SCIENTIFIC ABSTRACT VORONTSOV, P.A. - VORONTSOV, P.B.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001861010006-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 14, 2001
• Sequence Number: 6
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

14
01
.1-1 23
aml D~)bryshmnVn r. M., Soveshckanle P4 VOPfQ"M 1141144"AR&
Meteorological Abate I I -
tr omatall VOSM134- I.Conlerence on the riiiestion 0( InVestilgating the transformatlon of
Vol. ~ Ito. i air.] Afettorobflk i GUrplogiia, No. 8:49-50. Aug. 19$2. DLC-Revkw gir mettifts hdd
Jan. - 1954 by the Central GeophZsic%l Obse t In cooperallon wlth the CentrArAtrolor"I Ob.
Part 1 wrvatory, - IM11111te-14 F=Ati- nd - C~EVM 0
WSV and ~, The adialwfic air transformation (rcgx)rt by S &'GAt=ROV)-
cturs and Physics INA air Ms.- 1L.. 'k I W99 .........
Stru T 316ir-mat,91, .,-. W."
burT.", heat trans ormat
Of tho Atmosphere mass" (by NJ. I,, BERIJAN and Investilati= of free af-phae (by V.
ASTMV and IL Arjj=-xmw~ us . Special reports on air trand
~y ""My (fternfac*%Dblem)
lt]Dtm (change of climate). Subjed Ilea CS: 1.7 tr mudy gy
X Conference&- N. T.Z.

VORONTSOT, P.A.
wl
vr,~~ t, ,
i ~,
- d~iiacteristics of IOC&I vinde in the vicinity of the Mo=t Ilbrus.
Trud7 GGO no.32:47-62 152. (KIRA 1111)
(11brup'q Kount,Winds)

ve /?1- 14
VORORTSOV, ?.A.
Accuracy of the balanced pilot balloon method. Trudy GGO
no.32:69-80 152. (MIRA 11:1)
(Balloons, Pilnt)
(Hateorolog7--Observations)

A 7- - Z, '/ /..), )
,.~ C, ,
VORONTBOV,.P.A.
. Aerological conditions during the dry periods of the suzzw of
1951 in Kamennaya Steplo Trudy GGO no*36slO5-126 152a (MIU liti)
(Talovara District-Meteorology)

Tte Co=ittee on Sts.Lin Prizea (or tte vo=au of Ministers =*,R) xn tnc-
fio,lence and Inventions anxxxgacos t"t the falloving scientific workb, pojo-i-Iax- s:!Ier;-.
tific books, and toxtbooks have beLen submitted for competitiock fo7- Stalin ?rlzvti, for
the yeara 19.1Z and 1953. (~Emt~-B~N~KU~L-U-I-rav *.)bcaw,, No. 22-40,t 20 FeLo Apr
NWW Title of Work Flomitated bi
Of th,-,-
Lnykht7nn, D.L. "Icr-cli~iatc- of A~-icul- 1mmi A.T.
Yurlin, 1'.."
L. a Field:7, Ttn
K-Licherov
In'r nnl
Forlyand, I Y Cf artlclcs)
Kmslkov,
""inofeyev,
Vcrontsov,
SOt W-306)4, 7. JuLY 19514

r. A.
oome ;)ata on the Conditions for the Formation of Hoarfrost (izr-.orozl) in
Yountainous Re7ions," Yeteorol. i Eidrologiya, I.To P, lc,5), pp 2~'-330
According to observations on Ellbrus in the sun-:-er of" 1940 for a wind of 5-6mlsec
it seems that if a cloud or fog consists of supercooled drops less than 7-8 microns in
radius the formation of hoarfrost must 149 expected. For sizes of drcps 7-15 microns
the formation of snow-like hoarfrost is observed; for sizes 15 microns and larger the
hoarfrost is in the form of glnzed frost (gololed). (RZhGeol, No 5o 1954)
SO: Sum No. 5(8, 6 Jul 55

-le,-- of' uver `jtt~jn j.-iold
Avolo 1c,il
arld Ove~ n
Tr. G 1 0_1 I s e r 0
Reaultz; of e porimental i4ea5uremc.,itu of tkw structuro u;
I tbe
over Vac on a 13 ?a -it ral -in , over tia a ooal,laucrt "Lunit.fir otl
carried out durin.- t:;c O~umnor ol' 19'b-2 ,-Ire jp~~Cj~J etulp:,wilt,
such az c~ipi.,~_ve i~alloonz, wil on
viere used to reiiztar ti-e -,nf~ Vertleii]. romponontv W' tt~c;
wInd . 'i urbulo two COTIMIC, L, t. Ica 1 5 fl-A I w i~ lo , &Iv'I loli o 1). i
Vcijof~ItV, i.!,rr_lCU[-x!3 ;~i j~,t-~ ne6. 2)
19.,j5 )
S.J: ~Duii,,. 4',.~2, 12 ~,Iay 55

VORONTSOV, P. A. and KAZAKOV, L. A.
"Peculiarities in the Wind Cyole Over a Cotton Field and a Samidesertp"
We Ole geofiz* observe, No 39) 19539 pp 133-1112
Results of expeditional studies of aerial currents in the lower atmos-
Phere over a cotton field and a semidevert, aroung 20-25 km apart., are
de5oribedo Direction and velocity of wind were measured either by a pilot
balloon or by an aerostatic meteorograph,
RZhFiz$ No 3, 1955

VORONTSOV, P. A.
"Investigation of the Influence of Forest Belts Upon Wind by Means of Equipoised
Balloons".
Trudy Gl. Reofiz. observ. No Id4., PP 91-103P 1954.
Methods of studying the wind field close to forest belt by way of
basis observations on equipoised balanced pilot-ballons is described. By
means of them during observations in the Nansen sovkhoz, in Kamennaya Step',
and in Pakhta-Aral, it was possible to clarify the distribution of horizontal
and vertical component velocities, and also the presence and even dimen-
sions of atmospheric vortexes. Observations were maee most frequently of
all on weak winds. (RZhGeol, No 8, 1955)
SO: Sum No 884, 9 Apr 1956

VORONTSON, P. A.
."Investigation of the Influence df Balanced Spheres."
SOi Problems of Agricultur-1 and Forst Climatology." 116 44(106),, 1954p page 91.

VORONTSOV, P. A.
"Certain Problems of Instrumental Observations on the Bumpiness of Airplanes".
Trudy G1. Geofiz. ObseML.
., No 47, pp 28-39, 1954.
Procedure for handling of tapes from accelerographs is given, and
certain characteristics of the atmosphere's state which are obtained by
these readings are discussed. Use is made of the data of exreditions of
the Main Geophusical Observatory in Kamennaya Step' in 1951 and in Pakhta-
Aral in 1952. The accelerograph as receiver had a load suspended on springs
and joined by a system of levels with indicator. A correlation was obtained
between accelerograph readings and the roughness of the under-lying surface
(steppe, forest, etc.). The coefficients of turbulence were obtained from the
data of the accelerograph. (RZhGeol, No. 11, 1955)
SO: Sum No 884, 9 Apr 1956

"'!he Transform~ation of i--ir Uver a Liralted ','later :jurface In ~.Vlnter time"
Tr. bil. ueofiz. Obgerv., k, 47, -)p 63-70
Characteristics of aerial ~msisses 3W to ;.)OD trieterzi hi,--h ai4~,lyzed.
Records from a iaeteoro--.Yaph o-I-icj,.,ed a depeluence ol the altitude. of t'le
inversion layer on the ,.:ir temperature at a 2 rreters hei:;,it, rarii in the
~behavior of the -vertleal te-loorature r-radient 0"IL.-V VMter Or luni.
(RZhFiz, No 2. 19,55)
0"01 31.1111. 4~i2, 1~~, Mmy ~Jh

VOROTTES011) P. A.; Pinegin, G. 11.
"Concerning the Cloud Gauge OP-3"
Trudy Gl. Geofiz. Observ.,, No 47, 1954, 80-93
The results of tests of the cloud gauge OP-3. 'nie instruments ie con-
venient In handling, simple, and stable; itG principle of action Is based
on the variation in the resistance of a sensitive element due to humidity
of the surroundino medium. Variation in resistance induaca a chnn~e in
the tone of the sound signal received by n rQcctvcr. T.'ne T;ioment of cbnn~e
of tone of the si~,nal corresponds to the momont of' entering nnd ].eav1rLc,,,
the cloud. The results of investigations nhowed that, the cloud Gauge gives
a tone cbanE-e in re-gions where there is no visible cloudiness, but -wrliere
thereis a small quantity of fluid drops invisible to the eye. During
icing of the itrArument it al,3o gives a tone chan,,,7c independently of
change in mositure content in the medium. 'Fnisirstrument cannot be rec-
ommended as a network inctrument because of its errors in cloud thickre3s.
(RZhGeol, ITO 9 11955)
SO: Sum-0 845, 7 Mar 56

