SCIENTIFIC ABSTRACT YUDIN, M. F. - YUDIN, M. I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001963110006-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 15, 2001
• Sequence Number: 6
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

21826
B/115/61/000/004/005/010
Tissue-equivalent dosimeter... B129/B206
mixing graphite with polyethylene. The tissue-equivalent chambers of the
dosimeter are produced from pressed,,carefully mixed powder consisting of
2.4 parts by weight of polyethylene and I part by weight graphite. The
surface is homogeneous and smooth, which is important because of the
reduction of adsorption of gases on the chamber walls. The conduction of
the material was good; that of the surface, however, was irregular in
various parts of the chamber. The.calibration of the chambers in the
field of the Co 0 gamma rays showed that this fact was of no noticeable
effect on the quantity of the ion current. In order to obtain the radia-
------------tion--equili-bri-um-and--to exclude -the-- diff us ion of---the-gas-through the-wall,
.the latter was msde 5-mm thick, and the volume of the chamber was
953 (i13) cm3. The central electrode of the chamber was made from the same
plastic and mounted in the center of the chamber fixed by means of a
polished insulator from polystyrene., The leakage currents through it were
small compared with the ion currents to be measured. Fig. 1 shows the
scheme of the ionization chamber. The body of the chamber consists of two
parts which are glued together by a mixture of epoxy resin and polyamine.
This mixture polymerized quickly at room temperature and was used for
Card 2/5

21826
S/115/61/000/004/005/010
-,Tissue-equivalent dosimeter... B129/B206
mounting the inner electrode in the insulator. and the insulator in the
body'of the chamber..'A device-was provided-to produce a vacuum, fill the
Chamber with gases of required composition and seal the content
hermetically from the ambient medium. An electric measuring device built
by the,"Etalon" Plant served for measuring the ionization current during
irradiation of-the chamber with neutrons. iThis circuit is shown*in
Fig. 3. It is a quadrant electrometer which is supplied with a stabilized
voltage of,300 v. This electrometer was used for measuring-either the
potential at the condenser plates or the potential drop in the resistance.
..Ln the first case, the indication was proportional to the total dose, in
the second case, proportional to the power of the dose. The calibration
of the instrument, calculation of, the current caused by the neutrons and
the practical measurement with the instrument described are dealt with
next. As a result of the studies, a tissue-equivalent dosimeter for fast
neutrons was elaborated, which permits measurements of from 0-5 to Dome
hundredths microrad/sec with an error of 7-12~L There are 10 figures,
2 tables, and 14 references: 4 Soviet-bloc and 10 non-Soviet-bloc. The
four references to English language publications read as followsi
Rossi, H. H., Failla G. Nucleoniest 1956, 14 (no.2); Hughes D. J.'
Card 3/5

21826
S/115/61/000/004/005/010
Tissue-equivalent dosimeter... B129/B206
Harvey:I. A. Neutron cross sectionsp N-Y, Toronto, London 1955; Baum I.W.
Neutron dosimetry - a review, 1955; Snyder.W. S., Neufeld J. Brit. J.
.,Radiology, 1955, 28 (no-331).
~Legend to Fig. 1: 1) Body; 3 2
3.2
2 insulated electrode;
3 insulation material.
Fig. 1
Card.4/5

21826
S11151611000100410051010
.~Tissue-equivalcnt, dosimeter... B129/B206

YUDIN., M.F.; BALIYAN, L.G... red.; USHIRIN, A.G.., tekhn. red.
(Methods and equipnem~ for calibrating radiation monitoring
instnmento]Metody i apparatura. dlia graduirovki do2;jmetrjcbq-
skM priborovs HosWa., Standartgiz,. 196',,. 3a7 P*
(MIRA 15:12)
(Radiation-Measurement)

119348-63 -E%7(1)/EWT(M)/BDS/ES(j) AMIAmclA AR/~
ACCESSION IM: AR3005189 S/OM7163/000/007/0163/0163
JSOURCE: RM Metrologiya I lzmer. tekhnika. Otd. ".1 Abs. 7.32-1100
AUM01,1: Yudin, 14. F.
--------------- -
TITLE: Some corrections in the-determinatio n'~of x-ray dosage by means of a 250-
130DO kev ca]-ibiation apparatus
~j CITED SOMCE: Tr. in-tov Kom-ta standartov, ~,mejr I izmerit. priborov, pri Sov.
jMin. SSSR, vy*p. 69(leg).. 1962, 56-69,
dosimeetry,, dosimeter calibration..C
TOPIC TAGS: radiation 0. sup 60, gamma ray,
!measurement, dosimetry
iTRANSLATION: . The author considers.tbe problem,of.introducing corrections for
..the penetration of:radistion through the wells of a calibration diaphragm and
with the aid
scattering In the measurement of doDes of Y -radiation from C~66
!of a calibration apparatus. It is noted that in the assaying of test Y-emitters
iwith the aid of tbe calibration apparatus, the correction for tg8 penetration
;and scattering of radiation bythe calibration_diaphr~gm for Co -rays is
Card 1/2

L 19348-63
:ACCEESSSION NR: AR3005189
'about 0-945. The correction for air scattering In the measurement of Co6o Y-ra~r,
!varies from 0.988 for an air press of 8 atm to 0-97-
ure 2 for a pressure of 20 atm.
Five illustrations. Six tables. E. Vtyurina.
DAW ACq: 24.Tui63 SUB CODE: GE, NS ENCLi 00

AN 5--D-"!--'l:P I
N ---,2 'L r iz-
4 f
:.~r A' ~.l

Cur-
!-09-

YLJDltl. M.F.-, YATIOVSKIY, A.P.
Seattering of neutron radiation dwing the gradization of
and emitters. Nov. nauch,-issl. rab. po matr. VIIIII-I no.2143-45 16!,.
-Apparatus for reutrdn-dosimetry. Ibld.-6&.7C .'141RA 18:4)
K-2
nk

SHIROKOVP X.P.; YUDIN, M.F.
ThA Ath npqqinn nf thn TAphninAl nn".-fttpa ITA49 f%f, f~,=
ad RMF~, ~11
_0
-z

KARAVAYEV~ F.M.; YUDIN, M.P.
Nev s tat!) a tandard P-848-63 IlRadioactivity ard ionization radiation
units," lzmetakhe no*6:51-53 JS 164. (MIRA 17:12)

TUCIIIN~ V.N.; OSTROMMIKIMA, G.P.; VIDIN, M.F.
Effect, af a colliMliting de7lce on gra-duat-lon ar,-J
rot3atgenometers Wosir,.-m-ters) by meana of standard gdrf.21!'l MY
12n, tekh. no.308-61 I-Ir 165.

L 38475~6 - Vff (m)
AC-1 M' AR 017219 SOURCE CODE: UR/0058/65/C)OO/012/AO6,-i/i%oo'
AUTHOR: Yudin.
TITLE: Ionizing radiation dosimetry
SOUR.CE: REf. zb. Fizika, Abs. 12A.538
'F-BOURCE-:'%~-Tr4-'i~-tov-'136S.-~k~ni.-ta~standartoir m-ir'i izmerit.,.priborov SSSR, vyp.
._76(136), !965,,152-159
TOPIC TAGS: radiation dosimttry, ionizing radiation
ABSTRACT.. _M,& _~isper gives~.a brief,review of basic studies in ionizing radiation
Met
o
si ry carried out by the x-ray laboratory of VIMM from the time of its organiza-
tion to the present. Main trends of studies by the laboratoY7 for the immediate
future are indicated. Bibliography of 61 titles. [Translation of abstract] [KPI
SUB CODE: 18/ SUBM DAM none
pb
2,
N

VITIFIMIrE, l."YSANNOV, Yu.V.,~ S7AXOTNIX0111, V. V. KIIISBIlIKOV, K.K. MiN, M. F,
Trie :,D Mev. tat r on a z A I -Uni or, f -J,: Re S-e- ;~7 - -r-
1 V s e s oy u nyy n -a i c h r- c- i s 21 a d, r; v ae Ik y iristitu-, Tnetrn! ogil

