SCIENTIFIC ABSTRACT SHATILIN, A.L. - SHATILOV, A.P.
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Document Number (FOIA) /ESDN (CREST):
CIA-RDP86-00513R001548710018-6
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RIF
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S
Document Page Count:
100
Document Creation Date:
November 2, 2016
Document Release Date:
August 9, 2001
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18
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Publication Date:
December 31, 1967
Content Type:
SCIENTIFIC ABSTRACT
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GALEMIN, I.M.,-, SHATILIN, A.L.
Drawing pig iron from the hearth before blowing out a blarnt
furnace. Metallurg 8 no.124-6 Ja 163. (KIRA 1.61l)
(Blast fi=an-ea-Me-intenance and repair)
LI Z.17 1 7 1 ik
I fV
KONDRATIYEV. N.Ye., kandidat tekhnichaskikh nauk; ANDREYANOV, V.G.,
kandidat takhnichaskikh nauk, redaktor; SHATI re-
daktor; BRkYNIKA, M.I., tekhnicheskiy reda or.
[Calculation of wind movements and changes in reservoir banks)
Raschety vetrovogo volnenlia i pereformirovaniia beregov vodo.-
khraniliRhch. Pod red. V.G.Andraianova. Leningrad, Gidrometeoro-
logicheakoe izd-vo, 1953. 106 p. [Microfilm] (MLRA 8:2)
(Reservoirs) (Winds) (Waves)
6
KWMIN, P,P.,Imnd.geograf.naWk; SHATILIMk, M.K.,otv.red.; SOLOVEYCHIK, A.A.,
telchn.rod.
[Effect of forests on the thawing of snow] Vliianie lesa na
snagotaianie. Leningrad. Gidrometeor.izd-vo 1954. 67 p. (Leningrad.
Gos&&arstvennyi gidrologicheskii institut. Trudy, no.42)
(MIRA 12:1)
(Thawing) (Forest influences)
YITGENOV, Ilikolay Ivanovich; STWAZHINSKIY, V.A., redaktor; SHATILINk, M.K.,
redaktor; SOLOVEYCHIK, A.A., takhnicheskiy redaktor. ,
[ocean currents] Morskie techeniia. Leningrad, Gidrometeorlogichaskce
izd-vo, 1954. 106 p. (MIRA 8:4)
(ocean currents)
BOCHKOV, A.P., kandidat tekhnicheskikh nauk; SOKOLOVSKIY, D.L., doktor
tekhnicheakikh nauk, professor, redaktor; SHATILINA, M.K., redaktor;
SOLOTSYCHIK, A.A., tekhnicheskiy redaktor.-
[Influence of forests and afforestation improvement measures on the
vlow of rivers in the forest steppe zone of IVropean Russia] Vliianie
less, i agrolesomeliorativnykh meropriiatii na vodnost' rek lesoetepnol
zony evropelskoi chasti SSSR. Pod red. D.L.Sokolovskogo. Leningrad,
Gidrometeorologicheskoe izd-vo, 1954. 133 P. [Miorofilm] (MMA 7:11)
(Forest influences) (Rivers)
ZAYKOV, B.D., doktor geografichaskikh nan , professor; ~
redaktor; BRAYNINA, M.I., tekhnicheskiy redaktor _W~LINA.:K.K.,
[High waters and floods in rivers of the U.S.S.R. during the
historical period] Vyaokie polovodlia i pavodki na rekakh SSSR
za istericheakoe vremia. Leningrad. Gidrometeorologichaskoe
izd-vo. 1954. 133 P. (MLRA 7:10)
(Floods)
ALEKIN, Oleg Aleksandrovich; SHATILINA, M.G., redaktor; VORONKOV, P.P
otvetstvennyy redaktor';-jL&UM, M~Ta., tekhnicheskiy redaktor.
[Chemical analysis of inland waters; study under stationary
conditions] Khimicheskii analiz vod sushi; pri atatsionarnom
ikh isuchenii. Leningrad, Gidrometeorologicheskoe izd-vo, 1954.
199 P. (KF.RA 8-.2)
(Water--Analysis)
ANDRZYNVA, Yakaterina Vla4imirovna; KOIASNIK. S.V.i redaktor- SHATILINA,
redektor; BIUYNINA, K.L. tekhaicheakiy
[1U.N.Shokel'skii, ocaaaographer, meteorologist, geographer]
IU.M.Shokallskii - okeanQgraf, meteorolog. geograf. Isd. 2-ost
Uaingrad. Gidrometeor. izd-vo. 1956. 52 p. NLRA 10:10)
le Chlau-korrospondent Akedemii nauk USSR (for loleedk)'
(S4okallokii, W11i Mikhailovich, 1856-1940)
DUVANIN, Aleimandr Ivanovich; SIEZHINSKjY, V..A., otvetstvennyy redak-tor;
--494~T- 1~ 3.,K., re"ktor; BRAYNIM., M.I., tekhnicheBkiv redaktor
CSea level] Uroven, moria. lomingrad, Gidrometaorologichask-oe
izd-vo. 1950'. 5B P. (MLRA 10:4)
(ocean)
POPC7, Yevgeniy Grigorlyevich; SHATILINA. M.K., red,-; FLAUM, H.U., tekhn.
red,
[Analysis of the runoff formation of plains rivers] Analls formiro-
vaniia stolm ravninnykh rek. Ieningrad, Gidromateor. izd-vo. 1956.