~w . ~:- - - - - - - -
. 1. 1. r 11 ; .- - ". -A

AMIPOVA, Ye.P.;VORONTSOV, P.A.;GLIMA, M.Yo.; GOLUBOVA, T.A.; ROKMOVAJ9.1.
Outline of the operstional area and obserTation methods of the 1953
general hydrometeorelegical, expedition in a drained swamp. Trudy GGO
no.49:3--10 155. (MLRA 91-1)
(Keteorelogy, Agricultural) (Reclamation of land) (Swavpd)

VOROWTSOF, P.A.
IxTestigatiez of air current directions and zoaturnal radiation
inversion in Aections having varying degrees of drainage. Trudy
GGO se.49:68-84 155- (KM 9:1)
(Atmoshere) (Selar radiation) (Reclamation of land)

VORONTSOV, P.A.; SELITSUU, V-1.
Sounding balloon methods for investigating the atmosphere. Trudy
GGO no.51:3-16 '35. (KLRA 9:8)
(Balloons, Sounding)
(Meteorological instruments)

" I fl~`- I --~ -,.. w .
VORONTSOV P.
- .....
Using balanced pilot balloons and slov-aacent-rate balloons. Trud7
.GOO no.51:17-25 155. (KM 9:8)
(Balloons, Sounding) .

VORONTSOV, P.A.
Methods of recording horizontal and vertical pulsations of wind
velocity by means of captive balloon. Trudy GOO no.51:26-49 155.
(MLHA 9:8)
(Winds) (Meteorological instruments)

Z=WAKJ~ DUBOV, A. S.
Xethods of investigating the structure of air currents from and
airplane. Trudy GGO no.51:30-63 1~5. (XW 9-8)
(Atmosphere) (Aeronautics In meteorology)

VORONTSOV, PIA.
Using the P.A.Kolchanoy radiosonde for recording levels of possible
icing. Trudy GGO no.3it66-71 153. O= 9:8)
(Radiosondea) (Clouds)

ILI
VORONTSOV, P.A.
Convection awrents in ths lowest atmospheric layer. Trudy GW
no.34.-3-23 155. (Atmosphere) (Heat--Convection) (MLRA 9:8)

VORONTSOV, P.A.
Vertical gustiness in the atuosphere on the basis of airplane
observations. Trudy GOO no-54:44-58 155. (MM 9:8)
(Atmospheric turbulence)
Olphs"IM, FIN
I` IM
ITSW -t
K.- M-6US e R W, -M

VCRONTSOV, P.A.
Breezes of the TSimlyansk Reservoir. Trudy, ON no.54t8l-95 155.
(TSinlyansk Reservoir--Wind 19) MLRA p:8)

VCRONTSO;V P.A,
E4 ~~ , I-
"Ir
I Some problems In local air currents. Trudy GGO no.54:59-77 155.
OMU 9:8)
(Atmosphere)

VORONTSOV., P.A.
Vertical air movements in m==er in the Tsim2yanak Reservoir region.
Trudy GGO no.56:19-35 156. (MIRA 15:6)
(Taimlyanak Reservoir region-Winds) I

VORONTSOY--I!,,k. -
"wernow-
Profiles of main meteorological elementa in atmospheric bonruiry
layers. Trudy' GGO no.63:55-76 156. (YIAA 10: 5)
(Atmospheti)

VORONTSOV P.A.
4
- ~ .. ,
Aerolop4cal studies of ground Inversions. Trudy GGO no.63-77-IM
,56. (MLRA no.10:5)
(Atmospheric temperature)

VOROZITSOV, P.A.
Relation of the structnre of air currents to at-7ospheric corwiltions.
Trudy GGO no.63:103-121 156. (HLRA 10:5)
Otmosphere)

VOROTITSOV, P. A.
"Some Peculiarities of the Temperature - and Wind-Codnitions Above the Lake
Sevan, "
paper presented at The Scientific Session of Tbilisi Scientific Research
institute for Hydrometeorology, May 1957.
Metecrologiya i Gidrologiya, 1958, Nr 1, pp. 66-67.

3(7'j PHASE I BOOK EXPLOITATION SOV/1880
Leningrad, Glavnaya geofizicheskaya observatoriya
Mikroklimat severnoy chasti Kazakhskogo melkosopochnika (Microclimate
of the Northern Part of the Kazakh Hummocky Region) Leningrad,
Gidrometeoizdat, 1958. 207 P. Errata slip inserted. 800 copies
printed.
Sponsoring Agency: Glavnoye upravleniye gidrometeorologicheskoy sluzhby
pri Sovete Ministrov SSSR.
Ed. (Title page): I.A. Golitaberg, Doctor of Geographical Sciences;
Ed. (Inside book): V.D. Pisarevskaya; Tech. Ed.: N.V. Volkove
PURPOSE: This book is intended for meteorologists, agronomists, workers
on collective farms, and the interested layman.
COVERAGE: This book provides a climatic description of the Kazakh
"Melkosopoohnik" (hurmocky region). It lists^the results of studies
C ard 1/81

Mi6roallmate of the Northern Part (Cont,) sov/188o
made on the microclimate of the region. Individual chapters deal
with the physical phenomena underlying and shaping the microclimatic
features, and the effect the latter have upon the region's agri-
culture. The work was prepared by members of the 000 and the
KazNIGMI. A map on the recurrence of drought was drawn up by
Doctor of Agricultural Sciences A.M. Alpatlyev and scientific worker
A.I. Trofimov& of the Vsesoyuznyy institut rasteniyevodstva. Ye.I.
Kuznetsova worked on data dealing with the temperature of the active
slopes of Li Pkhill En and the changes in prevailing air currents
brought about under the influence of relief. The chart showing
the amount of precipitation during the warm period of the year was
drawn up by L.P. Kuznetsova under the direction of Doctor of Geo-
grahpical Sciences O.A. Drozdov (000), There are 89 references of
which 81 are Soviet, 6 German) I French) sid I English.
TABLE OF CONTENTS:
Foreword 3
Card 21g1_

Microclimate of the Northern Part (Cont.) SOV/1880
Ch, 1, Methods of Conducting Investigations
The Organization of Microclimatie Investigations in the Kazakh
Hummocky Region (I.A. Golltsberg) 5
The Methods of Field Observations of the,Combined 000 Expe-
dition and the Description of the Working Locality ~
(T,A. Golubova) 6
Weather Characteristics During the Period of the Expedition's
,kdtivities,(N,V, Smirnova) 11
Ch. 11. A Brief Characterization of the Climate of a Warm Period
I 'V.,Smirnova)
(N. .
The Physical Geographic Properties of the Region 16
Co"ditions of the Development of Climate and the Characteris-
ties of Its Individual Elements 17
Ch. III. The Mechanism of the Formation of Microolimatio Dif-
ferences Under the Conditions of a Dissected Relief
The Radiation Regime of Slopes (Ye.P. Barashkova and T,A,
Golubova) 34
Card 3/

Microclimate of the Northern Part (Cont.) sov/'188o
Determining the Temperature of the Active Surface of Slopes
. M. Pkhil' En) 42
Wind Conditions and Their Effect on Thermal Variations
M.N. Romanova) 45
The Microaerologic Features of the Cold Air Flow Over a
Slope (P.A. Vorontsov) 63
The Microaerologic Features of the structure of Nocturual
Inversions kj:L-_,A. 3U=Gntapv) 70
Ch. IV. The Microclimatic Peculiarities of the Thermal Cycle
and of the Humidity of Air Under the Conditions of a
Dissected Relief
Soil Temperature M.P. Arkhipova) 79
Air Temperature (M.Ya. Glebova) 94
The 24-Hour Cycle of Air Temperature (Z.A. Mishchenko) 117
The Relative Humidity of,Air (M.Ya. Glebova) 128
Ch. V. Main Features of the Advcrse Conditions of a Vege-
tation Period
Drought and Dry Winds (IsAo Go".1tsberg)
Card 4/1

- - YORDIITSOV. P.A.
Aerological studies of evaporation fog from the Angara River.
Trudy GGO no-73:24-36 158. , (Milu 11:9)
(Irkutsk region--Irog)
I