ACC'NRt AP7000128 SOURCE CODE: UR/0115/66/000/011/0015/0017!
AUTHOR., Yudin, M. F*
ORG: none
TITLE: Equivalent dose and unito for its measurement
SOURCE: lzmeritel'naya tekhnika, no, 11, 19660',15-17
TOPIC TAGS: ionizing radiation biologic effeit, relative biologic efficiency,
radiobiology, x ray radiation biologic effect, radiation shielding, radiation safety,
xr.iiation dosimetry
ABSTRACT: The author would modify the present practice of expressing the relative
biological effect (RBE) of both quantum and corpuscular radiation in the form of a
'ratio based on quantum radiation (x-rays) alone. Two modifications are necessary:
1) introduction of,a quality factor (QF), uniquely characteristic of each type of
radiation, to take care of the difference in biological effect of identical doses
of various kinds of radiation; and 2) the basing of all calculations on the absorbed
tissue dose (expressed- in rads) =her khan on the external - radiation dos e (exp~,sure) in 7
roentgens. 'The precise values of the quality-factors for various kindo of radiation
Will need to be established by worldwide research. The author gives the following
table of approximationst
Cgrd 1/3 UDC.- 577.391(017)

Rt_
ACC NR3 ..AP7001
1500-5000 53 -175--- 10-20,
The author would restrict the present concept of biological (RBE) dose, expressed
in bar units, to biological objects other than man. In its.place he proposed that
all research on shielding and human radiation safety (i.e., studying radiation
effects mau) use the "equLvaleut dose." Equivalent dose will r-orrespond to
Zil
q;~M 3
Table 1.
Average specific - Average ener& Quality
Type of ionization in water, transfer in fac-tor
particle ion pairs-n7l* water$ (QF)
kev-t-l
Quantum 100 or less 3.3 or less I
radiation,
electrons,
p6sitrons
Heavy ion- 100 or less 3.5 or less 1
Izing par- 100-200 3.5-7.0 1-2
ticles 200-650 7.0-23 2-5
650-1500 23-53 5-10

4 Viw

ACC NRi AP7000128
(but-not precisely equal) the product where D is the tissue dose in rad, and K
ZK
'
n.,.Equivalent dose (EW
-is.the 4unlity faitbrapplicable to that type of radiatio
will be expressed by tbe-unit "equivalent raId" (eq. rad). JDP]
--SUB " COm- ~ -ISS - ObI 03 May66/.0RIC REP: 001/ REF: 003/
SUBM DATE.
ATD PUSS: 5116'.

Card 3/3

Iligh-fr*quan oy corrootion in hondirootioml inicropl, onbs with
im*vlr)g ooils Tndy LIXI melo127-31 1649 Q41RA IM)
1s XkfodrA akuotiki LuingrAdokogo inatituts kinoinhencrove
M-

KORESIIEV~ G.P.; YUDIV 1-1 G.
Calculating- the friction in a nondirectional microphone vith
moving coil. Trudy LIKI no.10:33-35 164. (MILRA 18:9)
1.,Kafedra akustiki Leningradskogo instituta kincinzhonerov.

MkROKOVI HaI.; C-ABUZINA) A.G., Btarsbly nanchnYY i3otrudnir;;
TUDIN, 1491., mtarahI7 agTonom-Inspektor
Doaderana itB control. 2-ashcb. rast. ot vred, I bol.
5 no. 8:5 0 Ig- 160. (MIRA 13.12)
1. Zamantitoll direktora Pavlovakogo opytnoao lugovopo polya
Uor-Nanarokov). 2. Voronemhalm7a stantsiya zaBhchity racteniy
(f or Libuzina). 3. Vor'ons--zhBkaya goBinspektsiva po karantinu
raBtaniy (for Tudin).
(Dodder)
-IR- NRR
an,
IN
m
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m
AR
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Od.
Pliybicb bTA:he'atfnohpbere. 'Sv6rdlovik Gidrometiolzdat* 1945. 83 p. (ffO -czsm.
Glai6o&-uf~ratilbnie;gidir~69teorolibgii:hdakoi slilzbby SSSr Trudy nouchn-o-43spleAdoe-ats-11-
skikb uchrozhdonil. Sor. V Yeteomloglia,, vn. 7) i54-32128)
W9.15 .--18

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Jn Engljfih An r2fz-n-
pp.
Mon (111 Im oll t Phy'l, p11).
sip. 1/4's, r~ Pt~010-, 2044, VU-1, 8, ~-'J 21),
101 Im N Ru-zon.) to a cm vhcrv th, rnta, r

4r, le 'n
thr -7g), ri'varbim').
77

(Editor)
physics of the Layer of Air Ncar the Groand (5jmposiun, Of Artici6o) Works of ttv Sci- s
tion of the 11ain PcLdnistration of Ilydrom.Worolopical Service SS3R. Serleo 1,
Institu
iio 28. Hydrowteorological Press., 1946, 94 pp (Main Geqphy3icu
Ubservatory.)
(meteorologiya i Gidrologiyaj, Ilo o Nov/Dec 1W)
S'O: U-3218,:3 k-pr 1953

PDRI, M. !.
Voprosy teorii turbulenthosti i stuktury vetra s prilozhenien
k zadache o kolebaniiakh samoleta. Leningrad, Gidroneteorolog-Icheskoe
izd-vo,, 19L6. 99 p., tables. (Rii~sia-1923. Glavnoe upravlenie gid-
ron, ateorologinheskoi nlushby.- Trody nniicliiao-l.,3.9l,edovatellskil,-h lichresh-
denii. Serlia II I-Ileteorologiia, no. 25)
Title tr.: Theoretical questions of turbulence and wind structure
applied to the problem of oscillations oil an aircraft.
TL574- V5-18
SO: Aeronautical Sciences and Aviation in the Soviet Union, Library of
Congress, 1955-

T.
in the 11heory of Turbulence.and Wind Structure," TriLdX NIU
"Problems
GjUr,~Bl Serles 1$ No 35., 3.946.
F., M.
-M
X
kzZ

MORE
MINM
re on 'the 0MAs Of 'aterj"s
mrse of tUm5phoric ?remi
ttRoccarch on the Cc ii' d 10,
rr-- -T! M-by-the. ~!ethod* of- veparatinr, Dist.urbanneui.
-0 a rolor 2 19
nip rre ya (Theoretiel Vct 0 Y)x
+iche . toorougi
Leory-skaya
V

ME
gn'
7-71 11 S
g-..
A I
p m ~ gH
"I.lldi= 114 1
Sep 1946
TJSSRj moles
Sn
Temperature
Ltmosphere
Transf erence, 1. Budyko, 'fudin, 4 pp
the Atmospherew
11bri= iu
ndtons,O:f Thermal_Equi
0
(DpkIady)n Vol LIII, NO 7
11 Comptes Rendus and of atraosnh-eric
ge in the atmosphere* 1 6
jocussion Of the lieRt exchan 0-098 rate of temperatare
P-1
mathematic d d that the I - pinion that a Meal'
I conclude ted o
eddies, It 6 -ac0eP unda
turbulence Or the generallY rd the grO
end the abandonment Of phere towa
the atmos
The authors recomm the verticia direction from
heat flow exists iu
eddY

4R-149
nyt problemy taeniU ob atmosfetnal turbvientogs!J. [At)t)li!!d problems
t torbulence.] Mefrprotogiia i Gidrologiia. 3:3-10, 19-17. 29 rtft, IMB-171i
of atmospbeii
-uth- -450- the rjose connection b-tween turbulence and varloug mptcts of humfin activity by

4 - no
2 enumenting orey thirty pmrtlcal pmblorw depending upon the 1.1ws of turbulent motion- The

, phy-~Icul bsst-s of the gre-at majority of ,zlientlons of the theory of atmixiplicric turbulence can be
Yebi 1953 classified 2s followw Turbulent vertical tran-Jer of hent. rnoWure. and mm~q m-,ar thr underlying
C.

