SCIENTIFIC ABSTRACT GUNINA, A.I. - GUNKOV, V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000617410001-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 20, 2001
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

AEGIN

SEGI14

k fwlw A~Vow ~l it
q7kr
Q6UklitAN) lptw 4

W W-W W W w- JFD--W-~-w 9 6-4-4F476-16-4-fi-0-0 o e 0 9 a o 0 9 0 a 0 0
1
0 L 1
4 4 111) ut W 11 k
1. 6 b. .
14"Issinissm of auddoul SON w ffillowommm T"
L*d
i an
i A
1
Gu
j
*A
J
1
A
t
.
.
v
l
.
.
ag.
t
ikydMgva SUj"q p*JM
q
*
6
N
W
3
4
.
o.
t4IMA-4. i 1
06$A
,
,
A,
b 1
:1 thurt The lethill dLwo of N&IS do" die It a
lym
00 a. NoNO, k8- of bodf OL pt
Illif list
slow I tie Wlt$dUud jactim
so, an svwcw (nn
0
3
I
hi
tv
rtwop
1
citfiv), but as an olikhosing alictil.
Sillith
see
00 zoo
00 400
00 ce 0
00

00 X, so
as*
.00
400
lee

s, too
!see

0 0 0 0 0 0 0 0 0 0.0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0

0 0 o1 dio"
10*00*66066*0900 37 4 Mo WO -0 0 0 0 * 0
0 W-0 old 4-
I I I . 1 6 1 1 - , 1, 11 it ti 1. 11 r: it u Z. 1. n :4 : n 1. x It v It 1. 11 V Am .1 Q .1
"r A# is a Pu U
tv
00
-00
00
00
09
to "is Is OXW"d @k. A, 1. GUIMW 0YOW $;"I
ijo-t. iw. 14. No. 1. 1 1w:20(forlY, -11, 0111161"1 lilt. it 1,
(tie
Tlw misit. 'W'It (if ally) 1111111 Lw 1,
prr lie 44 41111jert. illInk"wd III
T11W "lilt IN tfl
IfAl P
god,
00
LA 4114ILLURSICAL LiTtRATURC C1,01111FICATICk
'14. lit
Joe
An L % a Ow 0 1 IV 81 5 Ala 111 3 1 IF
troll, coal stit MIN 11111111 HOI KLO A

-
-
W
W 0 W

t 01 u, 11 13
It A); 11 It Z) b .4 1? m N
m v
I.P.4 .1 1;. Pro
L L 1. 6 11 L As f- 0' t. A I V VIM A I I #A e0 ~L W It t
, I

~Acmstq Has
A-11 Go"i"a-
Aij oh,tf. p .5. tit""

00 lies on its interaetion with r"pirstory enzymc% it not sup-
Ported by the jWC.~tnt data. During prulongrd iistrave.
Stirissin*tion of Nasinto dop (0.2 lux.68. Nxiv wt, in
1 """' the"llm'Ittle WANOW) ut% dIABIV t10IwWtV*4I
ne a
I" lIW 0 "Ille"t -`( 'he Vrl""" Ali Inivo thm 4.1 1 7
06" oij./lig. vmuw,, tile lip rjW jjWijjX tit ult-Iv,IwIl (it.
000 1 III-Alivo rate rather than hytxbxla. That all im wa,vil ..I
l
c
itiatio" rate con lead to higher 0 contents of thr venum
l'I'A"11i'shownhy theflart that there i~ a f1wi,

49 The Wnm. 0 Content with A ti,* ill dmilmi,-.41 tmir a- x
0
:livasuretl by the niefflost of Rein. watt that thr Itilretion
-14) vAt. of imirmallne results in a rie ill t1jr () t.coirnt .0 sa
as of vrnims. Illooll. Willimum roe

00
S00

!"oe
A. I i C, coot
wee
U T1 A-
It
iv I, m K a it a n it ra it all --WT
law n I am 4,141,

0
0
0
, : 0 0
: : 0 ~~.
0 :!
04
0 0 0 0 ei~

11MI't
tie as 1?1 "a 430 0.: Ice
A 111 -L -4 A OtA M JM.,W.-0,4 A p_!- & o w I I
A~ _7 ..t. total
Ih6usy III Atulo 111"41111011 iulft;l .1161 .0
:".P,.I*. :' I. -
Olviii. A. 1, G"I'M-4 a ... i % 4 / '.q 1;
it 71 ItIVO; d. C I, P,
INS 1-14"Miltot 1, 1k.'1
60
lit'N.
sk.dis 411" 1, A 1"
0: Allihm"Ittv 14 A I... 1. - M I I ...
1 00
-Im 1-111 1111,14s 11, 00
o pjv-ion 14 qt~
: Mm"I 'mw .11.. 1 1, 1,%
ji- V'j.
Visit illm Im-6-1 lit, lit" " "" - - '""' "" 1. :00
I,
coo
0 go
lop o 7 lee
0
3o0
log
':06
00
Moo
CLAWFKATMM 12- is
it
141,1.j 441
u vt 0 43 L% r 'i 'Jo n i I iia
p it K K a m w pt it it it a KL tn it a 8
"not
0 o 0 o 0 0 0 0 0 0 0 O~

