
5.0
5.47
6.0
7.0
7.06
8.0
9.02
10.0
10.68
11.0
11.61
12.0
13.0
13.32
14.0
15 0
15.88
746
700
613
600
534
500
465
404
400
349
300
257
232
221
200
188
161
153
139
118
103
HIB1 t I
0.0
0.2
0.3
0.5
0.84
1.0
1.11
1.5
1.55
1.9
2.0
2.5
3.0
3.03
4.0
4.19
5.0
5.51
6.0
25.4 0149 01) = 7.15?17' X=192?29'
7/0 CN, Cs
044 --25.0
016 --I8.0
000 --16.0
975 --14.3
932 --12.9
913 --12.9
900 --12.9
856 --12.9
850 -12.9
812 -12.9
800 --13.1
750 --14.3
703 --14.9
700 --15.0
615 --16.4
600 --17.0
537 --21.3
500 -23.5
468 -27.1
99
090
1
-3.50
117
4
113
4
--1.23
102
4
--0.41
086
2
0.00
085
2
088
2
0.00
112
2
112
2
0.00
1
0.20
1
0.24
3
0.12
328
3
329
3
0.15
301
5
0.49
0.58
393
7.0
7.11
8.0
9.0
9.09
10.0
10.8
0.0
0.2
0.33
0.5
0.7
1.0
1.14
1.5
1.57
1.65
2.02
2.5
40.?
-----
- ? ..***04210104:1
17poa0A01C. 11pUAO.Ne4tillfl
ql d
v NV
--17.0
0.25
264
9
251
--17.7
0.14
271
9
--19.4
0.17
280
5
--20.I
280
6
--24.0
0.46
286
7
248
--26.5
301
8
--29.5
0.55
--37.0
0.75
--37.3
236
--43.8
0.68
no
--50.6
0.67
241 co
0.57
--60.2
0.59
--60.2
0.00
218
--55.1
--53.2
--0.70
--50.1
--0.31
216
--48.9
--0.37
--48.9
0.00
--48.9
0.00
--48.9
0.00
212
taatV.P4-0?
Hpooaitoic. npuAcacentot
7 U q
d V. W
406
400
352
304
300
261
230
-33.3
--34.0
--40.2
--47.3
--48.1
-52.9
--57.8
0.62
0.69
0.71
0.56
0.61
25.4 1354 q)=== 76?18' X=192?24'
010
046 --16.8 77 090 2
019 --17.5 0.35
000 --17.0
978 -15.9 --0.53
953 --14.6 --0.65
916 -14.6 0.00
900 --14.6
858 -14.6 0.00
850 --I4.6
840 --I4.6 0.00
800 -15.4 0.22
750 --I6.2 0.17
480
Declassified in Part - Sanitized Copy Approved for Release
?-?0001-Z009Z001?1701-0-1-8dCll-V10 LI-40/171-0Z -1A-09
2 -!
Ii
7
U
q
d
VI WI
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3.01
700
--16.7
0.10
350
0.7
4.0
615
--I8.1
0.14
1.0
4.17
600
--19.0
1.13
5.0
537
--24.0
0.59
1.5
5.51
500
--29.7
1.57
6.0
467
--30.0
0.60
1.95
7.0
405
--37.0
0.70
342
2.0
7.08
400
--37.4
2.03
8.0
350
--45.0
0.80
2.5
9.0
300
0.58
3.0
10.0
258
--57.0
0.62
3.05
10.5
240
--60.3
0.66
4.0
11.0
222
--60.3
0.00
4.19
11.3
211
--60.3
0.00
5.0
11.47
205
--58.9
-0.82
400
5.53
6.0
26.4 0129 p . 76?19' X.192?18'
7.0
3,0 Cs
7.13
8.0
0.0
047
--22.7
090
3
9.0
0.9
019
--I8.1
-2.30
9.06
0.33
000
--15.8
10.0
0.5
978
--14.3
-1.27
11.0
IB
953
--13.3
916
--13.3
900
--13.3
859
--13.3
850
--I3.3
809
--I3.3
803
--13.4
800
--13.4
753
--14.6
705
--15.7
700
--15.8
616
--I8.0
600
--18.5
538
--22.8
500
--26.5
468
--29.6
407
--36.6
400
--37.3
352
--43.1
303
--49.0
300
--49.4
260
222
--59.6
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7 1U ql d I V w
-0.50
0.00
0.00
0.00
0.20
0.24
0.22
0.23
0.48
0.68
0.70
0.65
0.59
0.57
0.49
290 t.D
01
220
210
220
222
17poaomic. npuAometiu.g
H
B
t
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11.13
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--60.2
0.46
1.61
850
--12.2
165
11.67
200
-60.2
1.7
839
--12.2
0.00
12.0
190
--60.2
0.00
2.0
806
--12.8
0.20
13.0
163
--54.2
--0.60
214
2.06
800
--12.9
14.0
139
--51.8
-0.24
2.5
755
--14.0
0.24
15.0
119
-50.9
--0.09
211 I
3.0
707
--15.8
0.36
158
16.0
102
--50.1
--0.68
1
3.07
700
--17.4
16.12
100
--50.0
1
4.0
619
--19.7
0.39
17.0
88
-49.3
--0.08
1
I
4.22
600
--20.3
156
18.0
78
--47.8
-0.15
220 1
5.0
540
--24.3
0.46
5.55
500
--27.3
26.4 1356 q) ... 76?21', k==.192P14'
6.0
7.0
469
406
--30.9
--37.3
0.66
0.64
155
0/0
7.1
400
-38.2
0.0
048
--16.0
91
112
5
8.0
351
-44.5
0.72
157
0.1
034
--16.4
0.40
9.0
301
=51.0
0.65
0.2
020
--16.2
--0.20
9.04
300
--51.4
166
0.35
000
--15.3
10.0
258
-56.6
0.56
0.5
980
--14.5
-.0.57
10.62
235
--59.3
0.44
1.0
918
-12.7
--0.36
11.0
221
--59.3
0.00
165
1.15
900
--12.3
11.16
216
-59.3
0.00
1.2
895
--12.2
--0.25
11.64
200
--55.7
1.5
861
--12.2
0.00
12.0
189
--54.0
--0.63
165
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14.0
15.0
16.0
16.12
16.46
0.0
0.2
0.33
0.5
1.0
1.13
