SCIENTIFIC ABSTRACT SMIRNOVA, G. - SMIRNOVA, G.P.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001651620010-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 24, 2000
• Sequence Number: 10
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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ACCESSION NR: AT4036016 S/2789/63/000/048/0098/0105
AUTHOR: Gorelik, A. G. ; Smirnova, G. A.
TITLE: Relationship between water content and Intensity of precipitation and the radar 1
reflectivity of a meteorological object for different drop-size distribution parameters i
SOURCE: Tsentral'naya aerologicheskaya observatoriya. Trudy*, no. 48, 1963.
Novy*ye vozmozhnosti metcorologicheskogo primcncniya radiolokatsii (New possibilities
for meteorological use of radar), 98-105
TOPIC TAGS: m e t e o r o 1 o g y, precipitation Intensity, rain water content, radar
rcflectivity, drop size, drop size distribution, weather forecasting, weather radar
ABSTRACT: A study has been made of the theoretical relationships between radar
reflectivity and the liquid-water content and intensity of precipitation for different drop-
size distribution parameters. It has been shown that the drop-size distribution is ap-
proximated satisfactorily by. a function of the form
-pd
n.(d) dd Ri e dd,
p".
~1 3

ACCESSION NR: AT4036016
where d Is the drop diameter, n(d) is the density distribution, and b and 0 are distribution
parameters. In certain studies on this problem the following formula has boon used
for drop-size distribution
n (d) dd - e- P1 (2)
-Palmer distrlbution~the coefficient 3. 67d sis of this
In the Marshall On the ba
dependence, Atlas and Chmela (Proceedings of the Sixth Weather Radar Conference, 1957)'
derived relationships between radar reflectivity and the liquid-water content and pre-
cipitation intensity. In this paper similar relationships are derived, but for a more
general case, when the drop-size distribution has the form (1). The theoretical rela-
tionships derived make it possible to use radar reflectivity to determine the liquid-water
content and precipitation intensity for any drop-size distribution parameters, provided
the number of drops per unit volume Is known. The number (concentration) of drops in
a scattering volume can be computed using a formula supplied by the authors, provided
radar reflectivity Is measured simultaneously with the drop-size distribution. Orl
9.
art. has: 27 formulas, 4 figures,and,2 tables.
2/3

ACCESSION NR: AT4036016
ASSOCIATION: Teentrallnaya aerologicheskaya observatoriya (Central Aerological
Observatory)
SUBMITTED: 00 ATD PRESS: 3076, ENCL: 00
SUB CODE: F-S, DG NO REF SOV: 001 OTHER! 003
Ewd 3/3

TURIYAN, Ya.l.; ~S~IRNCJVA, G.A. - TOLSTIKOVA, O#A*
- - --. - - --:- I
Polarographic kinetic currents of nico-b-ini,,; acid, Elektrokhimlia 1
no.&-922-927 Ag 165. (Mlp~ ls~q)
1, Institut monomerm dLya sinteticheskogo kauchuka.

K N B U
stq.- F-!
non-,,,oven fabrz.cs.
f nuftI.C.
Ag 165.
no.A:5,
C; 4 4 11 r.C~y iegkGY pr or
j.-;~vatellskiY
n r-, .7 rad s k i y nal, Zs
chal I nik
c t i for s'-- kGva) 3. Na
uachava). 4. Zaveduyush-
otcelzi i*abrj,~A (for -Po-
d6+vom fabriki
'ro PrO

f7ll~., aspirantka; KAHCHEVA, V.L.
l.onpurative analysis of' efflelency In the production of nonwaver,
m5tprlals.and fabrics. Tekat. prom, 25 no,1004-55 0 165.
(MIRA 18-10)
1. Leningradakiy inntitut tekstillnoy i legkoy promyshlennost!
imeni Kirova (for Smirnova). 2. Starshiy inzh. laboratorii
..Oriki imeni Nogina (for Karchava).