VORONTSOV, P.A,
etudy of the boundary layer of the atmosphere over
I a hilly region of virgin soil. Trudy GOO no.73:61-86 158.
(MIRA 1-1:9)
(Atmosphere)

VORONTSOV, P.A--,
." .Breezes over lake Woga. Trud7 GGO no.73:87-106 '58. (MIRA 11:9)
(Iadoga, Iake-Vinds)

VORDIRSOV, ?,A.; MIXH&L', Y.M.; ERLER. A.A.
'11tilizing model airplanes guided by radio for aerological studies of
the lower layers of the atmosphere. Trudy GOO n'o.73:107-115 '58,
.(HIRA 11:9)
(Atmosphere) (Airplanes-Rodels--Radio control)

_
~ T
V
3(7j qD-3 19f PHASE I BOOK EXPLOITATION 807/1734
Leningrad. Gla~naya e askaya. observatoriya
IssledavLiyP,.p'rotsessov ieplo- i vlagoo'bmena nad vodoyemsmi (Research in the
P;rocess6s'of Heat and Moisture Exchange Over Water Reservqirs) Leningrad,,
aidrameteclizdat, 1958. 130 p. (Series:* Its: Trddy,, VYP- 78) 1,375
copies printed.
Sponsoring Agency: USSR. Glavnoye upravlenlye gidrometeorologicheakoy
sluzbby
El. (title page): M.F. Timofeyev, Candidate of rbysical and Mathmatical
Sciences; Ed. (inside book): Yu.V. Vlasova; Tech. Ed.: N.V. Volkav.
PURPOSE'- This publication is intended for scientific and technical personnel
wording in meteorology, hydrology, hydrotechnology and related fields.
COVERAGE: This collection of articles, by several authors, reports the results of
*experimental work carried on in 1956 in investigating the meteorological con-
ditions over water reservoirs. It contains the results And an exmnination of
Card 1/4- 3

Research in the Processes (cont.) SOVAT34
the meteorological and aerological lnvestigation'conftcted at Lake Bevan under
,field conditions during the su=er of 1956. Two articles are devc~ted to meteoro-
logical conditions prevailing over Lake Balkhash. No personalities am mentioned.
The articles are accompajied by tables, diagrams, and bibliographic references.
TABTX OF CONTENTS:
Timofeyev, M.P., and T.A. Ogneva Relationship Between Evaporation and a
Deficiency in Air Hmidity 3
Drozdoy, O.A., Moisture Cy~le in a.M6untainous Depression 10
.Ogneva,, T.A. Computing Limporation From the Surface of Lake Bevan 16
Kiri)ldva,T.Vt Radiation Balatice of Lake Bevan 25
Kirillova, T.V., and R.F. Byuring. Results of Subaqueous Radiation
Measurements 34'
Vorontsov Characteristics of the Wind and Thezwa Regimen drek
Lake Seven 41
Card 2/1k

Research in-the-Processes (Cont*-) SOV/1734
C4pstnaya, I.I. Air Currents Over Lake Seven 65
Seleineva., Ye.S. The Origin of N8rthem Sumer Winds in the Lake Bevan
Basin 77
Matveyev, L.T. Airborne Studies of the Structure of Turbulent Air Curre~ts
in the Regime of Lake Seven 84
Matveyev., L*Ts Structural Function of the Vertical Velocity of the Air
Current and a New Method of Cmputing the Coefficient of Turbulence
In the Free Atmosphere 98
Vorontsov, P*A. Vertical Movements of Air Over Lake Bevan 108
Ogneva, T.A, Trial Computation of Surface Water Evapokation and the
Heat-Air Exchange Over Lake Balkhash 120
Card 3/4,

C>
470 p. T--.ALt& ..'LP
2,000 copies printed.
Sponsoring &Zrr.~y: 0arroye u;ra.l*rLlye CidrOsmt*OrOIQ61ch**"T
sluzhb7 pri Sovats Xinstrov
Rasp. td.t V.A. UryvLymvj Zd.i V.S. Protapopovj Tech. Z4.4 X.X.
Brayrilma.
PnPOS11 This vork~io Intended for metworclogiatep hTdroloSt and
hydrophyalciatep particularly those 4=904904 1A the StUdY Q*rtom*m
and too and evaporation processes.
C0V1RAaZx This book contains papers an hydrophysics which wore pro-
atnt*d and discussed at the Third All-Union Xydrological Conference
In L*nlngrad, October 1957. The Conference publlah*4 10 value**
on various aspects or hydrology or which this It mm~;~r
editorial board In charge Of the series Includai 4)T# O.N. Soromko
(Chairman), O.A. Alokint To.V. Bilanyak (datwase k. vr"*"v
X.A. Volikozov, L.K. Davydov, A.?. DomanItakly. O.P. Kallain. S.M.
Krlt~Aly, B.I. Xudelln, L.P. Mantle, M.P. Xtmkollp'B.P. *view.
1. V. Popov. A.K. Proskur7akov. D.L. 3oloolavokly. O.A. Spengler,
A.X. Chebotarev. and S.X. Cherkawskly. ThIs volusee In divided in-
to 2 sectional the first contains reports from the subsection
for the study of evaporation processes, " the second eantsina
reports from the snow " let subsection. Aeforencea accompany
each article.
Kril we [Candidate of Physical and Rathw%t1cal 3clanoos.
Leningrad) Radiation Balance of Water bodies 42
?~.A IC&ndldat* of Geographical Sciences, Goo lanth-
n
gra or n haract*rlatlca or Meteorological Conditions Okar
.YqkoVIevs, N,J. (Junior ScItntirle Worker, OW Leningrad) "as
Xr?vc_t-cf water surfaces on the Air Transformation 59
D%1~!r1TTXa_ N.G. (Candldat;,of Oeographicel Xcioness, Tair
Rostov] Inflitratton Into op Bodo In Relation to the D
Zion or xvaporation 64
mft,t_t1nOv_ A-P., " V.Pj_f%L11k~ (Candidate@ of Fhysjcaj
and Rath"Latle Sciences, 00 ftlawad) ~bamlc ?ra do In the
ScUdY of XvsPoratlon From a around 3urrace 72
VqIR!A_~~ [Corresponding Xmt*r of the Aterb"49hamm As*.
dvxy or 3clencsa. Doctor or Agricultural Sclenctal Relation so-
twtn 301-18 and the Xydrologleal Conditions 84
(Candidate ef Technical 3clamea, Odf igaingl4bal
bitiridning Irvaporstlon by the Beat balance Setb" Voing the ch.%&
Of 3tandLrd Meteorological Observations 92
Rusin X P lCandidate of avograpniesa Scianeops, Goo
for DotarmIntng Rvaporatlan rrm._%
and Its Application Within -the -station Xetworit
Korlstantinov-AJL. rcandldate or Physical and mathmatleal
- )1'101. 001 VLlday) CosputIng rvaporation From the arcane
Accord-mg to Data 3upplIed by Meteorological stations 103
Jtr%'ar__LJL rCiLndld*to or Phzelcal and xathematloal Balemos.
001 tGolA417101 latimatInS the Irrar In the Ralsting Meth"a fop
DetermlAing I'vakporation From the around Ila
bIrrukov 9_3. tCwAldate of 0001*gLeal and Mineralogical
or Forestry. upponsko") coaputing Total
IvsPoration or the yalga zone &A Rxemplifled by the Forest Range
Of the Kadnokovskoye Forest District in the VolaW&Wa able&%- I

3 (7 SG'1151;-~9 .',c-22/2:/'
ALMA-M: Vorontsov, P. A.
TITLLt At thp MI-ain Geophyzical Observatory
PERIODICAL: Leteorologiya i gidrologiya, 1959, Nr lo, p 36 (USSR)
ABSTRACT: On June 19, 1959 the Uchenyy sovet (SCientific Council) of th,~,
Glavnaya Geoflzichc3kaya ccservatorlya im. A. I. Voycykova
('Main Gcolp-hyzical Coservatory -rzeri A. 1. Voyay' '-C-~ ) held a
raectin3 or-the occasion of the 40th arn.1vprsary cf the death
of Acade-ician IU'r-hsii Alek3androvich Rykachev. 11~. V. Zavarina
.9poke about "Life ard'11ork of M. A. Illykachev". Lecturcs were
also delivered by D. F. Nezdyurov, whz, assisted RYkarhev ut the
Observatory, and by Alcksar-dra 1'ikhajlovr.3,, the daughter cf thE.-
scienti3t.
Card 1/1

