SCIENTIFIC ABSTRACT KLINKOVSHTEYN, G.I. - KLINOV, ILG.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000723130009-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 18, 2001
• Sequence Number: 9
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

TUDMIT, AiLl IMINNOw . 0-1-; USININ. A-A.
--- OWAIWA%IW
Cotook oare'la sports oomwtitioaal larilas avtomblll v skorost-
arkh "r9vwv&al&kh* Moskva, Gas, lod-vo *Flskulltvra I sport.0
190- 95 P. CXIarofllal (mm 718)
(Autombile molue) I I '-~;

ARMUMILISMY. Tu*Ag DOMMYSM Yu*A:I, ILnMDTSRXN
Inshoner, "tteasestj BAVW: Ismo lks"91w,
Me, tokftlohoakly rodaktaro
CTw automoUle dri"t's o"tj Uboches =$t0 TodItella "%a,-
mobilla. NoWwao Oeso sambso-tokhaoltd-vo wohimst"Ito US-rr,
1954, 86 P, (MM 8:3)
(Automobilso-Doelp and oonstruction)

-71
RUU"o 1). XUNZOTIR2M, 0,; pMZOMX, A.
PrOgPOINIVO Or"U" in Automobile dTIVIDS- Avi-tramspo 32 so.1s
9-11 Je, 154. (WAA ?SW
10 TGGIOYUIW W*0h"'IPIl0dO'Mt4l'IkIY InstitO ATtemobillsop
(Automobile drivers)

KLMOTSMYN,G.. Inshoner
ShorteWs-s-sls the oreanteation am roviation of higbvay =d
str"t traffic. Avtotramspo33 no.6$21-22 Jo (KM 8:10)
(Traffic owmering)
m
1. MR-
Oifl
RY,~. Vu V
g

VJBCM.B. - KLMOYSMI.N.G.
The 218-12? Interurban motorbus. Avtotransp~33 noo8s27-29 AC155.
(KLRA 8 3 12)
1. lossayusnyy nsuchno-looledoystellsirly Institut awtonobilOnogo
transporta
(Notorbuses)

MMUM, A. I XLIMYMM. I-
L-' --*ja4m-
Seven hundred thousand kilmotors without vajor overhma. Avt,
tr&A~P. 33 so.12s16 D 155. (X= 913)
(LsnlnpM-Xotor*bds drlvsrs)

-NOUN-IN f3flaht IM'FAN. Yurly Arkadlyeylch;
PAPMI# S.T.,rs__&k_f-or7UTMM. A*D*# ekbnIchoskly redaktor
CAutomobile cross-country runs; roadability and outosobile
driving] Avto*6bIIIrq* krossy; proktodivoetl I vozhdsnlo
avtomobilla. Isd. 2-os, Ispr. I dop. Noskya, Oos. Isd-vo 871skulltura.
I sport,a 1956. 164 p. (KLAA 10:5)
(Autosobile racing)

KLIJIQEWM fil;'Inshener. mA-Iya respublikanskey katoprilo
Percentages and norml competitions for economic operation of
automobile$# I& rult 14 A062:1010 1360 1 (XLU lot 3)
(Anto"biles-ruel consumption) I I

ZUBCHUI. B.1 KLI
Prospootive tnws of buses, Awt, transp, 34 no.6t25-2? Je 156o
(am 919)
to TessorustWy nauchno-leeledovatellskly tastitut avtmoblllwp
tranaporta.
(gotorbuses)
AIN MW~ TINUM -0- iz
P10 M
R2
C~ Im

IMIIMDYO=Nl 0.
The Nbecow-kinek-lbecow races, Alt, transp, 34 no,10130
0 (MA 9122)
(Automobile racing)

%ftu E611==UTXO G#
llmmwmqmmjmft~~
. U Ceschooloysidue Sa rtd. 15 nooltlS-19 J& 137s (9m lo: Q
I Osechoolovsklow-WanspwUS Ion,, AutomotiTe)

lusbonero
IWIU& wtoftu drIVIS99 by A,A. Drdskows I.P, foltako. hirimd
by 0. tHrOk"ahtelso ATto trw"p, 33 00.0339 Ag 1570 (XmL 1019)
1. WwW'aik 10or%torii pasmahirskikh avtomobtUy Imbso-le-
I=tltut& avtombillafto traaqvrtas
0 (Automoblls dri"rej
A*Ae (Vol tako I a. Ip.

zuwm, Be li=m=e 0.
CouMison of citr motorInwas basod on eove paronteres 1vto
transpo 35 no*UM-24 1 05?. (MINA 10112)
Notarbwos)
r". 4i
ME- 14.4

j, rT
TAKWAI, FT*,,
tolfto red#
Ewlvioc of antmblust a mau4 for lustrmto"3*211dolie
awtomblUal rWwod~Wo dlis IzArWom Isda6a Noskno Imufto-
toA26 wtotrulp, Se. 100 pe Mm Us?)
-twma"Ouls drive")

ILMOTSMIN, Osorsty- 1111ohi SMOTA, V.I.. red.: GALAKTICSOYA~ Teelo s
(Affect of baste operation factors on the braking of automobiles]
T111snia oonoynyM sksplustatatonAyM faktorov as tormothonte
aytomobilla. Koski&. Avtotransisdat, 1959. 26 p. (KIRA 12:12)
(Automobilse-Drakes)
TOTF

