SCIENTIFIC ABSTRACT BERLOVSKIY, V. M. - BERLYAND, M. Y.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000205010008-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 8, 2000
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB


BERUNSKIYp VX, insh.; SHPILIEMp G.1.0 inah,
Electric speed limiters for mine hoisting machinery.
Ugollprome
no.l16l-65 Ja-F 162. (MM 15:8)
1, KharIkovskiy slaktromekhanicheakiy savod.
(Hoisting machinery) (Electric controllers)

BERLOVSKIY, V.M.
Rack-type PGKh6OlO and PGKh6Ol4 stations for
regulationiof
asyncbronous electric motors. Energ. I elektrotekh. prom.
no.l-.61-63 Ja-Mr 163. (KM 16:5)
1. Khartkovskiy elaktromkhanichookiy savod.
(Electric motors, Induction--Starting devices)

BERLOVSKlY, VA; MPOLISMV B.1h.
-1 Automated electric driving sets for mine hoisting
machines.
Gor. zhur. no.5t4g lRy 164. (MIM l7r6)
1. Xharlkovskiy elektromakhanicheakiy zavod (for
Berloveldy).
2. Goeudaretyennyy proyektno-konstruktorskiy institut
avtomatizataii
rabot v ugollnoy proaqahlennosti (for Bogopolls)dy).

BFRMVSKIY V M in,,!h.,- SJITTTA$ Ye.P.,, inzh.;
TRFTIYAKOVA, I.V., inzh.,-
MINEVICHY AGBOP Inzh.
powei~ tran'amiaslon fn-" xr-Ina
hoisting systems. Faf-ktrotekhnike 36 noaW9-32- Je 16.5.
(YJRA 18c7)

MELIKUMOVt Lev Georgiyevich; BOGOPOLISKIY, Beko
Khaimovich;
BERLOVSKIY, Vacheolltv Mkh&ZjQj "c KOVALEV, Yuriy
Sergeyevi-di-ITMI ",uriy vladimirovich; NAY140,
Artitr
Yefimovich; FELIDMAN, Yelizar Samoylovich; SHUVAYEV,
Anatoliy Andreyevich (deceased); KORENDYAYEV, G.V..,
otv.
red.; EELOV, V.S., red. izd-v~; LCKILINA, L.N., to"
red.; IL'INSKAYA, G.M., tekbn. red-
[Automatic control of mine compressor stations)
Avtomati-
zataiia shakhtnykh kompressornykh stantaii. Moskva,
Gosgor-
tekhizdat, 1963. 151 p. (MIRA 16:8)
(Autopatic control) (Air compressors)

BERLOVSKIY, V.M.; BbGOPOLISKIY, B.Kh*; FELIDMAN, Ye*S.
Maximum spedds in starting and sloving multirope hoists,
Gore zhuro
no.3:43-45 Mr '63. (MIRA 16:4)
1. Kharikovskly elektromekhnnicheskiy zavod (for
Berlovskiy). 2.
Gosudarstvannyy proyektno-konstruktorskiy institut
avtomatizatsii
rabot v ugolfnoy promyshlennosti (for Bogopol'skiy',
Felldman).

BERLOVSKIYO V.M., inzh.
^-Z-5
Statious'series PGKh500CT for controlling electric motors
with short
circuited reters.in tropical i0w2ditions. Gar. zhur.
no.8:1,8 Ag 163.
(MIRA 16:9)
1. Kharikovskiy alaktrwakhanichaskiy zaved.
(Mining machinery--Electric driving)

13--,!-LOV5KIY,.V.M.., inzli.; MUNWINIT31:1Y.9 inzh.
Usin., induction transducers in the electric driving -'
-raftie
hoisting machinery. Gor. zhur. r-o.7-50-53 Jl 164. (faRA
17:10)
1. Khartkavskiy elaktromekhanicheskiy zavod.