1.5
1.57
2.0
2.03
2.5
3.0
3.05
161
139
119
102
100
95
27.4
047
019
000
978
916
900
858
850
803
800
759
704
700
--50.5
--49.0
--48.1
--47.6
--47.5
--47.4
0154
--22.5
--18.6
-16.2
--14.4
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--I2.1
-11.5
--II.5
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-12.3
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--0.15
--0.09
--0.05
-0.04
op =
0/0
--1.95
--1.40
--0.40
-0.18
0.14
0.99
0.32
76?22'
97
A=192?11'
135
149
152
152
157
156
154
153
5
12
19
12
8
7
8
7
169
190
383
4.0
4.2
5.0
5.51
6.0
7.0
7.09
8.0
9.0
9.05
10.0
10.6
0.0
0.9
0.34
0.5
1.0
1.15
1.5
617
600
537
500
467
406
400
352
303
300
258
939
27.4
047
020
000
979
918
900
860
--20.2
--20.6
--24.3
--27.0
--30.2
--37.0
--37.6
--43.8
--50.8
--5I.3
--57.0
--59.6
1434
--15.7
--15.7
--I4.5
--13.2
--11.5
--11.2
--11.0
0.53
0.41
0.59
0.68
0.68
0.70
0.62
0.43
cp= 76?23'
010
0.00
-0.83
-0.34
-0.10
94
A==
192?07'
135
164
168
167
173
170
156
5
8
8
7
6
5
4
420
495
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H
B
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7
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H
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1.59
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153
4
14.0
138
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3
230
2.0
806
--12.2
0.24
135
4
15.0
120
-48.2
-0.14
031
3
2,06
800
--12.4
131
4
16.0
103
-46.8
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020
3
2.5
755
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0.24
123
5
16.2
100
-46.5
024
3
232
3.0
708
--14.2
0.16
109
6
322
17.0
89
--45.3
--0.15
3.07
700
--14.4
106
6
4.0
819
--19.0
0.48
072
3
28.4 0149 q; = 76?25' A = 19T07'
4.23
808
--20.4
062
2
5.0
539
--24.0
0.50
344
2
co
5.54
500
-27.5
360
3
240
0.0
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--23.2
100
135
4
6.0
469
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0.60
017
3
0.2
019
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169
7
7.0
407
-36.9
0.69
012
4
0.33
000
--15.4
166
5
7.1
400
-38.0
018
4
225
0.45
985
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161
5
8.0
353
-43.1
0.62
030
5
0.5
978
--13.8
162
5
9.0
303
--50.4
0.73
022
6
1.0
916
--13.8
0.00
142
3
9.05
300
--50.7
021
6
1.14
900
--13.8
143
5
10.0
258
-56.4
0.60
020
7
1.5
859
--13.8
0.00
121
4
10.8
227
-59.9
0.44
024
6
220
1.57
850
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11.0
220
--59.9
0.00
026
5
1.9
813
--13.8
0.00
181
11.4
207
-59.9
0.00
030
4
2.0
803
--14.0
0.20
11.59
200
--57.0
032
3
2.03
800
-14.1
12.0
189
--54.4
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031
4
230
2.5
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0.18
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162
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3.0
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0.22
155
28.4 1319 cp =-- 76?26' X ==. 192?06'
3.04
700
-16.2
4.0
616
-20.4
0.44
0/0
4.19
600
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0.0
048
--16.5
89
112
3
5.0
538
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0.54
155
0.06
041
--17.1
1.00
102
3
5.53
500
--28.7
0.2
021
--17.1
0.00
128
5
6.0
468
--31.7
0.59
157
0.35
000
--17.1
119
5
7.0'
407
-37.6
0.59
0.5
979
--17.1
0.00
110
4
7.11
400
--38.5-
1.0
g17
--17.1
0.00
?
103
5
8.0
351
-43.5
0.59
170
1.14
900
--17.1
100
5
9.0
303
-49.4
0.59
1.5
858
--17.1
0.00
089
5
9.05
300
-49.5
1.57
850
--17.1
087
5
10.0
259
--54.1
0.47
167
2.0
800
--17.1
0.00
072
7
11.0
222
--57.5
0.342.2
780
--17.1
0.00
068
8
11.25
214
--57.5
0.00
2.5
749
=17,8
0.23
068
9
11.64
:200
--55.2
3,0
700
--19.4
0.32
062
11
294
12.0
189
-52.4
-0.68
168
4.0
613
-23.6
0.42
054
13
13.0
163
-49.9
-0.25
4.16
600
-24.4
053
14
14.0 '
139
--49.7
-0.02
5.0
534
--29.9
0.63
14.2
135 .