Hydrogen sulfld~,pu?s In hECR-9
. 4 1 -,food altvaki
sulfur baths. A. 1. Gun nq and V. A. Tlkhonfavo (I.
Stalin Inst.. Sochi). I Fhixmkol. i roksO61. 16, No. 0,
"1063)~Blood ffS was detected from the 3rd min.
after entering S baths contg. 290 mg-A, free and 400 mg./I.
totaIH?S. Blood llSrunged from 0.03 to 1.8-fA., and the
varying rates or absorption am significant as to mechanism
of 8 bath action. In the more dfl. baths, up to 150 mg-A..
9 oxidation Is last enough to keep free HtS out of the blood;
hence It hardly occurs In the usual 9 wattxs with 100-150
me-A. Exposure to 295 mg-A., 150 min. sit 36' u
to 0.21 -fA. In the blood, 15 min. at 3040.5* up to PO "IyIF
Julian, F. Smith -- -

OTVIN, I.A.; CAJNINA, A-I.: TIKIR)NRAVOV, V.A.
Mechanism of the physiological action of hydrogen sulfide
(Matsesta) water. Vop.kar.fisioter. 1. lech.fiz.kul't.
no.2:13-20 Ap-Je '55; 04LELA 8; 8)
1. Iz biokhimichaskoy laboratorii Ballneologiaheakogo 1nsti-
tata iment Stalins. i eksperimentallnoy laborateril Tsentrall-
nogo sanatorita iment Voronhilova (Sochi)
(MIKMM WATERS. of fects I
hydrogen a-alfide water, mechanism of physAol.
action)

ANDRIASYAN, G. K.; GLUINA, A. I.; MALKIN, I. I.
Thorapoutic use of hidmly concentrated KfttgOStIL water in skin diseases.
Vest. yen. I dorm. nO.';'-33-36 S-0 t55,. (MIR& 9:1)
1. 1z Goaudarstvennogo nauchno-isoledovatellskogo ballneologichookago
institute. imeni I. V. Stalina, Kintsterstva zdravookhraneniya SSSR
(dir. N. P. Vladimirov) i sanatoriya Moskva (glavnyy vrach A. A. Syrtsova)
(SKIN. diseases'*
balneotner.. KatBesta waters in high concentration)
(BAOROLOGT, in various diseases
skin dis., Matsesta wator in high concentration)

GUNINA, A. I.
Conversion of hydrogen sulfide H2S35 in the organism following
subcutaneous administration [with summary in English] Biul.
@kBp. biol. i med. 43 no.2:48-51 F 157 (MLRA 10:5)
1. Iz biokhimicheskay laboratorii (zaveduyushchiy-starshiy nauchnyy
sotrudnik A.I. Gunina, nauchnyy rukovoditell-professor I.A.
Oyvin) SochinBkogo instituta revmatizma (direktor-dotsent N.P.
Vladimirov). Predstavlena deystvitelInym chlenom ANN SSSR S.V.
Anichkovym.
(SULFIDES. metabolism,
hydrogen sulfide, conversion in rats after subeutaneoup
admin.) (Rua)

/V
"Transformation Within an Orgmiss of Rydrogen Sulfide (HO35)
Introduced Into the Blood," by A. I. Gunina, Sochi Institute of
Rhel-tism, imeni I. V. Stalin., Doai4_aa_aemii Nauk SSSR, Vol
112, No 5, 1957, PP 9M-904
Hydrogen sulfide is formed in the digestive tract from several sulfur.
containing amino acids and rapidly absorbed into the blood stream. A num-
ber of investigators have shown that the organism is freed of hydrogen
sulfide by the following methods: release from the lungs in unchanged
form, and oxidation in the blood with subsequent excretion of the trans-
formed products in the urine.
For a more detailed explanation of the above problems, the author set
up experiments using Na2S35. In studying the distribution of s35 in the
organs one hour after the administration of Na2s35, it was found that the
reatest specific activity was in the kidneys and secondarily in the lungs.
U')
T

