SCIENTIFIC ABSTRACT BERLYAND, M. Y. - BERLYAND, T. S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000205010009-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 8, 2000
• Sequence Number: 9
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

BERLYAND, M.Ye.; GENIKHOVICH, Ye.L.; LOZHKINA, V.P.;
ONIKUL, R.I.
Numerical study-of atmospberic diffusion under.normal
and anomalous
. conditions ofstratificatio~. Trgdy GGO no.158t22-31
164.
Characteristics of the diffusion of heavy pollutants in
the'atmosphere.
Ibid.:32-40 (MIRA 17:9)

CHISTYAKOV, A.D.; BURKOVA,- M.V.,- ORLOVA, Ye.M.;
GIAZOVAI O.F.;
lipz D.A., ABRAMOVICH, K.G.; POPOVA,
T.F.5 MATVEYFV,, L.T.; BACHURBA, A.A.; LEBEDEVA,
N.V.;
PESKOV, Mo.., ROMANOV. N.N.; VOLEVAKHA)N.M.; PCHELK09
I. G. ; PEMENKO, NOATIFIF110. I.V.- PINUS, N.Z.;
KININA
S.M. ]~kTHSYEVA,.T.F.3 I
SIRSTER , I , L.S.; EEL7SKAYA,
N.N.. nauchn. red.; ZVEREVA, N.I., nauchn. redo:
KURGiNSKAYA, V,A..'nauchn. red.; MERTSALOVA, A.h.,
nauchn.
red.; -101,,ASHFVICH, L.V., nauchn. red.;
SAGATOVSKIY, N.V.,
otv. red., -KOTTKOVSKAYA, A.D., red.
r
LManual ~f ahort-range weather Rukovodstvc,
Lenint-Tarl, Gidro-
po kmtkosrochrym prognozari pogody,
meteoi-:,dat. Pt.2. lzd.2. .1965. 2,91 p.
(MIIIA 18-8)
1. Moscow. TSentrallr*ry institut prognozov.
4*

TOPIC TAGS, atmospheric diffusion, atmospheric
contaminatior, nir -c~cjjuti-r

L 4-2503-6c
i ah f 1
p ~)j f lc ient exert an apprec

L 6255, -65
F - N,
W. IMF "Rov. 019 OTHM: 002
3 /j

L 2669-66 3a(j)/gW(m)/FCC/EWA(h) (;SIGW
ACCESSION NRt AT5023953 UR/0000/65/000/000/0380/03911
AUTHORi Genikhovich.-YA-,---1,.; Demlyanovich. V., K.t
onikul. 4-
TITLE: Effect of vertical distribution of temperature and wind
velocity on tile atmospheric diffusion of radioactive pollutants
SOURCE: Nauchnaya konferentsiva'po vadernoy meteoroloRiio_.,-Obn_ina
1964. Radloaktl4n~ji--fi-ioi- y v atmosfere L ikh ispollzovaniye v
meteorologii (Radioactive isotopes in the atmosphere and their use
ini
meteorology)-;--49klady-kopCereatiti:L. Moscow, Atomizdat, 1965,
380-39,
',TOPIC TAGS., nucl a r mSte
t- Qxaj&&y, air pollution, atmospheric surface
boundary layer,,,a mospheric bd%Ald~Wry layer, micrometeorology,
ti!. SL-4 0 --11
active fallo ut, ra dioactive pollution, lapse rate, atmospheric
turbu-1
lencep wind velocity
ABSTRACT: *Until recently, Soviet research dealing with p'roblems of
atmospheric pollution from continuously active point sources has
been;
based on models 'of conditions for wind velocity and the coefficient
of turbulent exchange prevailing in the surface boundary layer of
thei
atmosphere, The present japer discusses the inapplicability of this
Card 1 / 2

-------------
L 2669-66
1ACCESSION NRt AT5023953
model to many existing and planned point sources and to problems of
radioactive fallouts It presents a quantitative analysis of the
effects
of lapse rates# wind velocity, turbulent exchangep and other factors
and a mathematical model which reflects them as they actually occur
in the thicker boundary layers Orig, art. hast 8 formulas and 5
figures. [ER)
ASSOCIATIONi 'none
SUBMITTEDI 2SApr65 -ENCL: 00 SUB CODEt ES, N
NO REF SOVI 009 OTHERt 000 ATD PRESSI

1 1 $ M, Nuilli'll, V.-H.
BEFJ,YP.11!j, ',!.Yc;.; YO-I,-; I-`E YA
. I
0 .. . ~z A-e - -- -,
~kme Ei~- ii problem f studylL.--, I-le diffu'Jov -racy
CC-o
14~5. (,,!ITIA --1:8)

ACC NRiAT6035508 SOURCE CODE: UR/2531/66/000AW6015/
AUTHOR: Berlyand m. ye, (Doctor of physico-mathematleal
sciences)
ORO: none
-TITLE: Conditions contributing to the danger of atmospheric
pollution
by industrial effluents
SOURCE% Leningrad. Glavnaya geofizicheskaya observatoriya.
Trudy no
185, 1966. Voprosy atmosfernoy diffuzii i zagryazneniya
vozdukha tpro-$
bldms of atmospheric diffusion and air pollution), 15-25
TOPIC TAGS: micrometeorology, atmospheric diffusion, air
pollution,
brasa==~I~ aip-W-03 i , temperature inversion,AT.,ind field, r
smog, atmospheric turbulence,",-Z..k~
ABSTRACT:Previdus studies by the author have presentod
mathematics
approaches to the investigation of various meteorological
factors which contribute to hazardous air pollution condi-
tions in Industrial areas (Trudy Glav. Geoflzo Observ.,
n0.''158, 1964; no. 172, 1965.; Heteorologiya i geofizika,
noe B.".1963), These studies included the affects of turbu-

ACC NR.AT6035508 '
lent diffusion of pollutants from point sources (permitting
the calculation of variations in the exchange coefficient
with height) and the relationship of lifting inversions to
anomalous stratification conditions. The present paper
presents simplified mathematical formulas*for representing
the combined effects of lapse rate distribution (especially
during lifting Inversions) and wind speeds, emphasizing
-.turbulent intensity and the turbulent exchange coefficient.
Particular cases illustrated
include the distribution of
pollutants from hot jets of air (from thermoelectric power
station stacks) and relatively cool jets (from chemical
'-.plant stacks).discharged into atmospheres of various states
!:'of stability. Wind speeds of about 5 a/sac are Identified
as tendihg to produce hazardous pollution from thermal
power plant stacks, and of 1-2 a/sec for chemical plant
stacks. These-fin4loga ar* correlated with results from
studies of the effects of smokestack heightaq temperature
inversionag and atmospherle stratificatlone Orig. art--baw;
35 f0ZUU1aB,.
[WA-50; CBE No, 1
SUB CODE: O4/,-`-SMjM -1joile/ ORIG REP: 005/ OTH UP: C-06 [E
j:

u1 ACC
souncE coDr..; UP/2531/66/000/185/W
NR'AT6035507 D3/66ii~"
AUTHOR: Ba, d ~Ye. (Doctor cCpWc o -maffiematical Mlamw);
Gatkbadchs Te. L; Ilidio%a a3b.
none
'I'TITLr,,: Theory of the relationship of atmospheric aerosol
concentrations
their flow on horizontal plates
~SOURCE: Leningrad. Glavnaya geofizicheslcaya observatoriya.
Trudys no,
!185P 1966, Voprosy atmosfernoy diffuzii i zagryazneniya vozdukha
(Pro-
blems of atmospheric diffusion and air pbIlution), 3-14
1 OIL-
ITOPIC TAGS: micrometeorology, 'ak.-Ik5p*m=d;cYpollution,
atmospheric
.diffusion., aeroEol, M-MI-80-ft-EF meteorological
computerf /LUA/WAt- 0_40 _J~ t4jzc_.A,4,;.,
ABSTRACTMesults are presented of studies of the theory defining
the settling of aerosols from the atmosphere auto horizon-
talcollecting plates, the relationahip between the amounts;
of pollutants collected on the plates and the actual pol-
lutaut concentration at the level of plate installations,
the effects of plate dimensiona and meteorological factors,.
etc* These plates usually have dimensions of several