--49.7
0.00
167
5.47
500
-32.4
287
6.0
463
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0.54
7.0
402
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0.73
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0.5
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081
6
8.0
345
-49.4
0.68
0.8
936
--13.8
-0.57
075
7
8.9
300
-54.5
258
1.0
912
--13.8
0.00
075
8
9.0
295
--55.2
0.58
1.1
900
-13.8
074
8
9.6
269
--58.5
0.55
1.5
854
--13.8
0.00
072
9
10.0
251
-58.5
0.00
231
1.54
850
--13.8
072
9
10.7
226
-58.5
0.00
1.99
800
--13.8
0.00
069
10
11.0
216
-56.5
-0.67
2.4
758
--13.8
0.00
066
11
11.46
200
--54.3
2.5
748
--14.4
0.60
066
11
12.0
185
--51.8
-0.47
226
3.0
700
-16.2
0.36
064
12
284
13.0
159
--50.5
--0.13
4.0
614
--20.0
0.38
061
17
14.0
136
-49.3
-0.12
230
4.17
600
--20.8
061
18
15.0
117
--48.2
-0.11
5.0
536
-24.8
0.48
057
22
265
16.0
101
--46.8
-0.14
5.5
500
-27.5
061
26
16.04
100
-46.7
191
6.0
466
-29.9
0.51
062
25
17.0
87
--45.2
-0.16
7.0
405
--35.6
0.57
18.0
76
--44.0
-0.12
7.08
400
-36.2
234
18.6
69
--44.0
0.00
184
8.0
349
-42.0
0.64
9.0
300
-48.7
0.67
204
29.4 0106 q)==. 76?26' X = 192?03'
10.0
258
-54.4
0.57
5/0 Cs
10.41
242
--56.8
0.59
0.0
043
--25.9
99
112
1
11.0
221
--56.8
0.00
0.2
015
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104
5
11.14
216
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0.00
0.31
000
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093
6
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11.6
12.0
12.3
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0.9
0.25
0.5
0.9
1.0
1.06
1.5
1.95
2.0
2.16
2.5
2.95
3.0
4.0
4.15
200
--54.7
188
--53.1
179
--52.6
037
Q09
COO
909
919
907
900
850
800
795
777
743
700
695
607
600
--0.43
--0.17
13
29.4 1351 9.76?26' A=191?56'
0:0 Cs
92 045 6
--17.0
--17.0
--I6.9
--I6.4
-15.5
--I5.5
--I5.5
-15.5
-15.5
--15.5
--15.5
--16.5
--18.0
--18.4
-23.0
--23.6
0.00
--0.20
-0.23
0.00
0.00
0.00
0.00
0.29
0.38
0.46
900
278
5.0
5.41
6.0
7.0
8.0
8.93
9.0
10.0
10.5
10.88
11.0
11.59
12.0
13.0
14.0
15.0
16.0
16.15
17.0
18.0
19.0
20.0
21.0
529 --27.0 0.40
500 --29,5
459 --32.0 0.50
400 --37.9 0.59
345 --43.2 0.53
300 --48.4
297 --48.7 0.55
254 --52.7 0.40
235 --54.6 0.38
232 --54.6 0.00
218 --54.0 --0.50
200 --51.3
187 --49.2 --0.48
160 --46.8 --0.24
138 --45.7 --0.11
119 --44.9 --0.08
103 --43.4 --0.15
100 --43.1
88 --42.4 --0.10
77 --41.7 --0.07
66 --40.9 --0.08
57 --39.8 --0.11
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24.0
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0.0
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0.5
0.64
1.02
1.45
1.5
1.71
1.91
2.0
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1
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--0.04
--0.06
--0.06
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cp=76?25' A=191?44'
5/3
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0.6
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99
0.8
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100
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100
1.2
0.00
100
1.3
100
1.3
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100
1.4
0.00
100
1.4
100
1.4
0.28
100
1.4
0.36
100
1.2
100
1.0
0.76
100
0.9
4.0
4.04
5.0
5.35
6.0
6.89
7.0
8.0
8.79
9.0
9.83
10.0
11.0
11.37
12.0
12.32
13.0
14.0
0.0
0.2
604
600
525
500
455
400
393
339
300
290
256
249
213
200
181
173
154
133
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0.42
100
0.7
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100
0.7
367
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0.52
100
0.5
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100
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0.65
99
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97
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0.67
97
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0.70
289
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0.38
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0.00
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212
--49.7
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--48.8
--47.6
--0.21
--46.9
--0.22
--46.9
0.00
--46.9
0.00
201
30.4 1355 cp =76?25' k = 191?26'
10/0 Ci, Cs
027 1 --13.1
000 --11.3 --0.90
100 045
067
12
12
?
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
- - _
__,..............-. 141,14..acrAt.ertust
H
B
I
7
U
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0.5
0.64
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945
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072
071
12
16
1.5 0149 cp = 76?24' X= 191?04'
1.02
900
-- 7.6
0.00
067
15
10/0 Cs
1.47
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-7.6
073
14
1.5
847
-- 7.6
0.00
074
14
0.0
026
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94
0.8
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1.6
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12
0.19
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0.9
1.93
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-- 9.2
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0.3
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93
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792
-- 9.6
0.50
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8
0.5
960
--I2.8
0.00
93
1.2
2.5
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0.56
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11
232
0.99
900
--12.8
0.00
92
1.3
2.94
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1.43
850
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91
1.4
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0.56
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9
1.5
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0.00
90
1.4
4.0
607
--21.8
0.66
1.87
800
--12.8
89
1.4
4.09
600
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247
2.0
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1.4
5.0
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0.39
2.04
783
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1.4
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2.5
737
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0.50
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1.2
6.0
462
--31.2
0.55
174
2.89
700
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89
1.2
7.0
400
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0.51
3.0
689
-17.4
0.46
89
1.1
322
8.0
345
--43.4
0.71
175
4.0
603
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0.62
89
0.7
8.75
309
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0.75
4.03
600
--23.7
89
0.7
8.94
300
--49.0
4.77
542
--28.2
0.60
89
0.4
9.0
297
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0.00
5.0
525
--28.8
0.26
89
0.4
9.95
257
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5.35
500
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0.4
10.0
255
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175
6.0
455
--32.4
0.43
290
H
6.89
7.0
8.0
8.82
9.0
9.06
9.39
10.0
11.0
11.45
12.0
12.08
13.0
14.0
0.0
0.2
0.23
0.3
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B t 7 U 0:1 d IV 1 V/1 H B t 7 HI clH V
1.03 993 --13.2 009 10
1.14 888 --13.2 90:77 190
1.46 850 --13.8
1.5 845 --I4.0 068 10
1.92 800 --14.8 070 9
9.0 791 --15.0 068 9
9.5 741 --16.7 060 8
195 2.92 700 --19.0 065 11
065 11 346
3.0 692 --I9.5 N3
4.0 604 --24.3 90:55 190 cn
4.05 600 --24.5
5.0 526 --28.8 069 9
5.35 500 --31.I 070 9
195 6.0 456 --34.1 070 9
6.9 400 --39.2 102 7 318
78:90 34951 1196:3 103 7
115 8
8.84 300 --53.0 125 12
190.1.90 29448 154448i 12395 117 255
11.0 214 114590 44 213
1112:0 49 21 7
?83 --47:92
158 4
400
393
340
300
292
290
266
250
214
200
184
182
158
136
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--48.0
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--46.7
--46.7
0.64
0.72
0.80
0.00
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--0.41
--0.21
0.00
0.00
2.5 0152 p==76023' X=190?55'
1opo As
030 I --17.8 99 015
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000 I --16.1 068
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904 --13.2 I 0.00 070
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10
10
10
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236
0.00
0.22
0.20
0.34
0.56
0.48
0.45
0.53
0.59
0.63
0.79
0.00
-0.53
-0.17
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
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1.49
1.94
2.0
2.5
2.95
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11.0
11.54
12.0
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14.0
15.0
16.0
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17.0
18.0
19.0
19.45
500
456
400
395
342
300
295
281
252
217
200
186
160
138
119
102
100
88
76
64
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0.33
0.51
0.57
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0.5 965 --13.7
1.0 904 --13.7
1.04 900 .--13.7
1.4 858 -13.7
1.47 850 --I3.9
1.5 847 --14.0
1.93 800 --15.0
2.0 792 --15.3
2.5 740 -17.5
2.91 700 --19.0
3.0 692 --19.2
4.0 604 --23.7
4.05 600 --24.0
5.0 525 --29.7
p=76?22' A.190?49'
Ci
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0.59
8.42
319
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0.93