GUNINA, A. I.
Changes in blood carboanhydrase activity in persons taking hydrogen
sulfide. Top.kur.fizioter. i lech.fiz.kul't. 2) no.1:8-11 158. ' .
(KIRA
11:3)
1. Iz biokhtmicheakoy laborstorii (zav. - starshly nauchnyy sotrudnik
A.I.Gunine) lisuchno-iseledovatellskogo bellneologicheekogo instituta
ineni I.V.Stalina v Sochi (dir. - dotsent N.P.Vladimiroy)
(MIIMML WATIMS, SULFUROUS--PHYSIOLOGICAL RMECT)
(CAMONIC ANHYDRASS)

GIORU, A.I.
.
35-hydrogen
su
Ifide in the
Study of the transformation of 8
body during hydrogen sulfide baths. Vop. kur., fizioter. i
lebb. fiz. kul't. 24 no. 4:328-332 Jl-Ag 159. (MIRA 13:8)
1. Iz biokhimicheskoy laboratorii (zav. A.I. Gunina, nauchnyy
rukovoditell - prof. I.A. Oyvin) Sochinskogo instituta
revmatizma im. I.V. Stalina (dir. - dotsent N.P. Vladimirov).
(HYDROGEN SULYIDE-PHYSIOLOGICAL EITECT)

Eff-ict. o'' hydrcgt~ri w: C'da Inha'atioa:3 on t~-e (.- ond' i t,~ -xied ref I nx
aCtivi Ly and carbohydrase of the L-dood in ctildren v~ t~ rheww-tic
fe,,rar. Vop. k0r. fj-~Iotnr. i lech. fiz. k-.Ll.lt. 28 no.3.255-259
Mlll~. 17:5)

U-iii-LI1.1 , 1, . ;-. .
t -t" ir, brc,!(-;iriir ca,~A.c..
,periment of the kolkho- "Krasrl:i kollelftivl-z i.
Znanie, 19"-~2. 31 T).

GUNINAY V.
Timr permits. Sov. shakht. 12 no.609 Je 163. (MIRA 16:9)
1. Zaveduyushchaya neshtatnvm otdelom Prokoplyevskago gorodskogo
komiteta profeisionallnogo soyuza rabochikh ugollnoy promyshlert-
nosti.
(Coal miners) (Prokoplyevsk region-Trade unions)

1.
I. Improvivi, thc cO't';t--'t,cti0n Of the c-pin-drx babbIrs. p. )9.
Vol. 5, No. 5. 1956.
L~,A
TECHATIOLWy
Sofia, Bulgzxiu
so: 2--st ~ rope--.n Acr!cssion, Vol . 6, No. 3 , March 19'.;'(j

GUGUS9VILI, P.V.; red. ; SARKISTAN, L.N., red.izd-va;
TODUA, A.R., tekhred.
[Sariculture in Georgia and Transcaucasia in the 19th and 20tb
centuries] Shelkovodatvo v Grazii i Zakavkazle v XIX-XI vv.
Tbilisi. Izd-vo Akad.nauk Gruzinskoi SSH, 1960. 105 P.
(MIRA 13:11)
(Georgia--Sericulture) (Transcaucasia-Sericulture)

KHASIA, B.A. [Khasia, Bekirbi Archilovich]; GUNIYA, A.L., red.; MACHABBLI,
M.G., red.izd-ve; DZHAPARIDZE, N.A.,'-m�=rec-
(Expanded production on tea-growing atate farms in Georgia]
Rasshirennos vosproizvodstvo v chainykh Bovkhozakh Grtizinskoi
SSR. Thiliai. Izd-vo Akad.nauk Gruzinskoi SM, 1959. 165 P.
(MUIA 13:3)
(Georgia-Tea)

GUNIIYA, A.L.; GMERELIME, S.P., red.; KHAS114A, B.A., red.;
`---SMX-ISYAIJ, L.U., red. izd-va; KuNDRATENKO, N.V., red.
izd-va; DZI[APARIDZE, N.A., tekhn. red.
[Replacement of the labor force in the industry of the
Georgian S.S.R.] Vosproizvodstvo rabochei sily v pronyshlen-
nosti. Gruzinskoi SSR. Tbilisi, Izd-vo Akad. nauk Gruzinskoi
SSR, 1961. 522 p. (MIRA 151:4)
(Georgia-labor supply)

GTJTTIYA, P.T.
- - -- - :~ 1~.
Work at Georgian hatcheries in raising chickens for meat production.
Ptitsevodstvo 9 no.6:22-23 Je 159. (MIRA 12:10)
1.Direktor Tbilisakoy inkubatorno-ptitsevodchaskoy stantaii.
(Georgia--Poultry)

----------
:111 'Is6t -b-E
'j'ej -v 611
-A.d.fl

4. .... ....... -ooL
. '**E
.9.Lt Ssu ms -fam 1-idi Hy
.... d.A. L -0

: -d . ...... I .-A- -IV d- N...-
.od..
9 . ....... d. -c) I . . ......... I.. It ..... A.H
-56L ...,d,U ... -% ...... J 'Lot
.4.56t. lb-E
-L-M C" IVE
(d .Adj lly A- . I I.. I 1-cst

_x *v"" ~d-d.. .1. --.N-
..... .. -A , ...Ad ..
III.d.91111" ...Ad . ......