-TAT6o'-A '-*"-- __
'Xc-ctik -5507
tenths of a motor, are installed one to several motorm
above the ground surface, are coated with an adhesiv6, and
are assumed to be absolutely absorbent, During an inflow
of air, the aerosol'particle* distilbution is disrupted, re-
oulting in-,differences in pollutant concentrations on the
plates and In the surrounding medium. Equations are derived
to express the process of turbulent diffusion of aerosols
above a plate; the fields of motion velocity and the ex-
channe coefficients are taken Into account.
The parabolic-equation of turbulent diffusion of the
aerosol was converted to a difference equation and solved
numerically on a Ural-4 computer. This computer permitted
storage of up to 400 points along z in a single layer,
i.e., up to 400 values of the solution could be stored for
fixed x'O The computations were carried-out for different
values of the input quantities V (wind speed of inflowing
air), X (the turbulence coefficient in the inflowing air),
W0 (the gravitatIonal rate of aerosol settling), and L
(Plate length)* The results Indicated that turbulent
aerosol flows have comparatively little dependence on
changes In va in ithe O-Oel a/see ranges'

I _ACd_NRtAT6035507
The formulas derived permit estimation of the depend-
ence of a vertical aerosol flow on plate dimensions and
meteorological conditions, as characterized by values of
the wind velocity and the exchange coefficient at the level
0
f the plate. The dependence of the ratio of vertical
aerosol flows to their concentrations at the height at
which the plate is installed was established. The values
obtained here are considerably lower than those of the
simplest case, in which the flow around the plate is not
considered, the horizontal component of the wind velocity
u and the exchange coefficient k are not height dependent,
and the vertical component w coincides with the gravita-
tional rate of aerosol settling. Orig, art. has: 3 figures
and 27 foriaulass
[WA-50; CBE No. 141
CEO]
SUB CODE: OV S=.iDATE: none/ ORIG REp: 008/ OTH REF: 001
Card 3,/3

-.EERLYAND,.,N.q.; NIKPLISKIY, YU.I.
Evaluationof the methods of quantitative interpretation
of gravita-
tional anomalies above a vertical shelf. Izv. AN Turk.
SSR.Ser. fiz.-
tekh., khim. i gool. nauk,no-W7-65 163. (MRA 17:2)
1. Mel razvedochnoy geofizlki i seysmologii AN
Turkmenskoy SSR.

YANOVSKAUp B.I.;-~E ~, N.4.-, RESHETOVAp M.N.;
SOKRINAq A.M.
Effect of biomycin on vitamin C metabolism in
experimental Pn---Al
and human oubjectoo Vopomedokhlme 6 no-4:343-350
Jl-Ag 160.
(MIRk 14; 3)
1. Researoh'Teamunder the direction of prof.
B.A.Levrov, Chair
of Therapeutics, Central Institute for Postgraduate
Medical
X-4-4--j M000owe
(ASCORBIC ACID) (AuREancIN)

---BERLYANDP H.S.; R~SHETOVAP M.N.
Quantitative and structural changes in-blood proteins in
rheumtio
defdats of the heart. Nauch. rab. asp. i klin. ord. no.6:4-8
160.
(MIRA 14:12)
1. 1 kafedra terapii (zav. deyetvite,llnyy chlen:AMN SSSR,
prof.
14.S.Vovsl)TSentrallnogo instituta usoverahenat*ovAniya
vraebey.
(BLOOD PROTEINS) (RHEWATIC HURT DISUSE)

Tan AND NOS*J, kand. mad. nauk
I-
Aotivity of aminopherase (tranaaminase) in rheumatic
carditis.
rop. revm. 2 no.2,41-45. Ap-Je~62 (MIU 17 83)
1. Iz kafedry 1--y terapii ( Mv. - deystviteltn7y chlen
AMR
SSSR prof. M.S. Voval. [deceased]) TSentrallnogo
inatituta usover-
ohenstvovaniya vrachey, Moskva.

Ell

USSR/Meteorology - Atmosphere, Tem-
Tan/Feb 50
perature
Conductivity, 7herxal
"More Accurate Theory of the Diurnal
Behavior of
Air Temperature, Taking Into Account the
Change
in the Coefficient of Turbulent Heat
Conductivity
In 24 Hours," 0. S. Berlyand, Geophys
Inst, Acad
Sci USSR, 12 pp
"Iz Ak Nauk SSSR, Ser Geograf i Geofiie
Vol XIV,
NO 1
Shvets previously calculated diurnal
behavior of,
air temperature, assuming the
coefficient of
Om
USSR/Meteorology - Atmosphere, Tem-
Jan/Feb 50'
perature (Contd)
turbulent heat conductivity
depended-only on
height. Diurnal temperature curves
calculated,
~by this method differed by 1-20 C from
observed
curves. Berlyand calculated diurnal
behavior of
temperature, assuming the coefficient of
turbu,
lent heat conductivity depended on
height and
time of day. Submitted by Acad 0. Yu.
Shmidt
21 Jul 49.
0

USSR/Engineering Hydrodynamics Jan 51
"On the Coeff icient of HYdraulic
Resistance Dur- J
ing Turbulent Flow of Liquid in Smooth
Pipes,"
0. S. Berlyand, Cand Tech Sci
"Gidrotekh Stroi" No 1. PP 35P 36
Demonstrates that t he formula for coeff
of resist-
ance, obtained from -logarithmic law
of'veloci*
distribution, is justified also for new
general-
ized law, established by A. D. AlItshull
in his
work published in this same issue. This
is ex-
plained by fact that certain variations
of
1991*0
USSR/Engineering Hydrodynamics Jan
(Contd)
velocities in the core of flow have
almost no
effect on the value of hydraulic
resistance,
detd chiefly by near-wall conditions
subordinate
,to logaritbmic law.
l9w4o

PARIYSKIY, N.N.; BEHLYAND. O.S,.
Affect of seasonal changes in atmospheric circulation
on the
velocity of the earth's rotation. Trudy Geof.inst-
no-19:103-122
'53. (MLRA 7:3)
Narth-Rotation) (Atmosphere)

,--ISULUW.:,9.$. ; SOKOWVSKAYA, L.A.
The functions 106orfe ze Inzho-fixoshur, no.11:121-124 1 158.
(NIA 12:-1)
1. Iftstitut prikladnay geofiziki AN SSSR, G. Moskva.
(Thermal diffUoiVity) (Irrore, Theory.of)

BZMYAND, 00-B.: SEDUNOT, Yu.S.
-, - ~,-. ~ 'C -
Solution of the equation of turbulent diffusion.
Intbe-fizabur.
no.2-1107-112 7 159, (MM 12t3)
1. Institut prikladnor gwfIxIkI AN SSSR. g. Moskva.
(calculus of operations) (Diffusion)

24(8)
AUTHORs
TITIEs
PERIODICALs
ABSTRACT#
Card 1/2
SOV/170-59-5-10/18
Berlyand, O.S.
On One Method of Solving the Diffusion Equation Heat Con.duativity)
Ob..odnom sistode res*heni*a uravnoniya diffuzii 49ploprovodnosti))
Inzhonerno-fizicholskiy zhurnal# 1959# Nr 5, PP 70-87 (USSR)
The equation of-diffusion, having the followin forms
a
C&
W + K,;'~ + K + K
2t a 3 X:'
whers
oto?n
7n= 0
in solved by-th* author Under assumptions that W, ak and
Is are constant and the initial and boundary cond,tion:xipo'o~ is
follows$ 12J'(s~)S at t - o;
0 P +
0 0.

