SCIENTIFIC ABSTRACT ZVEREV, M.S. - ZVEREV, O.S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002065710007-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 26, 2002
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

MIKHAUZY, A.A., otv.red.; red.; mixoTswo ?.a,, red,';
KASVICH, A.G., X.R.o red,; BOBCW* V.V., red.;
SUBBOTIN, X.Y., redo; SAKSOMMKO, L.V.#.red.; TMUKINA, X.Ap,
takhn.red,
[Astronomy in the U.S.S.R. during forty yearo 1917-1957; collected
articles] Astronomiia v S$U sik vorok let, 1917-19,571 sbornik
statei. Rsd.koll6giis: A.A.gikhoiloy i ar. Moskvii, Oos.izd_Vo
fiziko-matem.lit-ry, 1960. 728 P.
(MIRA 13:7)
(Astronomy--History)

ZVEM N.I. kandidat tekhniches~lkh nmik
e- -6=alculation of the auction flue of baffle-type flyI-ash col-
lectors. Toploonergetiks. 2 no.5:44it9 MY '5,5. (KWA 81:9)
1. Vessoyusnyy teplotekhnicheskly institut
(Dust collectors)

R SV)
AID.P
Subject USSR/Electricity
Card 1/1 Pub. 110-a - 9/17
Author~ Zver~~~I., Kand. of Tech. Sci.,
Title Computing the outlet pipe of a screen-t,~pe ash ca'tch6r
.Periodical Teploenergetika, 5, 44-49, My:1
955
Abstract A mathematical analysis for designing a pareen-6 e,~ ash
Wi YP
catcher eqiiipped with an ejector:j.'s pr6sented th iables,
curves and equations. Five diagrams.
Institution All-Union Heat,Technology' Inatituie
Submitted No date

AUTHOR: Zverev N*I* Candidate of Technioal SciQnces*
TITIS: Modelling the motion of poly-dispex&~K/Rls-
(Modelirovani-i dvizheniya
li.)

polidisper6n
OY py

FSRIODICAL: No
"TeploeneMetikall (Thermal Power) 1957 Vol-41
-7,
.
:
pp. 35 - 38 (U-S-S.R.5
ABSTRACT: Ia a previous article Ithe author showed that thexe
are five criteria that characterisG the steady*otion
of dusty gas or liquid. Two of:these.'eriteriajina lude
the diameter of a dust particle., Conseqaently:th6se
criteria are only applicable to mono-disperse dusts
(that is dust consisting of particles of one size:on].yl
In practice we have to deal almost eiclusively"with
poly-disperse dusts, that is dus,ts,consisting of part-
icles of many sizes. At low dust boncentrations when
the motions of different fractions do,not inte.radt on
one another modelling may be effected by sub-dividing
the poly-disperse dust into,a number of narrow
fract-ions and using corresponding fractions in the
card 1/4 model. However, this pxocedure,As very laborious and
is quite inapplicable at high cLoncentrations, Neither
is it permissible to introduce some sort of means

Modelling the motion of poly-disp.erse d4sts. (Cont.)
96-7-7/25
diameter into the criteria since in order 'V-O choose
the diameter correctly it is necessary to know in
advance the function that it is required to find*
All this severly limits the possibilities of mode-
lling for the study of industrial equipment and* there-
fore, it is necessary to find additional conditions of
similarity of motion of poly-diroperse dusts. , ;,
The similarity of motion of tNo dust flows is then
considered. During the course of the examinevion.*the
dimensions of the dust particles.are .expressed,as,~a
ratio of a dimension which is characteristic for the
given dust so that the diameter of the particle is
expressed by a dimensionless number. It is then Shom
that in two systems with identical criteria consisting
of characteristic dimensions all the:dust particles
with identical dimensionless diameters have certain
criteria in common. As a result of the eyamination
additional criteria are in effect introduced'forl.poly-
Card 2/4 disperse dust.
In order to ensure cauplete similarity all five
main critoria should be the same for both model and

Modelling the motion of poly-dispe dusts. (Cont.)
.T;I-T-T/25
specimen. This is often difficult,i'and-sometimes imp-
ossible to achieve. It is therefore desirable to cut
down the number of criteria and the various waysAa
which this can be done are considered. It is shoun that
simplification is possible when the range of concen-
tration is from 0,05 to 0.1 kS/kgj'orAf t.4e force of
gravity is negligible compared with the inertia forces.
This latter point can be cleared up by using the test
equipment in different positions, for oxample, if its
performance does not change when it is. inverted, grav-
ity may be igaoredo- It is shown that when modelling
on the basis of three criteria the gaaspeed, dispem-
ness and density of dust in the model are fally defined
and cannot be selected arbitrarily, Therefore, this is
the most difficult case of modelling. When modelling
by two criteria two scales,are fixed and one is arbi-
trary. Still further simplifications,are sometimes
possible.
Card 3/4 When the necessary scales have:been found the nece-
ssary dust density is determined, then the best avail-
able material is chosen, and then if the density is

Modelling the motion of poly-disperse dusts. (Cont.)
96-7-.7/25
not qIlite of the value required the remaining scales
are altered somewhat. -The various:
I degrees of fineness
required in the model dust are calculated and the.
material is milled in a laboratory mill. Sieve anal-
yses are made during the course of 'milling until-most
of the dust is. of the required composition. If the
dust contains an excess of fines or coarse particles
these are removed by appropriate sieves. A quatity*of
100 - 200 grams of dust is usually necessary for tests
on laboratory models and the quantity of dust required
for a complete series of tests does not exceed 2
3 kg., In practice it is not difficult to produce such
a quantity of dust of a required composition and in
any case it is easier than preparing a larger quantity
of close fractions.
card 4/4 There are 4, figures and 2 references, 1 of which is
Slavic.
ASSOCIATION: All-Union Thermo-technical Institute (VTI)
AVAILABIL,

-7 /V
'
V.I. (zagineer) & Zverevo N.I. (Cand-Te
ch.sci.)
AUTHOR: igaat Yev, U I
TITLE: The flow of dusty gas round a cylinder (Obtekaniye tsilindra
zapylennym gazom.)
PERIODICAL: 1958
No.3.
Toploonergetika
pp. 30-40! (USSR)
,
,
.
ABSTRACT: There are muny processes in which dusty gas flows
round a c:ylinder.
,
Of the total number of particulea that pass through a cros4-sectional
area equal to that of the cylindor, but a considerable dist
ancd
in
.
,
advance of it, only a proportion roach tho surfaca of the.oylinder
and the remainder pass by. The ratio of those that touch the -
cylinder to the total number -jas determined in this work for various
conditions and the distribution of the dust oven the surface of the
cylinder was studied. The experimental device consiated of a vertical,
channel of 500 x 50 ima section. The tes-Voyliudor was located'at
the centre of the section, parallol to thl short side, at~a distance
of 45 hydraulic diameters from the inlet., Flow was always turbulent
at the position of the cylinder. Arrangements were made to ensure
that the conditions of air flow over the cylinder approximated~to
those in a boundless flow. The other experimental conditions are
described. The tests were carried out with friketions of milled
anthracite and metal dust (an alloy of chremi= and iron) with'
specific gravities of 1.055 find 7.3 -ram/cm'- respectively.. ,The
fractions were prepared in air separators, Tile procedureof
Card 1/4 preparation is described. The characteriatico.of the fractions in

The f low of dusty gas round a cylinder. 0/2
respect of the velocity at which they fly i1pich-7W specdf Md
hydraulic diameter (the diameter of a Bphero with~ isame density und
pick-up speed) are tabulated. Dust for the''Aasts was poured'into a
tube and blown into the collector by a strong yet of air from a needle
valve. It was shown by special tests that with Qis method of .
delivery the suspension broke up into individual~_Just particles,;
uniformly distributed over the working section. In order to determine
the proportion of (lust trapped on the cylinder ULO cylinder, iras
wrapped round with it ring of cinefilm, 10 mti~~ivide smeared with
petrolatum, wtUch trapped all. the dust particles .+,hat touched it.
The film was then compared with a transparent scale under a
microscope. Various experimental procedures were used ;md are
described. Hine series of tests were made with dowmward flow,
anthracite dust being used in Nos.1 - 7, and metal dust in Nos. 8 & 0.
Speeds of around 2, 4, 12 & 16 m1sec were used with cylinderu of
12, 25 & 50 mm. diameter. In each series ofAests the finest fraations
were used first followed by the coarser. The tes-ts were mado at rocm
temperature and pressure. 11ohen Reynolds number for the particles is
less than 0.1 the resistance to the medium acting' on the particles is
given by the Stokes' formula, and the St criterion defines the motion.
Card Mien Reynolds number for the particles is greater than 0.1 Stokes'
9//A formula is inapplicable and motion is not uniquely governed by the

The flow of dusty gas round a cylinder. 96-3-10/26
St criterion. 1-kevious authors have given the proportion trappeil as
tj
a unique fraction of St,asually there was,,a considerable scatter
of points and considerable difference between the general
relationships obtained by dilteront authors. This~ was probably
because in the experiments, Reynolds number was riot low anaugh and
instead of a unique relationship between the proportion of
particles trapped and St there should have been a family of curves.
The authors' test results are given in Pig.l. 11.ie accuracy of the
determinations is such that a family of curves can be plotted. Tlien
-the particles move in a vertical flow their relative velocity at
a distance from the cylind6r is practically equai to the speed of
pick-up, but the velocity increases near the cylinder. Iuthe I I
majority of tests the Reynolds number was 9'reator than 0.1 even.in
the part remote from the cylinder. Therefore, in inast of the tests
-the resistance factor according to Stokes' law was not deterTiinod.
Then particles move in a vertical flow their trajoctory and:thc~
proportion trapped may also depend on gravitatioilal force. To check
this point, trio additional series of tests~were made with anthracite
dust and rising air flow at speeds of 2 and NAM/secend. Jn ihese
tests the axial components of inertia iuid gravity forces wore opposed
sE, that if gravitation was important the proportion trapped,should
bo less than in the first series of tests. The ~results of -the tests
Card 3/4 given in Fig.2. confirm that this was so. This applies even to the

The flow of dusty gas round a cylinder. 00-3-10/26
finest of particles for which the air speed was'far above the
pick-up speed. Dimensionlesia curves of tile distribution o4 trapped
dust over the cylinder surface are of quite a different character
with upward and downward flow as will be~ seen from Fia.3,
t4
Therefore, gravity has a marked effect on the process. An
additional criterion D is introduced that, together with the
criterion St, determines the probability of particles hitting the
cylinder with a downward flow of air. Fir
,.6. gives curves of the.
distribution of trapped dust on the surface ot the cylinder with a
downward flow of air. There are 7 figures, I table and 10 literature
references (6 Russian and 4 Eliglish)
ASSOCIATION: All-Union MerMo-Teebtlical Institute. (VE30SOVUZnvv Teplo-
AvAnaLu: Li .brary of Congress. tekhnicheskiy Institut).
C or d 4/4

61
ACCESS IOIN NR. AT404 0568 S/2546/64/1000/135/0063iDo9,Q,v.
AUTHOR: Z Werev, N
TITLE: Waves I n the atmosphere w
SOURCE: Moscow. Tsentrallnrky institut prognozov. Trudrv, no. 135, 1964..
Sinopti,.ostatisticheskiye metodyfr prognozov pogody* (Synoptlc~statistical'methods
of weather f e
or casting), 63-90
TOPIC TAGS: meteorol f re culation, atmos-
ogy, weather o casting, atmospheric cir*
pheric wave, periodogram
ABSTRACT: On the basis of a review of the extensive' b1b,liography, the authors
analyzes the literature dealing with waveprocesses in the atmosphere and, des,'cribes
the statistical methods of perlodogram analysis used by :Various authors1dr de-
.,,.tecting large-scaie waves. It.is.s-hown that the statistically detect'ed V;aves'can
be used for forecasting atmospheric circulation for as much as a month In advance.
Particular attention Is given to an analysf~s of pressure and temperature waves
with periods of 5 to 7 days, discovered by a great many investigators. Considera-.
tion is given to the methods used by various authors who have. found wavei with
periods of,12, 17, 25,-11, 13 and 22 days and many'others. in each case: the.';.
-author hds attempted to determine whether these waves are real or a mathematical
Card 1/2