-BERLOVSKIL-MA*_Aj~~h-
Standard remote control units made by the Kharkov
Electric
Machinery Plant. Gor.zhur. no.10:5c~-60 0 1640
(MIRA 18:1)
1. Khartkovskiy elektromakhanicheskiy zavod.

inzh.
BERLOVSY
Standard unit equlpmnt mamifactured by the Kharkov
electromechanical
plant. Gor. zhur. no.4s54-56 Ap 165. (MIRA 18:5)
1. Khartkovskiy elektromeklianicheskly zavod.

-~BERLOVSKIY,-Y,.M., :Lnzh.; BORZYAK, Yu.G., inth.;
SIITEPA, Ye.P., inzh.;
MINEVT . A*B., inzhe
Automated electric drivb*:of min hoisting machines vith a
revolving stator. Gor.,xhtr. no. 12-49-52 D 165,
(MIRA 18:22)
1. Fbarlkorskly elektromakhanicheakiy zavod.

liOLAND
BERLOWICZ Aleks~d ~ and SZOSTEK, Mieczyslaw.
Department of
raffoTo~ftia~ilomy (Zaklad Anatomii Patologicznej)
(Acting
directors Docent, Dr, R. STANCZYKOWA) and the first
Surgical
Clinic (I Klinika. Chirurgicana) (Directort Docent,
Dr. Jan
NIBLUBOWICZ), both of the AN (Akadenia Medycana,
Medical
Academy] in Warsaw
"Liver rupture at the Site of the Gallbladder Cancer
Meta-
ataxia. Case Raport.00
Warsaw, Polski Tygodnik Lekarski, Vol 18, No 21, 20
May 63,
pp 736-757
Abstracts [Authors' English summary] Authors report a
came
of tum*7 of the gall bladder where blooding from the
digest-
ive tract (sedex cruente) wax observed. Death was due
to the
severe internal hemorrhage caused by the liver rupture
" the
site of the tumor metastaxis, Autopsy confirmed this
dia-
gnosis. IUere are 12 references, of which one is
Polish and
the others Western,
1VIL
L-A- - -1
-------------------------------------------------------
-- we ......... 00.0

BERLOWICZ, Aleksandra; SZOSTEK,, Mieczyslaw
Rapture of the liver at the site of the metastasis of
cholecystic canaer. Pol. tyg. lek. 18 no.21:756-757
20-My 163.
1. Z Zakladu Anatonii Patologicznej AM w Warazavis;
p.o.
kierownika: doe. dr R, Stanczykowa I a I Kliniki
Chirurgicznej
AM w Warazavie; kisrownik: doe. dr Jan Nislubowicz.
(LIVER NEOPLASMS) (LIVER DISEASES)
(GALIBLADDER NEOPLASMS) (NEOPLASM METASTASIS)

OLES, Andrzej; KURZWA, Kazimiers; BALIOMI, Jozef
Glinical and serological ourvvy.of convalescente
following fever.
Przegl. epidem.~ Wares. 12 no,2*.171-176 1958.
1. Z Wojewodzklej Stacjm San.-Bpidemiologiezuej w
Rzeszowie Wrektor:
dr Z. Hazursk.
(q YWM,
convalescence, clin. A enrol, aspects (Pol))

YE DU-GHZHEN [Yeh Tu-chen;]; CHM BAO-CHZHEN' [CIm Pao-chen];
VZUM=-,-RJ,jtranslator1; GIRS, A.A... red.; PROTOPOPOV,
V.S., red.; SOLOMCHIK, A.A.,, tekhn. red.
(Some important problems in the general circulation of the
atmosphere]Nekotorys vazhnsishie voprosy obshchei tsirku-
liatsii atmosfery. Pod red. A.A.Girsa. Leni ad, Gidro-
meteor. izd-vo,, 1961. 239 p. rfrIRA 150)
(Atmosphere)