Ao
on
t
sph -ion of mixttires In theatm p e , and r ly3i t r
urfart; the theory of turbulcrit 41flu. cm h re n ta ~ i of tie st ucture
-
f Me
h
I
l
)
i
h
h
E
g
y
Ti , w
t
!i afta
emp
aind. terriNrature, and premne.
ac
o
n gmups
ym
I the fic1da of
diff.
n its practkal sigm)ficanm SSJNICJ Heddimsy'. 1. TurbMent mbingo 2. Turbulent rJon
Vand gmctwg -C K
V

u-Investig-atiOns by the Soviet School of Meteorologists-
R. S. and YUDIII 14
SOLOVEYCH It 11
51 pp
.algoraticians., 110
weteordlog~-Ya 4 Gi6rologiya, 6 IWv/DOc 1947)
50; Tj-~W,3 Apr 1953

YUDIII Me I.
jan/Feb V
"Heat Exchange of the Earth's Surface With the Atmosphere and th-e-Equillbri
TemDerature Gradient," 14. 1. Budy1co, M. 1. Yuain
I'Meteorol i Gidrol" No 1, Pp 16-30
Proves "Schmidt paradox" is erroneous. -Schmidt, in contrast to generally accepted notion,
concluded average turbulent heat flow is.directed from atmosphere to earth, using equilib-
rium temperature gradient of.5-60 C:/km.
PA 167T9!
6~
E
!R7, Y~..r Ti- tig g~
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Farb,
-Rhj arologj
Crite'rill
-rdson
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o
es
-yuain
o 6 79-81
l i Gid-f 01
Veteoro
ct-
Po3.jovq dire
t conclusion Vhicb
,alus
Ig ti=bulent
S
ria "bat
t
e
hardson's cri
-rligh
'Ola matter how
~~
St alvaya the
Ut state c'
energY
jVUtf ere
jal leve 1, T or
table strat-
init
t
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i
=-,.. so for uns
ven
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wins of tbel
MttfDTVj,gjs6tskikb P' .. Trudy-!
I ()h' !E2Lsjl-n of the,
h
43~_-F I GI 'k ~,,4
J.,migned. - -, - , g, d 1=5-
A n
JYd;l1rlll --' Ci, ()Pllmuln~
'le M05pheric) MOIS. um~
tbr,Drv 3n, 2 figs.. 4 t2br-", to pb n dVTj3tjonsftOMthw-OPtlrd
1901).2Sb-314. 1950' 1 ,u,bAlnV M)IiD"' .11cal artennlnRtlOT`,- 11 . in intexpolatiOn!
Ab5t* t )JI"'tinn 0t throlly p it), U~e of them and jmgly crors -Qjrjcally~
3p] nce.
CW'dillons in O'lle 'I'd $p , rt and pr-LIt td tbevfc'ic:'lly Mr~- t T
2 clul" I the irmptralu,
.'I'leations are tro I Statistical thtt"fy
Vol. 4 thc 5'" ,prZature or Oir4, bule=. S"bjec fiesdi"Is:
1953 - re OT time In tt,
ntillj=1 throry
Bibliography on it. th- light " tht s" - t rbultAtO
Yeb- hjaLA~~ 3f
4Y
Turbillent E%ebange

la
351 ZSI:SS 1,556.2:632. I't
fluen-ce-o-M-e-Meller bell* CM turbulent exchAnte and the OptImM %vidLh of the belts.3 AhAetmiiaj
Ortfs.,Seqs. DLC-A shelter bell, reduce.,
)btel;,rojoglesl Absto :mt only the whid sperd but %that Is more im]~Zt for soculture, it reduces the turbulent exchange
Volt 4 not 2 by byesldpir up the Us eddir-- and fonnSrs =213y xVII ranCom eddlt3. Expcrimenta made In 1949 1
by the of the Cntrat Geophysical Obftrvatory (Leninvrn~in con- 1
Fab. 1953 neWOYT-~M, 1, Irlso to the Colarlul"Ort tBat lor mits Of ar"IM Irt-M MMvptlmurn
SibliograpbY-On- - wid1b would be from 3 to 25 metem (Sow ilm es 2.6-92. June 1931. MAR) Subject Hcadings:
Turba9nt,EXCbWlP
IMIT,
TWIN
Op
WIMWIRAI

YO-DIT41 M.
PHASE 11 TREASURE ISLAM BIBLIOGRAPHICAL REPORT AID 20 - II
BOOK call No.: Qc 861-T65
'Authors: ZVEREV, A. S., KIPYUKRINj, B. V-* KONDRATIME ~ K. Ya., S-EM-NEVA, Ye. S.,
TVERSKOY, P. N., YU0334, 14. 1.
Full Title: COURME OF 1EMOROLOGY (PHYSICS OF THE ADWPHERE)
Transliterated Title: Xurs meteorologii (Fizika atmosfery)
Publishing- Data
Originating Agency: Vone
Publishing House: nlydrome-teorological Publishing House (Gn4TZ)
Date: 1951 'No. pp.: 688 No. of copies: 10,000
Editorial Staff
Editor: Professor Tverskoy, P. N. Tech. Ed.: None
Editor-in-Chief: None Appraiser: None
Orthers; 1) Scientific Council and the scientific personnel of the Main Geopbysical
Observatory, 2) Prof. Khromov., S. P., who critically analysed the manuscript.
Text Data
Coverage: A funaamental course in Ue physics of the atmosphere, covering it.,3
properties.. methods of investigation, application of thermodynamics,
radiant energy, heat energy, water vapor, motion, weather and its
forecasting, atmospheric optics electricity, and acoustics.

1) 1 IV,
PHASE I TMASURE ISLAND BIBLIOGRAPHICAL REPORT AID 6-24 1
BOOK, Call No.: AF 5010R3
Authors: Doctors of Physico-Mthematical Sciences BUDYKOp M. I. and Prof, )!TIN
11L-jv.-Doctord-of Geographical Sciencesp Profs. DROMOV, 0. A.p LIVOVICH,
M. I.y POGOSYAN., Kh. P., and SAPOZHNIKOVA,. S. A.
FxLU Title: CLIMATIC CHATIGES IN CONNECTION WITH THE PROJECT FOR THE TRANSFOMMION
OF NATURE 114 THE ARID REGIONS OF THE TrSSR
PUBLISHTMG DATA
Originating Agency: None
Publishing House: Hydrometeorological Publishing House
Date: 1952 Noi. pp.: 206 No. of coPies: 3,000
Editorial Staff
Editor: Prof. Dr.,, Kh. P., Pogosyan
PURPOSE- Presentation in concise systematic form of the resUlts of fundamental studies
of climate amelioration by hydrometeorological institutes and the recommendations
to be followed by those intez;ested in climate transformation.
TEXT DATA
Coverage: The monograph is divided into seven chapters and a concluding chapter,
the chapters being subdivided intolseveral sections.

SAPOMIKOVA. 5.A.;
-BUDY] W, H.1 MOZDOV QIA~/-. LIVOTICH Role; POGOSYANI K'h'p';
X.11
Regularities of cli=tlc changes with respect to the realization of the
Stalin plan of transformation of nature. Vop.geog. 28:66-73 152.
(MMA 7 : 5)
1. Giarometsluzhba.- (MoteorologY, Agricultural) (Vinabreaks, shelter-
belts. ate.)

AVMAN, A.B.; BIMUO' 34.1.; TMIN, H.10; OOMOVSKIY, Yuje,; DAVYDOV, H.He;
-"'YM0VI NON*; ANTIPOR
AMIAM, D.L.; WWROVICE, ZKO, -XAWAYEV, I.N.;
SOOMNIKOVAt B&A,; ALISOV, B,?.; 70MYEV, IOU.
Discussion of, reports of the zeeting. vop.geog. 28:74-96 152. (ISRA 7:5)
--I. Gidrounergoproyakt Hinisterstva elektrostantsiy (for Avakyan).
-Glavwa geof izicbeskaya- olbservatorlyA A. I.Voyeykova (for Budvko
and Yndin). 3. Inttitut ckBanologii Akademii z~wuk SSSR tf or 0elwitove-kiy).
4
Gidroanargoproyekt Hinisterstva, elektTol-3tantsiy (Tor Davydov).
Inatitut geografii Akademli nauk SSSR:(for Armand, Fedorovich, and
Yoteyev). 6. Geografichankly fakulltet Mosiovskogo gosudar3tvonnogo
universiteta (for-Zubov and Alisov). 7-.Poehvennyy Institut Im. V.'V.
Doknchayeva Akadenii nauk SSSR (for Antipov.;Karatayev, I.B.). 8. Glavneya
g9ofizlcheBka7a obaervatoriya-in. A.I.V ykova (for Ba-Dozhnikova).
.078