SOV/170-59-5-10/18
Ofi One Method of Solving the Diffusion Equation (Heat
Conductivity)
Here Q is an amount of substance which appeared at the initial in-
stant in a point with coordinates$ X - Y - 0; z - 4 (in the
source). The solution of thim.equation is of importancep in par-
ticular in problies on diffusion of an admixture in A free atmo-
6phere. In this particular case, the meaning of the symbols in
th!a:juation in tho'followingi xy - is the surface of the Earth
z_-in,,yertical coordinate; T - is the velocity of the
falling particl *a I U(s) - is the horizontal componsn't of the
wind velocityj_lx~j ]~-and K are coefficients of turbulent diffu-
sion; q - in tWoone,entration of the 3ubstanoe. The author ex-
poiinds the method of solving this equation and explains the theo~-
retical basis-of this method.
There are 4 Soviet reftrences,
ASSOCIATIONt Institut prikladnoy goofisiki AN SSSR (Institute of
Applied Geo-
physics of the AS UOSR)p Moscow*
Card 2/2

AUTHOR: Berl-vand, O.S. SOV/20-124-3-2/6-,
TITLE% On Some Asymptotic Estimations (0 nekotorykh asimptotioheakikh
otsenkakh)
PERIODICALt Doklady Akademii naukSSSR,1959,vol 124,Nr 3,
PP 507 - 506 (USSR)
ABSTRACTs Theorem: Let be 0 and constant I a - 1 ; z = x.~;O If x and 3) increase simultaneously,
where
Y1x f2-;!51 then it holds
-x 2_ Y2Ax 2 2
2e 1 11 + 3 "4 (5)
Y7 9 + 1 2x2 44
r .(2x)
For (2x)2 > and V.> 1 it holds s
'0? + 1)0? + 3)
1 2(x) >~' 1 (8)
9 >' -1 Wi~' +1 (x)
S/020/61/140/001/002/024
Card 1/3

Asymptotic representationa ...
S/020J61/140/001/002/024
C111/C222
2. IA& - 9 > - 1 z x4-0 . Then for large x it holds s
(11)
X) 2 xv F~i + a-27k (2x)- 2k+ 0 [(2x) -211j + R3J
+Y 7__ k-o ki f- (1+9
f-17 )2 2
where R ~ ~~' (2/x) erfe (x/ T 2). For (2x >,2 it holds t
2
2
Y (- X) +1 - X)
(12) holds also for Y > -1 as (8).
3- 9.!5 - 1 ; z x>,,0. The formulas are obtained by using the
ana lytic continuation of r (1 + /4,) into the region Re /14,
i~- - I and re-
placing +i) by - i) in the developments of the points 1. and 2.
For
2x > i) + 1 it holds t
12 (x)> i
~O ,, 9 1 (x) i_ (x) for -1 (16)
Card 2/5

S/020/61/140/001/002/024
Asymptotic representatinns C111/C222
4. x6 0. The formulas are obtained as above by a
change of,the sign for 9 For integral s Y n and large x it holds
2 -x2 n-1
x) -v -7== a 2x) (19)
n
,r
For fractional y and large x it holds
i- W --j 2 x- Y (20)
__F__
r
A number of further partially known formulas (amongst others
concerning
the connection with the Hermitean polynomials) is given.
There are 3 Soviet-bloc and 2 non-Soviet-bloc referendes. The
reference
to the English language publication reads as follows i E.T.
Whittacker,
G.N.Watsont Kura sovremennogo analiza (Modern analysis), 2, 1934-
PRESENTED: March 21, 1961, ba A.A. Dorodnitzyn, Academician
SUBNETTED: March 20, 1961
Card 3/3

8/020/62/147/005/06t2/032
B172/B112
Oe Set Nazarov, I* Me# Pressmang A# Ya.
AUTHORS:
n
TITLE: An i erfe or complex Gauss - Poisson distribution
PERIODICAL: Akademiya nauk SSSRe Doklady, vs .14Tj no# 59 1962,
1005-1007
TEXT: ~'n events are considered obeying a Poisson law the parameter of
which is a random quantity which corresponds to a standard division
N(xoa,o) the intersection point of which has an abscissa equal to
zero:
2
00 C12
P(n) 2 xn e-x-(!R-x) /2 dx
a f
rf
1+9 Wx d n1 0
cr 2
2
y /4-a 00 2 2
n x-(&-x) /20
S X 0 dx (y 2).
i rf -V-2it d n!~ o
Card 1/2

b/02OJ62/147/005/002/032
n
AnA erf a or complex Gauss B172/B112
n
The probability distribution for such events is called an i erfe
distribution. The mathematical expectation and the dispersion of such
distributions are calculated.
0
ASSOCIATION! Inetitut prikladn y geofiaiki, Akademii nauk 353H.
(Institute
of Applied Geophysics of the Academy of Sciences USSR)
~PHESKNTED: June 259 19629-by N. Ne Bogolyubov, koademician.
SUBMITUD; JunQ 20, 1962
Card 2/2

PETROVA.. G.M.; EERLYAM ..-O.S.
Estimation of the vertical scattering coefficient of a
precipitating foreign substance in the atmosphere taking as a
basis its distribution on the earth's surface. Dokl. AN SSSR
346
P-n.6:3319-3321 0 1626' (MIRA 15:20)
1. Predatavleno akademikom Ye.K. Pedorovym,
(Air-Follutlafi)

L 07989-67 EWT(1) OW
ACC TIR: AP6009417 SOURCE CODE: M/0020/66/166/006/1315/1318
q- LI-
AUT11ORS p&tyqnj_G L it. jtke in, N. _t,; Dqr.~yand,.2 _&
A. ~3
ORG: none
TITIZ: Precipitation or a cloud of'intoracting particles and
the formation of
"dust" sources as 'a rosu1t-.-of_a_'t_r4osphor.ic -diffusion
SOURCE: 'AN SSSR. Doklady,.-V- 1660 no. 6, 1966, 1315-1318
TOPIC TAGS: atmospheric diffusion,'-:atmospheric cloud,
atmospheric precipita-
tion, turbulent flow
ABSTRACT: The concentration distribution of particles in the
atmosphere, in'ter-
j acting with precipitating clouds, is.calculatod analytically.
Particles Vnich
form dust sources and are distinct from the clouds are
described by the source
term =- --~, h
='Sof
Q_
To determine the particle ooncentratio~.q,, tho..fbllowing
equation of turbulent
mixing is solved: llij& Oe + K,,F 2`_5-X a2q i92"'- u 8q
q, Oy
R.04 0- Q
Card 1/2 UDGi 532.516

L 07989-67
i ACC INR: AP6009417
To integrate the above equation -all coefficients are assumed
constant and the
distribution of particles'on tho'earth's surface is expressed by
dt
The solution is given in term of"11hitaker and Gar,= functions
and iD expanded-in'
Taylor series around the point t = T (T hIV). This leads to an
expression of i
the form CO
Ir (2) A-' nP d..L- -L bT OXP BhI (t
b dt-
4
1~ I
I-T
0
XP C). F, (f, Q dt di
The equation is then.used. to calculate Xx and Kz (mixing length
coefficients)
in terms of experimentally,determined values of,q*. Several
special examples
are considered.* The authorsexpress their acknowledgoments to
A,,_Ya. Pressman
for his remarks. 'This paper was presented by Adademician Ye. K.
Fedorov on 9
June 1965. Orig. art. has: 3.1 equations.
SUB CODE: 04, 20/, SUBM. -DATE: .2014ayw ORIG REF: 001
Card 2/2

-BERLY A V'D, O.S. ; KER I CHENKO , L.11. 1; KOr,"N' ,
R.,k I ~
Theory of McDonald's incomplete Dokl. M! ~;Osjl 16A)
no.2;
306-307 Ja 165. (,'.l!Rfi IS: 2)
1. Institut prikladncy goofiziki AN SSSR. Submitted
July 6, 1964.