sm m
Do'l,' 117
~2c -
SO:

judg* abbigs by Ow witarnin content. C., A. Swz~E~,
-nova. .54wrt. WISFOX. I90. No. 6, 11-15.
for ,~WWC 'eki in 2 1 vark-tic,; of alfalfa in RI-15 and 27 -
varieties in IM. using the icav" a,sikir"I'At the start of
blooloing and when In full Monist. The early- arsil Aart-
SMSOU varieties, such as ArAls. drop theira-worbic acii I cim-
tent rApidly with the ad"ace In sromtth. The We- unit
long-scoms varietks, ssuch as Poltavka, drop the ascorbic
acid content %lowly. Dsta are given on the ascorbic acW
.in the Grim-7ailtevich variety over a petiod of 3 yran at
vurioulstag"o(Cma,th; when.~iciiis2pprAr,whrt)blixmii%_
begin to shim. full blomn, after bloonainK, ind io siLAturt-
%e"t. 'rhe vilansin C tontent varien will% 11u, %ravni%.
titne of day, and the assnp.anion crop. When Von's with
other gramm the vitAmin consent of alfalfa is highrr than
whm gn,.n alone. 1. ,;. I,)& #

SMIRNOVAJ, G. A., Candidate Agric Sci (diss) -- "The composition and properties
of the milk from cows of the black-spotted and Jersey breeds, and the quality
of the cheese made from it". Moscow, 1959. 17 PP (Moscow Order of IAnin Agric
Acad im K. A. Timiryazev), 110 copies (KL., No 25, 1959, 138)

SMIRNGVA, G.A.
Method for the preparation of casein hydrolysate under laboratory
conditions. Vop.virus. 5 no.3:373-377 My-Je 160. (14IRA 13:9)
1. Gosudarstvannyy kontrolinyy inistitut moditainskikh biologicheskikh
preparatov im. L.A. Tarasevichay Moskvu.
(CASEIN) (BACTERIOLOGY CULTURES AND CULTURE MEDIA)

SI,LIRNOVAJ, G.A.; GAVRILOV, V.I.
Characteristics of the growth of sheep kidney epithelium in tissue
culture. Vop.virus. 6 no.2:227-231 Mr-Apt"61. ~(WRA 14:6)
1. Gosudarstvernyy kontrollnyy institut meditsinskikh biologicheskikh
preparatov imeni L.A.Tarhsevicha, Moskva.
(TISSUE CULTURE) (KIDNEYS)

SMIRNOVA, G.A.
Whey proteins as a source of amino acids for the survival and
growth of various tiesue cells. Vop.'virus. 8 no.1:114 Ja-F'63.
(MIRA 1616)
1. Gosudarstvennyy kontrollnyy institut meditsinskikh biologi-
cheskikh preparatov imeni L.A.Tarasevicha.
(TISSUE CULTURE)

SMIRNOVAJ G.A., kand. jal'Bkokhuz. nauh; srAKHANOV.4, V.m., band. wd. naji~
Biological properties of Lhe influenza virus of andm1e.
Voterinariia 41 110-4:7-12 Ap 164. (MIRA 17:8)
1. Moskovskiy ordaua Tnidavoga Krasnogo Zriameni inatitut
naxodnogo khozyaystva imeni G.V. Plekhanova (for Smirnova).
2. InstLtut vlrusologji imeni D.I. Ivanovskogo AW1 SSSR (fa-
Sta-khallov4'.
I

Sl%l i..,, skok"
k
Inyy chlen AMN ")"Uq kl*klr "al"

Zi-'D,1U.'()V, V.,'-',.; SMIRl.'OVA, G.A.
On the nature of the inactivating effect cf ani=a' -..-ssuze
extracts against my-mviruo haanagglutinins. Acta virol.
(Praha) [Eng.] 9 no.2:137-143 Mr'65.
1. The Ivanovsky Institute of Virology, U.S.S.R. Academy
of Medical Sciences, Moscow.