ACCESSION NR: AT4040568
fiction, how stable they are If real, and whether they can be extrapolated for a
Ilong period. it k concluded..that wave processes with periods~of 5-6, 8 and 13-
14 days are stochasv:cally real. Contrary.to certain other investigators, the
t author believes that this fact can be.used~for practical"purposo*s and,that the
methodology used in earlier attempts was faulty. Three signif,icant forny'llas are
a
presented which can be used for judging the presence of wave p,rotesses in the at-!
mosphere, the most important being a spectral function of the entire process,:
it Examples are cited showing how wave processes in cyclonic and 41nticy~lonic acti-,
vity at the mean levet of the troposphere can be detected, The only period do-
tected simultaneously in both the meridional and zonal air flow components is!
T = 14 days. It Is shown, however, that there is no rlgorous,periodicity:in the
atmosphere; the periods of 5, 8 and 14 days are approximat Ions. Recommenoot I ons,-
are made for prediction of circulation at the mean level of the:troposphere, a)-
though only for August,'September and October. only tho5e wavcs which devielop in
quasi-stationary pressure systems are of practical value, for the forecaster.
Orig. art. has: 93 formulas and 6 tables.
ASSOCIATION; Tsentrallny*y ins'titut prognozov (central Institute of Forecasts)
SUBMITTED: 00 oAT EACQ: o2ju164 ENCL: 00
car~f 2/2 SUB CODE: 'ES NO REF SOV: 036 :OTHER: 020
77

JA llj~
L__1428q~.66 m
:EWT( IJP,4
AGG NR: AT6066666 souRcF, Gobr,-. u4/m
, , ~ Ki~i)!
AUTHORSi imov. L. 1(.,, (Kiev); KPJR_0D_cjwywl_&J
(Kiev);
T
__Ellsldn.
Zverev, 114
Taev); Lazareva. N. H. -ev)
Ki
ORG.- none
-Investigation ot the_effec'ts' of.,soveral: a~toi
TITLE,4
tant Alo- 'used-lor' t6r~ifi~
sties of heat resis -,blad'
SOURCE: _Vs
Ad V_
A
ir irua
--n.- v;; 5n- -noy
(J
or-
h th 1_kAUipw_oh~ra6t
t1jr:

L ohq~o_67 K~?J-r( 1) ow
-ACC ~NRt AT6_ ~28~,O -~o-il~ci-zd~iF-~-R-i2546/66/000/1531007910089
AUTHOR: 7-verev, N. I*
ORG: none
TITLE-. Long-range of the intensity of zontill:circ uAation of;the atmos-_
phere
SOURCE. 'Moscow. Tsentrallnyy institut pr2Z=~~y. Trudy~ no. 153, 1966..~
Statis;icheskiye metody dolgosrochnoso prosnoza pogody (Stnti6tical methods of long-
.,range weather forecasting), 79-89
JOPIC TAGS: long ranaa weatper forecasting, atmospheric current, linear:operator,
linear equation
.4,DSTRACT: The author examines the possibility of a long-range forecasting of the
tensity of zonal circulation on the basis of the theo'ry of~linear extrapolation,
ationary sequence, and stationary processes. A linear formula is derived for fare-
casting the jrit.e.nsity of zonal circulation which, the author asserts, ii the: best
extrapolation formula, since for Gaussian processes the linear operator 'is the beat
operator of forecasting. From the investigation it is concluded that long-range
forecasting of the intensity of zonal circulation and iarge-scale cLrculation in
general can be successful only with consideration of the effect of history on the
future development of synoptic processes or even of individual characteristics during
the development of macroprocesses. The use of altitud6-variation charts and the
Card 112

GW'
ACC IRR AT6028447 SOURCE CODEj UR/2546/66/000 X064/066&i~
7
AUTHOR: Zverev N,
L; Kashleva,
OR4: nont
TITLE: Statistical method of forecasting the.zonal in6x
SOURCE: 10scow. Tsentral'nyy instit6t PT ,Trudi, no. 153, 1966.
1&110 _Zuy,
StatisticheskiYe metody dolgoorochnogo prognoza pogodyi.i(Statistical methods Pf long-".
range weather forecasting), 64-68 i
TO IC TAG statistic analysis, long range weather forecasting, atmospheric curre
T.
p -ore
ABST~RRA ~T.The urpose of this investigation was to elicit the possibility of f
casting the mean monthly value of the zonal index statistically. In t7oiking out this
6ethod, the authors proceeded from the assumption that'by taking into account the.
past history of zonal circulation itlis"posuible to precalculate the value of the
zonal index in the future by extrap,3iation. Having found that purely zonaLcircula-
tion in its evolution undergoes variati6ns.with periods of 9 and 23 ntonths,tthe
authors set up multiple regrission equations for forecasting the zonal,index for a:
month with a zero and monthly length:lof time before the forecast phenomenon occurred,
The values of the zonal index for past months were calculated as the starting data.
The regression equations af or flacreening" the predictors had the form:
A5, ) = 011MI-4+ +91141"~+ d4;
Card 1/2 + PlAk-21, + PAY44), + (2)

ACC NRs AT6028447
Here AI(n + m) are,the forecast values of the devLation of the index from the monthI5
norm; n is the initial number; Ion of'~ the value of the zonal,
A I (n - k) is the deviat
index (n - k) of the month from the norm of the same th;
morl cli, 0i are empirical
influence functions-("weights"). These equations werelderived separately~ for'. the cold ~41,
and warm halves of the year, which in turn were divided J11to two halves. ~ Equation
(1) gives the forecast of the deviations of the mean monthly values of the index
from the norm in the.imonth fd1lowing'the initial month, and calculation by Eq~o (2)
gives the forecast for the next month, or the forecast'of the~zonal index'vith a
30-day length of time beforeithe forecasting of the phen'olmenon occurs, An anslysis
'of the data showed that the proposed method of extrapolation makes it possible to pre-
calculate the intensity of zonal circulation at the mesa level of the troposphere
a satisfactory guarantee. Thus; precalculation of the index can be'tieed when.-;..
Utica
compiling monthly forecasts by.theore I methods. Orig, art,. has: 5 f rmulas,,uidd~,
1 table and 2 figures.
SUB-CODE: 04/ SUBM DATE:Fnone/ ORIG REF: 007
7.
kh
d 2/2
Car

BAGROIIJI N-A,; VL-YIJXO',r, K.A.; "UVEREW, 14.1.
FIT
Principle of aralop7 and Its use ir pn-etteallvork.. Trudy TSIP.
no.132'.41..,47 164. (MIRA 17~!C),

IGIMTIYEV, V.I., insh.; ZYMNY, N.I., kandotekhn.nauk
laboratory air separator with a boiling layer. Toploanergetika
7 no.2:55-58 P 160. (MIRL 13:3)
lo Vseuoyut.nyy teplotekhnicheskiy, institut,
(Separators (Machines))

The Storm ~Ifind of 14 November 1952 in the South of' the Eurdnean TerritIo ry
of the USSR. Meteorol. i gidrologiya, No 6, 1953, pp 3-71
In the southeastern European part of the USSR from 91D 11,~Nbvember
1952 wind strengths up to 28-34. meters/second were observed. The author
discussed the variation of the wind regime during this period. ,For each
day be constructs tbe charts of wind velocity.for the ground level and
for the altitude 300, 600, and 900 meters above the level of tb6 ground.
The storm arose as the result of intense dropping pressure.in thelower
kilometer layer, which transferred the momentum from ton to bottom with
the simultaneous advection of cold masses from the northeast. 02,Geol,
No 5, 1954)

ZVXM,N.I., kandidat fisiko-vatematicheskikh nauk
ij
Meteorological works of.the Russian geophysicist 1. Smirnov.
Meteor.i g1drol. no.5:56-57 W '53. (Nm 8:9)
1. Wentrallnyy Institut profsoyusav, Moskva.
(Smirnov, Ivan Nikolaevich)

Z- VeR
Subject
Card 1/1
Author
Title
Periodical
Abstract
r, 1.
AID P - 180
USSR/Meteorology and Hydrology
Pub. 71-a 7/26
Zverev, N..I,-
on temperature forecasting
Met. i gidro.,, no.2,, 28-29, 1955
The article is an attempt to est~$JiA.with equdtio'ns
and charts the able played by turbulence in the,woving
of warm air.1~7C.*i...table and 2 charts are given.

SOVI 1,24-5~;54563
Translation from: Referativnyy zhurna.l, Mekhanika, 1958, Nr 5, p 91 (USSR)
AUTHOR: Zverev, N. I.
TITLE: On the Influence of the Temperature Field of. the Continent a~nd
the Ocean during the Warm Season Upon the.Atmospheri'c Ci'rcula-
tion in the Far East (0 vliyani, 'Lemper'aturnogo polya kontinienta
i okeana v teploye vremya goda na atm,osferriuyu tsirkulyatsiyu v
usloviyakh Dal' nego Vostoka)
PERIODICAL: Tr. Tsentr. in-ta prognozov, 1957, Nr 49, pp 250-263
ABSTRACT: Bibliographic entry
1. Atmosphere--Motion 2. Oceans--Th6rmal effects
3. Eartb--Thermal effects 4. Glimatic factors--Asia
Card 1/1

Problems in Long-range Forecastin4 Leninoad 361
rjidrozWIteojzdat, 1957.
Zverev. N.I. Influence of Ocean and Land Temperazure-67n-
.-A-Fmospheric Circulation During the Warm Season iri the Far
E~st 250
The author analyzes the influence of thermal.,inonuniformity
of,the surface layer on the atmospheric circulati6n and
,discusses some implications from'observation'results pertinent
to weather forecasting. The author defines nonuniformity as
the phenomenon of the accmulation 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 question of period-
laity, 1. 0 the-exiBtence of definite natural temperature
interval;
from 6 to 12 days), and the c6nneetion of ouch
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
Researc4,Institute of Hydrometeorology (DV IfIGMI),The'Inatitute
Card 8/10

problems in Long-range Forecasting 361
compiled daily temperature maps for sea and imid in:1934-38.
In addition, the author availed himself of the idaterAal
collected in the archives of the Central.Institute of Fore-
casts (TSIP). There are i2 maps, 6 tables, and 8 S oviet
references.
Byalynitskaya, V.G., and Ped', D.A. Formation of Night Frosts~
in Mraine 264
The authors place night frosts in Ukraine into the;category
of those that are'dangerous, i.e., capable of ':damaging cropd.
This type of frosts is common both in autumn and in spring..:~
but the authors analyze only the occurenbe of,frosts in May.
Crimea is included in this study. Tabular material includes
statistics of occurrence and duration of frosts. The article
analyzes the thermobaric field during the occurrence of frosts
and. compares it with the field when'frost is 'absent. Pertinent:
Card 9110

Problems in Long-range Forecasting 361
indices are deduced and data given on how to forecast the
onset of frosts one to two days in advance. There,:are 13
tables in the text and 2 in the appendix,, 8 ma s, 2drawings
P
and 16 references, of which 14 are Soviet and 2 are' English.
AVAILABLE: Library of Congress HM /kav
8-12-58
Card 10/10
7; TI 4!4
I I'l Iq aIFlril V~11

ZVEREV-9 N.
FRI
DO
Iq
-7: 1:- F, 11!T; ji-~,:Tjpj 111jr
1.1 W fit !,?t itll~ 11:1111, f. 9151A i!jl 11

-----------
.............
all
pul Wif 11

3(7) SO'[/50-59-5-20/22
AUTHOR: Zverev, N. 1.
TITLE; Final Meeting of the Scientific CoUncil:of the Contral.1natituto
of Prognosis (Itogovaya sessiya Uchenogo sovata Teentrallnogo
instituta prognozov)
PERIODICAL: Meteorologiya i gidrologiya, 1959, Nr 5; pp 61 62 (USSR);
ABSTRACT: On January 12-20, 1959' a meeting of the Scientific Council took
place at the Tsentrallayy institut prognozov (central'Inatitate
of Prognosis). It was dedicated to the:finafresults in the ful-
filment of the plan for scientific research: work- 3 reports were
delivered in the Agrometeorological Seciion,of the Scientific
Council. L. A. Razumova and S. B. Mastinskaya put forward,the
results of the three-year experimental,work at which'the formation
of ground humidity'reserves an& the correlation between the state
of the ',~summer wheat and corn and the~yiatorlsupply in the newly
won land (the steppe areas of the Kulunda Steppe and of northern
Kazakhstan) were investigated. S. B. MastiAshays., N.I* h. Meshcha-
ninova, Yu. S. Mellnik, ff. A. Baybayeva et al participated
Card 114 directly in the working out of this subject. Co-workers of the