BERMAN S.S.,
Now varieties of cultivated plants are
developed] Kak
sozdaiutsia sorta kullturrqkh rastenii. Moskvap
Goo,
izd-vo sellkhoz. lit-r7 1960. 62 p. (KMA 15W.
(Plant breedingi (Plants, Cultivated)
11

BERLYAND, A.S.
Berlyaridj A.S. and Gordinp G.A. "On a method of determining the
speed of blood circulation",
VracE'eT. deTo-, 1949, No. 1, paragraphs 33-36
SO: U-300, 11 March 53, (Letopis IrWkh Statey, No..9, 1949)

13 ,-. -,-L , - - ~ : ~,--!
Ii" ~,
22011 Btr Ard, A. S. I" patologii nadcochrchnflEov. Vrachrb celo,
lc~c - I ,y .1
-L. -*, ) "o. ( , ": tad ull -4,
SO: D~toplsl Zl,.urnvllnyl,:I-. Statey, No. 2-~., Voslva,

BERLYAND, A. S.
35465. 0 roli nadpochechnikov v patogeneze
gipertonicheskoy bolezni.
Vracheb. delo, 1949, No. 11, Ab. 981-84.
Letopis' Zhurnal nykh Statey, Vol. 4~1, l,"oskva,
1949

XMYAND* A.S.
Association of pulmonary and genitourin ary tuberculost
according to
autopsy date. ftob]L. tuberk., Nookwa No.6:30-37 Nov-Da:
51. (CLNL 21:4)
1. Candidate Modical Sciences. 2. Of Noscow Nanicipal
tuberculosis
. Institute (Dirac tsr--J~Pof . V.L. lynis), -

BERLYAND. A.S.; VILIKORITSKIY. A.N.
[First aid in accidents and sudden illnesses] Pervaia
pomoshcht Y
nesahastrVkh sluchaiakh i pri vuezaprqkh sabolovaniiakho
Moskva
Medgiz. 1957. 159 P. WU 11:5$
(FIRST AID IN ILLNESS AND I&TURT)
m

BIRLYAND, A.B., kendomedi-nauk
.
Organizing temporary disability examinations in
hospitals. Sov.
zdrav. 16 no.12:21-24 D 157. (MIRA 11:1)
1. Is kafedry organizateii zdravookhranenlya (zav. -
prof. N.A.
Vinogradov) TSeutrallnogo instituta
uaovershenstvovaniya vrachey
(dir. V.P.Lebedeva).
(DISABILITY EVALUATION,
in temporary incapacity in hosp. (RUB))

6YAND, A.B., kand.medonauk (Moskva)
Disability evaluation in the feldsher's work, FeI'd. i
akushe
23 no-9:31-36 S58 (Mm n :10)
(DISABILITY ITILUATION)

BXMYAND, Abram Solomonovich
[Rome care of patients] Ukhod sa bollnym na doma.
Nedgis, 1959. 63 p.
(I= N=NG)
Xoskva,
(KIRA 13:9)

BMU ZIUM; H
JANI4-Abx~w-m-.. Yaov redo; ROMOVAt Z*Aoj.tAkbes
red. .1
(Upertise on the tmporary loso of capacity to work]
Eksperiza vrown.-
noi netrudosposobnosti* Izd'*-2,g ispr. i dop. MosWag Goa.
isd-vo ved.
lit-ry Medgist 1961. 17f p. (MIRA 14:8)
(MSABI= EVALUAMION)

AND A.U.,
DOBROSILI.SM, K.N.; AJZNHW, F.I.; USPSNSKIY, VA.-
=Rl-T
redaktor-, KAIMIM, A-To., takhnicheskir redis
[The work of the station In winter] labota stantaii
zimol-Nookwa,
Goso treappozhel-dore lzd-vo. 1951. 175 p. (KL&A
10:3)
(Fpflroads--Stations)