Inveltlesting and testing bmklos Properties of motort.rwks.
Ayto transp, 37 U0,711942 A 139, (KU IVIO)
(Notortruaks-Braime)

hr more attontion to the maintenance 'of motor v4ohloles* Aite tronsps
37 no.1209 1) 159. OaRA .1313)
2elauchno-Aselsdovatalts)dy lustitut avtonobillmose, transport&.
(Rotor "hioloo-Vaintenance and repair)

'LURIONOYp log kandotakhoonsuki_ JMLKWWX1N. Goo lash.; MOGAWYAllat
lash
Methods for soWullog the speed of latembam boass. Awto
*Tanvp .38 no$ USIS-19-9 logo (KIRA 13M)
(Natorbut Una*)
I- U-1

ILINKOVSHTEYNt 0. lot Cand TpO4 801 -01study Of h
f U4~and method
Am:ftm qualities a a of
In operation." Mom jislITZ/9 1961. (Min of Higher and So*
Speo Ed RSPSR, Moo Autonsoh Inst) (KL, 8-61, 244)

,~NXOVSHTmg 0.
Impsov the quality of traffie "fety posters* Ayt,trans no,2t
le Xachallnik labomtoril besopeonosti ftisbenlya 11-m4wo-12910do-
vatellskogo ImUtuta aytomobiVoogo tmoporta.
(Traffie safety engineering)
T ~ Oqr

oosroy wica, mm, 4P., r"ol xzrouwj6 Tftv,
operating 60MItless] -uSUAcwmde tormosm7ft ksobseft am$*-
wbilel v okopluatatsile Xoskvat A"etraselsdaig 1961,
UM)
Notor Tobloles-fte3ces)

PMUOUlls AXS 3VfKAWV* I.Ta.1 TINOUAWT# T.T.1 VA, T. 3.
blidmall whastirat INSIMMo I,Tj T-ANALIMM TOP'l
1210=00 T,I*j I'M I to A.At MdOMMM-~L14:
FWI# A.O.*# red,lid-val takhasrod,
[Brief smal on motor votdoles] ltratldl avtoso'billayl
wavoobalk, Isdj,j, Voters I dop, Moskvaq Avtotr ass-A-60
P. (wu IAIU)
trassporta, 2,, Smokes-iselodowatellskly lustitut avt~eAlll-
nage transporta (for Posisovk1s. skaww. Vlsw&dow. SMIUSA).
Obter vWoUs)

ILINKOVSHTIMI 0 1 otvo sa vypusk; YkMOKOV9 V.I.,, red.; WDANOVA#
I *=Lp
A#Pop tekbno red,
(Manual on traffic s&fotyjRuk*"djtvo po obespecheniiu bes-
opasnosti dvishemila. Hoskvap Avtotransi2dat 1962. 107 p.
NCRA l5sl2)
1. Moscov, Youabno-issledovatool'shy institut avtorobillnogo
tramportao
(Traffic safety)
, x
Riv
-
3

ZNAKMKIYI, Aloksoy Nikolayrdah(doceased1l KLINKO
nlish; ifluppi, 1.6.p kand., to . no , red. j YABWKDT#
V,I,j rodAzd-va; CALAX?IDIIOVA, lo.N.,v toklm. red.
(Gorman-Fasslan autowtive transportation dietionsr7] go-
notsko-rujakli avtotransportayl slovarl. Pod red. I.S.ShILIppe.
Moskva,, Avtcytransisdatv 1963. 336 p. (KIRA 164)
(Transportation* AutmtIve-Dictionarles)
(Ceram language-Dictim"#ies-Russlan)

BADKOVo V.F,j 4LMKOVSI?MII-j 0.1.0 kard. tokbn. naukt retsonzent;
[Road conditions and traffic safety) Dorozhrqe unlovIla i
bezopasnostl dvizbonlia, Moskva# lzd-vo "Transport,* 1964.
168 Pe (MIRA 170)

kand. tekhn* naukp; AKSMOV., V.A.# Inzh,;
UMSIYARTSp Z.G.p insb.; SHMV9 A.V.p Inshej
KWWWANTSo D.C.2 inshtl TROSHINAj M*Ya*j inzh,;
SMSYVX# L,$, Iw&b*j PARSWp M.A.# iuhdl WPINSWAq
I'M*# insh.1 FILIMICH, B.S., daktor takhn, nauk;
ILARIONOVO V.A.0 kand. tekhn. zeukj POLTSVO M.K.t insh.;
WGAKj E.L* insh.1 CHIGARKO, G.T.j inzh.l KCVOWNA9 V.S.9
red
[Traffic safety w0 sarety measures In automotive transporta-
tion) Bezopamusti dvirhealla I tokbnika be2opemsti na av-
tomobillnom transports. Hooky&, Trarwsportp 1964. 74 Pi
(MIRA 1811
Is Moscove Gooudarstvannyy nauabno-iseledovateltski: insUtut avio-
mobillnogo tranq*rtao 2. Hoskavskiy avtozekbanicheskiy
itstitut (for Fallkovich), 3. Hoskovskiy avtotobillno-
doroshMI Institul, bwrA Molotov& (for Ilarionov). 4. Vse-
soy,uznyy zaaahMy politekhnichookiy Inatitut (for Poltev).