VOROMPSOV, P.A., -z-
Aerological cbaracteristicg of 9ea fogo. Trudy A"Il 228:
38-54 '59. (MIRA 13:2)
(Arctic Ocean--Fog)

VORONTSOV, P.A.; SELITSUTA, V.I.
war
- tical structure of summer fogs in the region of Dikson
Island. Trudy AAKII 228:87-99 159. (MIR& 13;2)
(Dickson Island--Fog)
___1

VORONTSOV, P. A., Doe Geog Sci (diss) "Aerological. research into
boundary layer of the atmosphere." Leningrad, 1960. 39 pp; (Lenin-
grad Order of Lenin State Univ im A. A. Zhdanov); 2CO copieS; price
not,given; list of authors works on pp 37-30, (50 entri'es,); (Ul, 27-60,
150)
MIN

TCIROY-~SOY, P.A.: KMCMSKAYA, A.Y.; SM32MA, Ye.S.; CHESTMAYA, I.I.;
A-,WiU, M.M.; KIRnWYA, T01.1 IGSINA, L,Y.; OGNETA, T.A,;
MMVI, !!,V.; TIMMYET, M.P.., kand.fiz.-mat.nauk; ZMANOTA. L.P.,
red.; RUINIU, M.L. tekhn.red.
[meteorological regime of Lake Sevau3- Keteorologicheskii reshim,
ozera Seven. Pod red. M.P.Timofeeva. Leningrad, Gidrometeor.
izd-vo. 1960. 310 (HIRA 14:3)
1. Leningrad. Glavnays goofizichaWmyo observatoriya.
(Seven Lake region--Meteorology)

?nM I D,.'% WEPTTATT0,7
Vorontsovs Petr Alekneyevich -
-----------
Aerologicheakiye Iseledovaniya pogreaiicbnogo.sloya atmosfery (Aerological
Studies of the Boundary layer of the Atmosphere). lAningrad,
Gidrometaoizdat, 1960, 450 P. 1)250 copies priuted.
Spousoring Agencies: Mniiqrad. Glawaya geofizichaskaya observatoriya;
and USSR, Glavnoye upravleniye gidrometeorologichookoy sluzhby.
Reap. Ed.: Yes S. Selezneva; Ed.: M. M. Yesnogorodskayaj Tech. Idt
M. I. Braynina.
PURPOSE: This book is intended for meteorologists and scientists vorking
-*on problems of atmospheric physics,
COVERAGE: The author discusses the structure of the boundary Iver of
the troposphere) loe. the layer betveen 20-500 meters above ground.
The characteristics of temperature, vindp and humidity flelds for
several regions in the;USSHO based on data obtained In aerologiesl
studies made by the GOO (Main Geophysical Observatory), are described,
An analysis Is given of the conditions of thermal and vind-regimes
Card 1/& --2-

Aerological Studles-(Cont.) SM/403
and humidity. Results obtained in stuAles of turtulenee,, vertical
currents, the transformation of air masses, and serological conditions
in fogs an given. Data on -the structure of loeal winds are given*
The book contains 335 references: 237 Sovietp 58 Germanp 31 Zngllsh~
6 French., 2 Japanese.. and I Bu34prisn.
TABLE OF C'11
Ch. 1. Boundary Layer of the Troposphere and the Characteristics of Its
Structure
General information T
Certain quantitative characteristics of the boundary layer 15
Scheme of the structure of the boundary layer. 25
Inner boundary layer 26
Protective role of the boundary layer 30
Ch. n. Wan Characteristics in the Distribution of Temperature, Wind,
H=idlty and the CoerfIcient of Ilirbulent Fxehnnge Jn the
Boundary T^vnr
Aercelimatic mothods of. procc-esing d~%tE, in aerostatic
eoundinge 32
Card 2/6, 9~-

PL40 I BOOK EXPIDITATION SOV/5860
~Vorontsov, Petr Alekseyevich
Metody aerologicheskikh issledovaniy pogranichnogo eloya atmoefery,
(Aerological Methods of Uvestigating the Atmospheric Boundary Layer)
L:.~ningrad, Gidrometeoizdat,' 1961. 221 P- 1500 copies printed.
ON-ti:?joring Agency: Glavnoye upravleniye gidrometeorologicbenkoy sluzlaby pri
5,-vetar Ministrov SSSR. Glavnaya geofizicheskaya observat6riya
im. A. I. Voyeykova.
Ree-n. Ed.: M. S. Sternzat; Ed.: M. M. Yasnogorodskaya, Tech. Ed.:
M. 1. Braynina.
AWOR: This book is intended for meteorologists and other readers con,.-exmel
"4-Va problems of physics of the atmosphere.
Cal'i

Aer--)loglaal Methods of Investigating (Cont.) SOV15860
COMAGE: The book describes the methodsand apparatus used in aerologi2al
.Az-festigations of the atmospheric boundary layer, temperature and hmdd-
Ity of the air, atmospheric pressure, vind conditions, turbulence, and
-T,-rtiim1 air flove. 'In his investigations of the boundary layer, the
e-Ahor tested almost all the methods and instruments considered in the
book smd made use of the available 11terature regarding this problem.
1~ethodz of sounding with the aid of aircraft, helicopters, captive bs1-
-ine., Idtes,, and other lifting devices are discussed. Some special fvi -
-1,:.-rea of meteorological-'balloon, observations, particularly the metltd rf
,-,.,!,JuEt.---d pilot bal1oons, are considered. Wherever it vas possible, errc-
:'--- nrO-aod and in the accuracy of measurements are pointed out. Sevt- MI.
-acls-l features of the cliw-'.-~ilogical treatment of the observation dB-%
6xa briefly outlined. Many p6reonalities are mentioned in the text.
,-~,re are 107 references: 78 Soviet, 21 EngUsh, 6 Gernian, 1 French, ant

5/169/62/000/007/096/149
D228/D307
AUTHORS: Vorontsov, P. A. and-Kirillova, T. V.
TITLE: Relation of the radiation balance to the boundary lay-
er stratification
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 7, 1~9621 22, abz
stract 7B128 (V sb. Aktinometr 'a i atmosfern. optika,
iy
L., Gidrometeoizdatt 1961, 32-36
TEXT: Tile relation between -the radiant energy balance in the at-
musphere's lower layer and the vertical temperature profile ',s in-
veatigated. The results of measurements of the radiation balance
and the temperature grkidiant on clear, cloudy, and overcast days
'used for this purpose. It was established that the ratio-for Y
a
re
the long-wave radiation balance (Bi) to the radiation of the under-
lyin., surface (oT4), which is considered as a black body when the
0 n
surface .temperature is T1,j is related tothe temperature gradient
-7-jr in the layer 0 100 m. In equilibrium conditions Bl/&14 -;~0.2-
n
Card 1/?

S/.1 6y62/000/007/096/149
Relation of the D228 D3,07
In case of inversions.AB .11Ar 0.01; in2the event of superadiabatic
gradients this ratio equals 0.05 cal/cm .min.,deg. For conditions of
contiInuous cloud -Bi--does--not depend-on(y. Analogous relations were
obtained too, for the ratio of long-wave atmoopheric radiation
(Ea) to ~T4 (T,b eing the air tempera-tare). Z-Abstracter's note:
Complete translation-_,7
Card 2/2

3/169/62/000/001/062/083
S-0 0 0 D228/D302
AUTHOR: Vorontsov, P. A.
TITLE: The question of compiling the boundary layer's aero,-
climatic characteristics
PBRIODICAL: Referativnyy zhurnalg Geofizika, no. 1, 1962~ 68, ab-
etract 1B430 (Tr. N.-i. in-ta aeroklimatoi".., no. 14,
1961, 150-152)
TEXT: The main problems confronting aeroclimatology in connexion
with the study of the troposphere's boundary layer with an average
height of 1.5 - 2 km are considered. Up to the present this layer
remains almost unexamined in published climatologic data. This is
mainly because the data of network aerologic observations (of ra-
dio- and aircraft-sounding) for the atmosphere's lower layers con-
tain many errors -- the result of the imperfection of repearch me-
thods (in particularp the high inertia of the temperature recei-
vers and the humidity during their ascent at great speeds). This
deficiency can be partly rectified by introducing corrections for
Card 1/2