Lt SS6,*,._ -d.9 .,UaA:) I
.... ....... I ..h-d.d,-. I..

3"' "'K To
L

1110C 191-61 fh.E
.7 d
A~d
;
16 W '!= dX) -9d-V HV -H) 'd-I _-(D ..H _...Id., '
t
L *-d . -.ZZI ;to, -. -T-9 11"t -ffn
.d-M --0 IA)( - v lot I
.9 v _9_ IF.,IV I A to *061 4-9
-I*cz loot .. .... d,.,. --
,9v6l d.*- "A' . .."'W ...."
'
"
...... i- 0 .
,
Am -.9v -r-E-1.9y WL
....... oll 'lot
.lb-E
:wor Iml
1._
d-dr- -9.L) ver lust
-956t -(-Ar-..d.X) I'l --- " 91:1 *061
o...... ...... .--d ..... dj
v....... _~..rd.o
. .frdAW d ... V..g -----r
....... q-, v9C t", cnl
H '06L -rc-f '-G qq 9c1 .. v6l
'IS'Z .5,61 R,E -vctM-3-s
So *ttta nyaq.m ?Z_A~-qp
nv .."g.)i -V .11 -6.d. 'r.,.. .%.jr2 .0,.Q.Z~r ..S.% 'COL
-c-z ls-E
-rp~ cgf
ZL Ml
on
j

GUIPM , ". U1.
27,003
PreINT-c-ld:31enle Tempattiry V Svohdnoy Atmonfere, 'A.'rudy (Gru,~. PoUtektin. in-'i' Im.
Kir 6va) Ifc. 18, 1%q, S. 3-8- Rezzyume Ila Gruz. Yaz.
F(': 11"E"TICTIS INC. 34

=~M, SO.
Role of humidityl, temperature, wA certain featm-se of atmospherld
airmIation processes in the formation and development of thunder-
ritormis. '11ruo Thil. TWKI no;2t68-77 15?. WRA nM
Mundorstorma)

I
I

AUTHOR: Khmaladze, G. N. 50-1-25/26
TITLE: The Scientlfi~ 8-essl6n of ThIlAsi Scientifl'c Fesearch
Institute for 1FyTF:)meteoro --Y.. 11 a Tc- 711M-y a
sessiya Tbilissko,-.) NIG1,11ty
PERIODICAL: Meteorologiya i Gidrologiya, 1955, Nr 1, pp. 66-67 (USSR)
ABSTRACT: In May 1957 this institute held its fourth scientific
session, where 16 lectures devoted to various branches
of the hydronneteorolo.~_rical science were held. Under the
conditionu of Transcaucasia the problem of the forecast
of thunderstorms is of great practical importance, thsre-
fore special attention was paid to the lecture by_q~a~
-9. U. on the method of forecasting thunderstorms under
the mountainous conditions of Transcaucasia and the
lecture by Shishkin, N. S. (Main Geophysical Observatory)
on the topic of the forecast of thunderstorm-processes
according to the method of layers. Papinashvili, K. I.,
Napetvaridze, Ye. A. and Lominadze, V. P. dealt with the
problems of the investigation and subdivision of the air-
and turbulence-currents above Transcaucasia.
Vorontsov, P. A. reported on some peculiarities of the
Card 1/2 temperature- and wind-conditions above the lake Sevan.

The Scientific Session of Thilisi Scientific PieaejLmh 50-1-25/26
Institute for Hydrometeorology. -
Kvaratskheliya, I. F., Tsutakiridze, A. Ya. and Kurdiani,
I. G. (State University Tbilissi) reported on the results
of their works in the field of the aeroclimatic
characteristic of thc free atmosphere, on the analytical
method of the treatment of observationc 7ith piInt balloons
and distribution of clouds in Georgid.
Chirakadze, G. I. and Gigineyshvili, V. M. expinined the
scheme of the radiation method of plotting the slipperiness
of ice in Transcaucasia and the characteristic of slush
and its distribution in Transcaucasia. Khmaladze, G. N.,
Tsomaya, V. Sh. and Poklepa, V. F. reported on the duration
of the vernal-aestival floods in the rivers of Trans-
caucasia and on the method of their calculation as well as
on the method of the determination of the water supplies
in the snow according to given records of snow routes.
Tsertsvadze, Sh. 1. held a lecture on the method of fore-
casting the main phenophases of grapes in Geortid,
Svanidze, V. F. - on the characteristic of-the agro-
meteorological conditions of the cultivation of potatoes,
various conditions of the cultivati- of Dotatoes, various
Card 2/2 terms for planting in the low grounds of valleys of EastGecrgia.
AVAILAME: Library of Congress
1. Weather forecasting 2. Meteorology

