SCIENTIFIC ABSTRACT ROMANOV, N.F. - ROMANOV, N.P.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001445220014-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 20, 2000
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


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NIUROV. Y.N.; ROK"OV.4rP.; SIXIGIN. ?.A.; TSVICTKOV, R.N., reteenzent;
retsenzent; PIANYANNIKOY ARI, redaktor;
MUTIMV. L.Ya.. tekhnicheskiy rediktor
[11snual an equipment of cotton finishing plants] Spravochnik po
oborudovanitu otdolochnykh fabrik '21o T#Vn- -TrT-Uhnoi promyshlen-
nosti. Moskva. Goo. nauchno-tekhn. izd-vo 'IrgIft-erstva legkoi
PrOMYBhl. SSSR. 1956. 467 P. (NLPA 10:3)
1. Moscow. TSentralInyy nauchno-isoledovatel'PTRy institut
khlopchatobumazha0y promyshlonnosti.
(Cotton machinery)

YaELIYANOV, Aleksandr Grigor"yevich; Prinimali uc~mstiye; GRYZLOVAq
retsenzent; VERBITSKAYA,
Z.A.; SHEFTELI, R.M.; ROMANOV4 N.,M
Ye.m.9 red.; VINOGRADOVA, G.A., tekhn. red.
[Direct dyes and their use in the textile industry) Priamys
krasiteli i ikh primenenfe v tekstillnoi promyshlennosti.
Moskva, Rostekhizdat,, 1963, 229,p. (MIRA 16:7)
(Dyes and dyeing)
(Color in the textile industries)

Nov 1947
USSR/Thermal Elec Power System 4501-0102
"Progress of Soviet Thermal Installation," S. F. Koplyev, Candidate
Tech Sci, M. B. Perlin, N. N. Romanov, Engineers, 7 PP
"Elek Stantsii" Vol XVIII., No 11
Discusses progress being made in construction and operation of thermal
stations. Includes comprehensive statistical data and diagrams, and
data on individual named plants.
LC 18G51

L

ACCESSION 119. AT4030523 S/0000/63/000/000/0004/0024
AUTHOR. Surkova, H. V.; Dzhordzhto, V. A.; Dzhurayov, A* D.; Neushkin, As to;
Petro5yanLS, M. A.; Romanov, N. N. i~ Emm, Z. G.
TITLE: Some results of a study of turbulence experienced by TU-104 aircraft along
the Tashkent-Moscow air route
SOORCE: flauchnaya konferentsiya pa avlatsionnoy moteorologii, Aoscow, 196o.
19G3, 4-24
TOPIC TAGS. meteorology, aircraft turbulence, atmospheric turbulence. tropopause.
av;atioR meteorology
ABSTFV%CT: A study of aircraft turbulence along the Tashkent-Moscow air route was
made on the basis of reports from crews of TU-104 aircraft during the years 1959
and 1960. The report is limited to the period autumn and early winter of 1959 and
the spring of 19GO (248 flights, 597, 519,krn). The most Important content of the
paper Is the Inclusion of a scale of Intensity of turbulence for the TU-)04 (8-unit
scale), a morpholojocal classification of turbulence for the TU-104 (10 classes)
and a genetic classification of turbulence for the TU-104 (14 classes. with many
sub-classes). Each of the units of the morphological and genetic classifications
._~re del2jibed fully. It,Is emphasized that the character of turbulence experienced
2-