6kj
BMYKO, R.I.; Y[WIN, Hole
ExpDrinentml investigation of the meteorological efficiency of field
protecting tree sheltarbelts. Trady GGO no,29:105-113 152.
(Windbreaks, shelterbelts, etc.) (MIRA 11,.l)

YUPIN, MOIO
Application of the statistical theory of turbulence to the
alupliication of equations describing atmospheric dynamics.
.Trudy GGO no.33:5-19 152.
(Atmospheric turbulence)
Oleteoroloa)
R-`~~z~

;,T. -i
7-- - w,- --?:, rv. lui, -- Llhi~ ~th--, rlira-ati, MI.,

YUDIN, H. 1. YAKOVLEVAO H. 1. and BUDYKO., H. L
nEvaporation From Irrigated Regions and EvapDrabilityll.
HeteDroi. J Gidrologiya No 1, pp 7-10, 1954.
Computations of evaporability for large and small irrigated territories
under various climatic conditions are considered. It is pointed out that in
the deteridnation of evalmrability from small territories under conditions of
a dry climate one must take into account the dependence of evaporation
upoh the dimensions of the wetted surface,, since evaporability from large
wetted territories is markedly less than from small arean, The difference
in the magnitudes of evaporability appears mainly for irrigated areas of
less than one kilometer extent, especially for areas of less than 100
meters, si2e. Under conditions of a wet climate the difference in evapora-
~tion from large and qmnll wetted surface is sm;;Il. The presence of blow-
through forest belts in irrigated fields ensures decrease of evaporation
from fields by 7-14%, thus lessening the irrigation nom. (RZhGeol, No 11, 1955)
SO: Sum No 884, 9 Apr 1956

1C
TION
~LHM BWX EXPIJDXTL
Gandiny Lev Semencrvich; La~rkhtmw, David VVoViCb; Matveyev,, Lemid Tikbmovich;
__Llzaakoich
id-Tudin ~(i4i#
_0snM ainami~iesk6~r Leningrad)
Oi4rcmeteoizdatj, 0 'W 3)~o k..000 ~~im~ winted.-
Ea. (title pago): Wkhtimat) Do Lo. Profeasor, and Yudin M# lot Professor;
V
Responsible Ed.: Pyatygin, K. V.; Ed. (inside book 100vap YUN ve;
Teeb. Ed,: Soloveychik, A. A.,
PUMWE: This book., vhia Is a treatise, on dyamuic-Mateorology devel0pBd by
the author in the coune of lecturing at varlow aniveraltiess Is
intenaea as a textboolc for meteorology studento of vuzen and a9 a
handbook,for specialists in the field of meteorology and clizatology.
COVERAGE: The book ew-alres- the basic methods of dyn=ic meteorology, neldng
extensive use of mathematical treatment in analyzing the vhysical
place in the atmosAere. The latest develoyments
3w~ceases taking

rge-Scale Atmospheric Pro
Invariant Values in,1A ceases," by
M. I, -Yuain, ir. Gi. geofiz. -observ. , Wo 55, 1955.1 PP 3-12
(from Referativnyy Zhurnal -- Fizike, No 9, Sep 56, Abstract
Tio 2715YT
The article is devoted to the determination of values remaining un-
changed during atmospheric motions on a large scale.- The analysis is
based on the order of smallness of the various terms of atmospheric dy-
namics equations, expressing motion for which the relation of the geo-
st,rophic deviation to vind velocity is a smaller number. Using these
positions as well as tables of the order of meteorologic elements and
of its-derilvatives, a classification of terms of the equation of the
vortex is ande according to their order of magnitude. It is shown t1mt
the potential and the absolute vortices previously considered as invari-
ants really remain invariable only in some particular conditions. All
.-these concluzions hold onlyin the free atmosphere and under condition
of adiabatic =-tion.
sum lag

P~ i'!~4
A)MO hark Y.
MAiM.TMO VOejrevlch
VA, r roDz,,
Jr. ot
roda vetstve:lw
ti Om and red&kt
Areds-ka "Ontr6l of .1
SIOla tekhalchookor'
oeat- con4l",
a-trj Air
rovanle In the or
! 096 1 '
the
re
_0 caotl ails prizem
Skao led J3 ogo
"ePherlc "o 1956.
(N'~A 9:7)

SOV/124-58-4-4298
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr 4, p 88 (USSR)
AUTHOR: cy-~~~
TITLE: 'The Variation of Meteorological Elements With Time and Space
(Izmenchivost' mete orologicheskikh elernentov v prostranstve
i vremen*)
PERIODICAL: . V sb.: A. 1. Voyeykov i sovrem. probl. klimatol. Leningrad,
Gidrometeoizdat, 1956, * 175-192
P
ABSTRACT: A review article.' A. 1. Voyeykov1 s interest is noted in the
studies of periodic and nonperiodic meteorological changes
with respect to time. The article enumerates the basic works
of Soviet and foreign authors related to nonperiodic changes.
The most important results of the research are indicated, and
their significance for weather forecasting is stressed. Further,
the article considers data related to the changes of meteorological
elements with space. The article deals with data related to the
variation of the mean pressure difference between two stations
as a function of the distance between them; the influence of the
direction of the line connecting the two stations is considered
Card 1/3 and is shown to be of extreme importance. In this connection,

SOV/124-,58-4-4298
The Variation of Meteorological Elements With Time and Space
and along with the usual correlational and structural functions, additional
statistical characteristics depending on the distance I alone are intro-
duced. (The said usual functions depend generally on two values, namely,
the distance between the two observation points and the direction of the
line betweenAhese points. The statistical characteristics are as follows:
correlational and structural functions .,averaged relative to direction, and
the scatter of the mean of the quantity f over a circle of the given radius
I which is called by the author the 'total- c or relation function of f .
The article gives new data on the structure of the humidity and geopotential
fields at different levels of the atmosphere. Basic results are given on the
connection between the structural functions and the mean values of the deri-
vatives of the meteorological fields. A table with collected characteristic
values of all the mean first and second derivatives (for space, time, and
-both combined) of the basic, meteorological fields in the layer from 0 to 5 km.
There are notes on the subject of variation of the urder of magnitude of the
mean derivatives as a function of the scale factors of the processes consid-
ered; these variations are illustrated by,a special table. In conclusion the
author indicates a number of values (geostrophic vorticity, advect-ive geo-
_str~ophic variation of the vorticity and temperature), the detailed study of
* d by-tbe modern development. of dynamic meteorology and
which is require
Card 2/3

The Variation of Meteo.rolog SOV/124-58-4
the nurne ical -Elements -4,298
adequate. -rical forecasting With Time and Space
Methods, but whic
hto date has been
Meteorology__St
atistIcal anaiy,i, A. yaalom
Card, 3/3

I
TITLE: Structural Furiction
(Strukturnaya
36-71-ii/A
of the Field of Absolute Humidit
funktsiya polya absolyutnoy vlazhnootiT
PERIODICAL: Trudy Glavnoy geofizicheskoy observatorii
j 1957, Nr 71, pp- 156-162 kUSSfQ
ABSTRACT: A better Imowledge of the distribution of humidity
fields lo desirable In.order to Improve meteorological ob-
servations. The structural field of absolute humidity,, which
is nothin else but the distribution of water-vapor pressures,
is expressed by a formula and differs from specific humidity
by a multiplication factor only. The structural field of speci-
fic humidlt7.follows the temperature pattern. Such relationA-
ships permit the construction of graphs.corresponding to ob-
servations made.by various staVions in different latitudes over
a long period of time. The published graphs,for spring (April)
and summer-(July) led to formulption of a linear low kpropor-
tional to saturating humidity), adequate even for very large
distancei ($W-800 km). However, the spread of values for
coaStal and continental stations-Is -quite notideable. Coinci-
dence of atrudtural temperature fiolds,, humidity and wind
.Card 1/2