50)
AUTHQR: GUniya, 5. U, SOV/50-58-10-1/20
TITLE: The Pas3ing Over of iviountain Rantges by Air Currents
(Perev--vaniye vozdushnykh potokov cherez .-ornyye i.hrebty)
PERIODICAL: bleteorologiya i gidrologiya, 1958, Nr 10, PP 3-6 (USSR)
ABSTRACT: The atmospheric processes arising above the area of Transcaucasia
are a result of superposition of mainly two kinds of disb=bances
1) One process is formed as a consequence of the thermally irregular
basement area (pods tilayushchaya poverkhnost') owing to atmospheric
processes; 2) the other one is due to unevenneso of the earth'a
surface. The theory of I'lowing around hindrances by air currents
(Refs 3-7) and further investigations (Refs 1,8,9) indicate the
extraordinarily important role played by mountain ranges in the
formation of local dijturbances and in the appearance of vertical
components of the wind velocity. This facilitates the forwation
and development of clouds, thunderstorm processes and causes pre-
cipitations,. The question whether masses of air are able to pass
the Transcaucasian mountain ranges if the masses possess a higher
vertical extension than the hindrance itself, is most important to
the attendant phenomena of the latter weather processes. According
to various computations the author determined the current function
Card 112 ~(xqy). The equationo for the determination of Y in the middle leval

The Passing Over of Mountain Rantges by Air Currents 30 V/50- 558- 10- 1120
of the troposphere were solved for 40 places in the Caucasus region
under consideration of the influence exerted by mountain ranges,
For the calculations a high-speed computer of the Institut tochnoy
mekhaniki i vychislitelliloy tekhniki AN SSSR (Institute of Fine
Nechanics and Calculation Techniques of the AS USSR) was ased, On
the basis of the calculated vallues of the function q for the casos
u = 0 and v = 1 (the axis X lies along the mountain ran6e, the axis
Y lies vertically) as well as for the casesu = I and v = 0 the
lines of the current distribution on the middle level of the
troposphere over the mountain regiono of the Caucasus were drawn
(Figs 1,2)~ As may be seen from them the irregularities of the
earth's surfat.-e form a disturbance field of the main current which
is extended upwards up to 4 - 5 km. An important factor is here the
passing over of the ranges by these distu:rbed ourrents according to
conclusions drawn by former authors (Refs 3-6). These i2onclusions
are confirmed by the occurrence of storm centers over the slopes of
the Greater and Lesser Caucasus (Ref 2) and by :-onsiderable pre-
cipitations in this area. 1. A. K-ibell gave valuable adv---ce and in-
dications. S. L. Belousov assisted in the computations on the high-
Card 2/2 speed computer.-There are 2 figures and 9 Soviet references.

i'k 'V i
3(l) PIMSE f .1-;00K K~HMTATtorl 3011/5090
.Y L' iJ1'o":;'.! ~1 (~L-'-Jl ()'!. 1e. Ile n 1'~ I Y I nn (A h It,
Tbilisi.
Trudy, Vyp. (Transactions of the Tt)1116~1 ilydro K.-teorolalgrical Scientific Re-
scarch Institute, No. 10 Leningrad, GiJrnnw!tco1zJat, 197~0. 178 P. 1,500
copies printed.
Additional Sponsoring Agency: USSR. Soviet Ministrov, Glavnow upravleniye
gidrometeorologichookoy alnzhby.
Ed. (Title page): V. P. Lominadze; Ed. (Inside book): V. D. Pisarevskaya; Tech.
Ed.: N. V. Volkov.
PURPOSE; This book is intended for rat-, t-.eoi.o'Log1tta a,,.d 1,ydv,)1(.%g1sLs.
COMAGE: This is a collection of 3-2 articles on jet streams and turbulent
c-arrentsY the analysis of the affect of orography on changes in atmospheric
pressure., the characteristics of the temperature regime In the free atmos-
phere., the development of methods of forecasting storms, low cloud ceilings,
fogs, water discharges, spring floods and various other hydrometeorological
phenomena in the Transcaucasia area. Of particular interest are articles on
visibility conditions around Transcaucasian airports the aerosynoptic
Card 1/4