HEWAAD,A.U., inzhener; BUMOV,M.A., redaktor;
XHITROV,P.A.,
"' INEM118skly redaktor
[Railroad switchmm's mamall Rukurodmtvo
strelochniku. Izd.
2-e. Moskva, Gon.transp. shel-dor. Izd-vo, 1955.
224 p.
(mm 9:2)
1. Russia (1923- U-S-S-R-) Ministerstyo putey
soobahcheuiye.
(Railromb-Svitches)

.ilbaqXi _Clinshg I TSARMW9 A.P., in2h., red.;
MMTAO,,A3L%kg&ndr ah
__V
IMITROT. P.A. 0, tokhn.rods
[Odtahmnis mnuall Rukawodetvo strolochniku. lxd.3. Kookwa.
Vass. isdatel I sko-pollgr. ob%dinanis X-va putei
soobahchaniir..
196o. 254 P. (Railroads-Witchas) (KIRA 13:5)

BMUZMD, A.U. oty, za yypuak; MISHTALI, L.I., red.;
VORMIKOVA,
L.F., tekhn. red.
[Materials on traffic oafety]Sbornik materialov po
bezopasnosti
dvizheniia; vyderzhki iz prikazov i ukazanii
Ministerstva putei
soobshchoniia po, bezopasnosti dvizhenila. Po
sostoianUu na 1
iiulia 1962. g. -Moskva., Transzhelaorizdat, 1962.
194 p.
WRA 15:12)
1. Russia (1923- U.S.S.R.)Upravleniye glavnogo
revizora po,
bezopasnosti dvishenlya. 2. Starshiy pomoshchnik
glavnogo re-
vizora po bezopasnosti dvizhenlya Ministerstva putey
soobshche-
niya (for Berlyand).
(Railroads-Safety measures)

BERLYAN I ! : oh TSARENKOp A,,P.p insh, red.; VASILIYEVAi
N.N,p tekbn.red.
[Handbook 'of the switebman] Rukovodstvo strelochniku.,
Izd,.3*
Moakvaj Tranomholdorisaat, 1962. 258 p. WIRA 15,11)
1. Russia (1923- U.S.S.R~)Mlgisterstvo patey soobahchaniya.
(Railroads-SwitchdO) (Railroads-Siinaling)

WJM,Q,,_AO" otv. za vypuskj KRISHTAL'., L.I., red.;
VOROTNIKOVA, L.F.', tekhn. red.
[Collection of materials on traffic safety; excerpts
from
orders and instructions issued by the Ministry of
Railroad
Transportation on traffic safetyj Sbornik materialov
po
bezopasnosti dvizheniia; vyderzhki iz prikazov i
ukazanii
Ministerstva putei soobshcheniia po bezopasnosti
dvizheniia.
Izd.2. Moskva, Transzholdorizdatj, 1963. 206 p.
(MIRA 17:2)
1. Russia (1923- U.S.S.R.) ljpravleniye glavnogo
revizora po
bezopasnosti dvizhenlya. 2. StELrshiy pomoshchnik
glavnogo re-
vizora po bezopasnosti dvizheniya Ministerstva putey
soobshche-
niya SSSR (for Berlyand).

BERLYAND, Aleksandr Usherovich; BUKANOV, M.A., red.
[Manual for the switcbmaa] Rukovodstvo
strelochniku. zd.4.,
perer. i dop. Moskvav Transportp 1965. 253 Pt
(FIIRA 16:3)

POPKOV, V.I., kand. tekhn.naukp otv. red.; red.
LTechnological instnictions for the manifacture of head-
gear from woven materials] Tekhnologicheskie instraktsii
po izgotovleniiu golovmykh uborov iz tkarWkh materialov.
Moskva,, Gosbytizdat, 1963. 169 p. (MIRA 17:9)
1. TSentrallrW naucbno-issledovatellskiy institut
shveynoy
promyshlennosti.