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300
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310
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090
089
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0.42 73 0.7 093
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0.39 73 106
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9.0 791 -15.2
2.5 741 -17.0
2.92 700 -18.8
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4.0 606 i -24.9
4.06 600 --25.2
5.0 526 --30.1
5.37 500 --32.0
6.0 457 --35.2
6.93 400 --41.8
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11.45
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12.0
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13.0
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14.0
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15.0
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16.0
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16.06
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3.0 692
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5.6 526
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0.38 92 1.1
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0.57 85 0.4
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0.54 84
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0.45 83
0.50 83
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0.61 82
0.59 81
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098
098
098
098
098
098
104
105
108
109
110
118
118
126
129
115
112
112
117
119
119
120
129
10
8
9
9
9
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8
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8
9
9
9
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330
315
283
11.0 219 --48.7 --0.48 80 124 4
11.55 200 --47.3 80 143 5
12.0 187 --46.1 --0.26 79 151 5
13.0 161 --44.3 --0.18 79 158 4
14.0 139 --43.2 --0.11 78 166 3
15.0 120 --42.7 --0.05 76 171 3
16.0 104 --42.0 --0.07 76 175 3
16.25 100 --41.8 172 9
17.0 89 --40.9 --0.11
18.0 78 --40.2 --0.07
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0.0 026 --23.5 100 045 2
0.19 000 --19.0 --2.37 081 4
0.5 958 081 7
0.98 900 086 8
(1.14) 881 (--13.1) 086 9
1,41 -850 --13.7 094 9
1.5 840 --14.0 0.25 096 9
1.85 800 --14.7 101 10
2.0 785 --15.1 0.22 102 10
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1.5
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6
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310
8.8
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6
160
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391
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0.66
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3
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0.59
180
2
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8.17
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0.29
184
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3
0.0
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2
9.0
290
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189
3
0.17
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9.21
280
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194
3
191
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282
6.79
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50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
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83
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168
168
6
6
1.86
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1.3
175
5
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1.2
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225
2.5
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6
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0.9
169
5
3.0
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169
3
360
4.0
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0.7
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6
225
4.03
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0.7
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400
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0
7.0
394
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379 (f)
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339
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0.82
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8.45
315
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8.78
300
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276
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344
11.0
214
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684
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3
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4
5
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400
389
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196
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7.45
363
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0.93
202
5
0,0
8.0
8.06
333
331
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0.26
206
207
7
7
279
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300
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297
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289
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7
0.5
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157 6
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250
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198
7
0.94
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11.0
216
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5
265
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150 8
11.49
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180
6
1.39
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142 8
12.0
186
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184
7
1.5
837
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141 8
13.0
161
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7
258
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141 8
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139
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263
3.95
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215
5
353
22.0
42
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595
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215
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23.0
37
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387
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12.0 180 --45.3 --0.08
13.0 155 --44.6 --0.07
14.0 133 --44.2 --0.04
15.0 115 --43.8 --0.04
16.0 100 --43.4 --0.04
17.0 86 --43.0 --0.04
18.0 74 --42.2 --0.08
18.5 69 --41.9 --0.06
19.0 64 --41.9 0.00
20.0 55 --41.9 0.00
20.6 50 --41.9
21.0 47 --41.9 0.00
21.25 45 --41.9 0.00
8.5 1338 cp =76?21'
010
0.0 011 --10.8 94
0.1 008 --12.4 1.60
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0.5 955 -12.4 0.00
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850 --14.9
838 --15.5
800 --16.4
783 --16.8
732 --18.7
700 --20.3
684 --21.0
600 --24.3
597 --24.5
520 --30.0
500 --31.8
451 --37.0
400 --42.3
389 --43.3
335
326 --50.5
300 --50.5
296 --50.5
288 --49.5
248 --46.1
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203
213
219
215
215
218
220
223
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225
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681
--17.3
0.32
76
0.9
18.0
78
--40.9
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3.93
600
--19.9
77
0.8
19.0
67
--40.9
0.00
285
4.0
596
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0.27
79
0.9
20.0
58
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0.00
5.0
520
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0.36
85
0.7
261
21.0
50
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0.00
5.29
500
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0.5
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44
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455
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0.59
85
0.5
22.04
43
--40.9
0.00
306
6.89
400
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85
7.0
394
--34.6
0.51
85
216
10.5 1343 cp = 76?25' X = 195?37'
8.0
341
--40.5
0.59
84
8.85
300
--46.1
83
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9.0
293
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0.65
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0.0
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1.5
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269
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0.58
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225
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252
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0.2
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3
10.26
243
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315
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1.73
800
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2.0
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100
1.6
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341
2.5
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100