ACC NR. - AT7-0.0-19-20 SOURCE CODE:
UR/3010/66/000/017/0055/0058
AUTHORi Berlyand, 0. S.; Yerokhtna, X. A.; Kolachavat Z. A.
ORG: none
TITLE: Exchange of air masses between the stratosphere and
troposphere In. the
Northern Hemisphere
SOURCE: AN SSSK. Hezhduvedomstvannyy geofisicbeskly komitet.
Goofinicheekly
byulleten% no. 17, 1966, 55-58
TOPIC TAGS: atmospheric circulation, stratosphere,
troposphere, atmospheric
temperature, temperature distribution
ABSTRACT: This article presents the results of an
Investigation of the mechanism of
exchange of air =ease between the troposphere and stratosphere
for given mean
annual zonal distributions of temperature In the O-rl6 km
layer and the distribution
of atmospheric pressure on the'EarthOo surface by finding a
wind velocity field for
determining the vertical motion of air masses. It was
calculated that during a year
an air mass weighing 3-1014t, which amounts to 52 of the
weight of the entire atmo-
sphere, descends from the tropopausa In the 25-35*N zone. The
weight of the 10-
16-ka air layer amounted to approximately 1/6 of the weight of
the entire atmosphere
Thus, It Is concluded that exchange of the entire air masa
between the tropospUm
and stratosphere occurs within about 3.5 years In the 25-359N
region. Origs art.'
cwd 1/2

0

BERLYAND, F. S.
ITresent Knowledge about the TransmissJon of Viruses by
Successive Generat-ions of Plants,"
in Abstracts of Reports of-the All Union Conference on the Study
of Ultra-microbes an
Filtrable Viruses (14-18 Ijecem')er 2935), Publishing Fouse of
the Aca,-Iemy of Science USSR,
FOSCOW, 1935, pp. 40-41. 448-39 Akl
So: SIRA Si 90-53, 15 Dec. 1953

SMYAND S S .
I How our country's high-
,foklity variety of cultured plants was created
Mookwa, Gov. tzd-vo sellkhoz lit-ry, 1951

BEWA)rD, S. S.
choir engineer Transportation Administration
Narkokchermet
IThe State and Problems or Reestablishuent or
Industrial Transportation in
Ferrous Metallurgy"
Vest. Ak. Nauk SSSR,uo.9,1944

AnLuw.l&.: PIRSEWT, I.Ye.; STOLTAROV, AJ.; YURRVICA, G.S.;
Rummuw. E.G.,; RMSEEKO, I.S., redaktor; Nrrm, O.G.,
tekhnicbe-
skIr re&ktor
Clelhvad transportation In ustallura: a handbook]
2halesnodoroshat
transport Y mt&Uurgii,- spravochnik. Moskva. Ggs.
nauchno-takhn.
isdi-vo Ilt-ry po obarnoi I tevetnoi metallurgii, 1951.
592 P-'
[Kicrofiw (KIM 10: 1)
Obilroads, 14A--trial)

BIRLYANIJ, S!O.. inzhener. r9daktor; MIRRAYLOYA. T.T.;
tekhnicheakiy redaktor
(General report on the progressive praotioe of
intraplant railroad
transport workers: 11ovo-Tagill Ody Notallurgimd Plant)
rmpleklmos
obobahchenie persdovogo opyta rabotnlkoy
vautrixavodskago shelesno-
dorozhnogo transport&. (Novo-Tagil'skil
metallurgicheskiy sayod).
MoBkvao Goo* twuohno-tekhno, Isd-vo lit-ry po qfiarnol
I tovetnot
notallurgil, 1954. 26 p. (MM 7110)
(Railrods, Industrial)

BMLYANDj Sigimund Solomonovich N15
631-303
.B5
Gibridizatsiya Rasteniy EThe Hybridization of Plants-I
14oskva, Sell
Khozgiz, 1957.
317 (1) P. Illus., Diagrs.
I'Literaturall: P. 317-318.

11 J/110 -- -,I
/V D J-1 !
133-11-14/19
AUTHOR: Berlyand, B.S.
TITIZ: rends in the Development of Works' Internal Railway
Transport (Puti razvitiya vnutrizavodskogo zheleznodorozhnogo
transportaL)
PERIODICAL: Stal, 1957, No.11, pp. 1028 - 1031 (USSR)
ABSTRACT: Types of rails and rolling stock, which are being
introduced on iron and steel works are outlined.
AVAILABIZ: Library of Congress
Card 1/1

BARLTAND, S.S.0 Inzh,
-
Strengthening the construction of railroad tracks at
Iron and steel
plants. Blul. TSMICHN rb.'3:,4.10 138. (MM 110)
(Railroad, Industrial-Tvack)

BERT-YAND, S.S.
[Basentials of plant acclimatization]
zataiia restenii. Moskra, Goe.izd-vo
67 P.
(Acclimatization (Plants))
Chto takoe ak-k-limati-
selikhoz.lit-ry, 1959.
(KIRA 13:10)

ORMUKH, Abram. Yefinovich; 5, S. q inzh. . rat
senzant j red.;
. SIDOROV, V.NOq inzh.., red.izd-~a7--rARLqNT, A.I.,
tekhn.rad.
(organization of railroad haulage at metallurgical
plants]
Organizatsila zhelesnodorosWifth perevosok na
metallurgicheakikh
savodakh. Moskva, Gos.nauchno-takhn.izd-vo lit-ry po
charnoi i
tovetnoi metallurgil. 1959. 483 P. (min 12:4)
(Metallurgical plants) (Railroads, Industrial)

SHIMOV, Viktor likolayevich: TAWTAXD, S.S., red.;
DWIN, I.A..
red.isd-va; DOBMINSrJ,jj-.-L-.T-.-.-T-9khn. red.
[Car dwoporo and their maintenanool
Tagonooprokidyvateli I ikh
remont. Kookwa, Goo.nauchno-takhn.isd-vo lit-ry po
chernot, I
tovetnoi metallurgii, 1960. .119 P. (MIRA 13:8)
(Railroads-Care-Maintenance and repair)
(Dumping appliances)

RTABINIKIT, Bronislav Takovlevich; _BRRLTAP S.S., inzh.,
retsenzent; GXRA--
SIKENKO, Y.F., iuzh., retsenzent; did ft IT, Ta.B., in2h.,
retsen-
zent; DASIOTSKIT, Ta.I., inzh., retsenzent; DIORIN, S.S.,
inzh.,
retsenzent; KAMALOT, O.M., inzh., retsenzent; KARPMAH.
M.A., inzb..
retsenzent; KASHCHMO, D.S., insh., retsenzent; KOROISY,
M.N.. inzh.,
retsenzent; KORSAKOT, A.A., inzh., retsenzent; LISEIMO,
T.P., inzh..
retsenzent; PMMIS, I.B., insh., retsenzent; RMAKIN, A.A.,
inzh.,
retsen2ent; ROMAROYIGH, N.D.. inzh.. retsenzent; FRITMAK,
I.A., prof.,
red.; AYRUTSKATA, R.F., red.izd-va; ISLHNTITEYA, P.G.,
tekhn.red.
[Plaiining and economics of metallurgical plants]
Planirovanie i
ekonomikEk mstallurgichesldkh zavodov. Izd.2., dop. i
parer. Moskya,
Goe. nauehno-tekhnAz!-vo-1it-ry po chernoi i tevetnoi
metallurgiig
196o. 736 p. (MIRA 13:2)
(Metallurgical plants)