ACCESS ION XR., AT4030523
is dependent on the type of aircraft; for-example, the engines of the TU-104 art
close together and the engines of the IL-18 are far apart, so that none of the
classifications appropriate for TU-)04 turbuience.are applicable to the IL-)8 or
other aircraft. It is stressed that "lower" turbulence differs sharply from "upper"
turbulence (8-10 km and above). Lower turbulence almost always is the result of
Lhe simultaneous affect of a number of factors and is chaotic; chaotic turbul enc.
i5 relatively rare at tho tipper levels. Upper turbulence is characterized by
patcl6ness. vertical stratification and anisotropy. all of which are discussed.
The acroclimatography along the air route was studied by construction of vertical
profiles (2148) on which werc.pIoLted oil vertical sounding data from stations along
the route and 200 km to either side, navigator's reports on temperature, wind and
spe,.Aal phenomena, and other data. These were supplemented by an appropriate AT.
3GO chart, a tropopause chart and maximum wind chart. It is noted that there are
;ireas with rrore frequent or more intense turbulence (three such regions are listed):
this contradicts Farthing's conclusions (Trans World Airlines, Met. Section,
Kansas City, 1959) that such regions do not exist. The most dangerous synoptic
situations are discussed. Turbulence at the tropopause is rarely strong; turbulence
under the tropopause Is encountered more frequilintly than above it. Turbulence i
conditions in various cloud genera and species are described. Orig. art..has: 3
tables.
Card 2/3

PETROSUN, M.A., red.; KOZIK, R.N.; PSMICHNYY, A,.YA.;_ROkANOV, N.N., red.;
BUGAYAV, V.A., red,; DZHCMHIO, 79A., red,; NAZAROVA,
CHIEWSHOVA. 0.N.; STRAUML. 0,N., red. izd-va.
[Atlas of typical synoptic processes over Central Asia] Atlas
tlpl~hnykh sinaptichookikh protsessov nad Brednel Asiel. 2adikento
1954. 116 mps (in portfolio). (KM n-*7)
1. Akademiya rauk Usbekskoy SSRO Tashkent. Institut matematiki I
makhar,dki.
(Soviet Central Asia-Climatology-Charts, diagrams, ate.)

JV4
AID P 3865
Subject USSR/Meteorology
.Card 1/1 Pub. 71-a - 28/35
Author Romanov, N. N.
Title Review of the article of K. I. Kashin and M. V. Gritsenko
"On changes of pressure at the earth surface
Periodical Met. i.,gidr.,, 6, 59-6o, N/D 1955
Abstract This article appeared in the No. 5, 1954 issue of this
periodical. The reviewer criticizes the article for
,careless and "foggy" deliberations on the movement of,
air and turbulence.
Institution None

95MM W59M
-)F 77 1- 1- T7_
BUGAYEV. V.A.; DZHCRDZIIIO, V.A.; KOZIK, Ye.M.; MWIMIMM111.4 M.A.; PS119HICH-
IIYY, CIORNMD.W. 0.1%; III'VHSAKOV. T.A..
skademik, red.,- GORIKOVOY. P.I., rod.izd-va; FOrNIZOVAYA. Z.P.,
tekhn.red.
[synoptic processos of Central Asia] Si.-wideIMMM"We protsesay
Srednei Azii. Tashkent, Izd-vo Akad. sank OPMT-17-oi SSR. 1957.
477 p. (MMA 11:7),
1. Akademiya nauk UzSSR (for Sar7msa kov)
(Soviet Central Asia--Climate)

AUTHOR: Romai iov, N. N.
TITLE: Pamir Tian Shan.Aerological Expedition (Pamiro-Tyan' -Shanskaya
aerologicheskaya ekspeditsiya)
FMODICAL.- Meteorologiya i Gidrologiya., 1957, No. 2, pp. 26-28 (U.S.S.R.)
ABSTRACT*. The preliminary report describes the scope of the aerological expedition
conducted from end of July to 20th of August 1956 and gilves no data since
the raw field data are still being compiled and ana3yzed. The studies were
in connection with preparations for the IGY and were organized by the
Institute of Mathematics and Mechanics of the Academy of Sciences of the
Uzbek SSR in cooperation with the Tashkent Geophysical Laboratory.
Student-geophysicists of advanced classes of the Central Asiatic State
University as well as teachers and student graduates of the Tashkent
Hydrometeorological Technicum also took par+,.
In contrast to previous field studies, the present expedition dealt with
a wider range of problems., the chief one being the influence of the
mountain chains of Central Asia upon atmospheric c1rculation. In