S/169/62/000/001/062/083
The question of compiling D228/D302
the inertia of these receivers. At the same time it in necessary
to develop new-methods of investigating the boundary layer - for
example, by radio-sounding apparatus -- and to expand the number
of measurable elements. It is pointed out that a number of the
boundary layer's quantitative characteristics may poceibly be ob-,
tained on the basis of the already available data of terrestrial
meteorologic observations and from certain parameters of the free
atmosphere. In the first place this applies to determining the
boundary layer's height Hb and the, coefficient of turbulent ex-
change R from the formulas proposed by D. L. Laykhtman. The author
mentions his own methods of processing the results of balloon sound-
ings with allowance for the criterion of thermodynamic stability
and also the standard schemes~ suggested by ShneyderwKarius, for
constructing the boundary layer under different weather conditions.
Z'-Abstractor's note: Complete translation._7
Card 2/2

KONSTA,NTIEQV,, A.R.; VORONTSOV) P.A.
Effect of forest belts on vinds and turbulent exchange in
the atmoophere. Trudy UkrVIG14I no.26:99-110 161.
(MIRA 15:2)
Forest influences)
nds)
M

VORONTSOV, P.A.
Conditions promoting the conversion of low clouds into fog
and the conversion of fog into low clouds. Trudy GO no.106:
10-18' 161. (MIRA 14:10)
(Cloud physics)

CUESTNAYAO I.I.j_,YOROh'TSOV, P.A.
Distribution of clouds in the basin of Lake Bevan. Trudy GGO
no.106:50-54 161. (MIRA 14:10)
(Bevan Lake region-Clouds)

VORONTSOVI ?.A.
Local winds over IALke Sevan. Trudy, GGO no.106-05-61
161. (MIM 14: 10)
(Sevan Lake region-Winds)

VORONTSGVP P.A.; OGNEVA., T.A.; SEROVA, N.V.
Formation of the temorature regime of soil and air. Trudy'GGO
no.1(77:22-33 f6l. WMA 14:10)
(Soil temperature) (Atmospheric temperature)
I
I
I.

VORONTSOV PsA.
Structural characteristics of the atmoBpheric boundarylayer
over the village of IUhtaly in September 1959* Trudy GGO
no.107:1-16-127 161. (MIRA 14:10)
(14steorology)

VORONTSOVp P.A.
I
Structure of the air otream in the lower layer of the atmosphere
0.5 km. above the village of Voyeykovo. Trudy GGO no.135t3-25
162. (KIRI 15t8)
(Voyeykovo region (Leningrad Province)-Winde)

VASILtCHENKO, I.V.; VORONTSOV, P.A.; DOVGALYIJK, YU.S.; HASLOV, S.I.
Wthodology and apparatus for studying the boundary layer of the
atmosphere from ships. Trudy GGO no.135t120-128 162.
(MIRA 15:8)
(Atmosphere) (Met*,Wological instruments)

VOR!'"'IR'LOV, P.A.; G-,:R!-iAl,
Ma,ods for V.-L, irriupt'gj-Orm of the r" a
boundary Iayf;r bwiefi -,,n uevelerograpb re%rding data In fakhtsi-
inral. Trudy GGO n~~.154;615-77 164. (141 7/1, 17:7)

V(;R0iiT3UII A.
r- -. Structure of the lowest layer of the atmoDphere 0-0-5km)
during the period of the Dnieper Expedition* Trudy GGO no.l":
102-110 163. (MIRA 17:6)

ACCESSION NR: AT4033572 S/2922/63/009/000/0284/0286
AUTHOR: Vasil'chenkop I* V.; Vorontsov, P. A.; Dovgalyuk, Yu. S.; Maslov, S. 1.
!TITLE: Problems in the method of studying the lower layer of the atmosphere from
ships
'SOURCE% Vossoyuznoye nauchnoye mateorologichookoye soveshchaniyt. let, Leningrad,
1961. Pribory* i metody* nablyudeniy (Instruments and methods oZ observation);
;trudy* soveshchaniya, v. 9. Leningrad, Gidrometeoizdat, 1963, 284-286
cal
'TOPIC TAGS: meteorology, aerology; atmospheric boundary layer, meteorologi
;instrument meteorological observation
!ABSTRACT: The problems of making systematic observations of the structure of the
!boundary layer of the atmosphere over the ocean surface are discussed. The
Glavnaya geofizicbeskaya observatoriya (Hain Geophysical Observatory) made such
studies in the summer of 1960 by balloon and helicopter ascents from two research
'vessels in the Atlantic. The difficulties involved in using helicopters are
described; the helicopter took off from an 8 X 8 w pad on the prow of an 8,000-ton
vessel. The standard KA-15 helicopter was equipped with the helicopter eleccro-
meteorograph developed by the Teentrallaaya aerologichaskaya observatoriya
Card 1/2

:ACCFSSION NR: AT4033-572
!(Central Aerological Observatory); a meteorograph with mechanical recording was
carried for comparative purposes. Temperature, pressure, temperature fluctuations
-and humidity were recorded. Fifty such flights indicated that the Central
7Aerological Observatory instrument is satisfac!~,:rv and easy to use. The vessel has
:a distorting influence on the measurements of air temperature and humidity; a
:,special helicopter'flight program is described which eliminates these'distortions.
;A MAZ-1 captive balloon was used in observations from a 1,200-ton vessel. The
iballodn meteorograph developed by the Main Geophysical Observatory was suspended
;to the cable of the helium-filled envelope. The balloon-launching method is
essentially the same as used on land; the balloon was poxmitted to assume the
ifollowing levels: 25, 50, 100p 150, 200, 300, 400, 500 and 700 motors, being hold
at each level for 3 to 5 minuces. Problems involved in the use of meteorological
'balloons aboard ships are discussed briefly.
ASSOCIATION: Glavnaya goofizicheakaya observatoriya (Main Geophys16l Observatory)
I SUBMITTED: 00 DATE ACQ: 16Apr64 ENCL: 00
iSUB CODE! NO REP SOVt 003 OTHER: 000
2/2
CarJ
_77-77

~ACCESSIOWFR:- AT4030531_-_____' --'---S/OOOO*/63/000/000/0092/0095'
:1AUT11OR: Voronteov,.P. A.
!TITLE: An experiment utilizing helicopters for sounding the lower level of the
~atmosphera (1,5 to 2.0 km)
SOURCE: Nauchnaya konferentaiya po aviatsionnoy meteoroloGii. Moncow, 1960.
Materialy*, bscow, Gidrometeoizdat, 1963, 92-95
TOPIC TAGS: helicopter, sounding, lower layer' synoptics, weather element, MI-1
~helicopter, KA-15 helicopter
!ABSTRACT: This paper is one of 13 previously unpublished reports of the 40 papera
Igiven at the Nauchnaya konferentsiya po voprosam aviatsionnoy meteorologii (scien-
tific conference on problems of aviation meteorology) that was held in June and July
of 1960 in Moscow at the Glavnoye upravleniye gidrometeorologicheskoy sluzhby* SSSR.
.In this article the author examines the application of helicopters for taking sound-
ings of the atmosphere at altitudes of 1.5-2 km. The helicopters most suitable for
.Investigating the boundary layer are the MI-1 and the KA-15. The placing of the
,meteorograph on the MI-1 in front of the fuselage at approximately the distance of
,0.5 of the radius of the. main rotor from its center was found to be most advantageous.
Caed 1/2

ACCESSION NR: AT4030531
A description of the instrument is given. Photographs of the installation an the
.MI-1 and the KA-15 are shown. The clectro-meteorographt developed at the Tsentral%-
naya aerologicheskay observaitoriya (Central Aerological Observatory) and registered
atmospheric pressure with a maximum error of +3.0 mb, mean air temperature at
maximum error �PZ10 and inertia of 0.5 see; temperature pulsations were measured
within a range of :L3*00 having a maxt%ium error of :L0.2o and a coefficient of inertia
of 0.2 sec. Meximum error Lit measuring humidity, within the range of 25-100%, was
-no mdre than-17% within the entire~ t~-~peratura rangal and the coefficient of
;inertia did not exceed 30 see* Orij-. art. has: 2 figa"..
1ASSOCIATIMs"; none
IUBMITUDs 1Web63 DAZZ ACQ: l7AVr64 9=: 00
:SUB COM AS NO UT SMS 000 01MZR: 000
Card 2/2