130 P. (NIRk 11:7)
(Rivers) (Runoff)
DIMAKSYAII, Arta3hes Movsesovich; ZBORYKIN, K.A.,otyetstvennyy redaktor;
SaTILIKA, M.K.,redaktor; SOMIKIIIN, K.F.,tekhnicheskiy rodaktor
[New telemetering instruments for hydrometeorological r)urposes]
Novye teletzmeritellnye gidrometeorologicheskie pribory.
Leningrad, Gidrometeor. izd-vo, 1957. 135 P. (MLRA 10:5)
(Meteorological instruments) (Telemetering)
bUGOL'fU':j,,.V.., Irina Vladimiroviia; ZAYKOV, B.D., doktor geograficheakildi
nauk. redaktor. redaktor; BRAYNIDA, M.I.,
tekhnicheskiy r
r
L.9roding streams and their extension over the territory of the
U..'j,.S.R.] Selevye potoki iikh resprostranenie as territorii Sssi.
?od. red. B.D.Zaikova. Leningrad, Gidrometeor. izd-vo, 1957. 150 3.
(Aros's. on) (MLRh 10:10)
KALIMN, Genadiy Favlovich; MAKAROVA, Tatlyana Timofe7evr*.; SOMOV, N.V.,
otvetstvennyy redaktor; SHATILINA.M.K., redaktor; FLAUM, M.Ya.,
tekhnicheski.r
[Hydrometeorological factors determining the occurrence of high
water in the flat land rivers of European Russiaj Gidormeteorologi-
ches*e usloviia formirovaniia vysokogo polovodlia na ravninnykh
rei*kh'Evropeiskoi territorii SSSR. Leningrad, Gidrometeor4izd-
vo 1957. 177 P. (MLRA 10:6)
(Favers)
PHASE I BOOK EXPLOITATION 361
Moscow. Tsentrallnyy institut prognozov.
Trudy. vyp. 49: Voprosy dologosrochnykh prognozov (Transactions.
v. 49: Problems in Long-range Forecasting) Leningrad,
Gidrometeoizdat, 1957. 287 P. 1,250 copies printed.
Sponsoring Agency: Glavnoye uDravlenlye gidrometeorolog~choskoy
sluzhby pri Sovete Ministrov EFFR.
Ed.: (title page): Morskoy, G.I.; Ed. (inside book-):
Shatilina, M..K.; Tech. Ed.: Braynina, M.I.
PURPOSE: The collection of articles is intended for specialists
in the field of weather forecasting, especially those
interested in long-term prognostication.
COVERAGE: The articles in this collection illustrate the present
position of long-range weather forecasting. The problems
discussed include the formulation of large mid-monthly
Card l/ 10
Problems in Long-range Forecasting 361
temperature anomalies, the analysis -of cycles and anti-cycleoge-
nesis in meridional" circulation and factors causing the appearanue
of autumnal frosts together with possibilities for forecasting
them.
TABLE OF
CONTENTS:
Morskoy, G.I.; Semenov, V.G.; and Kats, A.L. Formation of
Air Temperature Anomalies on Soviet Territory in the
Winter Months 3
The authors define the term anomaly (or a larger anornaly)
as a departure from a certain average climatological pattern,
or, in other words, from the average temperature during a given
period. The authors survey the occurrence of mean temperature
anomalies during three winter months (December, January, and
February) and analyze possibilities of forecasting such
anomalies for one month in advance. In general, wide departures
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Problems In Long-range Forecasting 361
from average temperatures are believed to be caused by
disturbances In the interrelationship -between air circulation
and thermal conditions at the surface layer of the atmosphere.
The entire article is divided into three chapters each
one separate factor causing the occurrence of anomalies. In thv-.
first-chapter, G.I. Morskoy states that the ho.oizontal transfer
of air masses is the main factor in the formation of average
temperature anomalies. He also deduces the ratio between the
zonal circulation of the atmosphere and the generLl thermal
conditions of the atmosphere. The author suggests a new
mathematical approach in calculating the mean monthly temperature
anomalies for absolute topography at the 500 millibar level. In
Chapter 2, V.G. Semenov analyzes the influence of the surface
layer of the atmosphere on the transfer of air masses arid-how
this transfer causes the occurrence of anomalies. In the third
chapter,A.L. Kats surveys the meridional and latitudinal
circulation of the atmosphere and evaluates the contribution
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Problems in Long-range Forecasting -61
of this transfer of air masses to temperature anomalies. The
meridional and latitudinal circulations are calculated for a
number of regions and altitudes in the Northern hemisphere.
The number of focuses on the Soviet territory, where large-
scale anomalies are formed during the three winter months, is
found to fluctuate between 2 and 4. This article is based on
the results of an analysis of 8 forecasts made on the 25th of
each preceding month, for December., January and February of
1955-57. Data on forecasts were compiled separately by three
different bureaus of the Central Institute of Forecasting
(TSIP), viz., the long-term prediction division (ODPP), the
division of dynamic meteorology (ODM), and the division for
methodological Improvement of forecasting service (ORUMDFP).