Card 115

Pamir 'Tian Shan Aerological Expedition
scope of program and uniqueness of problems studied.0 the expedition
was the largest in the history of aerological investigations in this
region. Wind, to and other observations were taken along a section,
the northernmost point of which was Dzhambul,, followed by Iake
Sary-Chelek (in the Chatkall Range) to the south; the latter point
is of interest owing to its-increased storm activity. The section
intersected the Ferghan Valley at Namangan and Osh, and the Alai Valley
at Sary-Tash. Pilot balloons uere sent aloft at these points and in
the great heights of the Eastern Pamirs (at Lake Kara Kull., the
headwaters of the Oksu River., in the region of Kyzyl-Rabot fthe
southernmost point7). In addition, balance and gradient observations
were taken at Kara Kull. Hence the expedition covered a vast region
from foothills to high-mountain regions 4000 m. above sea level,
and the resultant materials will permit the construction of vertical
sections across both main mountain ranges of Central Asia,,
Wind soundings (the chief observations) were taken thrice daily. Radio_
sondes were released only once daily. Serial pilot balloon and near-
ground meteorological observations were taken. During dry haze periods

Pamir Tian Shan Aerological Expedition
in the Pamirs., the usually excellent visibility (over 100 km.) decreases
abruptly., relative humidity drops quickly and convective cloudiness
assumes degenerative forms. All of the scientists who worked in the
mountains agreed on the need for describing and introducing in an atlas
new cloud types typical only of high mountains. V. A., Bugayev (not
referenced by number) had noted an icing of cumulus clouds in fine
weather in the Pamirs; his findings were confirmed. Original transi-
tions of Cu humilis to lenticularis and vice versa were noted. Sunmr
cold intrusions., often passing unnoticed across the plains regions
of Central Asia,, manifested convincing effects in the mountains,
0. V. Demenev of Stalinabad (not referenced by number) and other
Asiatic meteorologists had hypothecated the penetration of currents
from the Indian monsoon all the way to the SE sector of the Pamirs,
but the studies of Ue expedition failed to confirm this theory-, Mre
likely, serious worsenings of weather-in the Pamirs are related with
cold intrusions., cyclogenesis and efl~ctive wave activity at the
fronts of cold intrusions, because frequent SW air currents over
Card 315

Pamir Tian Shan Aerological Expedition
the Famirs and contiguous territory are common to Central Asia and
can not serve as signs of a monsoon. The same position is taken by
the German meteorologist H. Flohn (1). but he does concede the chance.
of rare interferences of cold intrusions with monsoons.
'Interesting observations were taken at Lake Kara Kull; a strong influ-
ence of the lake on circulation and general weather of the entire Kari
Kull Basin was revealed. Outcroppings of fowil ice were found on the.
lake shores.
The expedition contributed a valuable addition to the fund of
knowledge on atmospheric circulation above Central Asia.
The text containsno tables or other graphics. There is one
reference which is German.
Card 4/5

suvI169-59-7-7321
Translation from. Referativnyy zhurnal, Geoflzika, 1959, Nr 7~ p 123 (USSR)
AUTHORS- Bugayev, V.A., Dzhordzhio, V.A., FeTrozyants, M.A-, Roman~,v, N.
T ITLE - Aerosynoptic Conditions of' -the Elarp.-ing of AE-craft Ln Central
j~s_ _ia
PERIODICALg
ABSTRACT-
-ard 1/2
Tr. Sredneaz. n.-i. g1drome-teorol, in-ta, 1958, W 14, 46 p, iii.
Materials of observations are discussed, which were obt-ained by
128 special flights of LI-2- a-nd IL-12-alrcraft along the route
from Tashkent to Alma-Ata, carried out, from MarcL to June .1-956,
Cardinal attention was concentrated on the origin of bumping:
seven types of bumping are singled sut~ I) the.rmalj 2) cold
advection; 3) orographic, 4) frontal; 5 '' bump.!.-:q3 -o7une.sted
with insulated regions of cold air in the medvim tropos&here;
6) in jet streams; 7) dynamical bumpirg, Tl=ee *Ypt55 of'
synoptic situations are a.-:~ert-aln5d, whIch hamper the evolution.
of bumping, a) the, anticy3loris- field having irv;erEl-or- layers.

