SCIENTIFIC ABSTRACT KONDRATYEV, K.YA. - KONDRATYEV, K. YA.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000824210017-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: December 30, 2016
• Document Release Date: June 19, 2000
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

IDIMTOYN, K.Ya.., doteent; GAYJUSUYA. G.N., student.
Moisture tm-bidity and the deteralzation of the aacmt eL w&tGr IR
the atmosphere. ftwh. bW. Lone un. noo32:7-8 154. (Oak IOM
1. Tafedra flzW atmoefery.
(Hwaldity) (Atuaspheric transpe:rency)

KONMIfl1w, X.Ya., dotseRt; GRCHOWAO T.N., student* water
.......... the turbidity resulting from the COA149COnes Of
il~s~ -9 In
droplets suspended In the atvkosphers. lauch, biul. LOW. uIR* 28832-s
B-11 154. (ma 10:4)
1, jefedra f1sikIL atmoeferY.
(Rmtdi%y) (Atmospherle transpar ney) (LIebt-Scattering)-

XONDRATIM, Keism-datseat; PNVZNXR, S.I., student.
laterrolationshIp between stream of energy and light radiation.
Nauch. blul. Lea, uz. ao,32-12-13 154. (MA 10: 4)
1. Zafodra, f1sUd atmefory.
(Solar radiation)

XONMATII-XV, I.Ya.; PODDLISKAYA, 1.1o.
.~ "0l
On the theory or lWahovskilts pyrpometer. Test.Len.um,q no.5:
103-n7 N? 154. (=A 9:7)
(Alarth--Badiation) (RMiation-Measurement)

KoNr~)T
Subject
Card 1/2
.Authors
Title
USSR/Meteorology
Pub., 71-a - 5/26
AID P - 2495
4.t
Kondratl-vev, K. Ya., and Kudryavtseva, Kands.
rnys. Ana 00.
On the albedo of the sea surface
25-27, MY-Je 1955
Gidro.,
Periodical Met. I
3,
Abstract The computation of the albedo of large bodiesl6f~'Waier
is usually ~mide'theoretldailly on the basis of' the~-~
Fresnel formula, The article-'reports on experimenta
in caLou'lating the albedo of~~the' calm sea surfaceif;
under a cloudless sky for diffused and total radiation
disregarding the inverse diffusion factor by computing
the height of the sun and the diffusion angle at any
given moment. The authors maintain that this method,
Is x6re accurate than a theoretical analysis according
to the Fresnel formula. A table giving albedo data-
and a diagram showing the dependence of the albedo

.-V
USER/Physics
Gard Pub. 127 9/12
Authors I Kcpdrat 9 ev, K* Ya.; Kudryavtseva, Le A.; and Manolova, Me Pf
Title I Distribution ofthe energetic-(thermal) and light intensities of disper3e-d
radiat4on of the atmosphere over the celestial vault
Periodical I Vest. Len. uno sere mat. fiz. khim. 5, 119-128,, May 1955
Abstraot I An experimental.study.,of the-distribution of the thermal (energetic) and
light intensities-of the atmosphere over the celestial vault is described.
A pyranometer of Yhnishevskiy was used for measuring the thermal intensity
of dispeAed-radiationiand::Lhe light intensity Was measured with a photo-
selenium-element. Eight references: I German ard 7 MSSR-49364954)0-
Graphu; tables.
Institution
Submitted April 19,1955

----------
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ill t1le -kv J~Ilde~IML
M2;; -fiRT,- ta-bk-, eq~i. DLC-Appn~uL-'Lt af~
o" tk trice, ivv ratijiti qQ
6164thig re atiVe 1111te. r ace..
f fi~ c~unt~r6didtloq ~tihi (cra clear sky and complete and pru-31
0-M3. fi--thO Ab;idr= Of-aft- fn!Wc~6n, fite- -jxtuaL aunc~Ephew cart Ix, con'31dutd qitjst'
radiatioa %rid couaturad:atio -4 the 5L-Y~~
t-w- twe, trattficd6o le
resuks of exp&mie.taf detennina-loi-i f3f efff,~~fv- -idi:ttion a-rA atraospberi rt--rm LWwa,,
C COU
n a 2 Sky aj~~don
-T,ass. qraufAefs a lmd.L
F-4