Final Meeting of the Scientific Council of the Central 8OV/56-59-5.:20/22
institute of Prognosis
following organizations took part in the investigations:
Kazakhskiy nauchno-issledovateliskiy gidrometoorologicheskiy
institut (Kazakh Hydrometeorological Scientific Rsaearch In-
stitute), Novosibirskiy biologiolieskiy.inatitut (Novosibirsk
'Biological Institute), Kazakhskiy institut im. Villyamf3a (Kazakh
Institute imeni Viltyams), Kazakhekiy institut zernovogo khoz-
yaystva (Kazakh Institute of:Grain Econo ), as well,' as::the
MY
co-workers of the agrometeorological titations. B. P.Iono~larev
spoke on the evaluation of agrometeorological conditions for the
grow th )f surnmer wheat in tile area,2of the RSr-SR- 7;repprts
were delivered in the Hydrological Section of tile scientific
Council. The most important results mere obtained by~ V. D.
Komarov, A. 11. Vazhnov, and A. I. Karakasho V. N. Par4hin and
Ye. G. Popov worked out a new method for bhe evaluation of
hydrological forecasts. A. I. Afanaa2yev presented conclusions
on the features of the decay of the snow cover on the bas*is
of an interpretation of aerial photographs during thd melting
of snow. 7 reports were delivered in the Meteorological Section.
Card 2/4 F. I. Monakhov put forward the result-s,of experimental inveatiga-

"~o to, 6
4'o TO-90'- - -,I I I
ol~
10,fles -fit the j:or
I of
1 al V'-
"~s ,ISO ~e0l)~o
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.7~_~VF_RFW, M,1'
3(7) PHASE I LOOK EXPLOITATION SOV/,)249
Moscow. Tsentrallnyy InstiLut prognozov
Voprosy do, go erochnykh prognozov pogody (Problems In Long-Rnnge Weather Fore-
castina) MOBQOWI Gldrometeolzdat (otd.), 1959. 62 p. (Seriest lint
Trudy, vyp. 85) Errata slip Inserted. 900 copies printed.
Sponsoring Agency: USSR, Sovet ministrov. Glavnoye upravlonlye g1dro-
meteorologichaskoy sluzhby.
Ed. (Title pape): G. I. Morskly; Ed. (Inside book); L. V. BlInDikov;:Tech.
Ed.: T. Ye. Zemtsova,
PURPOSE: This issue of the Institute's Transactions~is intended for scientific
research and field workers in meteorology as well as for advanced students in
schools of higher education.
COVERAGE: This is a collection of three articles in oynoptic and Ceneral meteorology
Two of the articles deal with problems concerning the general circulation of the
atmosphere while the third discusses the matter of forecasting mean 7-day pres-
sure maps. Referencesaccompan-,r each article.
Card 113

=map
Problems in Long-Range (Cont.) SOII/324-9'
TABLE.07 CONTENTS:
Rayev, 1. K. On the Theory or the.Ge6eral Cir,culatioln ofithe Atmosphire
The author attempts aitheoretical description of.the general circulation In
the most general statement ofthe problem, This,entailso first of,'aallp the
consideration of nonlinear and viscoalty membersi'tin difforentlal !3quations,
and also the consideration at the nonadiabatic'ef'f'ect a yhich. play ;L bapic
role in the general circulation of,the,atmosphere,. This,work dIfFPr6,-. from
others on the problem . insofar L as the author pays , atria ter attention to ~ the
dependence of the thermal properties of the underlying surface onieographic
coo~.dinates. Computations are introduced to show that tem7jerature,ln time
and"space as well as all elements of motion may be determined when~thep'initlial
distribution of meteorological elementa and the heat influx from the S~n,as
a function of tIme,are known. There are 4 referencest 3 Soviet and 1~English, 3
Zverev, N. I. Forecasting a Mean AT 500 Seven-day,Chart
___Ti_nce most extended forecasts do,not deal with weather conditions to be ex-
pected in the week immediately following the date'of chart compilation the
author presents a statistical method of compiling mean 7-day chaAs. 'The
author works on the basic premise that the development or synoptielprocesses
in the future Is completely determined by the history of synoptic processes
over a given roglon. Thore are 7 raferences: 4 Ooviet find 3 English. 27
Card 2/3.
fj :~ 7 7:~T 1. TIfi:I FI !i VT
.111, !ZT,42 "'1., 111 11 11 1111 U-1r.1.11 HIM. Mill ill 9 1. 1 1

'3/10/62/900/007/i09/149
D228/D307
AUTHORS: Vasyukov, K. N.,, 4verev
N. I. and Ped', D. A.
TITLE: Using the:principle*of analogoul'ness~when for6ca6ting
synoptic prccesses and the weather for five dd a
PERIODICAL: Refera"--'vnyy, zhurnal, Geofizikat- no,,7, 191629,1 48 9ab__'
stract*7B257':(Tr. Tsentr. in-ta;'Tprogrk6zov, no.,:116,
1962,. 13-23)
TEXT: The N-500 values for a.standard grid'of points, located ev-
ery 40 of latitude and 120:of longitudo on tho territory ounded
by 360W, 840E, 760N, and 360Wt were taken from tbe'averageTmaps
for natural synoptic processes (NSP) in Janu~ry and Februgtr~y,::1938-
1955. After this the.eigns-of the,geopotenti~l differences, re'.spec-
tively characterizing the zonal and the meridional.flow co'Mpon ents
were determined for meridionally and latitudinally neighboring V/
points. Th 'e values +1, 0, and -1 were reepectivelY ascribed to
positive, zero and negative differences. The resulting magnitudes
--of the rAeridional and the zonal wind~components for all NSP were
Card 1/ 4
7i

8/169/62/000/007/109:/49
Using the principle ... D228/D307
printed on tape, The analogs of the N-500 averages for the para'-
meters P,,and , characterizing the similarity offields withre-
PA.
spect-to their--ciroula-tional.--features-, were selected for the first
20 maps by means of the electronic computer "Pagoda". The valu6ifj of
P(P (111d P,~.waro ouloulatud from tho f ormulad t
n n
nA -
+
n + n P/L n + n
+
k+
where no+, n. n n is the number of cases when the signs of
the meridional (n and the zonal (nA) flo on
w camp ents in two-com-
1P
parable N-500 fields of NSP do, or do not, coincide. The comparison
of all NSP with the-briginal 20 allowed the distribution of,the de-
gree of analogy for the fields of2the 500-mbAurfaPe's January,geo-
-potential to be obtained from-the parameters of a 'and a It aloo
Card 2/4

S/169/62/000/007/109/149 .
Using the principle D228/D307
allowed the natural frequency of analogous processes to be;ex osed
p
separately according to the development of the meridional and.the
zonal air-flow components. Utilizing the criterion p all processes
can be dividod according to their,dogroe of finalo~gy t 0throd ca-
tOgOriOG: '010 atlftlog > 0-4), the non-analog -0.3, 40-4),
and the reverse analog (p A-0-3)-.Utilizing ~the criterion-p too,
we will obtain the analog P ,';~0.8, the non-analoglp,, = 0.2-.+ 0.6,
cihd the reverse analog /4 0'2. The criteria.~are,established with
a 10% guaranty. In practical work, when classifying all processes
into three categories, the degree of guaranty sho.~-'ld be established
jointly according toboth criteria for the analog p,>,,0.4,and PA.`~_
0.6, the.non-analog -.0.3 4prp 1, 0.4 and 0.2-~ p/t /_ 0.6, and the re-
verse analog -p f,0.3 and p ~.O.2. Average estima'-tes are given for
ogousneL
the anal of subsequent pairs of NSP'in relation to the de-
of'analogy of.the original pairs of NSP~with'respect:to P(P
Card.3/4

-- - ---------- S/16'9/62/000/007/lb9/149
Using the principle.... D228/D30il
and
+ As the geometric likeness increases, the', analo
PA
-ousnese iii the development of atmospheric processes in subf3equeni,
NSP grows generally,.But in a number- of examples it is shown, too,
that the factor ok geometric analogy, though it.ie of great~signi-
ficance in estabi'lishing the analogousnooo Of~ ~,LtMOE.PherjO PI'0000-
son, does not always givo pracLically valuabI6 pointers -to the fu-
ture development of processes. In some cases originally similar
processes subsequently change int6 non-analoSs. Using modern com-
puters it is possible by means of the analogy.!parameters of p
rp
and + o -to take into account objoctiVely the develop-
PA P P
ment history op atmospheric processesi to solve pr'oblems cor-nec-
ted with the choice of analogs, and so.forth,;which is necessary
in order to forecae't thip weather for 3 7 days. Abstracter's
note; Complete trahslation.-7
Card 4/4

S/169/62/000/007/110/149,:
D228/D307
AUTHORS: Vaoyukov, K. N.j Zverevt Ne Is an&Ped").D. A.
------------------
TITLE: Application of-empirical functions~'of influence ford
forecasting mean monthly air tempe:~ature anomalies
PERIODICAL: Referativnyy zhurnal Geofitika, no'. 7,1962, 48-49, -
abstract 7B258 (Tr. Tsentr. in-ta prognozov, no. 116,
1962, 24-33)
iEXT: Particular synchronous and a,synchronous:(.December-january,
June-July) factors of correlation between the Moscow air tempera-
ture and the temperature.(pressure) at a number.of points were de-
termined for January and July in order to investigate the intluen-
ce of centers of atmospheric action (CAA) on the formation of mean
monthly air temperature anomalies in the USSR's Eur .opean territory
and in order to derive possible prognostic relations (by prepar-
ing the equation of multiple regreasion).-These points Were,chosen
for the characteristic of the intensity of CAA. and~Were located.'aB
followd: Ponta Delgada (Azores)) Honolulu (Hawaiian Islands), Be-
Card 1/4

S/169/6~2/000/007/110/149
Application of empirical D228/D3,07
ruferdur (Iceland), Irkutsk, Tashkent, and Petropavlovsk na Kam-
chatka. The correlative connections between the~eleqonts under con-
i
sideration (all instances of air temperature and pre0sure anoma-
lies over 50 years were taken into account) are small. The highest
stability (for synchronous relations) is observed between thead-
vection of the Azores anticyclone and-the mean monthly temperature
anomaly at Moscow. The relations obtained appear more distinctly,
in ca5es of greater temperature oi~ pressure d-eviations at CAA, se~-
lected from all the 50-year data. Magnitudes are given for synchro-
nous and asynchrono'us-fela~tiond betWben'the mean monthly air'tem-
perature anomalies at Moscow and the CAA, and between the mean
monthly air temperature anomalies at Moscow and~the mean monthly
pressure anomalies at the CAA; values are citedF too, for the,syfl-
chronous relations of the mean monthly Moscow air-temperature ano-
malies to the pressure anomaly differences between the main CAA.~
allowance is made' for the state at two CAA,,the:asyfLchronous
relations between the mean monthly air temperature anomalies at
Moscow and the pressure at the CAA are somewhat better than if
--Just one CAA is taken into accounts Allowance is mad.e for the aim-
Card 2/4

Application ofempirical D2289/62/000/007/110/149
/D307
ultaneous influence of all CAA'by means of empirical functions of
influence. The problem is simplified'b finding the-asynchronous
relations (with a month's displacemenZ between the state of.some
CAA, expressed by fluctuations in the mean monthly.air temperature
anomaly at Ponta Delgada, Beruferdur, Honolulu, Irkutsk, and Tash-
kent, and the mean monthly air temperature anomaly on the,USSR's
European territory according to the data of 11 stations for 1900-
10.40 (Arkhangellsk, Leningrad, Syktyvkar, Rig'a Moscow Yelabuga,
0renburg, Zemetchino, Volgograd,*Rostov-on-Don: Odessa~. Allowance
for the influence of CAA on the temperature conditions of:the
USSR's European territory was made by dividing all the original da-
ta into warm (April -September) and cold (October-11arch) periods,
whose empirical functions of influence were,deter 'mined separately.
Coefficients of the empirical functions of influelice are cited
for each of the 11 points on the USSR's Buropeanterritory; they
were obtained on the grounds of the data's climat~ic processing.
The values of,the mean monthly air temperature anomaly (At) predic-
table for each point and month are calculated from the multiple
.+d + ,
---regress*ion equation t d 16t + 0( At + c~ *At I At X At
0 0. 1 1 2 2. 3 3 4 4
Card 3/4