ISACHENKO, V.A.; SMIRNOVA, G.A.; GORBUNOVA, A.S.
Isolation of an irhibitor-sensitive va-~faLicn from w im-h--b--toi-
resistant culture uf A2 influenza virus by gel filtration on
sephadex. Vop. virus. 10 no.1:97-99 Ja-F 165.
(MIRA 18:5)
1. Institut virusologii imeni Ivanovskogo AMN SSSR, Moskva.

SI-IMNOVA, G.A.; MUGAIMA, L.A., red.
(Concise laboratory manual in Kra-~Ikoe ru-
kovodsLvo k prakticheskJai zardatiiam po biolk-fl-im,14i. Mc-
skva, Mosk. in-t narodnogo khoz., 1965. 59 P.
(m,lul 18-11)

SHIHNOVA, G.A.
Iffect of hydrogen sulfide waters. Med.sestra 15 no.3:5-8 W 156.
(MLRA 9:8)
1. Iz TSentrallnogo institute, kurortologii, Moskva.
(MINERAL WATnS, SULVIMOUS-THORAPBUTIC USI)

ZAYSTS, T.L.; SMIRNOV-4. G.A.
Penetration of radioactive sodium and calcium through undamaged
skin [with summary in English]. Med.rad. 2 no.4:66-68 Jl-Ag '57-
(MIRA 10:11)
1. 1z TSentrallnogo instituta kurortologii Hinisterstva zdravo-
okhraneniya RSFSR.
(SODIUK. radioactive,
penetration through skin from mineral water in animals
(Rug))
(GAMIUM, radioacti.ve,
same)
(MINERAL WATER.
penetration of rediocalcLum & radlosodium through skin
from water in animals (Rus))
(SKIN, physiology,
penetration of radiocalcium & radiosodium from mineral
water in animals (Rus))

SHIR-NOVA,,,G.A,.,.,
Adenosinetriphosohatase and phosphorylase activity of animal tissues
during the actioa of Narzan water baths following physical exercise.
Vop.krurdizioter. i lech.fiz.kul't. 22 no.6:40-44 N--D '57. (MIRA 11:2)
1. Zaveduyushchiy biokhtmicheskoy laboratoriyey otdala eksperimentall-
noy kurortologii TSentrsl*aogo instituta kurortologii.
(ANZYKIS) (HIMRAL VAURS) (IXERCISE)

c 0 0, 1:11 G:-
C DIA-ES
o v a G A F'~ 4 3 2
Los
lit ca- in
:J", o~ ',~ko lblood Ca
uitraNl,rou~ltc 'i-oo rapid-.ty o~ of C,-, ~rl the tissues rvnziiias al-
0!, ;~!,-,s af,*ect,!d. n:osL (11~ver and kidneys) it
Ca onltor~i tnz~ colliolidal fraction o4 a"I tho, t'ssuC6,
Thus nnv be by dccreased abilitv
Of prot'--ns to form C~,Inpllex corilljoulich; WiLli Ca.
(S)

ZHDANOV, V.M.; SMIRDIOVA, G.A.; BUKRINSKAYA, A.G.
.L~
Inactivation of the Sendai viru-- by proten-ases enid cellula-r extracts.
Vop. virus. 9 no.2317&-184 Mr-Ap t64. (MIRA 17,12~
1. Institut virusologii imeni Ivanovskogo AIMIT SSSR, Moskva~

SMIRNOVA G.A.- VIRKUS, A.Yu.
9 1
Gas-liqul-d chromatography of me-thyl esters of higher fatty
acids of li~'d components of the Sendai virus. Vop. virus
9 no.4:417 421 Jl-Ag 164. WIRA 18M
1. Institut virusologii imeni D.I. Ivanovskogo AMN SSSR, t-',oskva.