KATAYEVj OSTPMSUT, N.
Traffie safoty and organlution, Ayt. trtnsp, 43 no.lt46-48
U 165, (MIRA 18%3)

11 ka rid k hn . w-u k t
Trafric organlzation W, c4roy,
D 164, (MIRA 18s4)
1. Um4stttell nactialln1ka Ccottdar,~tv,~tunoy avf,4rf-,Hl'np-y
inn~ektalt Olamcgo uprav1prilya rAllunit okhrany
ctzh~zhpstvonnogo porludkPA 10F."ri (for
-XMIRM Tffim

Mrftio
EUXWSnT, Nq IMWt 0-
a -ui,%rolling plast dismal.
Prospects in the Ulf# of "titiottal I -
zhur"O'bA1010 17 uo~3s169-1& IV-Je 156. (a" gge)
10 fustrial tut rIn=skW Akads"I
007M0 6610110017 ISOU
sell sank, Berlin I T-Mitut fitOPIA810611s
Asherslobes.
(AITISIOUCS) (PIM -)I,~ ITM)
M11MR-M."Pi" M-1 r.28,

A. IkAR tl.j. Dis *#chw%rxkWlsk0V Ow ftu"hs-Attm
, . 6f YUK-4,"
420, blow a' IVA
From tho lwtitsito of tho Martin Whtr Unimidti, 1141k-
wittenhom tho flat" 4,*vito Nwi kggi"' tit wilt Dir. of brim lix*n
Aft W.1fal otiiris~y ~~ r4nlio (phattaw ("Uhifl~11 and mr4iolssuf oil dwirf
p at tb-- -xw.-i-n
IMAM'( is the
o"Im vil.*4, ot oft'SA61, omq"- -waL TIM- to,-Af w tho
tam Weltmid M th,~' of tw OWAA. tbo P"ding and
lally T m 0t'#,1j,'rf olm Tl~pfi,~,svk L- m tit W to
If Armo, thc po4o, tod porotv
c"vht mwtiq~ *.g, 14,40mari *M Juli mn,qw thp rurhm orid th~ drgrf
thst t6 lloamts of vj.C~4 rq,remmf
in Mok . -
p-ml,mts of toomim T6 4www is t pw#nt" thl, --uh IW
KvWm(v of Tim W-MY in tho P6.4,gy .4 the wilt was sff6rdpd I)$
vowfam imx"latinh oot vmWt grafting ellwlimplax,
767:7,~ ri~m

UMOTt alri
[-~~Agr, t4,.,,,th,,,
"Ampeats of the orgmia'ahmstrr of mulphurlm by Y. Chananger.
RW*w" by RA12inot. Chou p-m 11 no.111600 It 162.
2. larlova universits.
ai"
mm UA~

I=OTj J.; VMTRCILj A.
Bcckmm's rtgmpwnt of triUrpone-3-ketaximes, CoU Cs Chou 27
no,.P;Yn-396 7 162.
2. institut fur orgadsche Chasis, tarisunivw itat, pm.
vj
IT Of

KIANOT, J. I VYSTHCIL, A. .
By.proA,jots in the transitions of allobetz'in to hattrobetalln,
Coll CS Chen 29 no.2016-530 T 164.
1, Institute of Organic Chsaistry, 0.%4rlos University, Preps.

OZZMOJLOVAKIA
049wement Of OPNMIG MMIstry,, sarlova IhAverldtlo
(for both)
Asum of amboo" ,yak ml
AMtCRAlkAL No 58 maAa 19660 VP IMP1092
Ste"Ohmlotry of 2-bromG
ftrt 7$
aUeboterobstOllMe
T., 7
INK=

niNGTOY.Ta.
AD optical phosomawa darift a sunWalle Xoteore I g1drol,
no-3:56-57 Mr 15). (a& 8:9)
I* Avlaustaostantel", Terkhorank,
(Sam)

~ a A - -t - , -,Lf I - - I I .~- ~- -
f I k~ I Al 11 Vy J6, P A , , ~- -`
A ? A"
ll~- ~--. -- - - - . - . V, - . ~7. ~-.. r. I
. . . ~, 1-7,Z-1:177 -I -- -~,. -Z:tL,- 7

KLINOV, t. YA.
KLINOV, F. Yao "The solid phase of vater in the atmosphere at low negative
temperatures (frost )5 to 54 dogms)." Main Adninstration of the
Wrowtoorological Servicej Council of Ministers USJR. Central Inst
of Veather forecasting, Hoscov, 1956.
Knisbwa Istopislo No 39s 1956. Moscow.

Associated orystalliestlon of water TaPor of the atoollphorso
Kaiser- L eldrole-20.7122-25 A 157- (xm 1018)
(Al4vospbore) (Ci7stallintion) (orrosoopy)

P~T- ;. I
- - -, - , -
,, - ,
. I

SOV-,ft9-53-6-11/12
AUTHOR-.Klinov, F. Ya--_
TITLR., Polar snow (Polyarnyy snag)
MIODICALt Izvestiya Akademii Mauk SSSR, Scriya Geofizicheakaya,
1958, Nr 69 pp 796-799 (and 4 plates) (US3R)
ABSTUM The ice crystals forcing the snow flakes in the atmos-
phere at a temperature less than -4000 differ from those at
above -3500, The structure of the polar ("cold") snow, as
observed by the author in Verkboyansk in 1952-1954 is
described below. The most common shapes of the ice crystals
at -400C a" shown in Fig.l. They are groups of crystals
falling from :the free atmosphere. The size of theflakes
is 200-800 IL. The different crystalline forms at -5000 were
observed in the layer of the atmosphere nearest to the
Barth*s surface. Tbe size of those is 100 It or less (Yie.2)
It was observed that &W of the unusual crystal shapon were
mixed with the above mass-producod forms. The most interact-
ing ones are shown in Pig.3 and FiS.4 (too difficlilt to be
photographed). The variety of for= of the snow flakes is
caused by the heterogeneous conditions accompaiVing the pro-
duction of ice c-' stale. In the majority of the complicated
cases an original "maternal" structure could always be traced
Card 1/4
-7-
F"TMMM"M7777777