1.4
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2.75
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3.0
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100
1.3
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600
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100
1.0
333
20.0
56
-39.7
0.00
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593
-20.8
0.40
100
1.0
20.8
50
-39.7
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518
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0.37
95
0.8
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48
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5.25
500
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0.7
21.28
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377
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0.5
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400
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320
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0.7
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100
0.8
10.0
249
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0.00
85
344
0.5
944
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100
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0.9
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595
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78
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5.0
519
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0.47
76
0.6
5.27
500
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76
0.5
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6.0
450
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0.72
75
0.0
013
--13.9
100
1.1
338
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6.81
400
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74
311
0.09
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0.9
7.0
390
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0.65
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0.2
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0.9
8.0
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0.80
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0.24
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1.38
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0.9
8.74
300
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0.5
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1.0
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288
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0.69
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0.86
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88
1.2
9.17
281
--54,5
0.59
70
0.9
900
--12.9
87
1.2
9.6
264
--54.5
0.00
69
310
1.0
889
--12.9
0.00
84
1.2
10.0
248
--51.3
--0.80
69
1.35
850
--12.9
77
1.2
1-1
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1.5
832
--12.9
0.00
75
1.1
14.0
137
--42.3
--0.06
1.6 '
821
--I2.9
0.00
74
1.1
15.0
119
--4I.5
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1.8
800
--13.3
74
1.1
16.0
102
--40.0
--0.15
279
2.0
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--13.7
0.20
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100
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--15.3
0.32
80
1.1
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92
--39.0
--0.16
2.8
700
--16.5
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1.1
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86
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3.0
681
--17.5
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1.1
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18.0
72
--39.0
0.00
276
3.96
600
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0.8
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0.35
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0.8
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5.27
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0.5
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0.72
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0.2
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275
0.43
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8.8
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291
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0.74
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1.33
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11.48
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12.0
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500 --25.0
456 --27.7
400 --33.5
396 --31.0
343 --42.3
300 --49.0
294 --50.4
270 --54.2
253 --54.2
951 --54.2
218 --47.1
200 --44.6
187 --43.8
161 --43.1
140 --42.7
120 --42.7
104 --42.4
100 --42.4
89 --42.1
78 --4I.8
67 --41.4
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0.41 74
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0.63 71
0.83 70
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0.81 69
0.69 69
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7620' 190?25'
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1.16
871
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1.35
850
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1.5
835
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0.00
302
1.83
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313
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3.0
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11.59
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12
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137
11
292
9.0
296
-50 1
0.97
4.0
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--21.6
0.64
9.86
260
-50.1
0.00
5.0
524
-28.8
0.72
10.0
254
-48.6
-1.07
5.33
500
--31.1
11.0
219
--43.7
--0.49
6.0
455
-34.0
0.52
302
11.59
200
--42.5
6.86
400
-36.9
12.0
189
-42.0
-0.17
240
7.0
392
-37.4
0.34
8.0
339
-44.7
0.73
14.5 0123 ? = 76'18' ), = 190-16'
8.35
322
-46.0
0.37
8.84
300
--46.0
874
7/3 Ac (273), Sc
9.0
292
--46.0
0.00
0.0
011
-6.8
100
158
4
9.1
288
-46.0
0.00
0.09
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-6.7
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151
5
10.0
951
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0.2
985
-6.7
0.00
180
7
11.0
217
--42.6
-0.11
998
0.5
947
-6.7
0.00
140
6
11.55
200
-42.2
0.89
900
-6.7
175
12
12.0
187
-41.8
-0.08
1.0
888
-6.7
0.00
174
13
13.0
162
-41.8
0.00
213
1.35
850
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14
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140
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15.0
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0.00
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2.5
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0.42
76
1.2
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104
-41.7
-0.01
2.91
700
-16.8
73
0.9
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100
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3.0
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0.72
71
0.9
363
17.0
90
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4.0
605
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0.60
61
0.5
18.0
77
--40.4
-0.06
208
4.05
600
-23.5
59
0.5
5.0
527
--28.4
0.53
42
0.2
14.5 1332 cp = 7619' A = 190016
5.38
500
--29.7
42
0.2
6.0
459
-32.5
0.41
53
354
10/10 Sc -(172)
6.95
400
-39.5
51
0.0
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-3.5
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2.4
135
10
7.0
396
-40.2
0.77
51
0.09
008
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0.78
87
2.3
126
13
8.0
340
--49.1
0.89
48
0.15
000
-4.2
86
2.3
126
13
8.14
300
-49.6
0.36
47
0.2
993
-4.2
84
2.4
127
14
9.0
292
-46.4
-0.37
44
0.29
982
-4.2
0.00
84
2.4
132
14
10.0
252
-44.2
-0.22
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335
0.44
963
-2.8
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82
2.5
169
15
11.0
217
--41.7
--0.25
32
0.5
955
-2.8
82
2.5
165
15
11.55
200
-41.5
32
0.68
934
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0.00
80
2.6
147
16
12.0
187
-41.3
--0.04
32
0.97
900
-3.7
77
2.5
142
15
13.0
163
--40.8
--0.05
32
294
1.0
897
-3.8
0.31
77
2.3
142
15
14.0
141
--40.3
-0.05
32
1.43
850
-7.3
77
1.8
15.0
123
--40.1
-0.02
32
1.5
842
-7.9
0.82
77
1.8
16.0
103
-40.1
0.00
32
311
1.89
800
--11.0
77
1.5
16.3
100
--40.1
0.00
32
2.0
789
--11.4
0.70
77
1.4
17.0
89
-39.6
--0.07
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-0.11
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15.5 0127 p=76023'
10,10 St (57)
0.0 019 -4.8 90 2.2
0.15 000 -5.2 88 2.3
0.2 993 -5.4 0.30 88 2.1
0.5 956 -6.2 0.27 88 2.1
0.98 900 -6.7 88 2.2
1.0 898 -6.8 0.12 87 2.1
1.43 850 -7.2 78 2.0
1.5 841 -7.3 0.10 78 1.9
1.89 800 --8.0 78 1.9
2.0 789 --8.4 0.22 78 1.9
2.5 739 --10.9 0.50 78 1.6
2.91 700 --13.0 78 1.4
3.0 693 --13.7 .0.56 78 1.3
4.0 607 --MO 0.53 71 0.9
4.08 600 -19.5 69 0.8
5.0 529 -94.2 0.52 61 0.5
17poawzote npumacettua
V
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315
15.5 1347 p==76?24' k 190?17'
10110 St (10)
1901017'
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93
2.3
338
1
0.19
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1.9