36-71-11/16
'Structural Function of the Field of Absolute Humidity (Cont.)
components permits formulation of some principleEs of dynamic
meteorology. There are 3 figures, 4 tables and I USSR
reference.
AVAILABLE: Library of Congress
Card 2/2

forecasting wind fields and their associated meteorological elements.
-IDOkl-" SM 112 no.l.-49-32 Ja 137. (MLRL 10:2)
1.Predstavieno akademikom A.L.Dorodnitsynym.
(Winds)

YvD~IVIAI,77
20-5-37/48
AUTHORS- Yud in ff. I.
WITLEi Nature of Stkiated and Ptygmatic Textures of Hyperbasites
of the Borus Mountain Ridge (0 prirode poloschatykh i ptiGmatito-
vykh tekstur giperbazitov khr.Borus)
PERIODICALi Doklady AN SSSR, 1957, Vol- 116, Ur 5, Pp. 851 - 854 (USSR)
ABSTRACTs In 1955 the author found in the Borus chain (West Sayan) fresh
hyperbasites with extended striated structure which were scarcely
serpentized. These textures are morphologically and genetically
very similar to the pseudo-ptygmatic textures of the granitized
rocks and to the mygmaLtites (reference 4). As far as it is knovin,
similar formations in ultra-ba8ic rocks were never found. 2 types
of striated textures were observeds 1.) the first type is charac-
terized microscopically by the occurrence of a parallel system of
small Plivine veins in a pyroxenite to a great extent transformed
into talc (figpre 1). These pyroxenite atriae arc ash-Grey and
broadest (4 - 10 cm)- Olivine forme striao of a breadth of from
0,5 to 4 cm and is quite fresh. The mineralogical composition under
the microscope is described. Tale seams the pyroxene relies and
separates thentfrom olivine. Sometimes pyroxene is directly replaced
Card 113 by olivine. Tremolite occurs seldom. 2.) The second~type of striat-

~0-5-37/48
Nature of Striated and Ptygmatic Textures of Hyperbasites ot, Lkitj Borus
Mountain Ridge
ed texture is formed alternatively by a) broad dark-,-reenish-grey
dunite striae and b) smaller dark Grey or bla~.~k pyroxene atriae.
Pyroxene is more weathering resistant than olivine, a fact which
makes the striae of the first stand out in relief like ribs. PtyG-
matic structures are formed where in fragments of massive, not
schictose dunite folded "veins" of the same.coarse crystalline
pyroxenite are visible which also forms the small plate-xenolitos
in dunite. The pyroxenites of the two species of texture are do-
scribed macro- and microscopically . The author vas convinced by
the macroscopical observations that in all cases where pyroxenites
and dunites occur together the first represent earlier formations
than the latter. All texture varieties differ only morphologically
from one another and are genetically products of the same process.
On the strength of the above-mentioned the author says that none
of the textures described here can be counted to the magmatoaenic
formations; furthermore-the author is of the opinion that the for-
mation of rocks of not uniform compositiont pyroxenite - dunite
is a result of metasomatic processes which were, expressed as at
least 2 stages; these stages were separated from each other in
time by a tectonic phase Only by this the occurrence of cataclasu
C,qrd 213 in pyrozenites and its,c;mp39te lack in the dunites can be explained.

20-5-37/48
Nature of Striated and Ptygmatic Textures of Hyperbasites of the Borus
~Mountain Ridge
The replacement of each of these stages of the metasomatosis was
markedly selective. There are 4 figures, and 5 reference3, of
which are Slavic.
ASSOCIATION: Tomsk.Polytechnical.Institute im.S.H. Kirov
(Tomskiy politekhnicheskJyinstitut im. S. M. Kirov,.)
PRESEPTEDs March 5, 1957, by D. S. Korzhinskiy, Academician
SUBMITTEDs March 2, 1957
AVAILABLEs Library of Uvii.-ress
Card 3/3
-3

AUTHOR: None Given so-il 5o-58-6-22/24
TITLE: -Traneactiona of the Scientific Research Institutes of the
'OR. ometeorologic" Service in 1957 (Truk, nauchno-iseledo-
ydr
vatellskikh uchrezhdeniy Gidrometeosluzhby za 1957 c.)
Continuation (Prodolzhenlye)
PERIODICAL: lleteorologiya i gidroloeiyat 1958, 11ir 6, pp. 61 63 (USSR)
ABSTRACT:- TraDp ntin-nn of the Geopknical Main Observator imeni A. I.
Y.
---7-oYeY1-.oV ~Trudy Glavnoy geofizicheskoy observatorii im. A. I.
VoZreyhova Periodical Nr 67. Research problems of clouds of
mighty convection and of the zones of thunde~rstorm activity.
Editor: V. V. Bazilevich, 153 Pagest 11 articles.
Perioaicai Nr 66. Broblems of actinometry and atmos2heric
qgtics.- Editom: K. S.-Shifrin and V. L. Gayevskiy, 2oB pages,
Is articles*
Periodical TIr 62. Probloms of the physics of the ground-near
layer-of the atmosphere. Editor: D. L. Laykhtman, 107 pages,
16 articlea.
Periodical Nr 7o. P_"oblems-of general climatology. Editor:
Card 1/3 0. A. Drozdov, 135 pageat 6 articlest

SOV/ 50-58-6-22/24
Tra=acti6ns,of the Scientific Research Institutes of the "Hydroineteorol6gic"
Service in 1957- Continuation
Periodical 11r_71 Problems of the numerical forecast and of ~112~
climate theory. Editor: 236 pages, 16 articles.
Periodical Nr 72.Froblems 5-1-a-tUffo-spheric physics. Editor:
A, P. Chuvayov) 151 pages, 13 articles.
Periodical Nr 7,~. Atmospheric physics. Editor: V. V. Bazile-
vi7n,Tri, 132 pagor., 11 articles.
eriodical TIr 74 is not given).
Periodical Nr 75. Glazed frost and hoar-frost. Editor: 0. A.
Drozdov, 91 pages, 4 articles.
Iransactig :.. of the State Udrological Institute (Trudy Cosudarat-
vennogo gidrologichoskogo instituta)
Periodical Nr ~9* Experimental investigation of the elements 1.4
of the rater balance in Valday..Editors: A. R. Konstantinov
and-'I-.--Vi-Eupriyanovt---224-pages-f -6--articles,_ - in
i_~eriodical Nr 6o. Problems of the hydrology of swamps. Editor:
K. Yo. Ivanov, 1o8 pates, 6 articles.
Periodical Tir 61, Problems of.the flow formation and the moth-
ods for its calculation. Editor: D. L. Sokolovakiy, 3o6 pagesp
Card 2/3 11 articles.

-4
SOV150-58-6-2214
Trawactionx of the, Scientific Reaear~h Institutes of thie
'Service --in -1957-- Continuatiori:
-ometry. Editor: A. X.
Periodical Nr U. Problems of hydr
Ploskuryakov, IoB pagea2 6 artic'sq.
(Periodical'.Nr 63 is not mentiorzed).
Periodical Nr 64. P4-pbleme of the construction of hydrologi-
cal apparatusa Editor: X. D. Zav'Yalovq 56 Pages, 6 articles.
(Periodical Nr 65 is not mentioned).
Periodical Tr 660 Researnh problems of la%es and reservoirs.
Editor: A. P. Duiokanitskiyv 140 pages, 5 artiel3a.
Sclientificreports--.USSR 2. Meteorology, 3. Hydrology
Card 3/3

SOV/2547
PME I BOOX -WLOITATiom
Le"7a
~oprcsy4iusmichezkvy meteorologli (Problems -in Dynamic fulete6roloa)
Leningrad,,~Gidrometeoizdat. 1959. 91 pe (Series: Its Trudy, vyp. 81)
-~.:.--.Errats s1t]~-in~erteds -1.,200 -coplep yrintede
-8yonsoring Agency: G1avnqye.uprav1eniye gLdrmeteorologicbeskoy oluz4by
pri Sovete Ministrov SSSR9-
Ea. (Title page): M&II, Yuditp- Doctor of Pbyzical and Mathematical Sciences
and M.Ye. bhvet~s,, Doctor of Physical and Mathematics" Sciences;-.Ed.
(.:In-s'ide:boolc).i--LiP.,:_Zhdanova,* Te6A Ed*.- O.G. Vladimirov.
rURFOSE: This issue of the Geapbysical 7-ustitute's- Transactions is intended for
scieiiti:Uq -workera and.L BPOCJ&U8tB. In dynamic-and,synoptic,neteorology.
COVMAG~; This collection of articles tre ats prob).ems in dynamic meteorology.
for -the-nost Vart,, disews cmputation methods of forecasting
meteoroloaic:,elementst ..Close2y relsted, to this is a study airned at deteniining
Card 1/4