80',~/IL69-59-7-732 1.
Aerosynoptic Conditions of the Bumping.of Aircrall"t tn Central Asia
b) the warm sectors of cyclons having tropic a--:-., and ~i,- the szlne~- hav-lng
sharply expressed foehns. Twenty-four indications for foreca-s--ing the
bumping are presented, and a series of propositionz- fc,!- its furthe-r study
a-re suggested. Bibl. 19 tities.
Ye.-M. Kozik
Card 2/2

f
BUGKYEV. V.A.-, DZHORDZIIIO, V.A.; PETROSYAIUS, M.A.; ROAAMV, N.N.;
USHAKOVA. T.V.. red.: VOIKOV. N.V.. tekhn.re&.--~
[Aeroornoptic conditions causing the buxping,of airplanes in
Central Asia.] Aerosinop'ticheakto uslovila boltanki satioletoy v
arednei azli. Lenlylgrad, Gidrometeorofhd-vo. 1958. 44p. (Srodneaziat-
skii nauchno-Ionledovatel'skii g1dronoteorologichankit Institut,
Trudy, no.14) (KM 12:6)
(Soviet Central Asia-gateorology in aeronautics)

3(o)
ATJTIIOIC~;
T I T T, I-,
PERIODICAL:
ABSTRACT:
Card I/
SOV/ 0-59-1-17/20
Pshenichnyy, A. YR., 110111EMOV2 tl~ IT- , 5
Lev Aleksandrovich tlolchanov (Ills 60th Birthday) (Lev Alek-
sandrovich I'lolchanov (k 80-letiyu oo dnya rozhdcniya))
1.1eteorologiya i gidrologiya, 1959, Nr 1, pp 66-67 (USSR)
was born in 1878, Ile studied at the Physico-llathe-
matical Faculty of Moscoa University. Already as a student,
'--iolchanov worked at the ornithology of the Crimea, and took
part in many expeditions, including to the Yenisey. In
1911-14 he wrote papers on the geography and climate of Central
Asia. After completing his studies at the University, Molchanov
worked as a temcher at secondary schools and later at.the
Universities of Tambov and Saratov. In 1921-33 lie had the Chair
of Geography at the Sredneaziatskiy universitet (central A .sian
University). Since 1933 he has been Professor of Physics and
Farmin- Tleteorolo- at the Tashkentskiy sel'skokhozyaystvennyy
~y
institut (Tashkent Institute of Agriculture). In.1938 he
xeCe4ved the titles of Doctor of Geo-rauhical Sciences and of
Professor of Physics ani Agrometeorolo.-y. Beside his
peda.-o.-is netivity, Molahanov worked at the Sred-neaziatskiy
nauchno-ilssledova'ellskiy mteteorologicheskiy institut
U

Lev Aleksandrovich ~',-Iolchanov(ifis 90th Birthday) 307/50-59-1-17/20
(central Asian Scientific Research Institute of Meteorology)
where he headed the research riork on the climateof Central
Asia. He wrote a great number of climitological and agro-
meteorological mono graphs. His investigations were important
for the develop,r.,ent of cotton cultivation and other branches
of agriculture. Besides, Itfolchanov kept on occupying himself
with ornithology and huntinL-. fie also took part in public
life, and was for a lone, time President of the Uzbekskiy filial
VsesoyuznoFo geograficheslcogo ob3hchestva (Uzbekian Branch of-
the All Union Society of Geography), a member of the
Administration of the House of Scientists, and of the Hunters'
Federation. Molchanov was awarded the Lenin Order and the
Order of the Red Banner.
Card 2/2