BERLYAND, K.T.
---------- L~
Bibliographic index of published works completed by the
scientific
workers of the Tashkent Scientific Research Institute of
Vaccines
and Sera for a five year period (1954-1958). Trudy
TashNIIVS
6:281-293 161'* (MIRA 1511l)
(BIBLIOGRAPHY-VACCINES) (BIBLIOGRAPHY-ZERUM)

sov/*44-58-4-2959
Translation from: Referativriyy zhurnal,, Matematikax
1958P
Nr 4o P 76 (USSR)
AUTHOR: Berlyand, Kh. L.
TITLE: A roru-tio-n of Certain Problems of the
Heat-conducting
Equation (Resheniye nekotor7kh zadaoh uravmeniya
teploprovodnosti)
PERIODICAL: Nauk. zap. Kamlyanetal-Podillsik. derzh.
ped. in-t,
1956, Nr 2v PP 15-19
ABSTRACT: A solution in given for certain boundary
problems for
the equation
V. Ya. Skorobogattko
by the method of superimposing the solutions* The value
of
the solution of a boundary problem is giVeIL at the
origin of
coordinates.
Cardl/1

BERLYAW, 14. A., ORLOVA., N. N. and DMZIN, R. S.
"Cor:e,erning the Laboratory Diagnosis of Influenza and
Application of the
Diagnosis in the Practical Laboratory., pp. 15-16 of the
book Me Problem, of
Influenza and kcute Catarrhs of the YRer Respiratory
Tract,'1rs-c-a-w,--U5T-

BERLYAND, Mordukhay Yevseyevich
BERLYAND, Mordukhay Yevseyevich (Main Geophysical Observatony imeni
Voyeykov GUGMS
of the Council of Ministers USSR) - Academic degree of Doctor of
Physico-Yathemat-
ical Sciences, baded on his defense, 13 June 1955, in the Council of
bkningrad Order
of IAnin State U imeni Zhdanov, of his dissertation entitled;
"Forecasting
and Regulation of the Temperature of the Lowest Strata of the
Atmosphere."
for the Academic Degree of Doctor of Sciences
SO: ByUleten' Ministerstva Vys--heeo Obrazovaniva SSSR. List No.
.t
JPRSMY 55h

BEIMAND., YL. Ye.
"Determination'of the Horizontil Corponent of
the'Coefficient of Tur3Uent
Diffusion 11 0
Iz. Ak. ',!auk, SSSR, Sero Geograf. i Geofiz., No.l-', 1944
Central Geophysical Observatory, Red ArP7

L
1-4 zb
;, AA
AID-145
mateorolivied Abst. *Offhand. M. E.. Toorils. 12memenlis veur a
vysotoi. ETheor:, of wind-
T UX.73C Mat! Upr4ilemic GidropyttirorologicheAol
Vlothby. 'A'rudy Nom
tol, No$ 2 . ., :.., . mtki
Uthresuffoil. = 1. Afeleoroligiia, No, 2S. F41ka Prizernnogo S.ola
Atrn6Veiy, V, 14-61
18 fits.. $tables. 33 refs. DLC-Tlie problem o1constructing the And
profile up to 100010=
Feb. 1953 Is ~ Thmrct cni basis is discussed at lengthi
observations at two levels near the groundi -tudied.
Bibliagrapby on ~U,.A .. 0.."
d a valuable comparlson vvith ob3emationit results 19 gi-mu
(relationships beown grodiftitwind
-';Axcbanp and wind velocity at I In h0ght, b-CMven %ind devbtinh
anle ant' temper-tturt gradient 20 Vn
I . 6it4i did j
r lSn em. between height of friction taytr and whid velocity, wind
vofile. etr-) Su Red C
1. Frk on layer 2.1101jhgaty layer 3.jWLkaM=-A.A.
%
L
A
r
A; t,,:

1. BIERLY-hIlD, Y. Ye.
2. ussn (6co)
4. Frost .I
7. Theoretical principles in protecting plants fron, frosts by
smudge curtainso
Trudy GGO no. 12, 1948.
9. Month List of Russian Ac'cessions, Library of Congress,
APRIL 1953, Uncl.