3(7)

110 R
A
UT
ludin 11% 1.
TITLE: The International Symposium on Atmospheric Diffusion and
Contamination of the Air (Mezhdunarodnyy simpozium po
--,aimoaf erno,r- dif fuzii i--zagryazneni,.vu--vozdtikh,,~)
PERIODICAL: Meteorologiya i gidrologiya, 191`9~ Nr 1, pp 67-69 (TJSSR)
ABSTRACT: 'The author reports on the meeting hold in Oxford on August
24-299 1958- The Soviet delegation included. A. M. Ob-,ikhov
(Corresponding Member, ASUSSR, and Head of the delegation)
and the Professors A. S. Monin and it. I. Yudin. The Soviet
lectures were: A. S. Monin: A general survey of the
investigations on the theory of atmospheric diffusion.
A. M. Obu-%Aov.- The description of turbulence in Lagrange's
(Lagranzb)variables. 14.1. Yud'Ln: The diffusion of heavy
particles. A. S. filoniw The spreading of smoke in the ground
Inyer of tho ntmosphere.
Card 1/1

S"V/5, 0-5 9- 2- 14/25
'AUTHOR;. -Yudin, 14. 1.
TITLB:~ On the Development of Physical Foundations for Numerical
Short-term Forec~asts (0 putyakh razvitiya fizicheskikh oBnov
chislennogo kratkos .rochnogo prognoza)
PERIODICAL: Meteorologiya,i gidrolcgiya, 1959, Nr 20 PP 46 51 (USSIZ)
'ABSTRACT: The present stage of investigations in the field of dynamic
meteorology is characterized by efforts to solve the problem
of.numerical weather forecasts. The article under review
raises a number of basic outstanding questions and adds
some reflections on possible ways of tackling the problem.
The method most thoroughly developed and tested is that of
forecasting the geopotential on a medium altitude. However,
the important question of the range of influence of the
eddy-advection on the changes in the geopotential has so far
remained unsolved. In s more detailed consideration of the
.
InteLrral equation for the continuity (Ref 6) Poisson's equation
-,--
is-roplaced-by the-Helmholtz equation-(Bee formula (1)). it
Card 1/4 is shown that on account of the very small value representod,

On the Develoment of Physical Foundationa for Numerical
-Short-term Forecasts
by the correctIve term the two oquations must be practically
equivalent, which means that in the case of great distances
(r> 2.5. -~O km)'the eddy advect"Lon does not affect the
geopotential.1zhanges at,the point in question. This is actually
the tmospher-29 insofar as the ec1dy advection
-OLase in the a
on the isobaric area ohlanges,its mathematical signs a number
of times. It ~s shown that the contributions of areas with
positive and negativa eddy adveotions compensate each other
over great distances (interference effect) and that geo-
potential changes practically depend on the character of the
pressure distribution in the vicinity of the point in question.
This concept is confirmed by synoptic experience. At the same
time, however, the considerations quoted in this article
show that the results oT t:alculations may be distorted con-
sideratly (as a consequence of the gradual convergency of the
ntegTal if art4ficial boundaries are given even at a
great di Stanc 0 froM the point at which the geopotential
chanL-,e is to be- determined. Other possible ways viere pointed
>ut 'by other authors. It was also said in this connection
Card 2A that in the practical it-leating of "barocline"models" the fore-

On the Development of Physical Foun .dations for Nunerical SOV/5o-59-2-14/25
Short-term POTaCaStB
cast on the medium.altitude was not any better than in the
case of the ."barotropio model", In vievy of the reflections
voiced in this articlo it was decided not to use the
nearest points in the tr.Langular network (r % 330 km) but
those 6n the followin g circular circumference (r ?Qj 570 kin)
when drafting a forecast pattern for a model with two alti-
tudes (500 mb and 850 mb) at the Glavnaya geofizicheskaya
observatoriya (Main Geophysical Observatory) in the cal-
culation of the Laplacian of the geopotential at point 0.
The results for 1957 are given. Mention is made of the
various suggestions for the clarification of the physical
oontents of the theory of non-atationary processes in the
atmosphere. In this connection the method, suggested by
the author in the paper (Ref 11)t, for forecasting the wind
fields temperatureq and vertical currents is given. This
method is then studied from the angle of an oxact considera-
tion of the ouantities not dependent on the non-geostrophic
behaviour of the "ind. A number of outstanding questions
'Card 3/4 raif3ed in the application of the theory of these processes

on the Development, of Physical 'Foundations for Numerical S-U%r/5o-55-2-14/295
Short-tern Forecasts
to numerical forecasting are mentioned. The nain short- ..4
coming of tIlL application tests of tile nullarival fore-Onsting
method carried out so far has been the fact that Vie
initial matprial is -incommensurable. Moreover, a detailed
analysis of the results would be also required. There are
2 fi(raro97 1 table, and 16 rpforonoos, 11 of which are Soviet.
Card 4/4

1'311, arr.
i pal -.0 14!1; - IV
I I fil a
13
A Fivam-C .1 .21 3 -3 t-la
tit Allia -1l2 0-.8 ji-a 11;, ev
JAR a- I
Ila
Vj H 10 1 t 211-1 -*
.3,1131SIHM 4 4 IV
-Z
WCA"R . I p
!Ral .1.5
!3aa
10

'2. 9CC-C 67175
S1050160100010210011016
AUTHORS: Zavarinat 'A. Votjud1n) 146 It B000005
TITLE:_ Accurate Definition and Use of the Richardson Number for the
Identification of the Bump Zones~of Aircraft
PERIODICALS Mateorologiya i gidrologiyag 1960, Nr 2, Pp 3-10 (USSR)
.ABSTRACTs A physical-interpretation of the Richardson number is given
firstj and it is pointed out that in recent years it has been
widely used for,forecasting the bump zones of aircraft
(Refs 6D79,0). It Ri is less than unity, it may be regarded ae an
indicator for the level of turbulent energy (Ref 10). If it is
assumed ths-t the aircraft bump occurs at a very highly developed
turbulencep a Ri number considerably less than unity must be
the necessary condition for the origin of"vturbulenoo. In cal-
culating Ri in zones of increased turbulence causing thG bump,
some authors obtained Ri < I (Refs 12,14) and others Ri > I
(Refs 2,8). The present paper has the purpose of clarifying this
apparent contradiction. The causes of this contradiction are
as folloves 1) In a number of cases, the Richardson niunber is
not determined for the atmospheric layers where the aircraft
,card 113_ bump was observed. 2) In calculating Ri by aerological data;

67175
Accurate Definition and: Use ofItheRiebardson 3/050/60/000/02/001/016
Number for the Identification of the Bump B007/BO05
Zones of Aircraft
the derivatives in formula (2) for the energy transformation
are replaced by finite differences. Herey the authors average
these. differences by layers of different thickness - from some
hundreds of motors up to somo kilometers. Formula (11) is de-
rived. It expresses the relation between the Ri number and the
averaging thickness L. This formula shows that it is possible
to obtain Ri 1 and Ri. > 1 for the same turbulent state of the
atmosphere. Ri 4,1 is obtained In the case of a small averaging
obtained at -an averaging scale exceeding a
certain -value naximum--sealo---,6f-tiirbulence)*--3) In---,_
calculating the:Richardson numberst an important-source of
turbulent energy - heat of condensation - has not been con-
sidered up to date. In investigating the cloud layers, it is
necessary to renounce the adiabatic course of processes, and
introeLuce the moist-adiabatic lapse rate t-M instead of the
dry-adiabatio lapse rate rd. These 3 points should be co~-
sidered in the calculations. Thus, the authors attained a high
probability factor in determining the aircraft bump zone. The
Card 2/3 evaluation was carried out by = ans of the probability coef-