Transactions (Cont.)
SOV/5099
conditions causing air bumipiness iT1 the area. References accompany each
article.
TABIE OF CONTENTS:
Papinashvili, K. I. Distributic)n of Jet Streams in the Atmosphere Over
Transcaucasia 3
Guniya, S. U. Methods of Forecasting SLorms In Lhe Mountalnotis Regions
of-Trwwa-ucasia 18
Nozadze., R. I. The Problem of Evaluating the Effeet of Orography in
Forecastibg Atmospheric Pressure 38
Napetvaridze, Ye. A. Range of Horizontal Visibillty in Principal Air-
port Areas of Transcaucasia and the Caiwes of Its Diminution 54
Kepetvaridze, Ye. A. Forecasting Foga In PrincipEil Airport An-_,as In
Transcaucasia 71
Card 2/4

Transactions (Cont.)
BOV13099
Kvaratskheliya, I. F. Charactertsfloo )i' Lite Tei:irx~rature RegIme and Local
Atmospheric Circulation Over Sukfuuiti. 93
Lominadze, V. P., and Ye. A. Napetvarldze. Acrosynoptic Con~lltiona in
Turbulent Currents in the Atmosphere Which Cause Aircraft. Dumpiness on
the Sukhumi - Tbilisi - Yerevan Run 112
Chirakadze, G. 1. Map of Regional Glazing for Transcaucasia 124
Xbmaladze, G. 14. Method of Measuring and Computing the Discharge of
Vater In MountAin Rivers 153
Poklepax V. F. Establishing Annual Hy(J-rological Seasonal Boundaries for
Mountain Rivers 162
Tsomaya,, V. Sh. Methods of Forecasting Spring Floods in the Rivers of
Georgia on the Basis of Preceding Hydrometeorological. Factors 168
Teertsvadze, Sh. I.#N. P. Stolypin. Agroclimatic Characteristics for
the Cultivation of Corn in Transcaucasia 172
Card 3/4

_C!~M~IIIITA ~SULM____,
Air currents over obetaoloo. Trudy Tb,'l.]IIGMI no.5:11-15 159.
(mm 13:6)
(Caucasus--Winds)

S/169/61/000/010/0261/053
D2128/D30-11
AUTHOR: Guniya, S. U.
TITLE- Thunderstorm processes on the territory of Transcaucasia
PERIODICAL: Referativnyy zhurnal, Goofizika, no- 10P 1961, 31-32,
abstract 10B212 (Shromebi. Staliniris Ualzhelntsipo
pedago-iuri instituti, Tr. Stalinirsk. Cos. ped. in-t,
7, 1959, 13-29)
TEXT: The diversity of the Transcaucasian c-limate is chiefly caused
by the mountainous topoEraphy, geoGraphic latitude, and the proximity
of 'he Black and Caspian Seas. The Surariskiy and Arsianskiy Ranges, which
stretch perpendicularly to the direction of moist air Clow from the West,
have an especially great sianifioance. These ranjes divide Georgia into
two separate climatic regions-western and eastern. The moisture-rich
airmasses encroaching from the west bring abundant precipitation (from
1500 to 2500 mm per annum) to Western Georgda, principally on "he coast
Card 1/6

S/169/0-1/000/010/026/053
Thunderstorm processeso., D228/D304
of the Black Sea. Reaching the Suramskiy and Arsianskiy Ranges, the
airmass remains in their front part; in consequence..j precipitation
on the slopes of the ranges. The crossing of the airmass over the ranE-P
is often accomnanied by the front's erosion, the -raduil decrease of
cloudiness, and the cessation of precipitation. Thus, airmasses arri-e
in the eastern part of Tram-caucasia in a much less moist stnite~ The fLoi-
mation in the cold front of wave disturbances, which, durin,3 t2leir de-
veloDment over Transcaucasia?s territlorir, favor the stren-thpnin- of -02E~
vertical components of the And velocity, the enric',lininit of airmasse,5 by
moisture, and the fall of precipitation, often tualzes place to the south
of Transcaucasia. The author cites -Pacti.Lal data abou' thurtO., Pro to-z'r's on
Transcaucasia7s territorir. Me frequency of frontal thunderstorms fo,
~her in comparison -,,rith intr-uiviso thiindersto MI
Georgia is 1a1. hig fcl
Armenia and Azorbaydzhaa, on t.he contrary, the frequency Of L'rontal- ~ liuuri
dersto-.Eis is 14 and 31,'10 lower respecti-,ely. The freq-,,e-icy of intra-:3sp,
thunderstorms in coastal ~IL31ricto of' iNnstorn tho Kol'cn~-.rl
0111y I-
ukaya Lowlzandu eachos 20 - 25'/-% Ibur in
Card 2/6