5/169/62/000/007/110/149*
~~Application of empirical ... D226/D-
,507
Here c~ are the respective' coefficients of the em-
o (_X1 f 0(21 G(3, c-~4
pirl-cal functions of influence~for a given station on the USSR's
European territory and for the stations of each of the four.CAA':
the Azores and Honolulu highs, the'Iceland lo%.r / Abs.tracter's ...
note: It is assumed that Inelandskoy', should reid lislandsko~' 7,
the Siberian high for the cold season, and the~Mid-Asiatic low-for
the warm season. Atof Lt 16t are the respective mean
111~t2l AtP 4
monthly air temperature-anomalies at the same.~points for the pro-
ceding month. 18 out.of 22 of the forecasts f 'or the mean monthly
air tempera 'ture anomaly were proved to be correct. 23 references.
Abstracter's note: Complete translation.
Card 4/4

:''s/169/62/000/007/111/149
D228/J)507
AUTHOR: Zverev, N. I.
TITLE: Forecasting the baric height field's,evolutioh during
3 7 days
PERIODICAL: Referativnyy'-zhurnalp Geofizikaot no-:7, 1962p; 4 9 ~i ab-*
stract 7B259 (Tr. Tsentr. in-ta:prognozovt no, 11:6#
1962, 34-40
TF_XT: The author suggests a complex way of. forecasting th6l.evolu-
tion of the baria~ height field at the mean :troposphere level for
3 - 7 days. The method contains the clements.of theoretica 1and
synoptic-statistical trends, from which ways of numerically fore-
casting the baric field for ave'rage periods are being currently'
developed. In accordance with G. I. Morski 1,s theoretical model
(Tr. Tsentr. in-ta prognozov, no. 49, 19M themain equation is
recorded in the form:
Card 1/3

Porecastint, the baric
D228/D307
P
M H 6H 6H
+ +'(X +a AH +0( (HAH) FS (X, yl t).'
1 Tt_ 2 rx 3 4
where H is the value of the N-500 geopotential; AA6 the Laplacian
X11
sign; c,(, ,r42 F C'k3 P 0(4 are constants; and y, is, the arbi-
trary function, allowing the factors not Laken' into account in the
equation to be estimated statisticall Thie:;equation is linearized
relative to a certain function R(x, Y~," whicli may in a particular
case be considered as the field Of the N-5061values of a natural
synoptic period. The solution is made in the"~formof an analysis
With respect to Chebyshev's polynomials recorded in the form.of a
graded series, when H(x, y) is taken oniy in Ia firat approximation
,as a second degree polynomial. Certain coefficients confronting
different degrees of.X and y were determined.:Coefficients with
younger degrees of x and y include time in a higher degre.e,than
those with older degrees, This testifieErin,~part_~cular that the in-
fluence of the indices of zonal and meridional t~.anafer f;rows,as
Card 2/3
ism

S/16 62/000/007/111/149
Forecasting the baric D228YD307
tile interval from the original day increases, and that the influence
-of indices, characterizing the development of Bifialler-scale dis-
turbances, diminishes. The method allows the baric field's evolu"
tion throughout a natural synoptic period to be,calclulated ori.the
basis of average AT-500 charts for the period"s tendency, i.e it
enables.a natural synoptic period's peculiarities to'be taken into'.
account. /-Abatracter'.9 note., Complete translation*-7
Card 3/3

~S/i ~6q/62/000/~007/1~12/1 4~q-
8/169/62/000/007/112/149
M28/X'07
AUTHORS: Duytseva, Mc A. and
TITLE: Possibility of applying L. Kletterl,s method of fore-
casting.charts of the mean three-'day U-850 values
PERIODICAL: Referativnyy zhurnal, Geofizika):no.:7, 1962, 49,.ab-
stract 7B260 (Tr. Tsentr. in-ta,prognozov, no*-1160
1962, 65-66)
TEXT: The methods suggested by.L. Kletter (Praktische Erf.ahrungen
mit einer neuen Methode.zur Ausarbeitung mittelfristigerl'iette'r-
-prognosen, Arch. Ileteorol., Geophys. und Bioklialiatol. A,,1956, Bd.-
91 H 2), was verified in,conformity with the citculation conditions
over the USSR's European territory. L. Kletterls method is based-on
the use of the linear regression equationj~relating the mean three-
day N-850 values to the values at 18 hrs on the initial day. For
the USSR's European part the regression coefficients were deter-
mined by the method of least squares from"the daily AT-850 charts
-for Mosebwy Leningra.d, Kiev, and Sverdlovsk for January.and July,
'lard 1/2

S/169/62/000/007/1121/14.9
Possibility of applying D228/D307
1950-1952. Out of 27 forecasts 15 proved to be correct in the
-Aynamics of~
other 12 being incorrect. The:method does not give the
the development.of,pro.cesses.-.The reason for the"low'justifiable-
ness of the forecasts evidently consists.of the fact that no ad-
.equate allowance is made for the regression equationlB freo term.
Abstracter's notet Complete tranalation.-7
10ard 2/2
........................

VASYUKOVP K.A., kand. fiz.-matem. nauki ZVMEV.,_Njt,,,.kand. fiz.-matem
nauk; PEDI, D.A., kand. geograf;-nauk
Rhythms in the atmosphere and some methods of evaluating them..
Meteor. i gidrol. no.lt47-49 A 165. (MIRA 180)
1. TSentrallnyy institut prognozov.

L 10 406-67
ACC NRt
AT6033032
where (D is the scalar potential of the magnetic field; Ho 16~ the magnitude 'of the
:Longitudinal field; H is the amplitude of th p-th harmonlc~~of the helical fleld-
r, q) # zare coordinates. - Mere follows a ma(Zhematical development for the case Of a
holical field with n - 2. The article gives detailed mechanical drawings of:i evetal
of the main features of the equipment used, Including a-cross section viaw of7the-
apparatus, details of the helical winding, and a bIbck diagr4a of the feeding! system.,
A further figure shows an oscillogram of the current flowing'through the winding* Ihe
experimental data confirm the validity of the appiroaah to the probleme "In conclusion
the authors express their sincerG thanks to M. S. Rabing-vIch for h1s: continaing
interest in the work and for his helpful iis'e, ~80;~t'as ~W as U) rG4 P. AlekSM&OVI
V. 1. Dudin, V. I. Kryykavo and Ve P. Solov'm who took part in Uwaonstruation oif
the equipment,' and to G. L (b I kin& uho: took part In ths coAS'tmotJj*., *,f the
system*" Orige art. hast'~S formulas. 7 fiq%4vs, and 1~ table
SM CM38 '-20/ SUM DMs' none/ OkM~,RWs 014/`~ ='Dws'! 003
/241p
2

BATANOV, G.M.; BEPS7UTSKIY, M.S.; GREBE, NSHCHIKOV, SJe.;
POPRYADUKHIN, A.P.; RABINOVICH, M.S.; SBITNIKOVA, I.S.; SHPIGELI,,
I.S.
Magnetic surfaceB and the confinement of a.plasma by helical'fields
in a stellarator with external injection. DoU. AN SSSR 16o n&.6...'
1293-1295 F 165. (MIRA 18:2)
Submitted September 23, 1964.

S/08.1/61/0(iO/023/058/66i
B106/tloi
AUTHORS, Reznikovskiy, M.M.t verev, N-P., Denisolia, L.L.
TITLE: An improved chamber for laboratory test6,"Io~f tlje~ozonc
resistance of rubbers
PERIODICAL: Re'-~rativnyy zhurnal. Khimiya, no. 23,. 1961,*561, abstract
'P
2
3 354. (Tr. N.-i. in-ta shin. prom-util.eb. 7y' 1960t I
TEXT: An installation guaranteeing satisfactory accuracy and,reproducibility
of measurements even at nonuniform 0 distribution in the.werking chamber is
3
described. In order to exclude fluctuations in the 0 concentration, the
3
case containing the samples revolves at a rate of 2 rbm'.1 The contactless
transmission of torque from the Warren motor is attained by means of &,nlag7
netic clu$ch. CAbstracter's note: Complete translations
Card 1/1

AUTHOR: Zverev, B.S., Engineer SOV/133-58-.10-26/31
TITLE: On t-he-T-r-0b-1-em--"'of Production of Deep.~Dirawlng Sheets for
the Manufacture of Automobile Bodies~:(K voprosam proiz-
vodstva avtolista dlya glubokoy vjty4zhki)i
nRIODICAL: Stal 1958, rNr 10 $ p 9,48 (USSR)
ABSTRACT:* The paper contains critical remarks:dn the: previously
published paper'by G.D. Rogoza (Refs;J an!i 2) in which the
validity of Eriksen's test for deep drawi'Ag sheets wag
questioned. The present author considers that in,order to
supply quality sheets, the metal should be.extensively
tested on the producing works. T:iere are 3 Soviet.
references.
ASSOCIATION: Gorlkovskiy avtomobillnyy zavod (Gol".1cly Automobile,
Card 1/1

AUTHOR;
TITLE:
PERIODICALt
ABSTRAM
Card 1/2
Zverev, U.S.
Tests of Imported and Domestic Cold-Rolle-1 Plate for' Auto-
mobile Bodies (Ispytoniya impoitnogo1i 0t,30heJtvenn6_o A*vto-
kuzovnogo kholodnokatanogo lista)
Avtombillnaya promystilennoet', 1958,11ir 9, PP 38-40 (USSR)
The Gorlkiy Notor Vehicle Plant, an&also sevoral tber Sovi e t
automobile plants, satisfied part of its ,.requirement's for
cold-rolled plate for car productioinl!by ii6ports. Especially
the Gorlkiy plant obtained cold-rolled stoiel plate from;ithe
USA, England, West Germany and Francb. In order to compare
the chemical analysis, mechanical properties and prelssing
results of the imported steel plate and that produced by the
zavod "Zaporozhatall" (Zaporozhstal1jil Plant)'o tests of both
kinds were carried out. The test ra6ulta are preso,ntjcd.on
4 tables: The percentalge in the Plate of carbonp manganese
and sulphur (Table 1); yield point,~olongation, relation
between the yield point and the ultimate istrength at rupture,
hardness RB, extension by Erichsen c4ppinjr best in mm, grain
size in ball-marks, waste at punchinG (Table 2), the same
data for the angular body panels of the 111-lobedall car (Table 3)
and stamping results for other parts (Tab:.e 4). The author

SOV-113-58-9-15/19
Tests of Imported and Domestic Cold-Rolled Platelpr Automobile Bodies
evaluates these results and strongly.recommends their con-
sideration. in the e3tablishment of relevant GOST standard3
for the motor vehicle plants.
There are 4 tables and 3 Soviet references.,
ASSOCIATION: Gorlkovskiy avtozavod (The Gorlkiy Motor 'Vehicle Plant).
1. Automobile industry--USSR .2. Metal plati..,s--Effectiveness
Card 2/2

he It 11 Ifw it 46 it III it a it i, I
A I A-r_ A- 9 A I T T.: AA 0
to i.
Ar-Ot-

so

INTLITrNICE OF I REF FM11M. On IttItACT r-IRMIGTH. !-is
14qtft11pxrO14. 14. 1 5-102(193h) (in Russian) 1 1-01 AtItX'sat 16 .00
Allove 6, 508. L(
rif
v inomet strength absorved in pr"asvi.V, parto nM*
steel contz- c 0-31 --0.39, tin 0-33-0-46- Si 0-21-0-34 ~nd Cr 0, 1. 1 ZIA
a was due to the Drei ence of free forrlte either
'
'lowly V(w Ft-laininig it
in .41%.
C.. C..