ACCESSION NR: AT4043159 S/2531/64/000/154/0065/0077
-AUTHOR: Vorontsov, P. A. (Doctor of geographic sciences); Germanp M4, Aa
TITLE: method for invoatigating the turbulent regime of the boundary layer froin
accelerograph records at Pakhta-Aral
SOURCE: Leningrad. Glavnaya geofizicheskaya observatoriya. Trudy*, no. 154.
Voprosy* fizild atmosfery* (Problems In atmospheric physics), 65-77
ITOPIC TAGS: meteorology, atmospheric boundary layer, accelerograph, atmospheric
iturbulence
ABSTRACT: This article discusses a method for computing a number of characteristics
of the structure of the air flow from aircraft accelerograph records. Computations were
rnade with an electronic computer. The records of aircraft ovz.-loads were obtained
largely during the Pakhta-Aral Expedition of the Glavnaya geofizichaskaya observatorlya 0;
(Main Geophysical Observatory) in 1952. The authors also determined the values of the
coefficient of turbulent exchange more precisely. Only a sample of 12 cases out of 180
was used. Most flights were made on a PO-2 aircraft in the morning hours. The aircraft
made horizontal flights at heights of 300, 500, 750 and 1, 000 m. above cotton fields, the
Card 1/3

ACCESSION NR: AT4043159.
steppe and desert. Aircraft overloads were recorded with a ZP-11 accelerograph. Dataare
given on computation of the turbulence coefficient for flights over these underlying surfaces.
For convenience in further analysis the turbulence energy spectrum was represented In the'
in the form of a set of curves, as shown in Fig. 1, of the Enclosure. There Is a spread
of the curves of the energy spectrum which can be attributed to the difference In the intea-
sityof turbulent energy during flights over the different surfaces. With a decrease in the size
of turbulent eddies (with an increase in space frequency) all the curves have a tendency to
decrease. Ile individual peaks on the curves reflect the Influence of vertical currents
causing an energy increase in the spectrum. With an increase in scale of the eddies the
intensity of energy transfer from eddies of one scale to eddies of a larger scale increases
somewhat with respect to the high-frequency part of the spectrum. This is associated with
!the thermal stability of the investigated layer. The method descri'ied for determination of
the spectral density of turbulent energy can be used In various investigations of the free
atmosphere. Orig. art. has: 20 formulas, 5 figures and 5 tables.
ASSOCIATION: Glavnaya geofizicheakaya observatoriya, Leningrad (Main Geophysical 77
Observatory)
ENCL: 01
SUBMITTED: 00
NO REP SOV: 015 OTHER: 000
SUB CODE: ES
Card

'AC.CESSION NR: AT4043159
ENCLOSURE: 01
- --------- ---
I:zl " . . . ,
Figure 1. Turbulence energy spectrum over different underlying surfaces. Ordinate
2
(m/sec.Y .;abscissa= rad./sec.
rad. /m.
Card 3/3

VORONTSOVI,P.A.
Some,aerological observation problems in studying the dispersion of
chimney plumes. Trudy GGO no-158:56-68 164. (WRA 170)

VORONTSOV, P.A.; GPRMANV M.A.; DUBOV, A.S.
I',-, . '-. , . 7 , - "~
Methodology. and soms results of an airborne exploration of turbulet
exchange in the boundary layer of the atmosphere. Trudy GGO no.153:
77-83 T64. (MIRA 17-9)
11~

.VC.RONTSOV,I- P-.A.;. GALADZHIY, N.M.; KONSTANTOOV, A.R.
Study of the distribution of some structural characteristics
of the air flow along the vertical. Trudy GGO no.1":88-95
'63. (MIRA 17:6)

ACCESSION, 11R: AT4028749
AUTHOR: Vorontsov P. A.
S/2531/63/000/144/0102/0110
TITLE: Structure of the lower layer of the atmosphere (0-0.5 Ian)- during the
Dnieper expedition
SOURCE: Leningrad. G1. geofiz. observ. i Mr. n.-i. gidrometeorol. Inst. Trudy*,
no. 144/40 1963. Fizika pogranichnogo sloya atmosfery* (physics of the atmospheric
boundary 1;yer)'; *Dneprovskaya expeditsiya GGO i UkrNIGMI, 102-110
TOPIC TAGS: surface layer, balloon sounding, temperature change, humidity change,
i wind velocity, turbulence, Dnieper expedition, inversion layer
y4BSTRACT: in this paper, the author examines the structure of the lower layer of
the atmosphere (0-0.5 km) according to data from sounding balloons. The daily
changes of air temperature and air humidity, wind velocity and its pulsatiorts, as
well as the coefficient of turbulent exchange are presented. The data of the Dnieper
expedition, broken down into daily and hourly readings of soundings in relative
humidity and temperature gradients are given in a number of tables. Also presented.
are tables of the daily and hourly changes in the horizontal component ~f wind
velocity pulsation and the probability of turbulence. The average daily values of
C6id *J/2

ACCESSION NR: AT4028749
.the separate characteristics of air flow in the layer at 0.3 km are plotted in four
,.separate graphs. In general, all t6 presented characteristics of the lower layer
(0.5 km) during thh activity of the expedition, point to a considerable daily
variability of the meteorological elements in the investigated layer, with great
instability during daylight hours and often a powerful radiation inversion at night.
The rise of turbulency by day causes a decrease in the vertical gradients of wind
velocity, potential temperature and specific humidity, and a weakening of turbulence
at night causes 'an increase of these factors. Orig. art. has: 2 figures and 9
tables.
ASSOCIATION: Leningradskaya glavna geofizicheskaya observatoriya (Principle
Geophysical Observatory of Leningrad),
.SUBNITTED: 00 DATE.ACQ: l6Apr64 ENCL: 00
SUB CODE: AS NO REF SOV.- 000 OWER: 000
Card. 2/2

,ACCESSION NR: AT4028747 S/2531/63/000/144/0088/0095
AUTHOR: Vo t
_Fon sov, P. A.; Galadzhiy, N. M.; Konstantinov, A. R.
TITLE: Investigation of the distribution of certain structural characteristics of
the vertical air flow
SOURCE: Leningrad. Gl. geofiz. observ. i Ukr. n.-i. gidrometeorol. inst. Trudy*,
.no. 144/40, 1963. Fizika pogranichnogo sloya atmosfery* (physics of the atmospheric
'boundary layer); Dneprovskaya expeditsiya GGO i UkrNIGMIg C8-95
TOPIC TAGS: *;Karman co~ptant, wind velocity, turbulence# thermoanamograph
'ABSTRACT: Distributio4of pulsations of the horizontal and vertical components of
Pd velocity, the horizontal and vertical expansion of atmospheric turbulence, the'
Kjrman constant, and the values and the coefficient of turbulent exchange in the
,layer from 0.5 to 300 m is examined under various thermodynamic conditions. -The
structure of the air flows from an altitude of 0.5 m to altitudes of 300 m were
investigated in the joint expedition of GGOI UkrNICHI and LCM. In the lower layers
0.5 and 2.0 m altitudeg the wind structure was investigated with the aid of a thermo-
anemograph, and in the upper layers, from 3 to 300 m, with an aid of a mechanical
register of turbulent flow pulsations attached to a captive balloon. -The dependences
1/2
- -------------------------

-Ki
- - - - - - - - - - -
ACCESSION NR: AT4028747
of the horizontal expansion of vortexes a-tid the dependence of the Karman constant
on the altitude and temperature stratification,'of the atmosphere according to the
!
.thermoanemograph and the mechanical register ar;e presented in a table. The de-
pendence of the coefficient exchange on the altitude at various Richardson numbers
,and the temperature stratification of the atmosphere for variouc altitudes is pre-
sented in a graph; the authors draws the conclusion that if it is assumed that the
value of 'the exchange coefficient in equilibrium stratification is unity, then the
relative change in the intensity of thek turbulent volume, dependent on the stratifi',
.cat.ion of the atmosphere, is expressed more clearly at altitudes of 100, 200, and
'300 m than at altitudes' of 3.0 m. Consequently, with an inctease of altitudes the
effect of stratification Increases. Orig. art. has: 4 figuress .3 tables and 4
lormulas.
ASSOCIATION: Leningradskaya glavna geofizicheskaya observatoriya (Principle
Geophysical Observatory of Laningxad)
SMUTTED; 00 DA72 ACq: 16Apr64 RNCLS .00
'SUB CODE: AS. 'NO REF*SOV: 014 QTW331, 008