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1.9
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76
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--7.2
72
1.8
1.5
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0.64
71
1.7
1.92
800
--8.7
55
1.3
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792
--9.0
0.32
49
1.1
2.5
742
--I0.4
0.28
49
1.0
2.94
700
--12.6
49
0.9
3.0
695
--12.9
0.50
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0.9
327
4.0
610
--18.0
0.51
48
0.6
353
4.12
600
--18.5
48
0.6
5.0
533
--22.4
0.44
47
0.5
398
5.46
6.0
500
464
--24.8
--27.8
0.54
47
46
0.4
0.3
291
Ilpoaomic. npwicacetua
Ft
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NV
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B
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7.0
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0.56
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16.5 0127 q> ==. 76025' X= 190000'
7.04
400
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45
8.0
348
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0.61
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10/10 L-- (8)
9.0
302
-47.2
0.77
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279
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96
2.1
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0.5
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95
2.6
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253
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0.93
44
0.6
950
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94
2.8
10.5
240
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43
1.0
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90
2.9
11.0
222
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43
1.03
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86
2.8
11.64
200
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43
1.48
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-3.7
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67
2.3
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189
-48.0
-0.44
43
303
1.93
800
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51
1.5
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163
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43
2.0
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0.35
51
1.5
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141
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1.3
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15.0
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314
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4.17
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0.4
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22.0
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18.0
19.0
20.0
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304
300
261
235
224
223
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192
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0.59
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0.7
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0.20
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231
1.0
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60
1.44
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1.5
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59
1.91
800
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69
2.0
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252
9.5
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2.95
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262
3.0
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4.0
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5.0
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297
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6.0
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0.72
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0.00
329
7.07
400
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8.0
349
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9.0
303
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9.07
300
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329
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12.0
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0.7
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13.0
167
--45.3
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0.97
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13.45
156
-44.1
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896
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14.0
144
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1.3
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88
15.0
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16.0
108
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1.5
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16.56
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19.0
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2.93
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324
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56
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609
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21.9
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0.58
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361
5.45
500
-24.6
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6.0
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340
17.5 0121 p='76?28' X ... 189?47'
7.0
402
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Declassified in Part - Sanitized Copy Approved for Release
50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
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0.0 020 -- 2.2 90 2.9 180
0.15 000 -- 2.7 90 2.8 152
0.2 993 -- 3.0 0.40 90 2.7 152
0.5 955 -- 5.6 0.87 88 2.2
0.97 900 -- 5.6 . 87 2.3
1.0 896 -- 5.6 0.00 87 2.3
1.41 850 -- 5.6 86 2.4
1.5 841 -5.6 0.00 85 2.4
1.87 808 -- 7.0 84 2.3
2.0 786 -- 8.1 0.50 84 2.1
2.5 738 -- 9.9 .0.36 78 1.7
2.91 700 --I2.3 74 1.4
3.0 692 --12.8 0.58 71 1.3
4.0 607 --19 0 0.62 62 0.7
4.08 600 --I9.7 62 0.7
5.0 530 --26.1 0.71 57 0.4
5.43 500 --28.9 57 0.3
6.0 461 --33.2 0.71 57
6.97 400 --42.4 57
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9
10
10
351
7.0
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8.84
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8.91
300
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4.0 603 --23.0
4.03 600 -23.4
5.0 524 --30.5
5.34 500 --32.9
6.0 455 -36.6-
6.87 400 -42.4
7.0 392 --43.1
8.0 338 -48.7
8.3 323 --50.0
8.78 300 -50.0
9.0 290 -50.0
9.65 262 --50.0
10.0 250 -48.8
11.0 215 --47.0
11.45 200 -46.5
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13.0 159 --44.7
14.0 137 -43.6
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4.04 600 -21,0
5.0 526 --27.0
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6.0 456 -32.7
6.93 400 -38.8
7.0 396 -39.4
8.0 342 -46.1
8:65 310 -49.3
8.86 300 -49.3
9.0 294 -49.3
9.36 278 -49.3
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11.0 216 -45.5
11.54 200 --44.4
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Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
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Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
Declassified in Part - Sanitized Copy Approved for Release ? 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
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Declassified in Part - Sanitized Copy Approved for Release 50-Yr 2014/01/17 ? CIA-RDP81-01043R002600210003 3
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
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687
--14.1
0.40
57
1.0
340
2.0
786
--12.3
77
1.3
3.37
655
-.15.7
0.43
50
0.7
2.5
736
-13.2
0.20
71
1.3
4.0
602
--18.2
0.40
50
0.6
2.75
713
--13.6
0.16
71
1.3
274
4.03
600
--18.3
50
0.6
2.87
700
--14.3
71
1.1
3.0
526
-23.6
0.54
50
0.4
3.0
688
--14.9
0.52
71
1.1
5.38
500
--25.1
50
0.4
4.0
603
--21.0
0.61
70
0.7
6.0
459
--28.4
0.48
50
0.3
335
4.04
600
--21.2
70
0.7
5.0
525
--27.9
0.69
68
0.4
248
27.5 1439 cp =77?01' X = 190?02'
5.35
500
-30.9
68
6.0
456
--35.7
0.78
68
10/10 St (36)
6.9
400
--4I.5
68
0.0 020
-6.4
85
1.9
045
1
7.0
393
-42.0
0.63
68
268
0.15
000
-8.4
84
1.6
J g ?
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
.? a...?????""
Ilp000mic npuitoxetiuft
H
B
t
T
UqdVVilH
B 1 t I 7
Ulq1dIVI Vlf
8.0
341
--48.3
0.63
68
28.5 0129 q) ... 77?02' A =-- 190?02'
8.24
329
--49.4
0.46
8.84
300
-- 49.4
10/10 St (57), *0
9.0
292
--49.4
0.00
0.0
023
-7.3
83
1.7
045
1
9.24
282
--49.4
0.00
0.17
000
-8.0
85
1.6
064
.)
10.0
251
--47.2
-0.29
241
0.2
997
-8.2
0.45
85
1.6
063
,)
11.0
216
--44.4
--0.28
0.5
959
-10.2
0.67
89
1.5
11.51
200
--43.9
0.66
939
--11.7
0.94
90
1.4
12.0
185
--43.7
--0.07
245
1.0
900
--8.4
--0.97
83
1.7
13.0
160
--42.6
--0.11
1.35
860
--5.9
-0.71
67
1.8
14.0
137
--42.0
--0.06
1.45
850
--5.9
64
1.7
15.0
118
--41.3
--0.07
243
1.5
844
-5.9
0.00
62
1.7
16.0
102
--40.7
-0.06
1.91
800
-5.9
56
1.6
16.2
100
--40.7
2.0
790
--5.9
0.00
54
1.6
17.0
88
--40.4
--0.03
265
2.2
769
--5.9
0.00
52
1.6
?