There are 55 maps, 52 tables in the text and 24 tables in the
appendix. There are 30 references, 16 of which are Soviet, 11
are English and 3 are German.
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Problems in Long-range Forecasting 361
Rafailova, Kh. Kh. Influence of the Artic Region on the
Character of Merldional Circulation of Air in Europe and
Western Siberia. 181
The circulation of atmosphere in the Arctic was studied by
B.P. Mulltanovskiy. 'He concluded that the polar region is not
a solid high-pressure zone, but, contrary to previously
expressed opinions, is composed of a number of cyclonic
and anticyclonic areas. Other Soviet scientists, namely B.L.
Dzerdzeyevskiy and L.A. Vitel's confIrmed Mul'tanovskiy's
theory and proved that all circulation phenomena such as
occur in moderate zones, exist also in the polar zone. The
present article analyzes the effect of.air circulation in
the polar area on the behavior of meridional processes,
carrying cold arctic air masses to temperate zones and thus
bearing directly on changes in weather. Consequently, any
weather forecasting In the moderate zone must account for
meridional processes drifting in from the North. The author
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Problems in Long-range Forecasting 361
examines four possible types of thermobaric fields in the
troposphere over the Artic and also a number of variations.
Maps accompany this analysis and provide data nn absolute and
relative topography at 500 millibar level for all the types
Involved. The author concludes that a certain definite
character of the baric field in the Arctic produces a definite
type of meridional movements and that thermal conditions of
air masses in the Arctic are good Indices for the developing
synoptic , situation in the moderate zone. There are 11 tables,
22 maps, and 17 references, of which 13 are Soviet and 4 are
English.
Bagrov, N.A. Application of the Principle of Similarity in
Forecasting Mean Monthly Air Temperatures 231
By the "principle of similarit " the author understands an
attempt to trace similarities Tanalogies) in the development
of two or more atmospheric macroprocesses. The principle can
be applied in long-term forecasts when an atomospheric process
bears a similarity to a process which occur-red some time in
the past but during the same season and in the same locality.
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Problems in Long-range Forecasting 361
The author analyzes the applications of this principle and
refers to S.T. Pagova who opposed it and to L.A. Vitelts who
modified it. The latter worked out a theory of rhythmicity
(rhythmical recurrence) of temperature processes. Vitells'
theory is given in brief, but the author of the article
rejects it. The author establishes indices of similarity and
demonstrates their applicability in deducing mean monthly
temperatures The data used cover a period -)f over 50 years
and are derived from 45 unsDecified Ezelographical localities
in Russia shown on an enclosed map. The percentage of correct
forecasts by the principle of similarity has hardly ever
exceeded 70 percent; on an average It amounted to 63.2 percent.
The author urges expansion of this method of study and the
inclusion of localities outside Russia. He suggests examination
of other factors, such as near-surface pressure, to which the
principle of similarity could be applied. There are 8 maps,
7 tables and 14 references, of which 8 are Soviet, 2 German
and 4 English.
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Problems in Long-range Forecasting 361
Zverev, N.I. Influence of Ocean and Land Temperature on
Atmospheric Circulation During the Warm Season in the Far
East 250
The author analyzes the influence of thermal nonuniformity
of the surface layer on the atmospheric circulation and
discusses some implications from observation results pertinent
to weather forecasting. The author defines nonuniforraity as
the phenomenon of the accumulation of heat in the surface
layer and the unequal distribution of this heat in latitudinal
and meridional directions. The article consists of two chapters.
One examines the formation of temperature contrasts between
ocean and land and the other examines the auestion of period-
icity, i.e., the existence of definite -natural temperature
intervals (from 6 to 12 days), and the connection of such
periods with temperatures of the near-surface air layer.. The
subject of temperature variation was studied by personnel of
the'long-term forecast division of the Far Eastern Scientific
r
Research Institute of Hydrometeorology (D)f NIGMI).The- Lnst-itute
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Problems in Long-range Forecasting 3061
compiled daily temperature maps for sea and land in 1934-38.
In addition, the author availed himself of the material
collected in the archives of the Central Institute of Fore-
casts (TSIP). There are 12 maps, 6 tables, and 8 Soviet
references.
Byal.ynitskaya, V.(',., and Ped', D.A. Formation of Night Frosts
in Ukraine 264
The authors place night frosts in Ukraine into the category
of those that are dangerous, i.e., capable of damaging crops.
This type of frosts is common both in autumn and in spring,
but the authors analyze only the occurence of frosts in May.
Crimea is included in this study. Tabular material includes
statistics of occurrence and duration of frosts. The &.oticle
analyzes the thermobaric field during the occurrence of frosts
and.compares it with the field when frost is absent. Pertinent
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Problems in Long-range Forecasting 361
Indices are deduced and data given on how to forecast the
onset of frosts one to two days ln advance. There are 13
tables in the text and 2 in the appendix,