GIUSIN, Alskeandr Mikboylovich; MOSHMICH, Isay
Yevoeyevich; BEMAND,
S.S._, p2d.; KMORSKAYA, Ye.S., red. izd--ia; KLEYNMAN,
M.-R-.-,-twkbzr.-
~ -re.
iPlanning and work analysis of the railroad
transportation sections
of metallurgical plants) Planirovanie. i analiz raboty
zheleznodo-
rozbmykh tsekhov meta3-lurgichaskikh zavodov. Moskva,
Goa. naucbno-
tekbn. izd-vo 3it-ry po obernoi i tsvetnoi
metallurgii, 1961. 69 p.
(MM .14:9)
(Railroads, Industrial) (Metallurgical plants)

BEWAND _,U=n_SMenovich; DANILICVSX31 V.V. g red. j VAGIN p
A.A. v red
toklm:
iza-va;
rod.
[Brief rAmial for the F81*64d irorker in ferTous meta.Uurgy]
Kratkii stravochnik zhelemodoroibn3ka chernoi metallil gii.
Moskvap Goo, naubhno-teldib. izd-vo lit--ry po chernoi i
tsvetnoi
metallurgiip 1961. 231 (MIRA 34-.8)
(Railroadst Industrial-44aintaimmce and repair)

BERLYAND, Sigiumnd Solmnoviehl-BOYARSLAYAp L.Si,, red.1 GUREVICH,
H.M,j
-redo,
[Plaft bybridization) GibridizatsiU.rastenii. Moskva, Goo. izd.-
vo sellkhoz.lit-ry 1957. 317 P. (KM 15 2)
tkbridizatio3ij Vegetable)

HEIESHKIN, S.M., gornyy inzhener,-_EMYAND,_ S.S_.., gornyy
inzhener;
SIROTKIN, Z.L., inzh.; DBIUSOV, A.G., inzh.; TERNOVSKIY, G.I.,
izjzh.;
EEKHTEREV, Yu.I.p inzh.; ZOTOV, A.V., inzh.; IVANOV, E.I., inzh.;
VASILIMV, Ye.A., inzh.; SOLOVIYEVA, L.G., inzh.; D'YACIMNKO,
V.F.,
Replies to V.V. SbanIkola article "Efficient lindts of using
truck haulage in open pits.79 Gor. zhur. no.1:75-77 Ja 162.
(MIRA 15:7)
1. Gosudarstvennyy nauchno-ekoncmichookiy sovet Soveta Ministrov
SSSR (for I-Ielesbkiv). 2. Promtransproyekt Gosstroya SSSR (for
BerlyaW). 3. Belorusakiy artozavod (for Sirotkin,, Denisov..
Ternovskiy., Bekhterev,, Zotov) Ivanov). 4. Gosudarstven-yy
institut po proyaktirovaniyu razrabotki rudnykh mostorozhdeniy
v yuzhnykh rayonov SSSR, KharIkov (for Vasillyev, Solov'yeva,
Dlyachenko).
(mim haulage
(Shan'ko,, V.C

RYABINIKIY, Bronislav WrovIevich; ADARYUKOV, G.I.,
insh., retsenzent;
BERLYAND, S-S.. inzh., retsenzent; GERASIMENXO~
V.A., inzh.,
retsenzent; GRUDSKIY, V.A., inzh., retsenzentj
DASHEVSKIY,
Ye.B.~, insh., retsenzent; KARFMAN, Ya.I., insh.,
retsenzent;
KOROLEV, M.N., inzh., retsenzent; KORSAKOV, i.A.,
inzh...
retsenzent; LISENKO, T.P., insh., retsenzent;
FEKILIS, 1.B.,
inzh., retsenzent; REVYAKIN, A.A., inzh., retsenzent;
ROMANOVICH9 N.D., insh., retsenzent; FILIPPOV, S.M.,
inzh.,
retsenzent; BRUSHTEYN, A.I., red.izd-va;
DOBTIZHINSKAYA, L.V.s
takhn. red.
[Planning and the economics of metallurgical plants)
Planirova-
nis i ekonomika metanurgichaskikh zavodov. Izd.3.,
perer, i
dop. Moskva, Metallurgizdato 1963. 754 p. (MIRA 16:4)
(Steel industry-Management)

KOSTENETSKIY, Kirill Favlovich- BERLYAND, S.S.p
red.; YUSFIN, Yu.S.,
red.izd-va;
I
(Development of transportation in metallurgy;
problems in
the general plan of and transportation in iron and
steel
plants] Razvitie transports v metallurgii; voprosy
gene-
rallnogo plans. i transports metanurgicheskikh
zavodov. Mo-
skva, Metallurgizdat, 1963. 332 p. (MIRA 17:3)

~ T. G.
"Radiition ind Heat Balance of the ETC", Tru�Z GGO
(Broceedings of the GGO)
No 10P 1948.
SO: U-3039, 11 Mar 1953
0

30765. BERLYANPT. Of
Radiatsionnyy i ttPlovoy balansy poverkhosti sushi
vnetrop4-cheskikh shirot
severnogo polushariya. Trudy Glav. geofiz. observatirii,
vyp. 18, 190,
c. 22-50. -- Bibliogr: 26 nazv.

BEIMYAND, T.
"Dktirtinins t4 Earth's Effective Radiation Tak-
ing the Influence of Cloudiness Into Account,"
M. Bglyamaj T,.,Ber1yftndj Main Geop*o'Obs
"It.Ak Nauk BBBR, Bar Geofiz" No 1, pp 64-78
Suggests a theoretical-mothod for computing the of-
'fective terrestrial radiation under actual con-
ditiop'i takini Into account the influence of cloudi-
noes. Discusses cacparison and analysis of some
kn~vn empirical relations. Gives tables and eivple
formulas for cl6udy and clear siy. Explains effect
of cloudiness'in various clUates. Authors thi~ik
X.-I. Du4YbD.and_.Prof M. 1. Yudin for advice. Sub-
Mitted 41 _51. 205T45

6014-7 G
A
,%jQiXmD. T.G
Changes in soil moisture content and In the host balance
durivg arld'
yeare. 11rady GGO n0.29;85-96 132. (MIRA 11AI)
. (soil uoisture) (3olar radiation)

IVSc,R/ Geography - Meteorology
Card 1/1 Pub. 45 - 3/17
Authors sBudyko, M. I.; Berlyand, T. 0.; and Zubenok. L. I.
Title $Heat balance of the eartbts surface
FeriOdlWa I Izv. AN S55R. Ser. geog. 3. 17-41. May - Jun 1954
Abstraot I An account is given of the work of scientists in the past
in studying
the problem of the heat balance of the earth's surface. From the
results
of these studies a formula is derived as follows: R + LE + R A- A =
0,
where R is the radiation balance of the underlying surface; LE, the
ex-
penditure of heat in evaporation; P, the turbulent heat exchange
between
the underlying surface and the atmosphere; and A, the heat exchange
be-
tween the underlying surface and the lower strata. In harmony with
this
basic formula an analysis is made of the heat exchanee on land and
sea
over the whole world, taking into account also the factor of light
re-
flection. Thirty-four references; 27 USSR; 5 Germanj 2 USA
(1925-1952).
Maps; grakhs; tables.
Institutiont A. I. Boekov Main Geophysics Observatory
Submitteds