S/169/61/000/610/026/053
Thunderstorm processes... D226/D304
areas, this type of thunderstorm activity increases to 60%. The small
amount of intramass thundersto.-ms in coastal districts and in the Kolk-hid-
skaya Lovilands is e)Tlained by local processes, which are strongly de-
veloped, especially in summertime. The breezelike phenomena observed
over coastal districts of Western Georgia and the Kolkhidskaya Lowlands
do not favor the genesis and development of intr~masis thunderstorm pro-
cesses. In Western Georgia, thunderstorms are observed in the winter
months; the maxirnim value-of the mean-monthly number "of days with thunder-
storms reaches 1o6 (Otradnoye, January). According to the measure of
removal from the Black Sea, the number of days with thunderstorms in the
winter months gradually decreases. In Eastern Georgia, Armenia, and
Azerbaydzhan, hardly any thunderstorms occur in the winter months. The
sharp increase in the average number of days with thunderstorms is ob-
served from April throughout the territory of Transcaucasia. In June,
it attains its maximum value and then gradually decre,.ses over most of
the territory of Armenia and Azerbaydzhan, reaching -. minimum value in
November for the territory of Azerbaydzhan and in December for Armenia.
Card 3/6

S/169/61/000/010/026/053
Thunderstorm processes... D228/D304
Over Georgia's territory, a certain decrease in the number of days with
thunderstorms is noted in July in comparison with the previous month,
together with an increase in August; this indicates the presence of two
maxima for the number of days with thunderstorms in Georl-ia. For Trans-
caucasia, the least number of days with thunderstorms is observed over
the territory of Azerbaydzhan, particularly above the Kurinskaya Lowlands,
which is due to the presence of dry steppes with an arid climate. The___-;~
Tiflis-Akstafa-Baku districts are characterized by an exceptionally small
number of days with thunderstorms; this is observed especially in the
Yevlakh-Baku areas. The author notes t,ie connection between the local
relief and the yearly number ~f doys with thunderstorms. In Georgiat
a comparatively small number of days with thunderstorms (chiefly from 25
to 35) is recorded above the Kolkhidskaya Lowlands and the Vnutrenne-
Yaxtaiinskaya, Nizhne-Kartalinskaya, and Kakhotinskaya Plains. A consi-
derable increase in the number of days with thunderstorms (from 30 -to
60 - 70) is observed in Georgia's mountainous districts and over almost
the whole of Armenia's territory. It follows from the data of pilot-
Card 4/6

S/169/61/000/010/0261/05-13
Thunderstorm processes... D228/D304
balloon observations over the Krestovyy Pass during May - August, 1949 -
1953, that in the mountainous regions the air-streams have a southerly
and south-viesterly direction in the evening hours before a thunierstorm,
The influence of the topography on the Olisturbance of air-streams aad
on the appearance of vertical comj~onents of the wind velocity is More
abruptly displayod in mountainous country than is tha case over the com.-
paratively Vat localities of Tiflis and Yerevan. This coralusion is
confirmed by the presence of foci of intramass thunderstorms albove moun-
tainous areas. The author distinguished the local foci of thun0erstorm
activity for Transcaucasia's territory. Knowing the time of thunderstorms
in the focal areas and the routes of the movement, it is Fossible
warr, certain national-economy oreanizations about the danger of land
buildinGs beinr- struck by lightning. All cases of nearby thunderstorms
observed Trom May to August of 1949 - 1953--from the moment- of formation
to -their dying out--were studied to expose the routes follozed by thi-,nier-
storms over Trans caucasia Is territory. As research has shown, the trave-1
lines of thunderstorm processes are directed alonE Transcaucnsia*s
Card 5/6

S1169161100010101026.1053
Thunderstorm processes... D228/D304
mountain-ranges. This is caused by the presence over the rwiges of' verti-
cal components of the wind velocity--en'-endered by irrerlilaxitiec I- the
ground surface, which strengthen the process of thermodynamic convoction-
and by the increase in the atmospheric humidity in a direction toward',I
the ranges. As is 9hovni by examInation of the muaps. ', the dJ.spI!iconIGT_.L w
the frequency maximum for thunderstorms in the coastal zone o-f 'rhe V/
and Caspian Seas, and also along the Kolkhids%aya Lowlands, from 1.5
19 hr. to 19 - 01 hr. Z-Abstracter's note. Could be error -ior 21
may be explained by the influence of the basins of the Black 3P-a and
Caspian Sea on the fori;iation of thunderstorm processos~ Over the Sea,.
in connec~tion with the establishmnt of a nocturnal tenDiarature-3--adi"Ilt
whicl: favors rapid vertical convection, the thun'orstorTa CUI-N-1171-ari is oi)--
served at night. fAbstrarter's notei Complote translation...7
Card 6/G