67175
'Accurate Definition and Use of the Richardson S1059160100010210011016
Number for the Identification of the ~Bump Zones I3007/BO05
of Aircraft
ficient q'suggested by A, Mi, Obuk-hov (Ref 5): Formula (14).
Figure I shows a diagraza which was drawn on the basis of air-
craft- and radio-balloon observations made in Minsk for 2 years
(in April).It shows thatthe Richardson number can be used
to determine the possibility of bump develop,,.aent. It is pointed
out that Ri is mainly used to determine the turbulent state of
the atmosphere. The idea that a bump only develops under the
-
lave motions on
influence ofturbulence~is not quite exact. The I
the ihterface my also be the cause of the bump. There are
I figure and 15 references, 11 of which are Soviet.
card 3/3

TUDIN
ical short-range forem'OUDC on a Physicall
DevelopmoUt Of U=r -1:24-26 1600 (MRA 13:8)
baBis. Fek;Prcbl-M0t9Or- no.
(Weather forerast.ing)
001,
, 01

S/050J66/600/067/003/004/XX
B012/BO63
AUTHOR: Yudin, M., I.
TITLE: Synoptic Material for the Testing of Numerical Forecasting
PERIODICAL: Met.eorologiya i gidrologiya~ 1960, No. 7, pp. 22 25
TEXT: In order to determine the advantages and disadvantages of various
methods of numerical forecastihg,:the following recommendations were
made by the Vaesoyuznoye soveshebaniye po teorii izmeneniya davleniya
i protsessam taiklo- i antitaiklogeneza (All-Union Conference on the L/
Theory of Pressure Changes and on Processes of Cyclo- and Anticyclo-
genesis): Such methods should be compared on the basis of the same
material including the initial data. In order to prepare testing materi-
al, a team of expertB was established at the qektfiiya sinopticheskoy
meteorologii i aerologii Nauchno-tokhnicheakogo soveta GUGMS (Section
I_._o_T__Synoptio Meteorology and Aerology of the Scientific and Technical
Council 6f__GVGMS)._ This -te6m In3luded--the-following scientists:
A. M. Obukh~6v, Corresponding Member of the AS USSR, the Doctors of
Card IA

for the Testing of Numerical 8/05oj6o 000/007/003/004/XX
a t ,~g _Xe_tEd-d#-----
For(
Sciences I V But A. F Dxubyuk' A. S. Zverev,~:B. D. enski,
U sp y
M. 1. Yudin, Cota-Tr9man), the Candidates of Scien'ces Y Borjsenl_'Oy~
P. K. Dushkin$ S. A. Mashk2v
--gives--' e -propcoals- -made --by .1 hv and A. D. ChistyAkoy, The present paper
__t~k_teaz and approved by the above-mentioned
h 9 proposal -il _r
section. T e9 3 deal wii~ hamper onzahce of tests. Regarding
the comparison of various methodsp the team restricted itself to the
smallest regiong i.e., the European part of the Soviet Union. Since
electronic computers were not always availablev three variants of tests
were worked out; 1) a variant comprising 16 cases; 2) a variant Oom-
prising 32 cases including the first 161 3) a yariant compTising 64
casesincluding the 32 cases of.the first and second variants. The fact.
that the least number of samples is sufficient for eliminating bad fore-
cas4.s was taken into account. The fundamental condition required that
even the smallest sample contains a sufficiently large numl-er of dif-
ferent synoptic processes based on the characteristics of baric forma-
tions on the earth surface and on the results of analyses of upper-air
maps. The sampling was carried out only on the strength of data of the
last few.years with special regard tothe International Geophysical
Year, All cases which could not be clearly interpreted were not
Card 2/4

Synoptic Material for the Testing of S/05 60/000/007/003/004/XX
numerical Forecasting Methods BOI 2Y33063
considered. The variability of syaoptio processes in one ijample was
checked according to data furnished by Q.. Ys. Vangengeym-and E. A.
isayev. Besides, the particular features of atmospheric processes oc-.
curring in 1957 and 1950 were studied by the raschetnyye gruppy Severo
Zap adnogo byuro pogody (Calculating Teams of the Northwest Weather
Bureau) and the Akademiya-in. A.:T..Hozhayakog,o (AcademX imeni
A. F. Mozhayakiy). The preliminary selection of the cases was carried.
out by N. I. Bel'skiy, Ye. P. Borisenkov, 1. V. lb,+.'A. S. Zverevk
E. A. Isayev, A. 1. Morozkin, L. S. Oriova, 4. D. Chia yakov, and
others. The da't_e`s__o?_t_fi_e__6_4 cages are Ii d in Table 1. The accuracy
of forecasts of the geopotential field is,determined from the relative
error, i.e., the ratio of the mean absolute errorp (Eff-Ij of forecast
to the mean absolute actual changep 1~_Hj, of the geopotential in. the
same area. In many cases, the root-mean-square errors of forecasts an
actual changes were calculated instead of the mean absolute values,
after which the ratio was determined. Experience has shown that the
relative errors determined by-the two iaethods:agree up to 0-02-0-05.
It is shown that the correlation factor cannot be regarded as the prin-
cipal characteristic for theaccuracy of,forecasts. For an exact study
Card 3/4
M rt.

Synoptic Material for the Testing.of
liumerical Forecasting Methods B012/BO63
of error sources it iso however, very useful to calculate the correla-
tion factor. It is noted that the mean,relative error of forecasts is
the proper characteristic for "Vhe accuTacy of forecasts of the absolut'v/
geopotential and the pressure on the sea-level, as well as for fore-
casts of the relative geopotential and air temperature. Since the ac...
-uracy--of -a-.forecaot- cannot -bA_ - exactly~ -determined from the mean rela...
tive error,-it is necessary to take into account the ratio of the roct.
mean-square error in the determination of the geostrophic wind to the
root-mean-square value of the wind. The team believes that the problem
concerning the beet cbaracter-isties for the accuracy of forecasts has
not been fully solved as yeti and, thereforeo it recommends further in.
vestigations. In particular, it recommends the exchange of testing
material among tb; organizations concerned. There is 44 tabled
Card 4/4

(Atmospheric preamra)
Mectronic calculating machines)

IMIN 14 1 Acktor fiz.-wtatc =.a pprof.p red*; VW
OVAj Tu.V, p rod*;
BRMIIVA~ H,.I,v tekbno red,
[Materiaia of the cc6ferezica of thD Coardibating Cmnivalon on
Num6rlbal Forecast Methods) Haterialy soveshchaniia. Pod-red.
M.I.IUdina. Ieningradt Gidrometeor. izd-vo, 1961.1 133 N
M351A 14:8)
Russ-ia(1923- U.S.S*R,) "KoDrdinatsionn*a konissiya po
chislennyn natodan prOgnoza-0
(meteorology)

4U66
-3/169/62/000/009/080/120
~-000 J, D228/D307
AUTHOR:
TITLE: Corrblations of the elements of large-scale atmosphe-
ric movements and certain forecasting consequences
Referativnyy zhurnalg Geofizikaj no. 9, 1962, 34-35,
abstract 9B2,06 (1~ collection: Materialy Sovbshchaniya
Koordinats. komis. po~chial,'metodam prognoza, gidro-
meteoizdatq 19619 5-24)
~TEXT: 1. A. Kibel' (1940) was the first to..eistimate the items in
atmospheric dynamics equations* For this purpose-he applied scale
-..analysisi verging on methods of the similhrity theory. This ana-
not take into account changes in the mdteorologic ele-
:.ments~ which determine the serial order of the equations' terms.
,,In a number of cases, however, the characteristic significance of
-h meteorologic element's derivative is governed by its systematic
~change in space and is almost independent of the scale of movement
,_,when.the latter varies widely* In this case the similarity theory's
Card 1/4.