ACCESSION NR: AT4028747 S/2531/63/000/1"/0088/0095
AUTHOR: Vorontsovs P. A.; Galadzhiy, N. M.; Konstantinov, A. R.
TITLE: Investigation of the distribution of certain structural characteristics of
the vertical air.flow
SOURCE: Leningrad. Gl. geofiz. observ. i Ukr. n.-i. gidrometeorol. inst. T*rudy*,
:no. 144/40, 1963. Fizika pogranichnog ,o sloya atmosfery* (physics of the atmospheric i
:boundary layer); Dneprovskaya expeditsiya GGO i UkrNIGHI, 88-95
:TOPIC TAGS: jKarman conptant, wind velocity,Iturbulence, thermoanemograph
f
ABSTRACT: DistributiozOef pulsations of the horizontal and vertical components o
'~nd velocity, the horizontal and vertical expansion of atmospheric turbulence, the:
Kirman constant, and the values and the coefficient (.*f turbulent exihangu in the
layer from 0.5 to 300 m is examined under var16us.thermodynamic conditions, -The
structure of the air flow from an altitude of 0.5 m to altitudes of 300 m were
investigated in the joint expedition of GGOv UkrVIGMI and LGMI. In the lower layers
0.5 and 2.0 m altitudet the wind structure was investigated with the aid of a thermo-
anemograph, and in the upper layers, from 3 to 300 m, with an aid of a mechanical
%register of1turbulent flow pulsations attached to a captive balloon. The dependences
1/2
- -------------------------

ACCESSION NR: AT4028747
of the horizontal,expan'sion of vortexes and the dependence of the Karman constant
on the altitude a.nd temperature stratification.'of the atmosphere according to the
!
thermoanemograph and the mechanical register ar;e presented in a table. The de-
pendence of the coefficient exchange ork the altitude at various Richardson numbers
and the temperature stratification of the atmosphere for various altitudes is pre-
sented in a graph; the authors draws the conclusion that If it is assumed that the
value of'the exchange coefficient in equilibrium stratifiL-ation is unity, then the
relative change in the intensity of the, turbulent volumes dependent on the stratift-,
ocat'ion of the atmospheres is expressed more clearly at altitudes of 100, 200l and
'300 m than at altitudes' of 3.0 m. Consequently, with an Increase of altitudes the
'effect of stratification increases. Orig. art. has: 4 figures, .3 tables and 4
;'formulas.
ASSOCIATION.- Leningradskaya, glana geofizichesk&yA observatoriya (Principle
Geophysical Observatory of Leningrad)
SUBHITTED: 00 DATE ACQ: 16Apr64 .00
SUB CODE: AS NO REP SOV: 014 MUM, 008'
Card_21Z,

.VORONTS-0,VP P.ko,- SELITSKAYA, V.I.
Use of helicopters in sounding the lower atmospheric 31mrs. Trudy
GGO no.1400-16 163.
Methodology of atmospheric sounding by meants of helicopters.
Ibid.:17-64 I (MIRA 16M)

.A.CC.NR-1AT-60j5-5l75______ SOURCE CODE:
AUTHOR: '!orontsov., P. A.
ORG: none
TITLE3 Evaluation of,some of the components of turbulent energy balance
SOURCE: Leningrad. Glavnaya geofizicheskaya obaervatoriya Trudy, no.
185.0 1966. Voproay atmosfernoy diffuzii i zagryazneniya vo;dukha (pro-
blems of atmospheric diffusion and air pollution), 72-76
TOPIC TAGS: micrometeorology, atmospheric turbulence, btwb~
bakwwe-
q;ha;pft surface boundary layer,, kZ4".a.,_
ABSTRACT: Methods are presented by which some of the turbulent com-
ponents of kinetic energy can be calculated (ueglecting
horizontal diffuslon and advection), Data obtained by
balloon soundings in the vicinity of the Shchekinak State
Regional Electric Power Station are used to demonstrate
the nethod,
The ade7iji-b Jalince-equatioi-eimployed here is written'-
-dE JU
11
-'C Rl)
dt
Car
__ d UDCe one

NRIAT6035515
where E as 1/2 (u'Z -~ V'Z + W'Z) is the kinetic energy of
.urbulence (the kinetic energy of fluctuations) per unit
m-~sn, T au/Oz'ia the momentum of turbulence from the energy
of mean motion under the influence of frictional forces,
Ri is the Richardson number, 3/3z (Ew') ic the gradient of
the vertical energy flux due to diffusion (transfer to other
levels), and.F is therate of dissipation of the energy of
turbulence in heat,
Values'of the~jongitudinal u' and vertical W, compo'--
nents of the fluctuating compqnent of the wind velocity
were measured in the spring and summer of 1962 an~L4963.
These data were used to calculate the values of Vu12 and
V~7U which denote the kinetic energy of the flux, and the
dimensionless quantities 10=75. and iw'2/-U denoting the
intensity of turbulence. Here, u - 9 + ul, where %I is
the constant component of 'us The magnitude of /U#2 - 0u
is determined by horizontal eddies whose dimensions are
independent of the distance above.the underlying surface.
The vertical couponeut of fluctuations In the wind velocity
a was also caliulated fron these data..

,'.r.,kCC' 14R-AT603551 5
Values of the elements of the structure of air flow
in'the 3-300-m layer (u' - 0.1 m/sec) and (u9 0.6 m/sec)
were tabulated, as well as for 11, - Owl CFU2 2
Up YP Out I Ow 0
OU2 + Uw2 a /u' aw/au# and Ri; in addition, values
for Ewl as ou"t I
nd 5/3z iww- at the 100-, 200-, and 300-m levels
were calculated.
When the Ri in consiatently 0.4-0,5j the Aboolute
value of Ewl is maximum at either the surface of the ground
or at the 100-m level and decreases with height. With Ri
fluctuating between -;95 and 0.7, the maximum moves to a
height of 200 m and the gradient 3Ew'/az is especially
large in the lower 100-m layer.
The author recommends extending the number of uvaLsured
characteristics of the wind structure'by recording the
transverse component of the wind velocity and developing a
method for calculating the rate of din s1 ation of the energy
of turbulence* Orig. ar.t., has; 4 tables and T formula.
SUB CODE: 04/
[WA-50; CBE No. 14)
JEO]
SUBM DATE: -none/ ORIG pM.. 002/ OTH REP: 002
Card

L 1 - -66'' EWT( 1)/FCC GW
4278
ACC'NR.# AT6004153 SOURCE CODE: UR/2531/(5/000/167/0060/0097
~AUTHOR: Vorlontsov, P. A.
ORG: Main Geophysical Observatory, Leningra (Glavnaya geofizicheskaya observatori-
ya)
TITLE: Some characteristics of distribution of the coefficient of turbulence in a
boundary layer
SOURCE. Lenis)grad, Glavraya geofizicheskaya observatoriya. Trudy, no. l.' 1965.
rizika pogranichnogo sloya atmoafery (Physics of the boundary layer of the atmos-
phere), 80-97
:TOPIC TAGS. turbulent boundary layer, atmospheric turbulence
ABSTRACT. The author considers various methods for calculating the, coefficient of
:turbulence along the-vertical in a boundary layer. Methods for calculating the co-
.efficient of turbulence at isolated levels in the boundary layer are analyzed. The
coeffici6t of turbulence in ascending and descending flows is calculated for the
!case of fluctuations above various; types of terrain. It Is found that a character-
'istic feature of the coefficient of turbulence In the boundary layer is fluctuation,
tCard 1/2.-

L IU78-66
'ACC NR: AT6004153
'due to pulsations in 'the structure of-the air flow under various atmospheric.condi-
~tions. Consideration is given to the effect which terrain and the structure of the
underlying surface have on the distribution of the coefficient of' turbulence. It is
found that deformation of the air flow by forests during the sunm)er causes a maximum
in the coefficient of turbulence at an altitude of about 100 m which reaches an al-
titude of 200 m as the air movea over the densest part of the forest. A rather
tbic3c layer with, therral instabIlity is observed during the daylAght hours In July
over semi-desert areas, while a temperature inversion with atteniaation of turbulence
was observed above cotton field3, particularly during irrigation. Typical profiles
for the coefficient of turbulence are given. Several -examples are givei-i to iilus-
calculation of profiles for-thi coefficient-of turbulence in a boundary layero
'Orig. art. has: 7 figurets, ll.tables, 7 formulas.
'SUB CODE: 08/ SUBM DATE: 00/ ORIG REF: 009/ OTH MF: 000
Card 2/2