PMM I BOOK EXPLOITATION BOV/4624
Grozovyye protsessy Y uslovilakh 719-kavkazlya (Thunderstorm, Processes in Trans-
caucasia) Leeningrad., Gidrometeoizdat, 1960- 155 P- 800 copies printed.
Sponsoring Agencies: Glavnoye upravleniye gidrometeorologicheskoy sluzhby pri
Sovete Ministrov S=,~ Thiliaskiy nauchno-isoledovatellskiy g1drometeorolo-
gicheskiy institut.
Resp. Ed.: V. P. Lominadze; Zd.: T. V. Ushakn4a; Tech. Was; N. V. VoIXov, and
M. I. Braynina.
PURPOW; The book is intended for meteorologists. It will also be of interest to
engineers and technicians employed in the electric power industry, aviation,
and other activities concerned with thunderstorm phenomena.
Ca-rd 1/ 5

Thunderstorm Processes in Transcaucasia SOV/4624
COVRRAM.- The book d-ea" with thunderstorm procesees and their territorial
distribution. Special attention is paid to those problems which are of
practical importance to the aviation and electr1c power industry in Tr%.ns-
caucasia. The bo-ok is divided into three parts. The first part contains in-
vestigation of the climatic characteristics of thunderstorms over Tr%as-
caucasia. The second part attempts to formulate theoretical foundations to
explain tbe -Influence of the Caucasus mountains on the formation of thunder-
storm processes. The thini part presents the cha6mcteristics of the basic
factors in thunderstorm formation and analyzes methods for forecasting
thunderstorms under the local conditions of Transcaucasia. The problems
treated in this b,,,,ok were presented by the author at, a scientific: meeting
of the Tsentral"nyy in-stitut prognosov (Central Institute of Weatber Fore-
casting)in the beginning of 196o. The book was consideree'. to be the first
substantial contruLbu-tion to the research on thunderstorm processes under local
conditions in T-ranscaucasla. The results of fuxther investigations will ap-
pear in the works of the Thilisskiy nauchno-issledovatellskiy gidrometeorolo-
ggicheskLy institat (Tbilisi Hydrometeorological Scientific Research Instituto).
A supplement lists the names and elevations of 210 meteorological stations in
the GruziDsliaya, Arrqanskaya, and Azerbaydzhanskaya SSRI,. lbe author thanks I.A.
Kibell and N. V. Lebedevaya- There are 52 references: 47 Scyriet and 5 English.
Card 2/5

Thunders-,-:zm lllr-~esses ~a Wv IIA,)Il
TABIZ OF CONTEMIS:
3
Ch. 1. Chexac-t4--r of Thinderstorm Actiidty and Its Distrlbi~tlon
Over Trwiscaucasia 8
1. On The pniblem of the mchanism of the forma;tlaa and de-jejnp-
men-t r~f thunderstzrm processes 8
2. Physical geographic chazacteristies of Traneewacasia 13
3. Some weatber pecul-t&e..ties of Trmscalteasia 15
4. ltstribvtion of +~hlmderstoxms aver Trans ~mucmsia 16
5. ok' thumderstorm days o-mr ludiviAval evectors oll
3Q
6. -ru-4r-.PtlgA-1A-n of roi,~-es follawed by -uhimderetjorma o-;e.-
of Uimdeexretorm processes over individual
:,f TVIZE 'le.-'.~-aTb% 40
8. processes o-uer lmd4:v-Ldizal eectv-s
4.6

giW4624
9. Wind f-If"Id Tmo-pl-p4u,:as.!p.
Ch. Niflllewe 0, chav...-FUmp. WIMWW FMAEr-q- on
55
ot Tb%n4~x-? ~,crms 64
Mt, Mae GwZ~.,-~S,~- .4sage-z' 64
2. Pr,-,,hlc-m f'L,-:w o-my.- cbqtAz-les 78
-lk~ curreri~.t,
-f-wges 84
C*q---l~-i.-,:*~..~:%-e,",-~'I'l~r-,,~ Vie Risil~ Coliducl.,m- i. b e
A~d -z~f lht-ra-Mags Mnanderst.-rias ,
Yje.,~,L~~d5 ~:f Fcrt-:-q,-F!~~ng Tlb-,zade~mt~3.rvs Uride-z C,~rjd~tlcas Pzv&.-
I-a 89
1-7. V. 'If--bedevaLy,% --3 welhcd tm the con-
of a model f-7~ ~-be de+--imlna~t~-.-n .,f the
oz-1g!ji :Jr' ijv.~:s-mmq tbt-,~aderstcxwp. under the wuntaluous
cf, T-rsnscau,~asia 89
Use -cf V. M. Cberkasslmya's method fo-- thh- mo-xita.Lnaus
of Trsnq:7aiic%eia bun tsi.,xrm 91
U-9- of N. S. MishkWs mQhr.-d for floTt~-asting L de
1~_nder U-be condItI.-ons of T-anscaurAsi-~ 92
Card IL11 :;

Rrr),:ePseE 'L-j-L SCV/4624
4. Conside-.1mg tbe itffluen