-too
IVA
;so
so
LIt
4 44 1is 0
t w I I'a
0 0 0 0 0 0 a 0 a so 0 0 0, 0 0 0_4 0 0 0. 0~6
04 s. 0 0 0 OrS

(Kazakhstan--goonomic conditions)

v- R a I1 6 .
BUCHii&, Boris Aleksayevich; DOWOPYATOV, Yu.A., red. -, ZVEW. N.V.,
speteredaktor; NAGIM, P.A., tokha.red.
(Kazakhstan is a republic of large-scAle state,farm production]
Kazakhstan-reBpublika krupnogo sovkho2nogo proirvodotva. Alma-Ata,
Y,azakhakoe gos.isd-vo, 1956. 129 p. (MIRA 10: 12)
(Kazakhstan--State farms)
HEM,

Ni. MATSKEVICH, Oleg VasilOyovichl
ERE&
"7UKHODIKO, S. red.
(Kazakhstan, the country of eagle's wings]kazakbstan -
strana, orlinykh kryllyev. Alm-Atap"Kazaklistan", 1965.
172 p. (MUk M12)

MIKHAUZY, A.A., otv.red.; red.; mixoTswo ?.a,, red,';
KASVICH, A.G., X.R.o red,; BOBCW* V.V., red.;
SUBBOTIN, X.Y., redo; SAKSOMMKO, L.V.#.red.; TMUKINA, X.Ap,
takhn.red,
[Astronomy in the U.S.S.R. during forty yearo 1917-1957; collected
articles] Astronomiia v S$U sik vorok let, 1917-19,571 sbornik
statei. Rsd.koll6giis: A.A.gikhoiloy i ar. Moskvii, Oos.izd_Vo
fiziko-matem.lit-ry, 1960. 728 P.
(MIRA 13:7)
(Astronomy--History)

ZVEM N.I. kandidat tekhniches~lkh nmik
e- -6=alculation of the auction flue of baffle-type flyI-ash col-
lectors. Toploonergetiks. 2 no.5:44it9 MY '5,5. (KWA 81:9)
1. Vessoyusnyy teplotekhnicheskly institut
(Dust collectors)

R SV)
AID.P
Subject USSR/Electricity
Card 1/1 Pub. 110-a - 9/17
Author~ Zver~~~I., Kand. of Tech. Sci.,
Title Computing the outlet pipe of a screen-t,~pe ash ca'tch6r
.Periodical Teploenergetika, 5, 44-49, My:1
955
Abstract A mathematical analysis for designing a pareen-6 e,~ ash
Wi YP
catcher eqiiipped with an ejector:j.'s pr6sented th iables,
curves and equations. Five diagrams.
Institution All-Union Heat,Technology' Inatituie
Submitted No date

AUTHOR: Zverev N*I* Candidate of Technioal SciQnces*
TITIS: Modelling the motion of poly-dispex&~K/Rls-
(Modelirovani-i dvizheniya
li.)

polidisper6n
OY py

FSRIODICAL: No
"TeploeneMetikall (Thermal Power) 1957 Vol-41
-7,
.
:
pp. 35 - 38 (U-S-S.R.5
ABSTRACT: Ia a previous article Ithe author showed that thexe
are five criteria that characterisG the steady*otion
of dusty gas or liquid. Two of:these.'eriteriajina lude
the diameter of a dust particle., Conseqaently:th6se
criteria are only applicable to mono-disperse dusts
(that is dust consisting of particles of one size:on].yl
In practice we have to deal almost eiclusively"with
poly-disperse dusts, that is dus,ts,consisting of part-
icles of many sizes. At low dust boncentrations when
the motions of different fractions do,not inte.radt on
one another modelling may be effected by sub-dividing
the poly-disperse dust into,a number of narrow
fract-ions and using corresponding fractions in the
card 1/4 model. However, this pxocedure,As very laborious and
is quite inapplicable at high cLoncentrations, Neither
is it permissible to introduce some sort of means

Modelling the motion of poly-disp.erse d4sts. (Cont.)
96-7-7/25
diameter into the criteria since in order 'V-O choose
the diameter correctly it is necessary to know in
advance the function that it is required to find*
All this severly limits the possibilities of mode-
lling for the study of industrial equipment and* there-
fore, it is necessary to find additional conditions of
similarity of motion of poly-diroperse dusts. , ;,
The similarity of motion of tNo dust flows is then
considered. During the course of the examinevion.*the
dimensions of the dust particles.are .expressed,as,~a
ratio of a dimension which is characteristic for the
given dust so that the diameter of the particle is
expressed by a dimensionless number. It is then Shom
that in two systems with identical criteria consisting
of characteristic dimensions all the:dust particles
with identical dimensionless diameters have certain
criteria in common. As a result of the eyamination
additional criteria are in effect introduced'forl.poly-
Card 2/4 disperse dust.
In order to ensure cauplete similarity all five
main critoria should be the same for both model and

Modelling the motion of poly-dispe dusts. (Cont.)
.T;I-T-T/25
specimen. This is often difficult,i'and-sometimes imp-
ossible to achieve. It is therefore desirable to cut
down the number of criteria and the various waysAa
which this can be done are considered. It is shoun that
simplification is possible when the range of concen-
tration is from 0,05 to 0.1 kS/kgj'orAf t.4e force of
gravity is negligible compared with the inertia forces.
This latter point can be cleared up by using the test
equipment in different positions, for oxample, if its
performance does not change when it is. inverted, grav-
ity may be igaoredo- It is shown that when modelling
on the basis of three criteria the gaaspeed, dispem-
ness and density of dust in the model are fally defined
and cannot be selected arbitrarily, Therefore, this is
the most difficult case of modelling. When modelling
by two criteria two scales,are fixed and one is arbi-
trary. Still further simplifications,are sometimes
possible.
Card 3/4 When the necessary scales have:been found the nece-
ssary dust density is determined, then the best avail-
able material is chosen, and then if the density is

Modelling the motion of poly-disperse dusts. (Cont.)
96-7-.7/25
not qIlite of the value required the remaining scales
are altered somewhat. -The various:
I degrees of fineness
required in the model dust are calculated and the.
material is milled in a laboratory mill. Sieve anal-
yses are made during the course of 'milling until-most
of the dust is. of the required composition. If the
dust contains an excess of fines or coarse particles
these are removed by appropriate sieves. A quatity*of
100 - 200 grams of dust is usually necessary for tests
on laboratory models and the quantity of dust required
for a complete series of tests does not exceed 2
3 kg., In practice it is not difficult to produce such
a quantity of dust of a required composition and in
any case it is easier than preparing a larger quantity
of close fractions.
card 4/4 There are 4, figures and 2 references, 1 of which is
Slavic.
ASSOCIATION: All-Union Thermo-technical Institute (VTI)
AVAILABIL,

-7 /V
'
V.I. (zagineer) & Zverevo N.I. (Cand-Te
ch.sci.)
AUTHOR: igaat Yev, U I
TITLE: The flow of dusty gas round a cylinder (Obtekaniye tsilindra
zapylennym gazom.)
PERIODICAL: 1958
No.3.
Toploonergetika
pp. 30-40! (USSR)
,
,
.
ABSTRACT: There are muny processes in which dusty gas flows
round a c:ylinder.
,
Of the total number of particulea that pass through a cros4-sectional
area equal to that of the cylindor, but a considerable dist
ancd
in
.
,
advance of it, only a proportion roach tho surfaca of the.oylinder
and the remainder pass by. The ratio of those that touch the -
cylinder to the total number -jas determined in this work for various
conditions and the distribution of the dust oven the surface of the
cylinder was studied. The experimental device consiated of a vertical,
channel of 500 x 50 ima section. The tes-Voyliudor was located'at
the centre of the section, parallol to thl short side, at~a distance
of 45 hydraulic diameters from the inlet., Flow was always turbulent
at the position of the cylinder. Arrangements were made to ensure
that the conditions of air flow over the cylinder approximated~to
those in a boundless flow. The other experimental conditions are
described. The tests were carried out with friketions of milled
anthracite and metal dust (an alloy of chremi= and iron) with'
specific gravities of 1.055 find 7.3 -ram/cm'- respectively.. ,The
fractions were prepared in air separators, Tile procedureof
Card 1/4 preparation is described. The characteriatico.of the fractions in

The f low of dusty gas round a cylinder. 0/2
respect of the velocity at which they fly i1pich-7W specdf Md
hydraulic diameter (the diameter of a Bphero with~ isame density und
pick-up speed) are tabulated. Dust for the''Aasts was poured'into a
tube and blown into the collector by a strong yet of air from a needle
valve. It was shown by special tests that with Qis method of .
delivery the suspension broke up into individual~_Just particles,;
uniformly distributed over the working section. In order to determine
the proportion of (lust trapped on the cylinder ULO cylinder, iras
wrapped round with it ring of cinefilm, 10 mti~~ivide smeared with
petrolatum, wtUch trapped all. the dust particles .+,hat touched it.
The film was then compared with a transparent scale under a
microscope. Various experimental procedures were used ;md are
described. Hine series of tests were made with dowmward flow,
anthracite dust being used in Nos.1 - 7, and metal dust in Nos. 8 & 0.
Speeds of around 2, 4, 12 & 16 m1sec were used with cylinderu of
12, 25 & 50 mm. diameter. In each series ofAests the finest fraations
were used first followed by the coarser. The tes-ts were mado at rocm
temperature and pressure. 11ohen Reynolds number for the particles is
less than 0.1 the resistance to the medium acting' on the particles is
given by the Stokes' formula, and the St criterion defines the motion.
Card Mien Reynolds number for the particles is greater than 0.1 Stokes'
9//A formula is inapplicable and motion is not uniquely governed by the

The flow of dusty gas round a cylinder. 96-3-10/26
St criterion. 1-kevious authors have given the proportion trappeil as
tj
a unique fraction of St,asually there was,,a considerable scatter
of points and considerable difference between the general
relationships obtained by dilteront authors. This~ was probably
because in the experiments, Reynolds number was riot low anaugh and
instead of a unique relationship between the proportion of
particles trapped and St there should have been a family of curves.
The authors' test results are given in Pig.l. 11.ie accuracy of the
determinations is such that a family of curves can be plotted. Tlien
-the particles move in a vertical flow their relative velocity at
a distance from the cylind6r is practically equai to the speed of
pick-up, but the velocity increases near the cylinder. Iuthe I I
majority of tests the Reynolds number was 9'reator than 0.1 even.in
the part remote from the cylinder. Therefore, in inast of the tests
-the resistance factor according to Stokes' law was not deterTiinod.
Then particles move in a vertical flow their trajoctory and:thc~
proportion trapped may also depend on gravitatioilal force. To check
this point, trio additional series of tests~were made with anthracite
dust and rising air flow at speeds of 2 and NAM/secend. Jn ihese
tests the axial components of inertia iuid gravity forces wore opposed
sE, that if gravitation was important the proportion trapped,should
bo less than in the first series of tests. The ~results of -the tests
Card 3/4 given in Fig.2. confirm that this was so. This applies even to the

The flow of dusty gas round a cylinder. 00-3-10/26
finest of particles for which the air speed was'far above the
pick-up speed. Dimensionlesia curves of tile distribution o4 trapped
dust over the cylinder surface are of quite a different character
with upward and downward flow as will be~ seen from Fia.3,
t4
Therefore, gravity has a marked effect on the process. An
additional criterion D is introduced that, together with the
criterion St, determines the probability of particles hitting the
cylinder with a downward flow of air. Fir
,.6. gives curves of the.
distribution of trapped dust on the surface ot the cylinder with a
downward flow of air. There are 7 figures, I table and 10 literature
references (6 Russian and 4 Eliglish)
ASSOCIATION: All-Union MerMo-Teebtlical Institute. (VE30SOVUZnvv Teplo-
AvAnaLu: Li .brary of Congress. tekhnicheskiy Institut).
C or d 4/4

61
ACCESS IOIN NR. AT404 0568 S/2546/64/1000/135/0063iDo9,Q,v.
AUTHOR: Z Werev, N
TITLE: Waves I n the atmosphere w
SOURCE: Moscow. Tsentrallnrky institut prognozov. Trudrv, no. 135, 1964..
Sinopti,.ostatisticheskiye metodyfr prognozov pogody* (Synoptlc~statistical'methods
of weather f e
or casting), 63-90
TOPIC TAGS: meteorol f re culation, atmos-
ogy, weather o casting, atmospheric cir*
pheric wave, periodogram
ABSTRACT: On the basis of a review of the extensive' b1b,liography, the authors
analyzes the literature dealing with waveprocesses in the atmosphere and, des,'cribes
the statistical methods of perlodogram analysis used by :Various authors1dr de-
.,,.tecting large-scaie waves. It.is.s-hown that the statistically detect'ed V;aves'can
be used for forecasting atmospheric circulation for as much as a month In advance.
Particular attention Is given to an analysf~s of pressure and temperature waves
with periods of 5 to 7 days, discovered by a great many investigators. Considera-.
tion is given to the methods used by various authors who have. found wavei with
periods of,12, 17, 25,-11, 13 and 22 days and many'others. in each case: the.';.
-author hds attempted to determine whether these waves are real or a mathematical
Card 1/2