SOV-49-58-6-11/12
molar Snow.
(with few exceptions see Fig.1/15). The atmospheric con-
ditions connected with a deep, cold depression near the
surface and rather warmer upper air can produce the snow
flakes of *slate" type ice crystals. The ice crystals formed
in the cold air near the Barth are of small "stalk* shape.
When the stalk cryetals start growing from the slates
(originated in the upper levels), a very elaborate form of
snow flakes can be produced, often destro7ing the original,
maternal shape It is possible to forecast the
type of falling snow by considering the general synoptic sit-
uation. The observations of snow carried out on two occasions
during the nights of 11-12 and 17-18 February, 1954 gave very
interesting results which could add information to the meohan-
ics of snow formation. The respective air temperatures were
-5? to -5500 and -43 to -4100t the relative humidities 75 and
7% the water v pour pressures 0.02 and 0,11 mb and the
deficiencies of asaturation 0.01 and 0.03 mb. The snow flakes
were collected on the objective glaso which was kept out-
doors. The size of the ice crystals was 15-60 IL (Fig.5a).
The light scatter from the Moon could be observed. Dgring
the first night there was a bright halo of an angle 11201.
Card 2/4 The halo was surrounded by a faint greenish ring,' A weak

SOY-49-58-6-11/12
Polar Snow.
vertical column could be seenpoross.the Moon. It could be
assumed that the verticalooluan was the moonlight reflected
from the minute ice crystals, while the light ring was
caused by the diffraction from.tho particles of frozen drop-
lots and other similar matter. During the second ni&ht the
Moon was surrounded by a halo and an outer circle of 220.
It was observed that the size of the ice crystals gradually
decreased while the dimension of the halo increased from 481
to 20181. At the and of the observation time a space between
halo and outer ring became tinted violet. The top and the
bottom of the outer circle were much more intense than its
remaining area. The ice crystals (Pig.5/5) were very small
with no trace of larger particles. The position of the
individual crystals on the objective glass wus observed to
Gard 3/4

SOV-49-58-6-11/12
Polar Snow.
be tho same as that during the free fall. Thus the optical
phenomena of the sky could be explained by the shape and
size of the ice crystals, This kind of observations could
load to better determination of the physical and meteorolo
ioal effects in the atmosphere when considored together wit;
the general weather conditions. There are 5 figures, 1
table and 4 Soviet references.
SUBMITTED: June 12, 1957.
1. Snow-Phys1cal propertlois 2. Snow crystals--Structural analysIs
Card 4/4
t 7771,

KLINGY# F.Y&.q kandefiso-maten.na-ak
of W
Pangs do ond,pressures of a free air Ortex. Nauch. tnidy
HPI no*?19~s2?3-284 *58. (MIRA 14112)
7
(Vortex notion)

WI/49-59-9-20/25
AUTHOR: Klinov, P. Ya.
TITLN: On Super-Cooled Water in the Atmosphere
PERIODICALs Izvestiya, Akademil nauk SSSR, Seriya geofizichoskaqa
"'i
1959, lir 9, pp 1430-1431 + 2 platee(USSR,
ABSTRACT: A haze with ground visibility 4 to 10 kc, but only 1000 m
from the aircraft can be sometimes observed In conditions
not justified by the humidity. This condition develops
when icing occurs above the temperature Inversion at
heights correspotdinz to - 350C which can be up to
1000 m high. Investigations were made with.this kind
of haze by the author in Verkhoyansk. Samples were
collected and hotographed. Some of them are illustrated
in Figs 1 and K It was found that the particles of
mist were composed of ice crystals amples of which
are shown in Fig 2a, Their formatio'n'xcan be explained
by the presence of eqper-cooled water In layers of the
atmosphere above 400 to 600 m thick at about 900 to
1000 m above the ground level. There are 2 figures
qax4,10Q and 3 Soviet references.

VMS I BOOK BMWITATION SMAM
Klinov* nil Yak w' mw4 okl%
Voda v *ftos fen PA,:1148MM -t ftrakh (Water An the Atmosphere
at zow .1 "!%P!" AN MR* 1950. 168 9s
11iratures)'Noseow
Brrata Ile on the Inside of back oover.t 1,,&)b copies printed,
is
3ponnoring Agencys ~ Akademiya nauk SUR. Institut prikladnor gooti-
xlkI#
ResLgd.t V. Ve Plotroylahl -3d, of Publishing Houses G. 0.
tkdv,,o Toch Bd.s '0. A. Astaflyovae
rwoess: This publUation-Is Intended for geophysicists and meteor-
ologlets.
COVERA011 'The publication discusses the different phases of at-
mogherlo molstviri U.Iow tiwV#ratu"s-(-35 to -58*0),p andrew
let d Optical phen0ftena. The material Is basedon experiments
In the direat arystollization of water vaporp conducted tinder

KLINOV.
Observations in the lower otmosTheric 14W*r riade fron towers
srA waste. Meteor. I g1drol. no,12s37-42 J 160. (MW 13sll)
Ti~
-TIZ 7-FoV