7__
L 5021_-66 EWT'(I )/FCC GW_,
1/00()3/061,
UR/2531/65/ow/17
ACC HR 31 A'MM80 SOME CODE3 9
AUTHORS: Vorontsov, A.; German, M. As
!5-
ORGi Main (Glaviiaya geofizichoakaya
bse' valoriya
r
o
_.-TITU; SL~tidying atmoopharic turbulonce with tho- aid of a bolicopter
SOURG'Zi Leningrad. Glamiya.goofizichoikay- Trudy- no4 -1-71;-1965-
sarva orya,
Nj .11 ttat _iasledava atmq.vf empy -tlirbul~~til'oati--Ptt-yortolotnYkh transakh
Rosult-s of ;~ho invc3tigat- on-o. a mos hariowturbu once-on-
f t
4.tur) flight cqara(-,ttjr1stic j weathar forocasting, atmosphoroj
TOPIC TAGS.-, hrvlleot
wind, 0-,rij2p hor.1a turbulynco,/ 1 qvo~r_loitd g,, qtoj:j 141 1 holicoptor, ITI 11
-or
helicopL
mosphoric
ABSTVACT t Tho ust) of helicopter typos 1,11-4- aryl M-1. in studying at
turbulence - Is -douc-rib(KI, - -The advantages of helicopters w, ovar fixed-w1ng craft in
atmospheric research are briefly discussed. Loads, acting on a helicoptor are
;_dascribcd in ralation to the cooriinate'system shown in Fig. 1, where the origir,
Card 1/4

L 5021-66
i 7
&CC till tAT5024860
directions which are given by
Y
n,= n
I The lielicoptor Jn an arbitrary flij;ht.atUUt6a is skotched au a froe body for tho
purposo,of relating gcomcW-y and forco varj%bles. &pressions for resultant rotor
!.-aerodynamic torces, - draff re,,~istanco forecs, pm)pulaion forcos, and qavit~ are +
in(Alidor-10 The F,,ivon forco and trooriotric quantitlos aro Uien rolatud to the
Two mades :of helicopter flight are definedl,
dimensionless overload parameters.
ausponded flignt is flight in which the conter of gravity of the craft is fixed
with.respoot to the air mass modiuri and thore is no rotation of tile craft about
the center of ravityj horizontal fliGht i!j termed stationary when translational
L,
accoleration-is, -Piro -and -no-ii,~tationary-otlijr.4isoo---- Tho offocts of atmosphoric -
turbi;lonco on both sti5ponded and horizontal I'light modo3 aro dovoloped, and tno
aerodynamic forces rr.,neraLed by tho rotor'blades are derived. The computation
of vertical downdraft characteristics from flight control paramuter3 and accolcro-
raph data is domon--trated aril tabulated for both airplanes and holicopterst
g
Gotirputation of turbulence coefficient follows the algorithm of M. A. German (0
turbulentnorn obriono v oblakakh. lletaorologiya i gi(irologiya, No. 10, 1953) . The
Card

Im

VOHONT-Juv:~ i,A il T~4 V. A
a C a
y m ns of hell opt r
Trudy GGO nu.17101-19 165/. (MIRA 1819)
1. Glavnaya goof observatoriya in. A.I. Voyeykova,
Lanlngr~a.

L 177-3-66 EqT(d)/:-~67(1)/E7dT(m)/E7rlp(w)/~A/FCC/T-2/DP. (h) EH/GW
UR/2531/65/000/171/0020/0031
ACCESSION HH: AT5024881
____V6kontsov,-- P.--A
Atn%OR
TITLE: Program and method of investigating atmospheric turbulence! along helicoptet
routes in the mountains.
SOURCE.,- -Leningrad. Glavnaya geofizicheskaya observatorlyd.,Trudy., no. 171, 1965.
Rezulltaty issledovanlya atmosfernoy turbulentnosti na vertoletnykh trassakh (Re-'
sults of.the investigation of atmospheric turbulence on helicopter,routes), 20-31
TOPIC TAGS., aviation meteorology., helicopter bumin#,; flight chart, atmospheric
turbulence
ABSTRACT: The author presents the results 6f,an investigation or atmospheric tur-
bulence in the Caacasus and the Crimea conducted to provide background data for a
new set of instructions for meteorologists preparing forecasts for helicopter flights
in mountainous regions. The study was conducted with the cooperation of the Main
Geophysical Observatory, the State 3cientifict'Researdh Institute of the Civil Air- I
Fleet, the Central Institute of Weather Forecastirg, the Central Aerological Obs4rvd~-
tory, the Moscow.btate University, the Ukrainian Scientific Research Hydrometeoro-'.
logical Institute, the Transcaucasus Scientific Research-Hydrometeorological Instit~tej
edrj t/2

L 1.773-66
'ESSIOU MR: AT 0-4881
A
CC 5 2
and the Aviation ~Ieteorological.Station of the Civil Air Fleet at Simferopol MeasJ
urements -were- madi.- of. -temperature, --pretseure s -humidity, wind directionand veiocityl
and cloudiness using specially equipped MI-1 and MI-4 helicopters, LI-2 airplanes$
and ordinary helicopters flying on regular routes (Kutaisi-Shovi and Adler4ovoron'elyak).
The equipmentt instruments, and proceditres used and the' results obtained are dis-
c-use e-d.- in detail-. --Findings -obtained in- earlier--studies- are also clted.~ Samples-of
'Charts (perspective sketches vith rellef shown by hachures) used by pilots in designing
turbulent- -zones -:encountered en -route are -presented.--- Recommendations -are made for--- I___ ____
speciflcat'Loh6 to b6 incorporated ift the new flight inatructlobsi Origs art, has;I
18P)
4 -figures.-----
- ---- ---- ----
WS=ATIONt oi&vfi&Yd ge6ftzicheekaya observatoriyet, jArlitigrad (Main Geophysical
se."atory).,
___GtYBMITTED--,. 06 _ENCL., OO__ SUB CODE: -ES
No Mir SOVI 009 OtHERr 001 ),TD PMO!
a

VORONIIIISOVP P.A,~ VAS1111YET, A.A.
i-~-
Problems of metr-.orologJc~al flIght, security on bellcopter. routes
in mountidnoua*regiona. Trudy GGO no.l7]gl22-IP9 165.
(141-RA 18: 9)
1. Glavnaya geofizi-1hebkaya observatoriya Im. A.T. Voyeykova,
Leningrad (for Vorcntsov)'. 2. TSentrallnyy In3titut prognozov
(fa'-~ Vasillyev), -

. -M
-7 -2 ~v , . 11 " ~. . 'I
muommm r FEM - ~ Bab -0
-o
Mnmffl-

I Eli rnra
-fu
MOV
I-

I I ' - a
- 0-7-.- I
I
k %
I F I
-- - - - -1 - . .- -- -- - .. .
I'M'
;1,7 ~11 E,

Doe 48
Metallurgical 2quipumt,
.0peration of -Woundry *&-~,-iers witb rAyv.(;ra"
P. B, Tbrol, &,-V
~!Zft Skon Tbp" No 12
Discusses operatzon of 'foundri '-t~erlm vith jzv-
VMde fuel. Refers.to experjence6:~vhich show
,1%&t burning brovn coal in f0I driers is quite
"Possible wA can be achieved Vittv
61mcultiew; *. Thsatisfactorl use of brown coal
. j. in.nosVeases, aa
In driers can be expla:ined.
U149 duO to ftultY tanan c.e and c=ajtjon of

11 is w "16 Ito malla Bull MRAft'Iftil UU us lilt Olso
A a L A-L- it 2 a I I V V I-A . I- A AA Cc so Is j C a a I-Jo
00
.0, 0
Coatinuous drylag of Whopme. 11. 1.
00 0,jr. CAM. Ind, (U. S. S, R.) 7. 21 ~00
of ,f tim-trucliun cd km)p.tylw thirr. Tinir rrejuirrd few
-hyinx 2.5tim..ratiscity of dry wateiWouptut 11,3111ke., .00
00 -hift, ino6ture rrdurtkm from Mo to I 'hA moi~turr ir- .00
inuvAl per unit am of thirr WA lig./sq, m.1hr. and %traill Off
so -81"ImPlim 2210 kS./hr. at about 4 Olin. it. Z. X,
00
00 3 ago
golo
so
*6 goo
410 4F too
-00
'00
of
A I a SCULCV64KA1, 41TICAYWC Cl,411WKSTION
woo
'NIJA)i ca". 'All Foo
wt
U :6 As.
pe a a It 0 4 A a it a or a a It a MCI 1 14 Or IN I a 4 3 0
*off so of 0 off so* o so go so 000 0 0 0 0 0, 0 0000
0 0 goo 10 0 0 IS * 0 0 0 0 0 00 0 900 0 0 *is * So 000 00 so** 0000