18.0
77
-40.0
-0.04
2.5
741
--8.4
0.83
50
1.2
19.0
66
--39.5
--0.05
2.92
700
--10.8
48
1.0
20.0
58
--38.0
-0.15
276
3.0
693
-11.4
0.60
47
1.0
310
21.0
50
--37.2
--0.08
4.0
608
--17.2
0.58
40
0.6
22.0
43
-36.6
--0.06
4.11
600
--18.1
40
0.5
23.0
38
-35.9
-0.07
276
5.0
531
-95.2
0.80
36
0.3
5.44
500
--27.8
34
0.2
6.6
462
--32.2
0.70
34
291
17poaonotc. npunooicenun
H I
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U
q
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V
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T
U
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7.02
400
-36.4
0.41
34
28.5 1344 41:1 = 77?03' X === 190?02'
8.0
346
-42.9
0.66
34
8.94
300
--51.0
34
286
10/10 St (43)
9.0
297
--51.5
0.86
34
0.0
025
-6.2
77
135
5
9.6
270
-56.6
0.85
0.19
000
-7.8
0.84
125
7
9.94
256
--56.6
0.00
0.5
959
--10.6
0.90
10.0
254
-56.0
--1.00
0.6
947
-11.2
0.60
11.0
217
--48.6
-0.74
257
0.85
917
--11.2
0.00
11.54
200
-46.0
1.0
900
--9.0
--1.47
12.0
187
-45.2
--0.34
1.33
863
-6.5
-0.76
13.0
162
--44.2
--0.10
246
1.45
850
--6.5
14.0
139
--43.6
-0.06
1.5
845
-6.5
0.00
15.0
120
-42.8
-0.08
1.93
800
-6.5
16.0
104
-41.6
-0.12
249
2.0
792
--6.5
0.00
16.24
100
-41.4
2.5
742
-8.5
0.40
17.0
89
--41.0
--0.06
2.95
700
--10.9
18.0
77
--40.6
--0.04
3.0
695
--11.3
0.56
376
19.0
67
-40.2
--0.04
309
4.0
610
--17.6
0.63
20.0
58
-39.7
-0.05
4.12
600
--18.3
21.0
50
-39.1
-0.06
5.0
532
--24.3
0.67
22.0
44
--38.5
-0.06
5.45
500
-26.6
23.0
38
-38.4
-0.01
6.0
463
--30.0
0.57
24.0
33
--38.4
--0.00
94.16
32
-38.4
--0.00
313
CAD
Declassified in Part - Sanitized Copy Approved for Release
?-?0001-Z009Z001?1701-0-1-8dCll-V10 LI-40/171-0Z -1A-09
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17poaaore npunomemoi
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7.0
403
--34.8
0.48
375
29.5 0124 p = 77?04' X = 190?02'
7.05
400
--35.2
10:10 St 27)
8.0
348
--42 n
0.81
9.0
300
-49.3
0.64
0.0
021
--8.1
86
1.6
135
9
10.0
259
-56.5
0.72
347
0.16
000
-9.0
85
1.5
11.0
2216
-50.8
-0.57
0.2
995
-9.4
0.65
85
1.4
11.63
200
--47.6
0.5
957
-11.8
0.80
85
1.2
12.0
189
-46.2
-0.46
0.65
937
-12.8
0.67
84
1.1
13.0
162
--45.0
--0.12
0.97
900
--7.1
-1.78
83
2.0
14.0
139
-43.8
-0.12
323
1.0
898
-7.1
83
2.0
15.0
121
--42.4
-0.14
1.41
850
--7.1
81
2.0
16.0
105
-41.6.
--0.08
1.5
842
-7.1
0.00
81
2.0
16.32
100
--41.3
1.9
800
--7.1
75
2.0
17.0
90
--40.8
-0.08
316
9.0
790
--7.1
0.00
74
2.0
18.0
77
--40.0
--0.08
2.28
761
--7.1
0.00
70
2.0
19.0
66
-39.4
-0.06
2.5
740
-7.8
0.32
63
1.6
20.0
58
-38.3
--0.11
2.93
700
-9.8
56
1.3
21.0
50
--36.8
-0.15
378
3.0
693
-10.2
0.48
56
1.3
391
22.0
42
--35.6
-0.19
4.0
608
--13.2
0.E0
52
0.9
23.0
37
-35.6
0.00
4.09
600
--15.7
52
0.9
24.0
32
--35.6
0.00
5.0
531
-92.0
0.68
51
0.5 1
25.0
28
-35.6
0.00
382
5.44
.-40
-14.3
51 0.4 I
?
:71
-
0
17poaavic npunoycenuft
H
B
0
t
Y
U
q
d
V
NV 11
H
B
t 1
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6.0
461
-26.7
0.47
52
0.4
29.5 1320 cp=-- 77?06' X = 190001'
7.02
400
-33.2
0.64
52
10/10 St (43)
8.0
348
-38.4
0.53
52
446
9.0
302
-46.6
0.82
52
0.0
018
--9.2
79
1.3
135
10
9.04
300
-46.8
52
0.14
000
--10.0
78
1.2
139
10
10.0
260
--54.6
0.80
0.2
993
--10.5
0.65
77
1.2
133
10
10.23
231
--55.7
0.44
0.5
954
--12.6
0.70
75
1.0
10.8
231
--55.7
0.00
0.65
936
-13.3
0.47
75
1.0
11.0
224
-54.7
-0.50
0.96
900
-8.2
72
1.6
11.73
200
-49.7
1.0
895
--7.8
--1.57
72
1.6
12.0
192
--48.7
--0.60
396
1.41
830
-6.4
-0.34
64
1.7
13.0
164
--45.8
--0.29
1.5
840
--6.5
63
1.6
14.0
142
--45.4
--0.04
1.87
800
-7.3
56
1.4
15.0
121
--45.0
--0.04
2.0
786
-7.7
0.22
54
1.4
16.0
104
--44.6
-0.04
390
2.5
737
--9.1
0.28
53
1.3
16.3
100
-44.4
2.91
700
-10.9
52
1.1
297
17.0
90
-43.1
--0.15
3.0
690
-11.4
0.46
51
1.1
18.0
77
-42.2
--0.09
4.0
606
--16.1
0.47
47
0 8
19.0
66
--41.7
-0.05
4.08
600
--16.7
47
0.7
20.0
57
--41.2
--0.05
5.0
529
-21.5
0.54
47
0.5
21.0
50
-40.7
-0.05
496
5.43
500
-24.4
47
0.4
22.0
43
-40.0
-0.07
6.0
462
--27.3
0.58
47
0.3
266
23.0
37
-39.4
--0.06
7.0
402
-30.6
0.33
47
24.0 32
-37.7
-0.17
494
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
17poaoizoic. npuAooicenuft
H
B
t
7
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7
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7.04
400
--31.0
47
30.5 0120 tp =77?09' X==189?51'
8.0
349
--38.3
0.77
47
272
10/10 St (31)
9.02
300
-46.4
0.79
47
10.0
258
-52.0
0.57
0.0
015
-9.8
89
1.4
135
6
11.0
222
-47.3
--0.47
266
0.11
000
--10.6
88
1.4
11.68
200
--44.3
0.2
989
--11.6
0.90
87
1.2
12.0
189
--43.0
-0.43
0.35
970
--12.8
0.80
86
1.1
13.0
164
-41.4
-0.16
277
0.5
951
--12.8
0.00
85
1.1
14.0
142
-40.8
--0.06
?