MIMI Foyal
some Npeolf lo foata"s of the solid phaso of vater In the Atmosphere
at teVeraturos nuh bolow the froosing point.. Trudy OW no.U*tk6-
52 1600 (KM 13 s 10)
(Claud physics)

Some characteristics of a turbulent velocity field in Oe lowst
300-uter layer of the stmosphore. Irv. AN WSR. $or. pIrts.
no.IM1570-157? 0 161. IFURA 14:9)
An SWRt Institut priklednoy pofitikio
(Atmiosphorie turbulonc*)

KLTWVO y're,
OPt1W Pbsnomma observable an ice arystalp. TiWy 000 no.209sloo.
113 161. 1 (KM 14, 5)
(1030 "Ptals) Obteoralogical optics)

L1332"3
'ACCZMCK Stv 423003M

A sk
2 of the- loals# Atop the tam is usid for
-
maldog speaba Obse"Suoul iman"amts
s" "Oor4ed am instrwwnts,.
oodrolW from aspoeW buLbfl*'*Vtb9 base of Us toww. This article to
fm a cousation or artleles discri" the toww &W Its lantmats arA the-
res4ts of some -of the meafth owted out at th*- twjw.
AS&WIMCKs nom
Pj
St
semi 00 =A111M

XX COM AS
Iwo w

2/2

KLIWV r.Taj,--
Ilectria fmaswevients of aoroftsical valmes~ br L.O.K94hurin.
Redowd by F.U.Mmov. Ns".i gidrol# no.807-58 Ag 163.
(KIRA IWO)
.0-1t; IVRIRMI

V
ACCESSION NRt AT4010224 S/30$6/63/000/000/0053/0059
AUTHOil KIlnov, F4 Y4#1 Pqltavgkty, V. V.
TITLE: ft"Sureunt Of wind velocity In the lower 300 motor layer of the
atmosphere from a high meteorological tower
.SOURCE: Issladovsnlye nlahnego 300-metravago sloya atmosfery*. Moscow, 19630 1
03-59
OPIC TAGS: meteorology, wind velocity, wind velocity measurement# anemometer., i
l
ower atmosphere, photoelectric anamomster,_ wind velocity profile, wind velocity
altitude dependence
ABSTRACT: The authors present a Moo diagram and a detailed description of
the operating characteristics of an'Improved photoelectric anemograph developed
on the basis of the remote-controlled anemograph developed at the Laningradskly
91drometeorologIchoskly Institut (Leningrad Hydrometeorological institute). This
apparatus consists of a system of, photolmpulse transmitters situated at various
-levels of the tower a converter consisting of a pulse-shapIng cascade, an As-
sembly of Individuai converting i Inas, and a terminal ampI I fying cascadel & relay
recorder;snd a power unit, A -cal lbration curve for tho photolopulse transmitters
Is x W ]as of the wind velocity profiles
C0,.d shom The authors also present some
MO.

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11' Tg- attf ~-L ... -
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, - -?fil-,4im-tV. "M .- .1 ~ -, ~ " - ,,,.:
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A
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0"
ACCESSION MAI AT4OIOA6 S/3056/6)/000/000/W/0070
I-
AU
T
0
t
AUTHOR: Kllnov, F, Ya.; Androyev, v. oo
T
TITLE: Measurement of taverature in the lower 300 motor layer of iho atmosphere
IT
sur
LE
f rom ahigh mo
from a high meteorological tower
S RCE.
0U Isill
SOURCE: Issladovanlys ftlahnego 300-ostrovogo sloya atmosforylk. Moscow, 19630
64-70
64-70
I TOPIC TAGSi -aiiocrology.-lower atmosphere atmospheric temperature, temperature
P C I
0
measurement, atmospheric temperature messuramont,:!tamparaturo profile, air
toverature attitude dopendefto# thermogradlentograph A
ABSTRACTi The siructuie and operating characteristics of a new thormogradlento-
giaph developed on the basis of the remot&-controllod, automatic Instrument at
Ingrad dr ti rol I'
the Loningradskly gidrometeorologichoskly Institut (Lon Ify OWA 0
09
u
cal Institute) are described In detalle w(th a block diagras Illustrating Its ;G.
to determine the temperatures at various levels of a high meteorological-WwWo ~j
The apparatus consists of transmitters with the operating arms of measuring
bridges, a network of relays and a multichannel recorder; the bridges which serve
as the sensory eloments of the transmitters consist of one copper resistor and 3
wanig.res liters. 4everel temperature profiles obt&ln&d with this apparatus
.-Coan

MW vate

TSVANOt L.R.; ZUBROMITy S.L.1 rVANMp V.N.j KUNOV, F.T&.j
KRIVOMKO, T.Kj
MWasurevent of some c
,"ateristics of turbulence In.the
lower 300 asters of tM staosphers. Isy. AX SM Ser. goofts.
no.51769-782 My 063. (HIPA 16:6)
1, UsUtut fi%JJd atmoefery AN SSSRI
(A*ospMric turbulence)
'I@ M