BERLYAND, T, Go, BUDYKO, M. I. and ZUBaWK, L. 1.
"Procedure for Climatological Computations of the Components
of Heat Balance".
Trudy Gl. Geofiz. Observ, No 48,, pp 5-16, 1954.
The equation of heat balance can be represented in the form
a f LE-j-
P-4- A.10, where R is the radiational balance of the
underlying surface, LE
is the expenditure of heat in evaporation, P is the
turbulent heat exchange
between the underlying surface and the lower lying layers.
For dry
land the quantity A is equal to the change in heat content
of soil over a
definite period and inthe mean year is close to zero. For
oceans the
quantity A in the mean year is equal to the input or output
of heat in con-
sequence of horizontal heat exchange connected with sea
currents. In con-
clusion the authors present ekamples of computations of the
components of
heat balance for Moscow and a point on the ocean. (RZhGeol.,
No l1,, 1955)
SO: Sum no 884j, 9 Apr 1956

BERLYAND, T. G.
Yearly Behavior of the Total Solar Radiation According
to Data of Actual
Observations
The author summarizes the measured values of the total
radiation for
individual months and for the year as a whole at 139
pints arranged in
the Interval of latitudes from 840 soath to 340 north.
The graph of the
distribution of total radiation eccording to latitude
displays its gen-
eral increase from pole to equator and increase in the
range of the annual
variations In the radiation at one and the same
latitude. Decrease in the
values of the annual magnitudes of the solar radiation
in the lower lati-
tudes is explained by the increased cloudiness in the
equatorial regions.
The author graphically represents the latitudinal
variations in the ratio
of total radiation for June and December to the total
radiation for the
year as a function of latitude. In June this ratio
decreases with de-
creasing latitude, and in December it increases, but
the fraction of the
monthly influxes of total radiation (out of the yearly
value) for both
June and December is almost the same for the lower
latitudes. (RzhGeol,
No. 4, 1955) Tr. G1_ renfIZ. absery 9 No. 48, 1954,
17-25.
SO: Sum..No. 744, 8 Dee 55 - Supplementar7 Survey of
Soviet Scientific
Abstracts (17)

1IRLYARD, T.G.
Annual total solar radiation computed on the basis of
factual
observational data. Trudy GGO no.48:17-25 154. (MIRA 10:7)
(Solar radiation)

PAR" -WZ" MWINOVA. N.A.
Nonthly charts showing total solar radiation wA
radiation balance
for the Soviet Union. Trudy GOO no.30:4&82 135. (KML
9:8)
0501M radlatim)

SOV/124-58-1-845
Translation from: Referativnyy. zhurnal, Mekhanika, 1958, Nr
1, p I I I (USSR)
AUTHOR: Berlyand, T. G.
TITLE: Th~eAtmosphe`ric Heat Balance of the Northern
Hemisphere
(Teplovoy balans atmosfery severnogo polushariya)
PERIODICAL: V. sb. :A. I. Voyeykov i sovrem. probl. klimatol.
Leningrad,
Gidrometeoizdat, 1956, pp 226-252
ABSTRACT: Utilizing various data available from world
literature the author
constructs maps of various components of the atmospheric heat
balance of the Northern hemisphere. Annual maps, as well as
representative monthly maps for the various seasonal periods
(March, June, September, and December) are provided. The
presentation includes maps of the radiational balance, the
turbulent
heat fbix (annual only), the heat of condensation, assumed to
be
approximately equal to Lr, where L is the latent heat of
condensa-
tion and r is the amount of precipitation, which is
determined as
the residual term of the atmosphere heat-balance equation.
Graphs
of the zonal distribution of the above-mentioned quantities
are adduced.
Card 1/1 A thorough analysis of the material obtained is
provided. 96 refs.
Ye. M. Dobryshman

BIWAO, T. G.
Zonal distribution of currents of total molar radiation
entering
the earth's surface. Notoor.1 g1drol. no.9:22-25 8 156.
(Ma 9 111)
(Solar radiation)

UTIMAGANMOV, U.N., kand.geogr.nouk; 'BER T,G.,
kand.geogr.nauk;
BANXEMIT, Sh.A., kend.fiz.-Z riouTIO-MMM, M.1h., Imnd.
Geogr*nauk; KUSMSOV9 A.T.. kand.geogr.nauk; CHUBUKOV,
L.A.,
doktor geogranuk; MVYR19VA, Yu.G., mladshiy nauohnyy
storadnik;
UTISM, A.S.. kand.geogr.nauk; GOLIT93M, I.A., doktor
geogr.
nauk; KLYKOVA, Z.D., starshiy nauchnyy sotrudnik;
KRIISHIKOVA,
Te.A.. mladshiy nauohnyy sotrudnik; GELIMGOLITS.
N.F.. starshiy
nauohnyy sotru"ik; PRMOROV, I.I., starshiy nauchnn
sotradnik;
WOMO, N.S., mladshiy nouchnyy sotradnik-, EMANOVI,
L*P*,
red.; BRAYNINA, M.I., tekhn.red.
[Climate of Xazakhatan] Elimat Kazakhstana. Pod red.
A.S.Ute-
Bheva.. Leningradq Gidrometeor.izd-vop 1959. 366 p.
(MIRA 13:5)
1. Russia (1923- U.S.S.R.) Glavnoye upravlaniye
gidrometeoro-
logichaskoy sluzhby, 2. Kazakhakiy pedagogicheskiy
institut
(KazPI) (for Utimagambetov). 3. Glavnaya
goo-fizicheakaya observe-
to'riya im. A.I.Voyeykova (GGO) (Tor Berlyand,
Gol'tabarg). 4. Ka-
sbkhakiy nauchno-issledovateliskiy
gidrometeorologichoskiy insti-
tut-KazNIGKI) (for Bessvirkhniy, Baydal, Kisneteov,
Uteshev, Ily-
kova, Men'shikova, GelImplits, Prokhorov, Tkachanko).
5. Insti-
tut geografii Akademii nauk SSBR (IG AN 33M) for
Shvyreva).
(Kazakhstan--Climate)

P&M I BM MUUMATION &9/5475
USSR. Glavnoye upravleniye gib-pteor-ologicheskoy sluzhby
Teplovoy I vodnyy rezhin zemoy poverkhnosti (therml and
Water Regime of the
Earth's Ojerface) J&rdngrad1VzftvwL+,eo:Lza&tL, ig6o, 191
p. Errata slip
inserted. 600 copies printed.
Sponsoring Agencyl Glavnoye upravlemiye
gidtmeteorologicbeskoy sluzhby pri
Sov te Ministroy BSSR.
Eds.(Title page)$ I. P. Clerasiwwj, ~ca&micianj* M. L
Budyko,, Doctor of Physics
-A*d*Mathezf atic 6p' =4 k, Pq OeMltsov., Doctor of
Geographical Sciences;
Ed.: M. M. Yasnogorodskaya; Tech. Ed.: M. 1, Braynina.
F1 TOSE: This publication Is intended for geophysiclstsj,
geographers., clim-
tologistsp agronomists., and agriculturists.
COVERAGE: The seventeen articles contained in this VAb*
tion represent con-
densed versions of reports presented at the GonfereadeV
the Heat and Water
Regime of the Earthos Surface, convened by the QjwVnaY&
geofizicheskaya
observatoriya, im. A. 1. Voyeykova (Win Geophysical
Opservatory imeni
Card 115