ACCESSION NR: AT4040568
fiction, how stable they are If real, and whether they can be extrapolated for a
Ilong period. it k concluded..that wave processes with periods~of 5-6, 8 and 13-
14 days are stochasv:cally real. Contrary.to certain other investigators, the
t author believes that this fact can be.used~for practical"purposo*s and,that the
methodology used in earlier attempts was faulty. Three signif,icant forny'llas are
a
presented which can be used for judging the presence of wave p,rotesses in the at-!
mosphere, the most important being a spectral function of the entire process,:
it Examples are cited showing how wave processes in cyclonic and 41nticy~lonic acti-,
vity at the mean levet of the troposphere can be detected, The only period do-
tected simultaneously in both the meridional and zonal air flow components is!
T = 14 days. It Is shown, however, that there is no rlgorous,periodicity:in the
atmosphere; the periods of 5, 8 and 14 days are approximat Ions. Recommenoot I ons,-
are made for prediction of circulation at the mean level of the:troposphere, a)-
though only for August,'September and October. only tho5e wavcs which devielop in
quasi-stationary pressure systems are of practical value, for the forecaster.
Orig. art. has: 93 formulas and 6 tables.
ASSOCIATION; Tsentrallny*y ins'titut prognozov (central Institute of Forecasts)
SUBMITTED: 00 oAT EACQ: o2ju164 ENCL: 00
car~f 2/2 SUB CODE: 'ES NO REF SOV: 036 :OTHER: 020
77

JA llj~
L__1428q~.66 m
:EWT( IJP,4
AGG NR: AT6066666 souRcF, Gobr,-. u4/m
, , ~ Ki~i)!
AUTHORSi imov. L. 1(.,, (Kiev); KPJR_0D_cjwywl_&J
(Kiev);
T
__Ellsldn.
Zverev, 114
Taev); Lazareva. N. H. -ev)
Ki
ORG.- none
-Investigation ot the_effec'ts' of.,soveral: a~toi
TITLE,4
tant Alo- 'used-lor' t6r~ifi~
sties of heat resis -,blad'
SOURCE: _Vs
Ad V_
A
ir irua
--n.- v;; 5n- -noy
(J
or-
h th 1_kAUipw_oh~ra6t
t1jr:

L ohq~o_67 K~?J-r( 1) ow
-ACC ~NRt AT6_ ~28~,O -~o-il~ci-zd~iF-~-R-i2546/66/000/1531007910089
AUTHOR: 7-verev, N. I*
ORG: none
TITLE-. Long-range of the intensity of zontill:circ uAation of;the atmos-_
phere
SOURCE. 'Moscow. Tsentrallnyy institut pr2Z=~~y. Trudy~ no. 153, 1966..~
Statis;icheskiye metody dolgosrochnoso prosnoza pogody (Stnti6tical methods of long-
.,range weather forecasting), 79-89
JOPIC TAGS: long ranaa weatper forecasting, atmospheric current, linear:operator,
linear equation
.4,DSTRACT: The author examines the possibility of a long-range forecasting of the
tensity of zonal circulation on the basis of the theo'ry of~linear extrapolation,
ationary sequence, and stationary processes. A linear formula is derived for fare-
casting the jrit.e.nsity of zonal circulation which, the author asserts, ii the: best
extrapolation formula, since for Gaussian processes the linear operator 'is the beat
operator of forecasting. From the investigation it is concluded that long-range
forecasting of the intensity of zonal circulation and iarge-scale cLrculation in
general can be successful only with consideration of the effect of history on the
future development of synoptic processes or even of individual characteristics during
the development of macroprocesses. The use of altitud6-variation charts and the
Card 112

GW'
ACC IRR AT6028447 SOURCE CODEj UR/2546/66/000 X064/066&i~
7
AUTHOR: Zverev N,
L; Kashleva,
OR4: nont
TITLE: Statistical method of forecasting the.zonal in6x
SOURCE: 10scow. Tsentral'nyy instit6t PT ,Trudi, no. 153, 1966.
1&110 _Zuy,
StatisticheskiYe metody dolgoorochnogo prognoza pogodyi.i(Statistical methods Pf long-".
range weather forecasting), 64-68 i
TO IC TAG statistic analysis, long range weather forecasting, atmospheric curre
T.
p -ore
ABST~RRA ~T.The urpose of this investigation was to elicit the possibility of f
casting the mean monthly value of the zonal index statistically. In t7oiking out this
6ethod, the authors proceeded from the assumption that'by taking into account the.
past history of zonal circulation itlis"posuible to precalculate the value of the
zonal index in the future by extrap,3iation. Having found that purely zonaLcircula-
tion in its evolution undergoes variati6ns.with periods of 9 and 23 ntonths,tthe
authors set up multiple regrission equations for forecasting the zonal,index for a:
month with a zero and monthly length:lof time before the forecast phenomenon occurred,
The values of the zonal index for past months were calculated as the starting data.
The regression equations af or flacreening" the predictors had the form:
A5, ) = 011MI-4+ +91141"~+ d4;
Card 1/2 + PlAk-21, + PAY44), + (2)

ACC NRs AT6028447
Here AI(n + m) are,the forecast values of the devLation of the index from the monthI5
norm; n is the initial number; Ion of'~ the value of the zonal,
A I (n - k) is the deviat
index (n - k) of the month from the norm of the same th;
morl cli, 0i are empirical
influence functions-("weights"). These equations werelderived separately~ for'. the cold ~41,
and warm halves of the year, which in turn were divided J11to two halves. ~ Equation
(1) gives the forecast of the deviations of the mean monthly values of the index
from the norm in the.imonth fd1lowing'the initial month, and calculation by Eq~o (2)
gives the forecast for the next month, or the forecast'of the~zonal index'vith a
30-day length of time beforeithe forecasting of the phen'olmenon occurs, An anslysis
'of the data showed that the proposed method of extrapolation makes it possible to pre-
calculate the intensity of zonal circulation at the mesa level of the troposphere
a satisfactory guarantee. Thus; precalculation of the index can be'tieed when.-;..
Utica
compiling monthly forecasts by.theore I methods. Orig, art,. has: 5 f rmulas,,uidd~,
1 table and 2 figures.
SUB-CODE: 04/ SUBM DATE:Fnone/ ORIG REF: 007
7.
kh
d 2/2
Car

BAGROIIJI N-A,; VL-YIJXO',r, K.A.; "UVEREW, 14.1.
FIT
Principle of aralop7 and Its use ir pn-etteallvork.. Trudy TSIP.
no.132'.41..,47 164. (MIRA 17~!C),

IGIMTIYEV, V.I., insh.; ZYMNY, N.I., kandotekhn.nauk
laboratory air separator with a boiling layer. Toploanergetika
7 no.2:55-58 P 160. (MIRL 13:3)
lo Vseuoyut.nyy teplotekhnicheskiy, institut,
(Separators (Machines))

The Storm ~Ifind of 14 November 1952 in the South of' the Eurdnean TerritIo ry
of the USSR. Meteorol. i gidrologiya, No 6, 1953, pp 3-71
In the southeastern European part of the USSR from 91D 11,~Nbvember
1952 wind strengths up to 28-34. meters/second were observed. The author
discussed the variation of the wind regime during this period. ,For each
day be constructs tbe charts of wind velocity.for the ground level and
for the altitude 300, 600, and 900 meters above the level of tb6 ground.
The storm arose as the result of intense dropping pressure.in thelower
kilometer layer, which transferred the momentum from ton to bottom with
the simultaneous advection of cold masses from the northeast. 02,Geol,
No 5, 1954)

ZVXM,N.I., kandidat fisiko-vatematicheskikh nauk
ij
Meteorological works of.the Russian geophysicist 1. Smirnov.
Meteor.i g1drol. no.5:56-57 W '53. (Nm 8:9)
1. Wentrallnyy Institut profsoyusav, Moskva.
(Smirnov, Ivan Nikolaevich)

Z- VeR
Subject
Card 1/1
Author
Title
Periodical
Abstract
r, 1.
AID P - 180
USSR/Meteorology and Hydrology
Pub. 71-a 7/26
Zverev, N..I,-
on temperature forecasting
Met. i gidro.,, no.2,, 28-29, 1955
The article is an attempt to est~$JiA.with equdtio'ns
and charts the able played by turbulence in the,woving
of warm air.1~7C.*i...table and 2 charts are given.

SOVI 1,24-5~;54563
Translation from: Referativnyy zhurna.l, Mekhanika, 1958, Nr 5, p 91 (USSR)
AUTHOR: Zverev, N. I.
TITLE: On the Influence of the Temperature Field of. the Continent a~nd
the Ocean during the Warm Season Upon the.Atmospheri'c Ci'rcula-
tion in the Far East (0 vliyani, 'Lemper'aturnogo polya kontinienta
i okeana v teploye vremya goda na atm,osferriuyu tsirkulyatsiyu v
usloviyakh Dal' nego Vostoka)
PERIODICAL: Tr. Tsentr. in-ta prognozov, 1957, Nr 49, pp 250-263
ABSTRACT: Bibliographic entry
1. Atmosphere--Motion 2. Oceans--Th6rmal effects
3. Eartb--Thermal effects 4. Glimatic factors--Asia
Card 1/1

Problems in Long-range Forecastin4 Leninoad 361
rjidrozWIteojzdat, 1957.
Zverev. N.I. Influence of Ocean and Land Temperazure-67n-
.-A-Fmospheric Circulation During the Warm Season iri the Far
E~st 250
The author analyzes the influence of thermal.,inonuniformity
of,the surface layer on the atmospheric circulati6n and
,discusses some implications from'observation'results pertinent
to weather forecasting. The author defines nonuniformity as
the phenomenon of the accmulation 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 question of period-
laity, 1. 0 the-exiBtence of definite natural temperature
interval;
from 6 to 12 days), and the c6nneetion of ouch
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
Researc4,Institute of Hydrometeorology (DV IfIGMI),The'Inatitute
Card 8/10

problems in Long-range Forecasting 361
compiled daily temperature maps for sea and imid in:1934-38.
In addition, the author availed himself of the idaterAal
collected in the archives of the Central.Institute of Fore-
casts (TSIP). There are i2 maps, 6 tables, and 8 S oviet
references.
Byalynitskaya, V.G., and Ped', D.A. Formation of Night Frosts~
in Mraine 264
The authors place night frosts in Ukraine into the;category
of those that are'dangerous, i.e., capable of ':damaging cropd.
This type of frosts is common both in autumn and in spring..:~
but the authors analyze only the occurenbe of,frosts in May.
Crimea is included in this study. Tabular material includes
statistics of occurrence and duration of frosts. The article
analyzes the thermobaric field during the occurrence of frosts
and. compares it with the field when'frost is 'absent. Pertinent:
Card 9110

Problems in Long-range Forecasting 361
indices are deduced and data given on how to forecast the
onset of frosts one to two days in advance. There,:are 13
tables in the text and 2 in the appendix,, 8 ma s, 2drawings
P
and 16 references, of which 14 are Soviet and 2 are' English.
AVAILABLE: Library of Congress HM /kav
8-12-58
Card 10/10
7; TI 4!4
I I'l Iq aIFlril V~11

ZVEREV-9 N.
FRI
DO
Iq
-7: 1:- F, 11!T; ji-~,:Tjpj 111jr
1.1 W fit !,?t itll~ 11:1111, f. 9151A i!jl 11

-----------
.............
all
pul Wif 11

3(7) SO'[/50-59-5-20/22
AUTHOR: Zverev, N. 1.
TITLE; Final Meeting of the Scientific CoUncil:of the Contral.1natituto
of Prognosis (Itogovaya sessiya Uchenogo sovata Teentrallnogo
instituta prognozov)
PERIODICAL: Meteorologiya i gidrologiya, 1959, Nr 5; pp 61 62 (USSR);
ABSTRACT: On January 12-20, 1959' a meeting of the Scientific Council took
place at the Tsentrallayy institut prognozov (central'Inatitate
of Prognosis). It was dedicated to the:finafresults in the ful-
filment of the plan for scientific research: work- 3 reports were
delivered in the Agrometeorological Seciion,of the Scientific
Council. L. A. Razumova and S. B. Mastinskaya put forward,the
results of the three-year experimental,work at which'the formation
of ground humidity'reserves an& the correlation between the state
of the ',~summer wheat and corn and the~yiatorlsupply in the newly
won land (the steppe areas of the Kulunda Steppe and of northern
Kazakhstan) were investigated. S. B. MastiAshays., N.I* h. Meshcha-
ninova, Yu. S. Mellnik, ff. A. Baybayeva et al participated
Card 114 directly in the working out of this subject. Co-workers of the