A-1 j 5
LA
S
L 23471-65 CWT (1) /yQQ QW
ACCLSS 1W A i AY50a1817 S/0M/65/000/0M/0Q5)/bM
.MaticAl
A 300--fteter netsomia teetl toimrNr'rind Its apparatus ocarlax to used to
iower luqsr of tho atwsphgm
SOURC-Bi MetoorologVa i gidroloClya, no. It 196% 53-58
TOPIC TAGS s astooralogleal tower,, alorometeoroloo, atompharLo bounftry layor
JUL TRACT t ki arrfwy of equipient. tar autwatle p in the
-- I a Ktoorol'Wigg-1 Veas-ure-banta
(V--tnotar laynr of the stxosphlj:~e has boon ot the Institut
geofizlkl (Inatitute of ApplIed Geopl'Msics) in acceirdnnee Wth the
0: n. -?gA2M. The tcu--r Le a tubular wta'14c vast, 310 a hiCh vid
2.4 m in diameter. A Mat at the, top extends Ule'tota~ t to 3.15 a. Tho
'.~,ver Is znde of 6-foot steel units welded toesther. Gt~&Gl cables am attacneJ
8,- suvcws~ halehtm to serve as CW. Cm-riors are ourpendod at different holghtb
.cr rrie'-n~ ntL)arvatlons. Thar* u,* work areas on the ~-vLepdahla yerticAl rpat
a), on the upper platXors (310 a), ine 3n 13 other piatfirm
!n helght trom 24.6 a to 310.2 a. These rd-Lrorw are 1-1.5 a wide.
Four t)o 6 m 1=V extend from eaoh platfam (N,I!OJ, sM W) w1th samor arrik-8
C.'d

L 23471-65 p"
AMESS ION Wt i AMOM817
at the and of each. An olfffttar a too kthin the Lower, and PoWr lift" Md
UM rea
rocordine lines are also 9trMg Wide. k% Uri= b019MO aut tIG 4 bV &M
nndo of tamperstvres, wind y4o*1tyg tvo-dimensional vind diraction, huxddIty.
c~iaractaristias (total, direct, d1frwe, rpflseted, and radiation bal-
BIX-31,, irvj norm turbulence altaraoUmistIca. Tho nutomtla recorde are kept on
Jllrectly rrom the sensors, some Its discrete data supplied trf c4mput4a
wind direction). The p"sent equipment provides what Is called Opassivs*
non The goal it "aotiveg measurements, i.e., data on variations in
tLn,n (neonrnal fluctuations. trarAs, and so forth), in order Ln vAka better pro-
nni '-o understand broader problems *Y_, D
torath
Y 5 1MV
S. P. Luk%yanov, V, V.~ Poitay"01 , V 0. Sterfanove. a.-A others conBCj6Uy7-%j6jk&d
W1 u~Rcr to make uxG or the res
The photoCraphs
rat'ng the present artiole we" made b7 V, SL_Atqrozhko and V. P. Vorw-tia's"
.irt. hasi 4 figures.
(IneUtate A
-P~,:AT:3N'j Institut priklad=V C*of;%ik1
.'71~ ~' f 00 ZWL t W SUB 00091 ES
iuy SOV I Oil OTM # WO
C0, d 2 /2

,ACC Nits AT60IW594 SOURCS U-765
j7oFz: WBF01/65/0007002 074/0083
A)THOR: X1100-1-4,J11"YA
j4
OROS Institute -of -APPI144 -1 :(Institutpriklaftc7 poftsik
TITLE: In--- an observed a"* of a frontalators
SOURCE: Leningrad* lintitut prUdsdwW geofisiki. Trudl no. 2 5. PovantebM7
slay atmostary (Bound*4 lsysr.,,otUa xtmosPhen)t 7h-83
TOPIC VMS: - alaromet*arologys- -afteordlogiesl.tower&, frontal movement 6 frontal
gredient-
turbulence llghtAlngt tWindence, lapse ratel.vind gridlent.9 pressure
ABSTRACT., Watinuous ssfisvl~ftmts sads at the 300-m meteorological taker Ineluft'
those carried out, during storm'. -, Ibis paper gives a detailed account of -the, wt*or6'-:
logical conditions In the lover 300-P layer ofthe atmosphere as a front passed the
tower on 9 July 1963 boWeen .2000'and 2300 hr. The front approached fromi the West
at a speed of -20 30 ka/see andvan connected with a low vhose centir vas, In the
northern European UGSH. Back of thez, front, -and traveling at about the saw speed t
V" a rather zarrov -higb*pressure, rldge. Vomewbat went of the higb there VAM
another, rather shallow low (1005 ab) moving toward the northpast. ne M1 range.
of temperature changes took place -in 2 1/2 hr and wintl-direttion cbanxea, in 1/2'br,
LightnIng and rain thvwere preceded and 4cctopflled thf, fro
nttl rmn- ne -
1" a ut atmospheric Lamperature,.pXessure, and vind 41-r-ictlan -mid npetd st4o at, the
c-ai4l
L

NC2
AT6OiiO5�V
ACC
-
-
- 0 7
tower mv described, snsipsd~ .=47111ustftted graphically by disigraw# pr*fil*s
and tablas. 9"aial tout
on$ such utue6ulebeet piriods of 4alm, ox*unt Ond- locs.-i
tion of addling and gustat and, tem"raturs in"ralon are Identified and theIr
interrelatioubips.-bdicatid.7,-,,orts's, &A@ hass 4 n gures and 3 tables,
BUD COD19 Oh/ Oulu, DMC~,,,'- no, nit' O-MO Wo 003/ M Wo OW ATO NMI

42

o

A)

wd
C
112

2A-66-

-ACC% - ft__
-ACC
SOUM COWS UR13MI/65/000/002/0084/0098-

AUMAI lainov. Ir" Ya.