AID P - 3844
Subject USSR/Meteorology
Card 1/1 Pub. 71-a - 7/35
Authors Kondratlyev, K. Ya., M. P. Manolova
Title On the occurrence of diffused and total radiation on
a sloping surface
Periodical Met. i. gidr., 6, 31-34, N/D 1955
Abstract The authors give atheoretical analysis of the angle
of radiation diffusion on the basis of tests made at
the Karadag actinometric observatory in June-July 1953.
Some data on the diffusion angle under cloudless and
cloudy skies are given in tables. Three diagrams.
Two Russian sources, 1950, 1952.
Institution : None
Submitted : No date
MMCVT0FA,L.1.
*Solaz energy.* I.IA.Kondrat'ev. Reviewed by L.I.Kamontova-
1zv.V9e*.g9og.ob-Ya 87 no.4078-380 Jl-Ag'55. (KLRA 8: 10)
(Solar radiation) (Kondratlev,K.IA.)

pHM I B= EnWITATTOff 450
Kondratlyff Kirlll Uk"lavich
Mp in the Atmosphere)
Luchistyy teplodbmen v Stgogfere (Radiant Beat Ew-b
Leningrad, oi9;;aiZzdmt, 1956. 419 v. 3,000 copies printed.
Ed. (title page) -. Tver~kjy, p. N. , professor; Ed. (inside book): VIMSM#
Yu. V.; Tech. Eds-1. srequins, M. 1. and Soloveychik, k. A.
PUFITM: 'This systematic presentation of basic problems in thermal r8dittlOnt
the radiative balance of the atmos9here and subjacent surfacesp and
the radiant inflow of heat into the atmiosphere,, is intended for science
workers, advanced istudants anWthose concerned vith problems in "lam
of the atmicalhS", astro"Ics, climatology, egroalimistology and
therma radiation*
COVERAGE: Radiant energy is the asin source of energy for all processes
occurring on the ewth . Rest transfer is an Important factor in the
- thermal balance betveen the earth and the atmosphere. The present
csft~V-10
Radiant Heat Exchange (Cont.)
45o
'c1Joaot4"er1s* 'IM' ProblM Posed in the above Xlentloned fields. The eight
Of the book am sgamerLzed an follows:
Principles and concepts, Chapter I Presents basic
absoiltely black body is The Problem of radiation from the surface of an
radiation Of material bod"cu"ed and the methods Of computing the thrmsi
1e. in described. In Chapter II the theory of actlno-
'26tric 2e"uramts of t
discusses the aboorption-heof=alclvgranawe&t:Lon streams 18 presented- Chapter M
radiation in the ILtROSphere and gives
AYPrOxIMate methods of co"Uting such absorlption.
general problem of heat Chapter IV presents the
radiation transfer in the atmosphere..
studies aPproxiMate methods of ccaputing thermal radiation streChapter V
ms. Radiation
into space extensively discussed* Chapter VI considers the determination of
counter-radiation in the atmosphere and effective th Ub ace
surfaces, both of great practIcs, importance. radiation of e a j ant
of research In the radiative balance of th- Chapter VII Presents the results
e atmosphere and subjacent surfaces
and the earth-atzosiphere system. Chapter VIII undertakes the solution of tbLe
rad.im*hest exchange Problem4 the cause of variations
atures. in atmospheric temer-
Consideration 'a 9L'Wen to differences in turbulent and radiant heat
exchange- The author thanksprofegsor-p. N. Tversky and Professor
A. A. -Do.itriyev for adview and 8541stonce In PrePOXIM9 the manacript.
-?/101

rcmMTIYJCV, I-Ta.; LOGINOVA, Z.A.
Direct methods for determining the temperature of soil surfaces.
Yest.Lon.un.11 no.22:79-9 '56. MU 10: 2)
(Thermometry) (Soil physics)

UWVSKIKH, K.p.; KOMUT17N. K.Ta.; TAIMSHITMU, I-T*-
Atmoapherle &bgorptiom
un. se.210:3-8 156.
(Atsompheric
fumtjoss for boat radiation.
tsq~erature) (Solar radiation)
Uch.sap.Lon.
(su 9: 8)

zon"T112y, 91
I .
. Appllca'blllty of &IM~Ioa concopts to the problem of calculatift
the radiant lanow of heat In the atuospbs". Uch.sap.Lon.un.
no.210:20-28 156. (SM 9:8)
(Atmosph"le to"Mrsture)

ZOMUT I By, 1. Ta.
21he fty"tashIlld approzimatlea method In the theory of radl&tloa
trusalselon. Vah.sap.Lea.un. no.210:29-39 136. (an 9:8)
(SoUr radimism)

XONDUTIM, X-Ta.; MNOLOTA.. M.P.
--------
Arrival of scattered radiation on the surface of &slope during a
cloudless sky and &continuous cloud cover. Uch.sap.Len-un. no..210:
4" '56. (NM q: 8)
(Solar radiation)