(Weather forecasting) (Xibell, I.A*)
Blow&

S/049/59/000/03/01?/019
AUT11011S: Gubin,11, Dzhordzhio_, V. A., Petrosyants, M. A.
and- Romanov, N. N.
TITLE: Book Review
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geofizicheskaya,
1959t Nr 3, pp 489-492 (USSR)
ABSTRACT: The following book is reviewed: I. A. Kibell "Intro-
duction to the Hydrodynamic Methods of Sho__ e-riod-Weatha~rx-
Forecasting". The book originated as a course of-lectures
given by Professor I. A. Kibell in 1955 to 1956 at the
Moscow State University. According to the reviewers, this
is '.he first -real monograph embodying the whole field of
mpteorclogy at the hig~nest level, never before published
in the USSR.
Card 1/1

ROMANOV, R.N.; CHANYSHIVA, S.G.
Brief characteristics of aerosynoptic conditions during the period of
the expedition to the Golodnaya Steppe in February - March 1957.
Trudy Sred.-Az.nouch.-issl.gidrometeor.inst. no.2:17-25 159.
(Goloduaya Steppe--Winds) (MIRA 131:6)
(Soviet Central Asia--Meteorology)

S/169/62/000/002/044/072
D228/D301
AUTHORS,. Petrosyants, M. A. and Romanov~
TITLE: The prospects of regional,synoptic investigationq
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 2, 1962, 46, ab-
stract 2B335 (Tr.Sredneaz.'n.-i. gidrometeorol.'in.-'~---a.,
no; 4 (19), 1961, 3-9)
TEXT.- It is suggested that the chief problem of regional synop-
tics in the next 2 - 3 years will be the verification of the in.-
structions contained in the guidance documents of central hydro-
meteorologic institutions. Then, the meteorologic study of terri-
torie3 .. airports and air-routes is necessary. Serious attention
sbould be paid to study of the influence of orography on synoptic'
processes and to the development of the principles of synoptic
analysis in mountainous districts. In'the field of long-term foxe-
casting one of the first problems is the clarification of the type-
alternation patterns of synoptic processes and the organizational.
improvement of work on the preparation of long-term forecasts. The
Card 1/2

Card 2/12
- 7" --:1T: . - - ~7 m:~- ~ I- -- , w ~. 4 , . - -
. - 1~ 7 ;

ixassim na: AT4030528 S/0000/63/000/0v-0/0055113071
j,jj,j-a0a: Bugayeva, 1. V.; 43urkava, M. V. ; Dzhordzhio, V. A.; Dzhurayev,' A. D.
I.; Ovcharenko, V. P.; Petrosyants, ',14. A.; Rornanov, IN. N.; Z. G.
A. 171.7, On the upper cloud boundary along Tashkent-2-floscow route according to obs
T
Vations froin TU-104 pascenger aircraft
~'OUPCF.: ',auchnnya konfcrentaiya po aviatsionnoy meteorologii. Moscow, 196G..
Natt2rialy*. IjoBcow, Gidrometcoizdat, 1963, 65-71
70-111C -AAC5: 7U-104 aircraft, cloud boundary, flight condition, tropoaphere, strat-
osphere, jet strewn
10W',TIV%CT: 71iis paper is one of 13 previously unpublished reports of the 40 papc-.-S
given at the ANauchnaya konferentsiya po voprosan, aviatsionnoy meteorologii (Gcica-
c! fic conference on problens of aviation mateorolory) that was held in June and July
of 1960 in ',",oacow at the Glavnoye upravleniye gidrometeorolo&ichcokoy sluzhby* SSSR.
in thir, paper the authorc nrenent some visual weather observations made from aircraft
,and the results of their piocessing. Reports from TU-104 crewo along tho. Tashkent-
11.011cow route,lmade during the period of 16 Sep 58 throurh 31 Doe 59, awl a4rborna
L.10 series of f1i -Ito
obnervations of a group of Tashkent meteorologists, made in g"
CO"I 1 /2