1. B"IRLYAND. M.Ye.; KMASIKOV, P.N.
2. u3sr, (6oo)
4. Frost
7. Studying smudge methods as a means of frost control M.Ye.
Berlyand, P.N.
Krasikov, Trudy GGO no. 12, 1948.
9. Monthl List of Russian Accessions, Library of Congress,
APRIL 1953, Uncl.

6 Z.-Olf r" ROOM M, Rl RE V

V
LAW ovanle offekdroosti w
Meteorological Aboto
DLC
Vol. 4 No. 3 In
Part 2 0(
WhIte a It for the
Marg 1953 deterad
Biblio aL -~- Cm ll~mqt
irrost Fore casting
Ile

SSI.584:551 5201
J~o' Berliand ~1~-
e mm";pIletic by"r "rat the ginilml.1 r"'Rin 1.11, GI
Tmdy, No. 2YIk5);)ll 48, 1951. 3 i,m-..
of valim)i InvOllitk for dt-ImIliaing thcorvOcall., tile (hallgc 0
Aficr a li~tf cdlkal j
-tell I 1wral ur, in t 1), 1 ow" a t " I(hpl' vI ;c I'l Y'i Ilva r I
It "i md, i t i A ~Icl a dLj t hat th t 1114
jlpj'r,ijCh ij tht wic in%~jlying ~ubit;ilu of Ou tNlualikitis of
hl~u conduction g;%-,i
tl~e. illifi.il di'tubuti'm of tulliN.".1tilre bt 111C i'il old m)il
told the fmlm6a"'l
im,th-i ~f 0,~. J!envill r.Akltinli f thv~~. cilmaiwl", mid a
vomNfl~n (if tfiv actis.11 Iltarch
in the lower Illumpherv, with the themeOctilly ealcidatid nwrth lire
%tio~g
2. Tempouilure

Ye-
7, Wy, Nu. 23(85M 7S, 1951. 2 figs, 5aT,7-Trvqwtt1m)%. PLU-1hiii,
theimairal analy~i!:of: 1) the daily zwlruh of thv wiout and 2) tile
detetminalimi'of tile Varia'.
ti- Di willd V,I:.ity ;Ih tinke If the h6ght di~uikmi-' 0 Lhe ix; I
and th, "-'t4-11
W the gradl.ai wimi il k C A tjuation, (.r ki.-lining tlje~ ph-un-
derived. Saf-jm HeQdilw.- 1 2. Diumid wind variations 3. Wint
velocity.-I. L.D.

BERLYAND M
"Determining th~ Earth's Effective Radiation Tak-
ing the Infiuence of Cloudiness Into Account.."
M. Berlyando T. Berlyands Main Geophys*Obs
"Iz AX Neuk SSSR, Ser Geofiz" No 1, pp 64-78
Suggests a theoretical method for computing the ef-
~fective terrestrial radiation under actual con-
ditiops taking into account the influence of cloudi-
ness. Discusses comparison and analysis of somo
known empirical relations. Gives tables and simple
formulas for cloudy and'clear sky. Explains effec
of cloudiness In various climates. Authors thank
K. I. DWyko and Prof M. I. Tudin for advice. Sub-
mitted 3 May 51. 205T45

BERIPTA K. e., dat flulko-matematicheskilch -.1r;
GOLITS . I.A.
n -- sellskakhosynystwaWkh sank; DATITAU,P.F.,
doktor
sell BkokhozyaystvmWkh nank.- ERASIKUF,P.N.,
kandidat fisiko-
matematiebeekilth unuk.
Combating frosts In the U.SeS.R. Ket*or.1 g1drol.
no.2:17-23
7 152. (KIRA 8:9)
1. GUM prI Sovete Kinistraw SBSR, Leningrad.
Owmaya, geo-
fivichesk2ya. observatorly&.
(Front) (crops am cluate)