14-1-481
Translation from; ReferativW Zhurnal, Geografiya, 1957, Nr 1,
P. 53 (USSR)
AUTHORS: Kondratlyev, K.,Ya. and Ter-Markaryants, N. Ye.
TITLE-. Reflection of Radiation by the Sea (Ob otrazhenii
radiataii morem)
PERIODICAL: Uch. zap. LGU, 1956, Nr 210, pp. 41-56
ABSTRACT: The calculation according to the Fresnel formula of the
amount of radiation reflected by water does not take in-
to account the reflection of diffused radiation, the
counter diffusion of radiation by the ocean, and th6
swells of the sea which change the albedo in relAtion to
a smooth surface. In June - July, 1954, the Main Geo-
physical Observatory and Leningrad University organized
at the Black Sea (Naradag) comprehensive measurements of
the ocean's albedo at different heights of the sun, the
flux of thelrAdiation coming from-the water, the direct
solar and diffused radiation, and also measurements.of
-
the distribution according to the angular intenfLjU.0.g
_
.
,,
the radiation diffused on the sky. The method used for
Card 1/3 these measurements is described by D. L. Grishphenko

A! 4) i~ A I
14-1-565
Summary translation from: R6ferativnyy Zhurnal,'Geografiya, 1957,
Nr 1, p. 64-(USSR)
AUTHOR: Kondratlyev,, K. Ya.,, Yakushevskaya, K. Ye.
TITLE: A New Method for Calculating the Radiant Influx of Heat
(Novyy sposob rascheta, luchistogo pritokaitepla)
PERIODICAL: Uch. Zap- LOU, 1956, Nr 210, pp. 57-63
ABSTRACT: A practical method for calculating radiant heat influx
based on the premise of the homogeneity of the atmosphere
along a horizontal level is presented. The radiant heat
influx (LPT) is expressed by the formula E = -dP/dz, where
F is the heat radiation current. The magnitude of the
derivative is determined by the values ef the transmission
function derivative at different atmospheric levels.
A radiant heat Influx (LPT) formula, convenient for nomo-
graphic use, is obtained by using approximate radiation
transference equations.. Data on the transference function
derivative Is the basic initial material in making up the
nomogram, which in turn permits detailed Investigation
of the vertical profile of,radiational changes in atmos-
Card lZ2 pheric'surface temperature. Scales provided by the

14-1-565
A New Method for Calculating the Radiant Influx of Heat (Cont.)
nomogram are convenient for surface-stratum calculations;
for free atmosphere calculations, however, the scales
must be modified.
I. Sh.
Card 2/2

XONDRATIM, K. Ya.:
K%IDRATIYEV, K. Ya.: "The transmission of radl-nnt energy in the atmosphere."
Leningrad Order of Lenin State U imni, A. A. Zhdanov. Leningrad, 1956.
(DISSERTATION For the Degree of Candidate in PHYSICOMATMIATICAL SCIENCE.)
So: Knizhanaya letopis', No. 24, 1956

I . ..
'x6gaulfm' x. Ys~'
t Radiation in the Atmosphere and AlsOcie'ted
*Transference Of B40 ational Assoct of MateorologY Meetingsp
Problems," paper sutuitted at BAwn
TorontOv Canada, 3-14 SOP 57
C-3,800,327

K
XT) PBASE I BOOK MMWITAnOff sav11685
kksdwi~& Aadk NO. Kmitit P0 6eq&Z11'1 geoflzikIe.
Teziby doklMov na XI Genersl1n6ya8se&b1q;je Mezhdunarodnogo, geodazicheskogo
I geofizichesko4oIo0yuga. -X*Zlidunaroduaya assotsistsiya meterologif
(Abstracts'af Reports at the 11th G6er&l*Msewb1j of the International
Uni6n,of Geodesy and Ge6yhysics. The InteroAtional. Association of Meteorology)
Moscov 1957- . 38 P. /Parallel texts In Russian ~nd English or Frezi&/
1,500 copies printed. No additional contributors mentioned.
PURPOSE: This booklet 1;e Intended for metebro sts.
l:09i
COVERAGE: These repoks cover varim-is- oubjec.to in the field'of meteoroloa. Among
the specific quWviA3ime discu4sed are: the hLoat balance of ~he E~Lrthls surface,
'Jet, strLaw transte4nee of heat radiiLtion, electric coagulatton of cldud~partl-
clesi t bulent diffusion, cloud studies;and others. Abstracts of all the arti-
clis are traasla~ei'into either'Frezich.or English.There are n.o references given.
TABLE OF - CONTENTS:
Bu4ko,IM.1. The Rest Balance of the Earth's sulace 5
Card 1/*