0R03 Institute or_-.~~Uaa (Institut prikl4dwy Stoftelki)

TITLEt Certain thar"teristift, of-' fjoroloxical regime of lover W-ometer
'Layer of the ~61"Jr
atmosphere

RCE: toeningrads Insti ixt,'*Ikladaor~ go' %IU* Trudy's .9650
so no, 2 1 ;v

r -
11110Y atmosreri. (B&Jn
6f i'itJ
Iwo L AN
l
.
TOPIC TAW: microme eoiv2o%r# imete orological twert Aiurnal Upse, rate 4jurw
pressure graditato dlUnii_4"a ti4&ant. atimspherio bomdarl layer, lov le"I
jet stream, atmospheric tuiWenco
AWT PAM' s Results are prosented or a istU47 of U690scals Ishomo sheities -in the lVier
laorer ofthe stmospherej ilkch took into account the diurnal changes in temperature
and v1nd speed and direction during aperiod characterlz*d by a stationary summit"
time, high-pressure art& (atize generaW considered an loast favorable for the de-
velolaent of these Inbomormeities)# 7brot trjpes of Inbcoogeneitles are co id red
1) jet stron-rim in the 1*wee 300-0 Is
Wer,or, the atimusphtre, 2) eddying in both lear
bir,h-pressure vesther cbnditfona and in other weather aLtuaUons , and 3) during-th
P11-.40age of a frontal tone. Ma Uto-'a In the ana3lois vere continuous temperatur*
rtcordlnga %n4 sk-tourments.of the, horlsoutol coaponea-~ of wlW speed and vlnd"_~

C4
d
A(A
1L
d0
LC6
d
&
r
AW, -S51
%M-2t5Q
40
!
5

33M Ty V
'FAR ONE

SOURCEs LeaLulgrad, ldstlt~t`~06UMCW Potisikia TruoWq ooe 2. 1965o POP
610Y atmOdfOrY (2o=d&W-1tW*r.Pf,:th&.*tmosph -122
qrs) nh
70kC TAGOt idaromteoro2olys 0040~40100941 Instruiento wtooroloolcal tower,
measuring set$ --birwo
ABSTRAM A wind-direction Vassurbs set is Used to measure the horizontal and'
.vertical components or the d1reatto 'of the wind-yeloalty vector. 7be set a:
of transducers whose sensift sieneit to
:axpecial "bivsne," a reeorder,~ a dijatal-'-~-
printing devIce,, and & p6vgr.du
~VV4; It to Installed on the high meteorologlcsl~-
of the Institute of Applied Goo-b-y-sics* The bivane consists of a three-&M systok
kmlanved on a column, the belngvet 1200 apart. A ring stabilizer Is mounted
on the end jor me arm, 320 ft f " the syetftla center of rotation. It ves estah-
14.1sherl experimanWly that the flov of air to dloCortl-d by the trnni�du"..r casing to.
dintiinor-- not more than i?00-2% = frvm the tantrig; I-hjjr t1j"! C'tLaM11%tr 5a vithin
~'JLC till(
I-urbcd flw, vhich enevres actmrate track.1ne, or vine dlre,~tionc (Vithl
the lialts.of sjrstem errors).' The instrment and thi`tIyAnt are destrAbed. At
UDC., 551-5064508+508.24508.54510
3 i"

L_~~_2342U"
ACC Nib k6d~%#' -
present* the transducers ire installed an 5 levels of the tower; the threshold sons't.
tivity (both vertical. and, horisdAiQ. of the transducers to about 0.6 a/ste. V'04
initittl mismatch betvton, the b1vtqe:*M the vitiA direction It 10 -or 1800 -the
threshold value .10 hishor m/w. ' The. pr%nctple mewurement error$ a MI
1) error In the horizoatai orCeutttioh of transducers relative to the sire on
vorking lovels~1.5_2.001, isteh of th
(transducer seloryn, 0. $-LOO sid -sensor selsyn 0. 75-1. 50) t 3) error In reaft".P
.from the diagram tape In ~the..rsaordlng sysfes-4. 50 Thus # Pe total error in
measuring wind directions It 'abo", 52r ~ (see ftg. Some variations In Profuse
of the vind direction In thl.106:010 a or thestaosybore as Mom These,mmil
vere constructed for 30-ainintervaltj IVhIeh permitted stable forms or curves that
represent "sets" of Possible lbiiai.of vind-diroction profiles in the liver-(SAID
Table 1). One group of 40cillot-, shows A sMft:to the right vith Mfgbt in Us Vied
throughputUo, Wer-
(I jp) I and to the loft (M-XVIU) in S
number of esses$ the ~wind it", 4ce6stant througbout met of the entire.W."
(IV); Oars Were lsvqred'~C dbinsti4iisof Asht and left, skjIlrin the
Const- 077 re
vith ant directlow tested
.(X, nag% -1461good and
j gaidlng bi
~undsr the supervision no- 11 T(
oftnebuk, Y. 0. Storo&Wmg V, Go'.
Steranoyo 604 04.04.is;i Win ddY.Olopi o wind-are rus"Uro
- - -3 for twordimensional.- wind -
ITS set instaJaed Ob the 11 -f~tpVsr and procedures
"I 7_~
4:0
t Card

23427."
77
-,A#
rh
4 &-p 5~ mljj~ ~ ffig
ah
3
p r
Fig4 114 winil-di'voction meojurllos s e t. twl Use rai~ordlnr, devi"

ACC 14Ri AT6012596
Table I Sam of -thv vajeticas In vind-directlan pro-
jr1lea in tho'la"M-400, a, 1q". of -tho at4wapbere
d
A ll 60
10
A -
40--
1s
W
2

masuremeds b the lower" 30 -'m"' dt 7the airs-vrig, arts bu t fig'urem =a Ittol

DAM' ~Uma ox
001/
SUB CODBf Oh/ em to 14pti., 009/ ow nips
M,
Primes
.