__62/000/009/080/120
correlations of the ... ~D226/D,)
.1ormal application for determinin&the significance of various
items in-the thermodynamic equation system in order to forecas t
~lmeteorologic elements,in the atmosphere is incorrect and can lead
-..to imprecise deductions. The.allowance. for-systematic changes in
.the meteorologic elements isq from this viewpoint, substantial
~enough. Since t, e scale of movement concept is quite'definite only
h
for "one-scale'.' movements, its extension to the case-of actual mul-
itiscale atmospheric movements involves theelimination'from their
total'aggregate of a narrow spectral.section -- i.e. of the spectral
analysis of velocity, density, and pressure fielde.'If no such ana-
is madeq-the concept.of the scale of movement, which,is most
fundamental in the theory of similarityt aoes not appear to be
quite clear, and the conclusions resulting from considerations of
he similarity are deprived of their definiteness. The most expe-
:dient way of investigating the set problem is to analyze spectrally
'the meteorologic fields and substitute the corresponding expres-
sions in the atmospheric dynamics equations. For this it is'sug-
~gested that a linearized system of equations should be examined in
..order to'avoid cumbersome nonlinear equations. Th-is linearization
Card 2/4

8/169/62/000/009/080/120
CorrelatAone of the ... D228/ 307
is made with respect to the main movement, which for large-scale
atmospheric processes may be taken as a stationary zonal motion
caused by the temperature's ayBtematic variation with latitude.
Here the characteristic values of the items of the linearized equa-
tion system are close to those of the corresponding terms of the
original nonlinear equation system. The application of scale ana-
lysis to the linearized system of thermohydrodynamics equations
and the spectral analysis of the~ineteorologic fields result in the
~.Sollowing new deduction: however small the divergence of the hori-
amount of movement in the atmosphereo,it is, nevertheless,
one of the factors determining the.character of atmospheric pro-
ceases. It henap, follows that models of the atmerBpheret in which
horizontal divergence is dieregarded,through6ut the atmosphere LA~
(.the-so-called "quasisolenoidal" atmospheric models), cannot 6or-
reflect large-scale movements ando in particularg the Bpec-
Aram's global section. Thus, for examplef disregarding horizontal
divergence when forecasting at,the.atmosphere's average level re-
sults in seriously exaggerated velocities of global wave propaga-
tiong as was discovered, too, in operative forecasting practice in
Card 3/4

6/169/62/000/009/080/120
Correlations of the D228/D307
the USA. It is also-sh.own that, of the amplitudes and phases of
pressure waves vary little with altitude in a certain spectral area,
...the conditions of existence of slow glo-bal-movements are disturbed-;-
This, in its turn,' involves the appearance of rapid waves and the
abrupt reorganization of meteorologic fields to a state where they
onform to the*criteria of the existence of slow global
definitely c
movements. Such a:~conclusion is oonfirmed in the empirical rule
:.(established by T. A. Duletova ' 1956)., which indicatos that in a
of cases "rectifications of,the axes" of baric-formations
are observed over~much of the northem''hemisphere.b6fore the in-
tense.reorganizat'ion of meteorologiatfields and the evolution~of
new cycles, CAbstraCter's note,:, Gomplete translation-1-
Card 4/4
qpl,

-tit

AC&SSION NR: AT4016871 8/2531/63/000/143/0036/0050
Solution of oquation's-oHyiiamieB of the stmospliere using patterng of structi4ro of
incteorological fields for purposes, of short-range weather forecasting
SOURCE: Leningrad. Glavnaya geofizicbes1mya observatoriya. Trudv*, no. 143, 1963,
Voprosy* chislennogo prognoza I strukrura meteorologicheskikh poley (Problems in
-numerical forecasting and structure of meteorological fields , 36-5,0
TOPIC TAGS: meteorology, atmospheric temperature field, atmospheric pressure field,
dynamic neteorolc~gy, Bhort-range weather forecasting, weather forecasting, meteoro-
logical field, numerical forecasting, ageostrophie model, wind, geostrophic wind
ABSTRACT: Due to the development of work ~on the use of an ageostrophic model in
numerical weather forecasting It Is deemed-desirable to publish the original work on this
3fiethod; the work was done in 1951-1952. The author derives equations for the model and
presents a solution of the three-dimensional problem of changes of meteorological elements
by, the ray 3nethod. The manuscript, twelve years old, has not been revised and there is
no indication of whether individual formulas and conclusions -remain valid. The first part
of the paper gives the derivation of equations malting it possible to determine deflectiona of
1/2

ACCESS101; IM: AT4016871
the -wind from the geoBtrophic wind in the case of large-scale movements when the spatial
distribution of pressure and temperature is known. The formulas cited can be used for
determining the direction and movement of a pressure center relative to air particles.
Similar formulas can be derived for the.rates of movement of troughs, ridges and other
elements of the pressure and thermal field. The key formula cited can be adapted to many
problems in forecasting; solution of the equation Is given. Orig. art. has: 42 equations
and. 2 figures.
ASSOCIATION: Glavnayu geoftiche9kaya observatorlya (Main Geophysical Ob6orvatory)
SUBMITTED: 00 DATE ACQ: 20Feb64 tNCI, 00
-SUB CODE: AS NO ILEF SOV.- 005 OTHER: 000
WOW,
2/2
Card
5F
OF

OBU"OV~ A.M.., red. j YUDIN$ 14.-1.,.-doktor fis.-matem. nauk, red.;
BRAYHINA~ H.I., tekhn. red.
[Transactions of the All-Uni on Scientifle NgIteorological
Iij,
Conference] Trudy Vses#-uznogo nauchnogo mateorologicheekogo
soveshchanila, -1961. Leningrad, Gidroneteolodat. Vol.2.
(Dynamic meteorology] Dinamicheskate. raeteor-bloglia. Pod Md.
AX.Obukhova i H.I.IUdina. 1963. 241 p. (14IRA 16:lj
1, Vs:)Boyuznoye nauchnoye meteorologichaskcye soveshchaniye,
1961. 2, Chlen-korrespondent All SSSR (for Obukhov). 3. Glav-
naya geofizicheakaya,observatoriya (for Yudin).
(Meteorology)

ILL
a r
o o
rn,
:w

I BOOK EXPLOITATION SOV/6482
PHASE
14-11ftil Isaakovich
NOVyye Matody I problemy krAtkosroahnc)SO Prognoza pogody (Nelf Methods
and Problems In ShOrt-Range Weather Forecasting) Leningrad,
Gidroxeteolzdat, 1963. 403 po Errata slip inserted, 3000
-coples printed.
Resp. Ed.: S,I,Tjtov.*, Ed,:. 7U*V,-Vlasov&;' Telch. Ed. t N. 1.
Brnvnina,
MPOSE.- The book Is Intended-for-meteorologists engaged In
asting, as well
theoretical researah or praotleal weather forec
as for advanced students in meteorology emd specialists In related
brruncheis of science, Emphasis is on.the techniques of modern
dynamte meteorology,
1des. a generall review of the Y)resent
COVERAGE., Thts monopaph prov
stetus of studien the field of',short-range numerIcal ~eathar
Ctxd, 1/~
~~l 77
M M M
MEN

New 'Methode and Problema (0013tj sov/6482
forecasttn% especially on the rapid development of forecasting
Methods and their routine use &- Emphasis Is placed on the formula-
tion of.problems and the logical and physical basis for the ideas
u-nderlying the theory of large-scale 'atiaospheric movements and
methods for the-2x prediction. The statistical properties of
atmospheric movementB, which must be known for the evaluation of
various forecasting models: also are eMhasized. Sources of erzo-rs
in numerical- forecasting and means for elirdnating them are di13-
cussed in detail. A special chapter deals with the -- objectlv-c,*
lysis of metoorolo --of - t
n a -6ieotioonic compu ers.
a
X\
ce.rtain -have. not been discussed- in------
--the- author mentlona
that thr~i6, major -special--prob ems
should be -,-tieated __separate -booke4t-7, 111 long-range hydrodynaimic
)---fititnerical -forecasting of meteorological elements in
oreca
the boundary layer of the atmosphere.. and (3) statistical methods p
-ther
of forecasting. The author Lks A,M,Obu1dhov., S,A.Mashkovich.,
S.I.Titov; A.S.Monllpp AJI.Yaslomy L.StGandin., A,S,Dabov., K.V.
r-yatygina.. and DLYe,Shvets, There are 277 references; 1-89 of which
are Soviet,
Card 2/6
7

YUDINP H.I.
A.A. FrIdnan and his works In the field of meteorology. lz,7-.
All SSSR. Ser. geofiz. no.7.-1086-1099 JI 1631. (MM 16.-8)
,(Fridman,, Aleksandr Aleksandrovich., 188-3-1925)