ACCES31011 ITR: AT4030523
(Oct-Dec 59 and Mar-Apr 60) in TU-104 aircraft along the narne route, nerved P..') tlie
raw data. Results of these observations are given in graphs. 248 research flielts
made in the warm half of the year, have nho,.-n a principle difference between the
frontal stratonimbus clouds and the same,clouds in extrafrontal zones, located ia
che central, western. and northwestern regions olf deep se--ted, well developed cycloacs.
This difference is ohown' Frontal stratonimbus clouds have an upper boundary of 2
to 3 times greater then stratonimbun clouds in central, western &nd c3pecially north-
western sections of deep seated, well developed cyclones. In these portions o~` the
cvclones the ascending currents are caused by friction convergence which in any
of the cyclone do not extend high enough and even at levels of .'rom 2 to 4 ka
.alternate. %rith intense decanding movements. Orig. art. haule 2 figures.
ASSOCIATION: none
:SUBI,UTTEDI lgFeb63 DATE AGq: 17Apr64 EXCL: 00
SUB CODE: AS NO REF SOVI 000 MIER: 000
.Corel 2/2

ACCESSION NR: AT40311118 5/2648163/000/010/0067/0087
AUT1101t: Rom4nov, N. N.; HU4Ay6VA, 1. V.
TITLE: Synoptic-statistical characteristics of flight conditions relative to
clouds
SOURCE:. Tashkent. Sredneaziatskiy.nauchno-isoledovatellskiy gidrometeoro;.
1logicheskiy,inatitut. Trudy*, no. 10(25), 1963. Voproay* aviatsionnoy meteoro-
ilogii (Problems in aviation meteorology), 67-87
TOPIC TAGS: meteorology, aviation meteorology, cloud, troposphere, aircraft
turbulence, atmospheric physics
ABSTRACT: An analysis has been made of-8,0.00 reports submitted by aircraft crews
concerning flight conditions relative to clouds. It has been determined that the
use of data from only ~igh_level aircraft is inadequate for such a study; reports
from all levels of the tropo phere are required. The massiveness of available
data forced the author to base the study on data available at Vnukovf,,aero-
meteorological information applying primarily to the central regions of the
European SSSR for Januar~-May and August-October 1959. Findings have been
summarized in 14,tablea: I Forms of pressure fields and fronts encountered;
2-3 Flight conditions relative to clouds in different Synoptic situations;
Card

I-ACCESSION-NR: -AT4031-118
4 - Flight conditions relative to clouds in troughs; 5 - Flight conditions,r,ela-,
tive to clouds in ridges; 6 -* Flight conditions rela.tive to clouds in the planetary
to cldluds during warm and
high-level frontal zone; 7 - Flight conditiqns relative
cold advection and divergence-convergence (at the 300-mb level); 8 - Flight con-
ditions relative to clouds in high-level troughs; 9 - Flight conditions relative
to clouds in high-level ridges; 10 - Reports on flight conditions relative 6o
clouds in cyclones and anticyclones; 11 - Flight conditions in well-developed
cyclones; 12 - Flight conditions at levels of B-12 km (relative to clouds) and
surface pressure (in mb) at centers of cyclomes and anticyclones, reduced to sea
level; 13 - Flight conditions during various pressure trends in flight area;.
14 - Flight conditions associated with precipitation in flight area. Aspecial
rsection.of the report deals with a method for mapping the topography of the upper
0
cloud boundary for typical lynoptic situations; Fig. I of the Enclosure is an
example of the mapping of sdch situations. The vast amount of data available from
aircraft flights can be highly useful in making aeroclimatic generalizations; tho,
approximate character of mubh of this information is compensated by its bulk.,
Such data are scattered widely throughout the country'at various meteorological
establishments; there should be a central office for collection and automatic
processing of this information. Orig. art. has: 1 figure and 14 tables.

- -- -
I

~T
ACC NR- AT6018240 SOURCE CODE: UR/3021/6______
4/006/259/0076/0087';
AUTHORS: Medvedevat I. F.; Petrosyante, M. A.; Romanoyj,N. No
ORG: none-~,