-4
41

4f

Acd

ACC N21 AP7010696 SOURCE CWZI Mt/0050/66/000/008/0023/0028
AUTEO-3: Minov, P, Ya. (Candidate of physico-mathowtical sciences)
ORG; Irwtl~uto of Applied Geophysics (Institut prikladnoy Soofittki)
TITLE: Variability of the height of the upper boundary of & fog
and low clouds
SOURCE4. Notaorolonlya I sidx9loglysp no. $# 19669 23-28
TOPIC TAGSt ;. fot4atmospheric cloW
SM COM 64
ABSTRAM Study of the xaviability of the upper boundary of a fog and
low stratiform clouds Is being cArried out on the high meteorological
mast of the Institute of Applied Geophysics both visually during
ascents to its upper lovals and by evaluation variations with time of
the principal meteorological elements. This paper describes in detail
the analysis of two particular observations$ Illustrating the observe-
t1onal mathodag analyt I cat 'procedures and the results uhich can be
obtained from such observations, The first case Is a thorough analysis
of temperature and wind velocity conditions In the lwjor 300-M layer
of the atmosphere during the developmentg stable state and disappearance
of a radiation fog ott 29 December 1962 at a tivo whan the r4st was
Card 1/ 2 UDC, 5510575+531.576.4
1#9 V it A --,.I AWJV

ACC N4' AP70106 96
on the pariphory of an anticyclone In a stable air moo, The second
case described vas observations of stratiform clouds In the Wier 300-m
layer on 15-16 October 1964 at A number of different heights prior to
the appoaranco of low clouds# during their presence &M vhen thay
reached the upper bouMary of about 300 a with the formation of a fog In
this layoro At this time the sast vas In the varn sector of a cyclones
bohind a warm front, Thareforas the nature of this paper to a =ethodo-
lo.-Ical studyt and the observations described Varrant dravirtS no
onora I ited jonclus tons, OrIge arts,'b"I 2 figuzss# 5 formulas and
tables* LJPRSt 40p2�9
Ccwd 2 /2

WXOV, Ye.A.I. XLIWV, G.I.
CoVosition wid conditions govorning the formAtion of ainaral
wators in Transbalkallao Trudy V3F.GKI IOWC-88 163,
(o',U RA 17 10)

KLIIIOVo 1.
gThe Increasing Production of Substitute Waterials,N Tro from the Russian. e16
(STRWIRMTVIt Vol. 3t go. Ils love 1"3) Probe, Czeehoslov"Ia
SOS Monthly List of East Suropeas Ascessicas, Ubru7 of CoWessi, Vol. 39 No. 4p
April 19546 Unclassified,
';~77 41~~

%"rinental and Theoretical Imesti;ation of Some Matters
In the Prestressing and Mechanical Str*n;thenin, of Steel Peams.
In
r
.ar"
Cand Tech Set, 1*nIn:rad Construction En-.1-neerin; Inst, Lanln~-rad,
19511. (U)-&1ekh, Mat' 55)
195
SO: Sumv No, 6704 29 Sep 35--Survel of Scientific and Technical
Dlesei-tatlons Defended at USSR 1111,-her Mucatiolvial Institutions (15)
... . .........
'4M

SOV/1 37-58-7-15680
Translation from: Referativnyy shurnal, Metallurgiya, 1958, Nr 7. p253(USSR)
AUTHOR: Klinov, I.G.
TITLE: Experimental Investigation of the Effect of Linear Work Harden-
ing of Low-carbon Steel on its Ductility During Subsequent Do-
formation In the Opposite Sense (Eksperimentallnoye Issledo-
vanlye vllyantya lineynogo mckhanicheskogo uprochneniya
malougleroOlstoy mali na yeye piastichnost, pri posieduyu-
shchem deformirovanit v obratnom napravlenii)
PERIODICAL: . Sb. nauchn, tr. Leningr. inzh. -stroit. in-t. 1957, Nr 26,'
pp Z24-238
ABSTRACT: Previously stretched cylindrical specimens (S) 22 mm In.
diameter and having a 320-mm long working section were cut
into short cylindrical S which were then subjected to compreso
Mon; conversely, S 6 mm in diameter Were machined from
previously compressed cylindrical S 30 mm in diam and 75 mm
long for tensile'tests. Also studied was the ductility of steel
on stretching after double hardening (H), namely, first by
stretching and then by compression. It Is shown that It the
preliminary mechanical H and the consequent loading are of
Card 1/2

ILINDYs LO#
Sta'bility srAlrels of the flat beading of rolloid 1-beans beyond
.the sUstle UsH6 Imaha4aklov"oshicoly: Orot. no.2tl49-155
159. (Ulu 1324)
1. Rokovendoy" Imfe4ray otallnykh konstruktoly Laningradskop
lasboneran-strottellaom lustituta.
(41-rders)

ILTIOTO T*G9 # kud,t#kMtftk
Stability.of plmw beading beyond elastic lialts, Sbor. nauch. trud.
1, 159* (HERA Ilt?)
(steel, Structural) (strains and stresses) (Girders]

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