EV,
, ri-
Y
AUTHORS: Yelovskikh, M. P. and Kondratlev, K. Ya. 49-5-3-6/18
TITLE: Angular distribution of the intensity of thermal emission
of the atmosphere. (Uglovoye raspredeleniye intensivnosti
teplovogo izlueheniya atmosfery).
PERIODICAL: "Izvestiya Akademii Nauk. Seriya Geof4zicheskaya"
(Bul in of the Ac.Sc., Geophysics Series)t 1957, No.5.
pp. 683-688 (U.S.S.R.)
ABSTRACT: In a previous paper (1) the authors gave the results of
theoretical and experimental investigations of the angular
distribution of the intensity of atmospheric emission. A
number of problems were, however, left unsolved because of
a lack of experimental data. In the present paper a more
complete account of the above is given. These new results
allow some conclusions to be made which are of interest in
practice. The angular distribution of the intensity of the
effective emission over the sky is characterised by the
function r, (0) = f (IYI)/f 0 where f(III) and f0 are the
intensity of the effective emission at a zenith angle 17 and
Oard 3W in the direction of the zenith respectively. The distribu-
tion of the intensity of the counter-emission of the
atmosphere relative to the vertical is characterised by the
11-K..' analogous function ~(11*) In the case of a
0
49-5-16/18
Angular distribution of the intensity of thermal emission
of the atmosphere. (Cont.)
clear sky the theoretical formulae (derived by one of the
authors in Ref.2) has the form:
re 0& PI(W'W see A.")
PI(Wco )
where PI(wcd is the atmospheric transmission function for
a directed radiation and w is the water vapour content
of a column of the atmospheA having a unit cross section
g1c 2-,
(in m ). Further expressions which are available are
the following:
(a) clear sky: r. (.0%) = osr.01 (empirical)
or 0 - 18 Ym (l - Cos -1p 11 1n 10
_-(O
r(O) r 7 c os -0%
(b) cloudy sky:
Card F,(wh see&
P, (Wh)

49-6-19/21
On the influence of the stratification on the thermal
radiation of the atmosphere. (Cont.)
Thus, the model of the horizontal uniform atmosphere is
fully satisfactory for the purpose of calculation of the
counter radiation and the effective radiation.
There are 2 graphs and 4 Slavic references.
SUBMITTED: November 6, 1956.
ASSOCIATION: Leningrad State University imeni A. A. Zhdanov.
(Leningradskiy Gosudarstvennyy Universitet im.A.A.Zhdanova).
AVAILABLE: Library of Ca2gress,
Mrd 313
/i
YBWVSKIKH, M.P.; KONDRATIYXV. K.Ya.
A radiometer for measuring the intensity of the heat" radiation
of the atmosphere and comparison of the radiometer with the
pyrgeometer. Meteor. I gidrol. no.7:49-51 J1 157. %Rk 100-8)
(Radiometer) (Heat-Radiation and absorption)
(Atmospheric temperature)

jEONMTlyAV. X.Ya.; LOGINOVA. Z.A.
Indirect methods for the determination of earth surface temperature
based as standard actisometric datalwith 9UMArY 11 309119h, P923210
Test. Len, us. 12 zo.4:79-84 157. (KM 10:4)
(larth temperature)

AUTHOW, Kondrntlyov, K. Ya., Manolova, L-1. P.
54-1-1/17
TITLE: The Daily Course and the Daily Sums of Scattered & ToUa
Radiation on Slopes of Different Orientations
(Datmoy Miod i duoviiyye mimmy rftaso ';' rannoy i summarnoy
radiatsii na razlichno oriyentirovannykh oklonakh)
PERIODICAL: Vestnik L nin.radskogo Universiteta Seriya Fiziki.
i Khi mii (Nr 1 1958, Nr 4. - p p;
ABSTRACT: The initial values of the present paper are the results
of the pyranometric moasurementn of scattered total radiation
acting upon surfaces of different orientations. Investigations
were carried out by the authors by means of Yanishevskiy's
pyranometer. The latter was mounted on the stand of
a theodolite in order that the receivinG 3urface might be
turned in any desired direction. Measurements were carried
out in summer 1956 on days with a cloudless sky on a
horizontal platform of the actinometric observatory of
Karadag. Surfaces with gradients of 5, 10y 15, 20, 30, 501
70 and 900, which were directed towards South, 11orth, East
Ca"A 4,4 and West, were measured. It was found thatIthe xelative

The Daily Course and the Daily Sums of Scattered & Total- 54-1-1/17
Radiation on Slopes of Different Orientations
amounts of total or scattered radiation in the case of a
cloudless sky depend practically only upon the position of
the sun and the direction of the 31ope. This means that the
geographical position of the point of observation is of
importance only with respect io whether the observed range
(sunts altitude h