SCIENTIFIC ABSTRACT KAZAKOVA, N.M. - KAZAKOVA, T.B.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000721310012-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 13, 2000
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

KAMOVAS Home
Terrace profiles as IL method Of studying the most recent tootoula
movements of the earth's crusto Trudy Instogeog. no.62-ioo-13.1 154.
(Valleys) (Zarth movements) (MIRA 8:5)

UWOVA, N.M.
Axperience, in compiling geomorphological-tectonic maps.
Trudy Inst.
geoge no 62:112-123 154. (MMA 8:5)
ZGeology-Haps)
vs- ~r-"4

KAMOVA.H.H.
Origin of Lake Seven. Trudy Inst.geog.
no.65:135-146 155.
(Seven, Lake) (MLRA 8.11)

ATI--K--
KkZAKOVAj N.M.
Basic features of the relief of Moscov Province. Vruo
Inst. geog.
no.71:5-14 157. (KLRA NO)
(Xoscow ProvInce-Physical geography)

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Ao
job
2% Am k!
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Ilk
van
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KAZAMVA, If.".
Division of the Seven Basin into geomorphological sections.
Trudy Inst. geol,,. 74:43-75 158. (MIRA 11:7)
(Sevan recion-Physical geography)

GAYGFROV, S-F.; ~~AYGHDKOV, P.F.; KjVAKOVA, N.N.
Some characteristics of the vertiuil stmuctur~ of *I-I
str%tc.7phere.
Trady TSAO no.59:3-10 164. WIR4 39.3

ACCESSION NR: A51020753
SOURCEs RZh. Geofizika, Abs. 1B327
S/0169/64/000/001/BO58/BO58
AUTHORSt Kazakovaq N. Nq Matyeyevq L. T.
TITLEs Methods and main results of calculation of vertical
motions of air
(based on the data of the drifting station "Severnyy polyus-7")
CITED SOURCEs Tr. Arkt. i Antarkt. n.-i. iii-ta, v. 253. 1963,
161-171
TOPIC TAGSs Vertical air motion, pulsation air velocity,
turbulent air
velocity, convective air velocity, ordered air velocity,
vertical atrato-
spheric air velocity, vertical tropspheric air velocity
TRANSIATIONs A brief classification of vertical motions as a
function of the
scale of the process (phenomenon) is given. Three categories of
vertical
velocities are distinguisheds pul 8ation (turbulent)
velocities, convective
velocitiesp and ordered (large-scale) Telocitied. Calculation
of vertical
velocities of the first and second category van maAe by using a
method proposed
Cord 1/2

ACCESSION NRt AR4020753
by P. F. Zaychikov and one proposed bi one of the authors of
the article. At
the limits of the troposphere, the values of the vertical
Yelocity calculated
by the two independent methods are in satisfactory agreement.
In the strato-
sphere, the f'rat method gives high values for vertical
velocities.
L. Matveyev
DATE ACQs 03Uar64
SUB CODEt ASp Al ENCM 00
Card 2/2

C 7 114 11) 6 11 ~~ 9 S / 3 1 16 / 6 3 / 2 5 3
A UT110R t Kazakovs, V. U.; flatveyey, L, J.
T I TL MC010EIG :!nd rAatn results of the computation of vertical -4
i n
To t i on 9 (,Accvr(MnP, to data of the drifting station "Severny"-W
Pn J tj 7
S 0 V P C E - Lenin. grad ArktichesRiy i antarkticheskiy nauchno- -a
!7 1 e. do -
1 1 t u t 'Frudy*, v. 253, 1963. Sburnik ? ta rev ~7'
n C h e -I ~n i , i V V . e r n I o v i t v o p r o 9 -1 st i d r o
m e t L, C, r o c- r
y n n o f .3 r t I c 1 e 3 1 U nic r, f) rv C) 1 7
-7-
-radiosonde -measurametito
TOPIC TAGS, wind rapt -VaTt
vertical wind gradient, tropospheric wind gradient , stratospheric
wind"
gradient
AB ST RA CT i investigationt of vartical currents are of great
scientific
an d i c t t ,)rtlance since these currento citro--t I-,- ,i
f-, g- c f i! r- raf , &nd the transfer of
1 L; t v io ~,ollutants. V r t i cq I M.0 t i 0 n 9 -n 0 ne If za
at

A C CE S s 10 N IN', R 1 1, T4 0 4 6 14 6 9
tno 8 ph it re can be divided into three basic classes on the basis
0 f
t-0,cal 1,oz lzonta-l dimensionsi 1) irreguler (puleational)
c u r rc ve rtl cal currents, and 3) re~:-j .~T v
c!.t r r 43 zi Firticulltr attention in thiN article is g1von
uI i r i t! a r 2 s t I_mal) and convectional vertical curr-unl~.
dat I indi cites that the depiandefici; o I
-a I of r o 2 L I j
i valocity o z the thermodynamic parameters of the 0 tate of t
phere can be expreun2d by the formula%
!,--:z
2. Ow"
tv 2. 10
_1_1w -he re-u _Ts--t h C f. e 6
within which these, vertic-a-1--turrents Rreserve, their -sign may
extend----!-
several kilometers. The absolute value of the vertical velocities
varies f rom tons of centimeters to aeveral meters por secand. in
t~'('
troposrhire there In basic ngreenont between the valuen for verticnI
-rclocltfe,i de,erroliied by radiosonde and those determified