Thermal and Water Regine (Cont.) SOV/5475
A, I. Voyeykov) in April 1950. 'Individua articles deal
with the investi-
gation of the thermal balance of the ewthts suxfacep
problems of the genesis
of climate related to beat and moisture exchange., the
indicators of heat and
vater balance in agricultwe,, and problems related to the
effect of hydro-
mteorological factors upon complex geographical processes
and phenomena.
No personalities are mentioned, References follow
individual articles,
TANZ OF COMBOM:
Budyko,, X.I. [Main Geopibysical Observatory Jim-ni A.I.
Voyeykov).
Heat Balance of the Piarth's Surface 5
BeNj "an p-T~G. EWJ- Geopbqsical (Ibserv&t6ry imeni. A.I.
Voyeykov].
Global Distribution of So1w Radiation 3A
Yanishavoldy., Yu. Do [YAln Geolftelcal Observatory Imeni
A.I. Voyeylwvl. Nethods 6f Actl tric Imstigations 23
Dzerdzeyevskiyp B, L.p wAYU, L, Rauner jUstitut geografii
AN SM -- Institute'of Geography~AS UM], The State and the
Tasks of Investigating the Reat Balance of a Forest 29
Card 2/5

Thermal and Water Regime (Cont.)
SOV/54T5
Kalinin.. G.P. (Tsentralinyy institut grognozov -- Central
Institute
of Weather Forecasting]* GerAeral Re"ons for the
Investigation of
Water Balance 42
ropov.v O.V,., and V,X, Kuznetwv 14osudarstrennyy
gidrologicheakiy
institut -- State Hydrological Institute]. ExperAwntal
Investigation
of the Plements of the Water Balance on Dry Land 48
Llvovich, X.I. (Institute of Geography,AS USORI, Wthods of
Ruoff
Investigation on the Basis oflWater Balance 62
Budagovskly., A.T. [Institute of GebgMVhyyA8 USMI.
Investigation
of the Water Balance of Soil T1
Galltsov A P. [Institute of Geo, ~VjjAS USSR]. The State
and the
Tasim Studi a of-the Qimte
82
Go
ry iment At I
i ,
rk
0_;W -en
-Nwie'- bUii bf Ue~'. ry-'o- 0' 96
.1. in d 1, tory i meni A.Wl'~,'Yeftov].
Lqsturs e-In 108 are 107
cam 5/5

Thermal and Water Regime (Cmt.) SOV/5475
Timofeyev, M.P. (Main GeoAysical Obsermtory IMU1 Aj,
Voyeykov].
Heat Balance and the Microclinat-e- 120
Grigorlyev, A.A. [Academician, Institute of OeogrspbyyAS
USSR], The
Role of Heat and Moisture Exchange in the Structure and
Developmut
of the Geographic Mantle (Mainly in the Lowlands of the
Temperate
Zone) and Their Significance in the Productivity of
Agricultural Crops 128
Gerasimov, I.P. (and G.S. Pogodina, Institute of
GeographyAS USSR].
Hydrothermal Factors in Soil Formation 144
Volobuyev, V.R. [Akademiya nauk Azerbaydzhanskoy SSR -- AS
Azerbay-
dzhanskaya SSR3. Total Expenditure of Energy for Boil
Formation in
Relation to the Hydrothermal Conditions 162
Lavrenko, Ye. M. [Botanicbeskiy institut AN
SSSR--Botanical Izetitutep
AS USSR1. Hydrothermic Factors and the Geography and
Ecology of the
Vegetation Cover 180
Card 4/5

Thermal and Water Regime (Cont.)
MV/5475
Davitaya, F,F. [Central Institute of Weather Forecastirig],
Water and Beat Regime of the USSR sod Sam Problems of
Agriculture .1,86
AVAILAM: Library of Congress (OB665.R8)
Card 5/5
JA/dvm/ms
9-12-61

B007YI3007
AUTHOR: Barlyand, , G.
TIME: Methods for Climatological Calculations of Total
Radiation
PERIODICAL: Meteorologiya i-gidrologiva# 1960t No. 6p ppe 9-12
TEXT: The elaboration of an indirect method of calculating
total
radiation is described. This method consists of two.stages:
the first
stage consists in determining total radiation under a
cloudless sky, the
second - under a oloudy sky* For the first stage the method
used by V. N.
Ukraintsev is mentioned. He determined the possible radiation
for several
points of the USSR, whereas the author of the present paper
worked out
this method for.the purpose.of determining radiation on the
entire globe
for a cloudless sky (Ref. 2). On the basis of the data for
arctio
latitudes at present available as well as of those for the
tropics of the
northern and southern hemisphere, Table 1 gives the precise
values for
the total solar radiation for all latitudes at a cloudless
sky, reduced
to the international standard scale of 1956. On the basis of a
comparison
80845
S/05 60/ooo/o6/u/ov
Card 1/2

80845
Methods for Climatological Calculations of S/050/60/ooo/o6/02/021
Total Radiation B007 B007
between the precise values for the possible radiation and those
obtained
previously (Ref. 2) by the author, conclusions are drawn. As
regards the
second stage, the author in his earlier paper used the linear
relation
of the Angstroem-Savinov type. On the basis of these new data
this
relation was chocked. It was found on this occasion that the
relation
mentioned is not linear, but that it may best be expressed by
the formula
Q
- . I - (a + bn)n. Q is the actual total radiation. qo - the
total
Q0
radiation at a cloudless akyp n is the cover of clouds, a andb
denote
certain coefficients. b remains approximately constant and is
equal to
0.38, which simplifies the calculations. By means of these
relations one
obtains values with the relative error - without considering the
sign -
of not more than 8 to 10%, and a mean error - considering the
sign - of
about 3%. In Table 2 the a-values varying accoriding to latitude
are given.
There are 2 tables and 6 references: 5 Soviet and 1 English.
Card 2/2

BE=
_PP99APL'Ta ar otv. red,j USHAKOVAt T.V.p
-Adsox-mm BUDY p a
red.; YPMOGORMSKAYA, M,M,q red.; BRWINA, M.I.9 taklm.
red.
[Distribution Of solar radiation ov'-6r continents]
Raspre4sienie
Soln8Qhnoi-TaAiatsii*xm kontinentskh. Uhingradl
Gidkrometeor.
W-vo, 1961. 255 p. 'maps (KMA 140)
(Solar radiation)

AUTHOR:
TITLEs
PERIODICA:L:
8/169,/62/000/009/074/120
D228/D307
Berlyand. T. G.
Solar radiation distribution on continents
Aeferativnyy zhurnalp Geofizikaf no. 9, 19629 16-17j~
abstract 9B112K (L.,,Gidrometeoizdat, 1961', 227 pp.,
illust., maps, tr. 4k.)
.TbJLT: Tne main pavuerne in -une geograpnio aiairiouTion oi soiar
radiation are stated. They were'obta:ined as.a result of generaliz-.
ing observational data and using contemporary climatologic calcu-
lation methods. Ch. I is devoted to the question of the world dis-
tribution of-solar radiation in relation to astronomic factors.'
Ch. II describes methods of measuring solar radiation (instrulaento
for measuring the short-wave*tadiation intensity and methods of
..meaBuring the sunshine duration and determining cloudiness). Me-
thods for climatologic solar radiation calculations are stated in
Ch. III. Ch. IV considers: the dependence of solar radiation on
--.the form of cloudiness; the ,-geographic distribution, the annual.
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S/169/62/000/009/074/120
Solar radiation distribution D228/D307'
variation, and the diurnal variation of cloudiness; and the geo-
graphic distribution of the duration of sunshine. Ch. V gives-the'
characteriatic of the current data of observations on the world
actinometric network. The question of the solar radiation's diur-
nal and annual course, the correlation between summary and scat-
tered radiation in different.parte of the world, and-the variabi-
lity of total solar radiation and its components is considered.
.The state of the question on the stu4 of the summary radiation's
geographic distribution is discussed in Ph. VI, and new world to-
tal solar radiation charts are described. Information is given
about the radiation regime of.Europe,Asia, Pfrica, Australiap
North and Central Americat the Aretic and Antarctica. 421 refe-
rences. /-Abstracter$a notevOomplete:iranslation-_7 -