Final Meeting of the Scientific Council of the Central 8OV/56-59-5.:20/22
institute of Prognosis
following organizations took part in the investigations:
Kazakhskiy nauchno-issledovateliskiy gidrometoorologicheskiy
institut (Kazakh Hydrometeorological Scientific Rsaearch In-
stitute), Novosibirskiy biologiolieskiy.inatitut (Novosibirsk
'Biological Institute), Kazakhskiy institut im. Villyamf3a (Kazakh
Institute imeni Viltyams), Kazakhekiy institut zernovogo khoz-
yaystva (Kazakh Institute of:Grain Econo ), as well,' as::the
MY
co-workers of the agrometeorological titations. B. P.Iono~larev
spoke on the evaluation of agrometeorological conditions for the
grow th )f surnmer wheat in tile area,2of the RSr-SR- 7;repprts
were delivered in the Hydrological Section of tile scientific
Council. The most important results mere obtained by~ V. D.
Komarov, A. 11. Vazhnov, and A. I. Karakasho V. N. Par4hin and
Ye. G. Popov worked out a new method for bhe evaluation of
hydrological forecasts. A. I. Afanaa2yev presented conclusions
on the features of the decay of the snow cover on the bas*is
of an interpretation of aerial photographs during thd melting
of snow. 7 reports were delivered in the Meteorological Section.
Card 2/4 F. I. Monakhov put forward the result-s,of experimental inveatiga-

"~o to, 6
4'o TO-90'- - -,I I I
ol~
10,fles -fit the j:or
I of
1 al V'-
"~s ,ISO ~e0l)~o
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.7~_~VF_RFW, M,1'
3(7) PHASE I LOOK EXPLOITATION SOV/,)249
Moscow. Tsentrallnyy InstiLut prognozov
Voprosy do, go erochnykh prognozov pogody (Problems In Long-Rnnge Weather Fore-
castina) MOBQOWI Gldrometeolzdat (otd.), 1959. 62 p. (Seriest lint
Trudy, vyp. 85) Errata slip Inserted. 900 copies printed.
Sponsoring Agency: USSR, Sovet ministrov. Glavnoye upravlonlye g1dro-
meteorologichaskoy sluzhby.
Ed. (Title pape): G. I. Morskly; Ed. (Inside book); L. V. BlInDikov;:Tech.
Ed.: T. Ye. Zemtsova,
PURPOSE: This issue of the Institute's Transactions~is intended for scientific
research and field workers in meteorology as well as for advanced students in
schools of higher education.
COVERAGE: This is a collection of three articles in oynoptic and Ceneral meteorology
Two of the articles deal with problems concerning the general circulation of the
atmosphere while the third discusses the matter of forecasting mean 7-day pres-
sure maps. Referencesaccompan-,r each article.
Card 113

=map
Problems in Long-Range (Cont.) SOII/324-9'
TABLE.07 CONTENTS:
Rayev, 1. K. On the Theory or the.Ge6eral Cir,culatioln ofithe Atmosphire
The author attempts aitheoretical description of.the general circulation In
the most general statement ofthe problem, This,entailso first of,'aallp the
consideration of nonlinear and viscoalty membersi'tin difforentlal !3quations,
and also the consideration at the nonadiabatic'ef'f'ect a yhich. play ;L bapic
role in the general circulation of,the,atmosphere,. This,work dIfFPr6,-. from
others on the problem . insofar L as the author pays , atria ter attention to ~ the
dependence of the thermal properties of the underlying surface onieographic
coo~.dinates. Computations are introduced to show that tem7jerature,ln time
and"space as well as all elements of motion may be determined when~thep'initlial
distribution of meteorological elementa and the heat influx from the S~n,as
a function of tIme,are known. There are 4 referencest 3 Soviet and 1~English, 3
Zverev, N. I. Forecasting a Mean AT 500 Seven-day,Chart
___Ti_nce most extended forecasts do,not deal with weather conditions to be ex-
pected in the week immediately following the date'of chart compilation the
author presents a statistical method of compiling mean 7-day chaAs. 'The
author works on the basic premise that the development or synoptielprocesses
in the future Is completely determined by the history of synoptic processes
over a given roglon. Thore are 7 raferences: 4 Ooviet find 3 English. 27
Card 2/3.
fj :~ 7 7:~T 1. TIfi:I FI !i VT
.111, !ZT,42 "'1., 111 11 11 1111 U-1r.1.11 HIM. Mill ill 9 1. 1 1

'3/10/62/900/007/i09/149
D228/D307
AUTHORS: Vasyukov, K. N.,, 4verev
N. I. and Ped', D. A.
TITLE: Using the:principle*of analogoul'ness~when for6ca6ting
synoptic prccesses and the weather for five dd a
PERIODICAL: Refera"--'vnyy, zhurnal, Geofizikat- no,,7, 191629,1 48 9ab__'
stract*7B257':(Tr. Tsentr. in-ta;'Tprogrk6zov, no.,:116,
1962,. 13-23)
TEXT: The N-500 values for a.standard grid'of points, located ev-
ery 40 of latitude and 120:of longitudo on tho territory ounded
by 360W, 840E, 760N, and 360Wt were taken from tbe'averageTmaps
for natural synoptic processes (NSP) in Janu~ry and Februgtr~y,::1938-
1955. After this the.eigns-of the,geopotenti~l differences, re'.spec-
tively characterizing the zonal and the meridional.flow co'Mpon ents
were determined for meridionally and latitudinally neighboring V/
points. Th 'e values +1, 0, and -1 were reepectivelY ascribed to
positive, zero and negative differences. The resulting magnitudes
--of the rAeridional and the zonal wind~components for all NSP were
Card 1/ 4
7i

8/169/62/000/007/109:/49
Using the principle ... D228/D307
printed on tape, The analogs of the N-500 averages for the para'-
meters P,,and , characterizing the similarity offields withre-
PA.
spect-to their--ciroula-tional.--features-, were selected for the first
20 maps by means of the electronic computer "Pagoda". The valu6ifj of
P(P (111d P,~.waro ouloulatud from tho f ormulad t
n n
nA -
+
n + n P/L n + n
+
k+
where no+, n. n n is the number of cases when the signs of
the meridional (n and the zonal (nA) flo on
w camp ents in two-com-
1P
parable N-500 fields of NSP do, or do not, coincide. The comparison
of all NSP with the-briginal 20 allowed the distribution of,the de-
gree of analogy for the fields of2the 500-mbAurfaPe's January,geo-
-potential to be obtained from-the parameters of a 'and a It aloo
Card 2/4

S/169/62/000/007/109/149 .
Using the principle D228/D307
allowed the natural frequency of analogous processes to be;ex osed
p
separately according to the development of the meridional and.the
zonal air-flow components. Utilizing the criterion p all processes
can be dividod according to their,dogroe of finalo~gy t 0throd ca-
tOgOriOG: '010 atlftlog > 0-4), the non-analog -0.3, 40-4),
and the reverse analog (p A-0-3)-.Utilizing ~the criterion-p too,
we will obtain the analog P ,';~0.8, the non-analoglp,, = 0.2-.+ 0.6,
cihd the reverse analog /4 0'2. The criteria.~are,established with
a 10% guaranty. In practical work, when classifying all processes
into three categories, the degree of guaranty sho.~-'ld be established
jointly according toboth criteria for the analog p,>,,0.4,and PA.`~_
0.6, the.non-analog -.0.3 4prp 1, 0.4 and 0.2-~ p/t /_ 0.6, and the re-
verse analog -p f,0.3 and p ~.O.2. Average estima'-tes are given for
ogousneL
the anal of subsequent pairs of NSP'in relation to the de-
of'analogy of.the original pairs of NSP~with'respect:to P(P
Card.3/4

-- - ---------- S/16'9/62/000/007/lb9/149
Using the principle.... D228/D30il
and
+ As the geometric likeness increases, the', analo
PA
-ousnese iii the development of atmospheric processes in subf3equeni,
NSP grows generally,.But in a number- of examples it is shown, too,
that the factor ok geometric analogy, though it.ie of great~signi-
ficance in estabi'lishing the analogousnooo Of~ ~,LtMOE.PherjO PI'0000-
son, does not always givo pracLically valuabI6 pointers -to the fu-
ture development of processes. In some cases originally similar
processes subsequently change int6 non-analoSs. Using modern com-
puters it is possible by means of the analogy.!parameters of p
rp
and + o -to take into account objoctiVely the develop-
PA P P
ment history op atmospheric processesi to solve pr'oblems cor-nec-
ted with the choice of analogs, and so.forth,;which is necessary
in order to forecae't thip weather for 3 7 days. Abstracter's
note; Complete trahslation.-7
Card 4/4

S/169/62/000/007/110/149,:
D228/D307
AUTHORS: Vaoyukov, K. N.j Zverevt Ne Is an&Ped").D. A.
------------------
TITLE: Application of-empirical functions~'of influence ford
forecasting mean monthly air tempe:~ature anomalies
PERIODICAL: Referativnyy zhurnal Geofitika, no'. 7,1962, 48-49, -
abstract 7B258 (Tr. Tsentr. in-ta prognozov, no. 116,
1962, 24-33)
iEXT: Particular synchronous and a,synchronous:(.December-january,
June-July) factors of correlation between the Moscow air tempera-
ture and the temperature.(pressure) at a number.of points were de-
termined for January and July in order to investigate the intluen-
ce of centers of atmospheric action (CAA) on the formation of mean
monthly air temperature anomalies in the USSR's Eur .opean territory
and in order to derive possible prognostic relations (by prepar-
ing the equation of multiple regreasion).-These points Were,chosen
for the characteristic of the intensity of CAA. and~Were located.'aB
followd: Ponta Delgada (Azores)) Honolulu (Hawaiian Islands), Be-
Card 1/4

S/169/6~2/000/007/110/149
Application of empirical D228/D3,07
ruferdur (Iceland), Irkutsk, Tashkent, and Petropavlovsk na Kam-
chatka. The correlative connections between the~eleqonts under con-
i
sideration (all instances of air temperature and pre0sure anoma-
lies over 50 years were taken into account) are small. The highest
stability (for synchronous relations) is observed between thead-
vection of the Azores anticyclone and-the mean monthly temperature
anomaly at Moscow. The relations obtained appear more distinctly,
in ca5es of greater temperature oi~ pressure d-eviations at CAA, se~-
lected from all the 50-year data. Magnitudes are given for synchro-
nous and asynchrono'us-fela~tiond betWben'the mean monthly air'tem-
perature anomalies at Moscow and the CAA, and between the mean
monthly air temperature anomalies at Moscow and~the mean monthly
pressure anomalies at the CAA; values are citedF too, for the,syfl-
chronous relations of the mean monthly Moscow air-temperature ano-
malies to the pressure anomaly differences between the main CAA.~
allowance is made' for the state at two CAA,,the:asyfLchronous
relations between the mean monthly air temperature anomalies at
Moscow and the pressure at the CAA are somewhat better than if
--Just one CAA is taken into accounts Allowance is mad.e for the aim-
Card 2/4

Application ofempirical D2289/62/000/007/110/149
/D307
ultaneous influence of all CAA'by means of empirical functions of
influence. The problem is simplified'b finding the-asynchronous
relations (with a month's displacemenZ between the state of.some
CAA, expressed by fluctuations in the mean monthly.air temperature
anomaly at Ponta Delgada, Beruferdur, Honolulu, Irkutsk, and Tash-
kent, and the mean monthly air temperature anomaly on the,USSR's
European territory according to the data of 11 stations for 1900-
10.40 (Arkhangellsk, Leningrad, Syktyvkar, Rig'a Moscow Yelabuga,
0renburg, Zemetchino, Volgograd,*Rostov-on-Don: Odessa~. Allowance
for the influence of CAA on the temperature conditions of:the
USSR's European territory was made by dividing all the original da-
ta into warm (April -September) and cold (October-11arch) periods,
whose empirical functions of influence were,deter 'mined separately.
Coefficients of the empirical functions of influelice are cited
for each of the 11 points on the USSR's Buropeanterritory; they
were obtained on the grounds of the data's climat~ic processing.
The values of,the mean monthly air temperature anomaly (At) predic-
table for each point and month are calculated from the multiple
.+d + ,
---regress*ion equation t d 16t + 0( At + c~ *At I At X At
0 0. 1 1 2 2. 3 3 4 4
Card 3/4