S/194/62/000/007/130/160
D413/D308
AUTHORS: Gorelik, A.G., and Smirnova,...G.A.
TITLE': Relation between radar echo fluctuations and the
,;,icrostructure of precipitat'lon
P_"RIODTI,'~,: Heferativnyy zhurnal. Avtomalika i radioelektronika,
U to
no. 7y.1962, abst-ract 7-7-132 ts (Tr. Tsentr.* aerol.
observ no. 36, 1961, 91-101)
TE-M: The authors consider new possibilities of obtaining informa-
tion on the m--;crostructure of precipitations by studying..fluctua- :-
tion s~.ectra of radar echo signals rather than measuring their mean'
-Int-ensity. They prooose an inertia-free statistical radar method fcir
usin-the relation between the fluctuat4on spectrum of echo-signal"_,~
magnluude and the random velocities of the scattering particles to
measure the velocity of turbulent motion. The authors give the theo-
retical basis of the new method and consider the theoretical rela-
tion between the magnitude of the effective scattering area of a
meteorological formation and the mean dimensions of a scattering
drop. An experiment is described and the results obtained from it
Card 1/2

S/194/62/000/007/130/160
Relation be'u-vieen radar echo ... D413/D308 /",
are given, 7 figures, 11 references. [Abstracter's note: Complete ' ,
translation.j
Card 212

27259
S/020/61/139/005/011/021
B104/B201
AUTHORS: Gorelik, A. G., and Smirnova, G. A.
TITLE: Relationship between fluctuations of radio echo and the
microstructure of precipitations
PERIODICALt Akademiya nauk SSSR. Doklady, v. 139, no. 5, 1961, 1098-
1100
TEXT: Radar study of the microstructure of precipitations is based on thei
measurement of reflectivity from meteorological objects. The fluctuation
spectra of the reflected signal are specially informative, as they are
closely related to the relative velocities of precipitation particles.
In the fall of the latter due to gravitation, a clear relationship exists
between the size of particles and their velocities. In this
the
case,
fluctuation spectrum has, at the output of a square-law detector, the
form
J
2*!~F4
Card 114

27259
B/020/61/139/0051/011/021
Relationship between fluctuations of ... B104/B201
P (AF) A (V) P AF dv,
+
0
L'i AF 2Au
P (V) WT (U-) I I
Here, Ti is the mean power of the reflected radar beam; v ia the projet-tion
of the velocities of the precipitation particles onto the beam direct.'elil
w(v) is the distribution of the projections of velocities-, c)'(v) - r
describes the fall of particles; /'~ is the wavelength of the station-,A
v is the differc-ace between the projections of velocities. if tf(v) is
known, the mean size of particles can be found by (1). For raindrops
with diameters ranging between 700 and 400041, a diameter distribi.ition of
f(r)dr,exp(-plr)dr, P, = n/r- was measured (A. B. Shupyatskiy, Tr.
Tsentralln. aerologich. obs, no. 22 (1957)). According to K. S. Shifrin
wherer'~ is a
(Izv. All' SSSR, ser. geofizi, no. 2, 1958)) r. 'v) =v2/,
factor- in this case, the fluctuation specti~um can be rendered in the
. u
A
Card 2/ 4

27259
S/020/61/139/005/011/021
Relationship between fluctuations of ... B104/B201
-kv2(v'A A )2
v
13. 3exp(-k(v+ dv, where k=�, 0~2. Thus,
form P(AF) 2
Pi can be determined from experimental measurements of,6F, wherefrom r- C
is then obtained. An analogous investigation can be conducted for drops
some *en/-4 in diameter, Regarding drops of this order of magnitude,
distribution with respect to diameters is not known and the following
is assumed; JI(r)dr-r2e-P4 rdr., with r=f( v) 'v'6(2 being taken from the
work by K. S. Shifrin. Thus, the fluctuation of the radar echo can be
~O
written as P(4F)=- v 6e- kv (V+ A AF) 8exp(-k(v+- --~-&)dv, -where k=p,/-/O, 0,