P
4 PERLYAND., T. 0.
Dissertation defended at the Institute of Geography
for the academic degree of Doctor of Geographical
Sciences:
"Solar Radiation on Continents."
Vestnik Akad Nauk No. 4, 1963P pp. i19-145

iACCESSION NRs AT4026426 S/2531/63/000/139/0003/0015
JAUTHORt Berlyando To Cog Mukhenberg, Vo Vo
TITL9: Role of absorbed radiation in forming a radiative balance
SOURC'Et Leningrad* Glavnaya goofiticheekaya observatoriyao TrudY*0
no. 139, 1963. Toplovoy batons (Heat balance), 3-15
I
TOPIC TAGS: total radiation, absorbed radiation, reflected
radiation'.
albedo, climatic condition, humidity, effective emission,
temperature
radiative energy
ABSTRACTt The total radiation received'by the earth Is partially
absorbed by the incidence surface and partially reflected* The
reflectivity is called albedo, The absorbed radiation Influences
local climatic conditLonso Maps have been drawn for various lati-
tudes at various seasons which characterize the distribution of
absorbed radiative energy on the earth, especially on the territory
of
the Soviet Union, 'Snow and Lee cover increase the local albedo, In
C,,j.1/2

1ACCESSION MRS AT4026426
Ivinter, the absorbed radiation In low In the Northern
Hemisphere be-
~susa-0 thesuall quantity of total radiation and high refleation
.from snow. The local radiative balance depends upon the absorbed
I
ienergy and the effective emission in apse** The latter Increases
iwith temperature increase and diminishes with an
Lncre&se,Ln'humL-!
idLty. In summer# Antarctica and the Arictic Ocean receive more
radia-
itiva energy than the xquatorial belt, but the high reflection I
!-diminishes the thermal influence* Orige arto hass. I tablop 7
filures,
!'and 2 formulas.
1ASSOCIATIORt none
;SUBMITTEDs'- 00 DATE ACQi 16Apr64 ZNCLt 00
gU'B,
CODES As no RRIP SOVI .011- OTHERs 003
7Cmd 2/2

BUDYKOO M. I.; BTMR~~ YEFIbUVAj, N. A.
"Study of the solar radiation regime on the surface of
the earth."
paper presented at the Atmospheric Radiation Symp,
Leningrad, 5-12 Aug 64.

BERLYAND, , doktor geogr. nauki ROGOVSKAYA,
Ye.G., red.
- --I- ~. I., ~
[Actinometric reference book: foreign countries;
annual
data] Aktinometricheskii sprdvochnI : zambezhnye
strany;
ezhogodrqe dannye. Leningra , Gidrometeoizdatp
1964.
261 p. (MIRA 17:6)

L1733-66 Dn(l) GJW
ACCESSI6~ NR:" AT5022066 UR/2531/65/000/179/000
_/0027
AUTHOR: h=&and, T. Go
ITITLE, Daily variation in solar radiation in the principal climatic
zones of ibe
earth
SOURCE: Leningrad. Glavneya geofizicheskaya observatoriya. Trudy,
no. 179, 1965,~i
Teplovoy,balans (Heat balance) -3-27
I' ~_, L4 915 5
TOPIC TAGS: climatology, solar radiation
ABSTRACT: The factors controlling the daily variation in direct,
scattered, and
total radiation are examined for a cloudless sky and for actual
conditions. The
data used are hourly values of solar radiation obtained at 64
stations of the world:-
wide actinometric network over a period of 2.5-15 yr. The primary
factor considered
was sun height and how this is reflected in latitudinal radiation
variation. Graphs
are presented to Bhow how the hourly radiation value varies with sun
height and with
latitude for different times of the year. In the equatorial zone the
sun is very
high, and the length ceft is hAtky constant, with cloudiness the
principal factor
affecting amounts of radiation.~ Monsoon regions show seasonal
variations because
of seasonal cloudiness. The characteristic feature of the tenperate~
zone -is thin- -
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L 1733-66
ACCESSION- NR: AT50220 0
!great contrast in solar-radiation between summer and winter, caused by the
large
annual amplitude of sun height at noontime and by the length of day. Greatest
vari_~
ation in noon height of the sun and In length of day is found in the Arctic
and
~Antarctic. Because of cyclonic circulation, the Arctic offers less favorable
con
ditions for incidence of solar radiation than the anticyclonic circulation of
the
!Antarctic. Orig. art. has: nfigures and 13 tables. [041
JASSOCIATION: Glavnaya geofizicbeskaya observatoriya, Len.ingrad (Main
Geophysical
Observat2a)
4 4, 5
SLMMTM: OD ENCL: 00 SUB CODE: Es~ AA
RO REF SOV: 015 MM: 010 ATD PRWS:
L/A.

L 1961-66 EWT(l) GW
4ACMIMON NR: AT5022061 UR/2531/65/OOO/lT9/0028/0040,
AUTHOR: Berlyand, T. G.
MITLE: Variability of solar radiation reaching the earth's surface
SOURCE: Leningrad. Glavneya geofizicheskaya observatoriya. Trudy,
no.,179, 1965.
Teplovoy ballans (Heat balance), 28-40
~~"scattered radiation, total radiation,
TOPIC TAGS: solar radiation~ solar height,
,climatic condition
!ABSTRACT: The ratio of maximum to minimum solar radiation for
various regions of
-:the earth is determined and represented in a table in the original
article. The
'edifference between the diurnal maximum and minimum of total and
scattered radiation
.is greatest in desert and monsoon regions. The relative change in
the minimum and
7maximum of scattered radiation depends upon total rad-istion,
Diurnal changes in
rscattered radiation are less in equatorial regions. The change in
total radiation
rdepends upon the change in direct solar radiation. Variations in
monthly values of
;,total and scattered radiation were determined from their deviations
from a mean vallue
-based on observation data obtained over a ten-year period.
Variations in total an 'd7
,scattered radiation increase from winter to sit er because of the
increased solar
Card JJZ

L 1961-66
'ACCESSION XR, AT5022061
~height at noon and the longer daylight. Monthly variations in total
radiation are
t
7greater at high and middle latitudes and in regions of unstable
weather conditions,
!Variations in direct, downwelling, solar radiation depend upon
climatic conditions
,:and the position of the observer; In polar regions the variations
are greater than
.in the tropics. Orig. art. has: 5 tables, 3 figures, and 2 formulas.
[Er)
.ASSOCIATION: G'Lavnaya geofizicheekaya observatoriya, Leningrad
(Main Geonhysical
-4,
2SUBMITTED: 00 ENCL: 00 SUB CODE: AA EJO
JNO REF SOV: 008- arm: 000 ATD PRESS:

- nIVOKHATSlIT. L. rodaktor; XOGIUMXIT, B.,
tokbutchaskiy
or
(Odessa; a guidebook and directory] Odessa;
sprovochnik. [Moses]
Oissakoe obl. lid-vo, 1957o 246 p, (KIM 10:6)
(Wesse-4irectories)
4