5/169/62/000/007/110/149*
~~Application of empirical ... D226/D-
,507
Here c~ are the respective' coefficients of the em-
o (_X1 f 0(21 G(3, c-~4
pirl-cal functions of influence~for a given station on the USSR's
European territory and for the stations of each of the four.CAA':
the Azores and Honolulu highs, the'Iceland lo%.r / Abs.tracter's ...
note: It is assumed that Inelandskoy', should reid lislandsko~' 7,
the Siberian high for the cold season, and the~Mid-Asiatic low-for
the warm season. Atof Lt 16t are the respective mean
111~t2l AtP 4
monthly air temperature-anomalies at the same.~points for the pro-
ceding month. 18 out.of 22 of the forecasts f 'or the mean monthly
air tempera 'ture anomaly were proved to be correct. 23 references.
Abstracter's note: Complete translation.
Card 4/4

:''s/169/62/000/007/111/149
D228/J)507
AUTHOR: Zverev, N. I.
TITLE: Forecasting the baric height field's,evolutioh during
3 7 days
PERIODICAL: Referativnyy'-zhurnalp Geofizikaot no-:7, 1962p; 4 9 ~i ab-*
stract 7B259 (Tr. Tsentr. in-ta:prognozovt no, 11:6#
1962, 34-40
TF_XT: The author suggests a complex way of. forecasting th6l.evolu-
tion of the baria~ height field at the mean :troposphere level for
3 - 7 days. The method contains the clements.of theoretica 1and
synoptic-statistical trends, from which ways of numerically fore-
casting the baric field for ave'rage periods are being currently'
developed. In accordance with G. I. Morski 1,s theoretical model
(Tr. Tsentr. in-ta prognozov, no. 49, 19M themain equation is
recorded in the form:
Card 1/3

Porecastint, the baric
D228/D307
P
M H 6H 6H
+ +'(X +a AH +0( (HAH) FS (X, yl t).'
1 Tt_ 2 rx 3 4
where H is the value of the N-500 geopotential; AA6 the Laplacian
X11
sign; c,(, ,r42 F C'k3 P 0(4 are constants; and y, is, the arbi-
trary function, allowing the factors not Laken' into account in the
equation to be estimated statisticall Thie:;equation is linearized
relative to a certain function R(x, Y~," whicli may in a particular
case be considered as the field Of the N-5061values of a natural
synoptic period. The solution is made in the"~formof an analysis
With respect to Chebyshev's polynomials recorded in the form.of a
graded series, when H(x, y) is taken oniy in Ia firat approximation
,as a second degree polynomial. Certain coefficients confronting
different degrees of.X and y were determined.:Coefficients with
younger degrees of x and y include time in a higher degre.e,than
those with older degrees, This testifieErin,~part_~cular that the in-
fluence of the indices of zonal and meridional t~.anafer f;rows,as
Card 2/3
ism

S/16 62/000/007/111/149
Forecasting the baric D228YD307
tile interval from the original day increases, and that the influence
-of indices, characterizing the development of Bifialler-scale dis-
turbances, diminishes. The method allows the baric field's evolu"
tion throughout a natural synoptic period to be,calclulated ori.the
basis of average AT-500 charts for the period"s tendency, i.e it
enables.a natural synoptic period's peculiarities to'be taken into'.
account. /-Abatracter'.9 note., Complete translation*-7
Card 3/3

~S/i ~6q/62/000/~007/1~12/1 4~q-
8/169/62/000/007/112/149
M28/X'07
AUTHORS: Duytseva, Mc A. and
TITLE: Possibility of applying L. Kletterl,s method of fore-
casting.charts of the mean three-'day U-850 values
PERIODICAL: Referativnyy zhurnal, Geofizika):no.:7, 1962, 49,.ab-
stract 7B260 (Tr. Tsentr. in-ta,prognozov, no*-1160
1962, 65-66)
TEXT: The methods suggested by.L. Kletter (Praktische Erf.ahrungen
mit einer neuen Methode.zur Ausarbeitung mittelfristigerl'iette'r-
-prognosen, Arch. Ileteorol., Geophys. und Bioklialiatol. A,,1956, Bd.-
91 H 2), was verified in,conformity with the citculation conditions
over the USSR's European territory. L. Kletterls method is based-on
the use of the linear regression equationj~relating the mean three-
day N-850 values to the values at 18 hrs on the initial day. For
the USSR's European part the regression coefficients were deter-
mined by the method of least squares from"the daily AT-850 charts
-for Mosebwy Leningra.d, Kiev, and Sverdlovsk for January.and July,
'lard 1/2

S/169/62/000/007/1121/14.9
Possibility of applying D228/D307
1950-1952. Out of 27 forecasts 15 proved to be correct in the
-Aynamics of~
other 12 being incorrect. The:method does not give the
the development.of,pro.cesses.-.The reason for the"low'justifiable-
ness of the forecasts evidently consists.of the fact that no ad-
.equate allowance is made for the regression equationlB freo term.
Abstracter's notet Complete tranalation.-7
10ard 2/2
........................

VASYUKOVP K.A., kand. fiz.-matem. nauki ZVMEV.,_Njt,,,.kand. fiz.-matem
nauk; PEDI, D.A., kand. geograf;-nauk
Rhythms in the atmosphere and some methods of evaluating them..
Meteor. i gidrol. no.lt47-49 A 165. (MIRA 180)
1. TSentrallnyy institut prognozov.

L 10 406-67
ACC NRt
AT6033032
where (D is the scalar potential of the magnetic field; Ho 16~ the magnitude 'of the
:Longitudinal field; H is the amplitude of th p-th harmonlc~~of the helical fleld-
r, q) # zare coordinates. - Mere follows a ma(Zhematical development for the case Of a
holical field with n - 2. The article gives detailed mechanical drawings of:i evetal
of the main features of the equipment used, Including a-cross section viaw of7the-
apparatus, details of the helical winding, and a bIbck diagr4a of the feeding! system.,
A further figure shows an oscillogram of the current flowing'through the winding* Ihe
experimental data confirm the validity of the appiroaah to the probleme "In conclusion
the authors express their sincerG thanks to M. S. Rabing-vIch for h1s: continaing
interest in the work and for his helpful iis'e, ~80;~t'as ~W as U) rG4 P. AlekSM&OVI
V. 1. Dudin, V. I. Kryykavo and Ve P. Solov'm who took part in Uwaonstruation oif
the equipment,' and to G. L (b I kin& uho: took part In ths coAS'tmotJj*., *,f the
system*" Orige art. hast'~S formulas. 7 fiq%4vs, and 1~ table
SM CM38 '-20/ SUM DMs' none/ OkM~,RWs 014/`~ ='Dws'! 003
/241p
2

BATANOV, G.M.; BEPS7UTSKIY, M.S.; GREBE, NSHCHIKOV, SJe.;
POPRYADUKHIN, A.P.; RABINOVICH, M.S.; SBITNIKOVA, I.S.; SHPIGELI,,
I.S.
Magnetic surfaceB and the confinement of a.plasma by helical'fields
in a stellarator with external injection. DoU. AN SSSR 16o n&.6...'
1293-1295 F 165. (MIRA 18:2)
Submitted September 23, 1964.

S/08.1/61/0(iO/023/058/66i
B106/tloi
AUTHORS, Reznikovskiy, M.M.t verev, N-P., Denisolia, L.L.
TITLE: An improved chamber for laboratory test6,"Io~f tlje~ozonc
resistance of rubbers
PERIODICAL: Re'-~rativnyy zhurnal. Khimiya, no. 23,. 1961,*561, abstract
'P
2
3 354. (Tr. N.-i. in-ta shin. prom-util.eb. 7y' 1960t I
TEXT: An installation guaranteeing satisfactory accuracy and,reproducibility
of measurements even at nonuniform 0 distribution in the.werking chamber is
3
described. In order to exclude fluctuations in the 0 concentration, the
3
case containing the samples revolves at a rate of 2 rbm'.1 The contactless
transmission of torque from the Warren motor is attained by means of &,nlag7
netic clu$ch. CAbstracter's note: Complete translations
Card 1/1

AUTHOR: Zverev, B.S., Engineer SOV/133-58-.10-26/31
TITLE: On t-he-T-r-0b-1-em--"'of Production of Deep.~Dirawlng Sheets for
the Manufacture of Automobile Bodies~:(K voprosam proiz-
vodstva avtolista dlya glubokoy vjty4zhki)i
nRIODICAL: Stal 1958, rNr 10 $ p 9,48 (USSR)
ABSTRACT:* The paper contains critical remarks:dn the: previously
published paper'by G.D. Rogoza (Refs;J an!i 2) in which the
validity of Eriksen's test for deep drawi'Ag sheets wag
questioned. The present author considers that in,order to
supply quality sheets, the metal should be.extensively
tested on the producing works. T:iere are 3 Soviet.
references.
ASSOCIATION: Gorlkovskiy avtomobillnyy zavod (Gol".1cly Automobile,
Card 1/1

AUTHOR;
TITLE:
PERIODICALt
ABSTRAM
Card 1/2
Zverev, U.S.
Tests of Imported and Domestic Cold-Rolle-1 Plate for' Auto-
mobile Bodies (Ispytoniya impoitnogo1i 0t,30heJtvenn6_o A*vto-
kuzovnogo kholodnokatanogo lista)
Avtombillnaya promystilennoet', 1958,11ir 9, PP 38-40 (USSR)
The Gorlkiy Notor Vehicle Plant, an&also sevoral tber Sovi e t
automobile plants, satisfied part of its ,.requirement's for
cold-rolled plate for car productioinl!by ii6ports. Especially
the Gorlkiy plant obtained cold-rolled stoiel plate from;ithe
USA, England, West Germany and Francb. In order to compare
the chemical analysis, mechanical properties and prelssing
results of the imported steel plate and that produced by the
zavod "Zaporozhatall" (Zaporozhstal1jil Plant)'o tests of both
kinds were carried out. The test ra6ulta are preso,ntjcd.on
4 tables: The percentalge in the Plate of carbonp manganese
and sulphur (Table 1); yield point,~olongation, relation
between the yield point and the ultimate istrength at rupture,
hardness RB, extension by Erichsen c4ppinjr best in mm, grain
size in ball-marks, waste at punchinG (Table 2), the same
data for the angular body panels of the 111-lobedall car (Table 3)
and stamping results for other parts (Tab:.e 4). The author

SOV-113-58-9-15/19
Tests of Imported and Domestic Cold-Rolled Platelpr Automobile Bodies
evaluates these results and strongly.recommends their con-
sideration. in the e3tablishment of relevant GOST standard3
for the motor vehicle plants.
There are 4 tables and 3 Soviet references.,
ASSOCIATION: Gorlkovskiy avtozavod (The Gorlkiy Motor 'Vehicle Plant).
1. Automobile industry--USSR .2. Metal plati..,s--Effectiveness
Card 2/2

he It 11 Ifw it 46 it III it a it i, I
A I A-r_ A- 9 A I T T.: AA 0
to i.
Ar-Ot-

so

INTLITrNICE OF I REF FM11M. On IttItACT r-IRMIGTH. !-is
14qtft11pxrO14. 14. 1 5-102(193h) (in Russian) 1 1-01 AtItX'sat 16 .00
Allove 6, 508. L(
rif
v inomet strength absorved in pr"asvi.V, parto nM*
steel contz- c 0-31 --0.39, tin 0-33-0-46- Si 0-21-0-34 ~nd Cr 0, 1. 1 ZIA
a was due to the Drei ence of free forrlte either
'
'lowly V(w Ft-laininig it
in .41%.
C.. C..

-too
IVA
;so
so
LIt
4 44 1is 0
t w I I'a
0 0 0 0 0 0 a 0 a so 0 0 0, 0 0 0_4 0 0 0. 0~6
04 s. 0 0 0 OrS

(Kazakhstan--goonomic conditions)

v- R a I1 6 .
BUCHii&, Boris Aleksayevich; DOWOPYATOV, Yu.A., red. -, ZVEW. N.V.,
speteredaktor; NAGIM, P.A., tokha.red.
(Kazakhstan is a republic of large-scAle state,farm production]
Kazakhstan-reBpublika krupnogo sovkho2nogo proirvodotva. Alma-Ata,
Y,azakhakoe gos.isd-vo, 1956. 129 p. (MIRA 10: 12)
(Kazakhstan--State farms)
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