0.73
924
--12.8
0.00
84
1.2
15.0
123
-40.2
-0.06
0.94
900
--9.7
84
1.6
16.0
105
--40.0
-0.02
291
1.0
893
--9.0
77
1.5
16.33
100
--39.5
1.07
884
-8.3
--1.32
71
1.5
17.0
92
-38.6
-0.14
1.38
850
-8.3
58
1.3
18.0
80
-37.8
--0.08
1.5
836
-8.3
0.00
55
1.2
19.0
69
-37.2
-0.06
314
1.84
800
--10.2
55
1.1
20.0
58
-37.2
-0.00
2.0
783
--10.6
0.46
57
1.1
21.0
50
--36.6
--0.06
2.2
763
--11.2
0.30
61
1.2
22.0
44
-35.5
--0.11
2.5
735
--11.9
0.23
61
1.1
22.8
39
--34.2
--0.16
2.87
700
--12.9
61
1.1
23.0
38
-34.9
0.00
354
3.0
687
--13.5
0.32
61
1.0
329
21.0
33
--34.2
0.00
4.0
602
--20.0
0.65
61
0.7
25.0
28
--34.2
0.00
4.03
600
--20.2
61
0.7
25.37
26
-34.2
0.00
338
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
?
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5.0
525
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0.51
61
0.5
30.5 1335 cp --= 77?09' k = 189?52'
5.36
500
--26.4
56
0.4
10/10 -St (43)
6.0
456
--29.9
0.48
49
0.2
6.93
400
--36.8
44
330
7.0
395
-37.2
0.73
44
0.0
016
--7.9
85
1.6
135
7
8.0
342
--46.0
0.88
43
0.12
000
-
88
-
122
8
8.28
327
--47.7
0.61
43
0.2
989
-
-
88
-
124
9
8.88
300
-47.7
42
0.5
952
-
-
88
--
9.0
295
-47.7
0.00
41
0.93
900
--
86
--
9.32
281
--47.7
0.00
41
1.0
893
--
-
86
--
10.0
234
-44.3
--0.50
40
295
1.37
850
-
84
--
11.0
219
--43.0
--0.13
40
1.5
836
-
--
84
--
11.6
200
-41.6
40
1.84
800
-
82
--
12.0
188
--41.2
--0.18
40
273
2.0
783
-9.3
-
81
1.8
13.0
163
--41.2
0.00
40
2.14
770
-9.4
0.07
81
1.8
14.0
140
-41.2
0.00
2.5
734
-11.0
0.44
79
1.7
15.0
121
--41.2
0.00
280
2.83
700
-14.0
0.91
78
1.2
16.0
104
--40.8
--0.04
3.0
687
--14.0
0.00
77
1.3
334
16.25 100
--40.6
3.45
648
--14.0
0.00
75
1.4
17.0 90
-40.0
-0.08
4.0
604
-17.2
0.58
71
1.0
18.0 78
--39.5
--0.05
4.04
GOO
--17.3
71
1.0
18.92 67
-39.5
0.00
302
5.0
527
--23.3
0.61
62
0.6
5.38
ZOO
--24.8
58
0.5
6.0
439
--26.7
0.34
57
0.4
302
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
Z9 'xIS - Ot
17poaomic. npumocemuit
H
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6.98
400
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0.50
55
26.0
26
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--0.10
8.0
346
--37.8
0.61
53
26.68
23
--29.4
--0.09
399
9.0
300
--44.0
0.62
52
302
9.9
265
--44.0
0.00
46
31.5 0130 cp = 77?10' X=189?49'
10.0
258
--43.2
--0.80
45
10/10 St (15), *?,
11.0,
222
--40.6
--0.26
11.7
200
--39.8
12.0
192
--39.5
--0.11
307
0.0
014
--5.8
96
112
5
13.0
166
--38.8
--0.07
?
0.11
000
--6.6
14.0
144
--38.4
--0.04
0.2
989
--7.4
0.80
15.0
124
--38.0
--0.04
315
0.5
951
--8.2
0.27
16.0
108
--37.6
--0.04
0.93
900
--9.4
16.5
100
--37.4
1.0
892
--9.6
0.28
17.0
93
--37.1
--0.05
1.37
850
--10.6
18.0
80
--36.4
--0.07
314
1.5
836
--11.1
0.30
19.0
70
--35.6
--0.08
1.84
800
--12.9
20.0
60
--35.0
--0.06
2.0
783
--13.8
0.54
21.0
52
--34.5
--0.05
2.5
734
--13.8
0.00
21.3
50
--34.4
2.85
700
--13.8
22.0.
45
--33.7
--0.08
390
3.0
686
--13.8
0.00
341
23.0
40
--32.5
--0.12
3.28
661
--13.8
0.00
.
24.b
34
--31.8
--0.07
4.0
COO
--18.2
0.61
23.0
-30
--31.0
-0.08
5.0
525
--24.0
0.58
Declassified in Part - Sanitized Copy Approved for Release @ 50-Yr 2014/01/17: CIA-RDP81-01043R002600210003-3
H
B
t
i
U
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d
V
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5.34
500
-25.5
31.5 1330 y = 77?12' k =189?35'
6.0
456
--30.2
0.62
312
6.94
400
-35.8
10/10 Ns (38), -)