MSR/~ftteorology '- Meetings Aug 52 1~
bbeting on Problems of Investigation of
Transfor--;
tion of Air, " M. Ye. Berlyand, Ye. M.
Dobryshman
"Meteorol i Gidrol" No 8., pp 49., 50
A, meting on studies of air tran formation
was held
in Leningrad at the GGO (Main Geophys Obs ')
- Rep-
resentatives, of the TsAO(Cen Meteorol iots)
TsIP
(Cen inst of Forecasting), and Tashkent...
Iffe7.,
and Minsk research centers participated in
the
conferences. A number of reports by
representa-
tives of the above-mentioned institations
were
229T108
discussed. At the conclusion Kh. P. Pogazym,
Pres, of the Hydrometeorol Sv, was asked
to'either
evaluate the resul ts of discussions or to
call a
nev conference in 1953.

("olb IVI, -Q.
i:z
BUT-YAWn. M-Ye.
Scattering of long-wave radiation In aerosols and the
selection of
efficient snake . leties for front control, Trudy OW
vo'29r6l-?l
952" (;Ii! 11:1)
(Prost protection)

NUUM. Mae.
Step-by-step defrosting of plants following frost.
72-77 152. (Proot Protootion)
Trudy NO no,29:
(KIM 11111

BIRLYAND. N.Ye.; XOROMUZ, GJ.; XUSIXOT, P.S.
Feasibility of using oil fog for the frost protection of plants.
Trudy 000 no.29.-M-104 152. Nnu liti)
(Trost protection)

- -~ jM411A. Mao.
-wU--7 - ---I
" ` " " - "Re Uwl;'Zz~i;Cko tion of moving air muses.
Trudy GGO no-33:46-56
Trudy GGO no.33:46-36 132. (MIRA 11:1)
(Atmospheric temperature) (Winds)

IMRLTAND, M.Ye.; ZAVARINA, M.V.

Analysis of the heat transformation of moving air
masses.
Trudy GGO no.33:57-70 '52- (MTRA 11:1)
(Atmospheric temperature) (Winds)

~- ft---M~N r- 'M
ZS Tk
ROM's 40;
-, I
-UmM f! Ml

The Comittee on Stalin Prizes (of the Counall of Ministers
tMR) in tne aeldz of
saience and inventIms annouuces that the ftUoving scientific
works, popular ecten-
tific books, and t*xtbooks have been submitted for cuspetition
for Stalin Prizes for
the years J-952 and 1-9~3* (Sovet"s xultur&, moscowt go.
22-40, 20 Fel~i - 3 4r 1954)
4A
Raw
Title of Wart
Fkadnated b-v
E-u6yho, ". 1.
L-~ykhtnaan, D.L.
YuHn, !.'.A.
Rucherov, 11.1.V.
-Beriyard, 'I.Ye.
Krasikov, P.N.
1,nofeyev, !%P.
GLyevaldy, V.L.
Vorontsov, P.A.
fInly"Sica-1 Thaos of tha
icroclLriqte oll A~7ricul-
turnl T.-T1.1cls, I's Forecast-
ing tmd Fegtilationll (snrlcs
of V-rticles)
'!aAn C`L-sorv---,tc)i-r
Y ~
iinr.,ni A.T. V~--yr:yk.cv
SO: W-306041, 7 July 1954

BERLYAND, M. Ye.
"Formatioh of Dew and Evaporation From Soil and Their
Influence Upon
Temperature and Humidity of the Layer of Air Near the
Ground".
Trudy G1. geofiz. obsery", No 28, pp 65-83, 1954.
The problem of evaporation and condensation upon a
horizontal under-
lying surface is refuced to the solution of t-,,m
interrelated systems of
differential equations of heat and moisture exchange, One
of these systems
describes only the change of temperature during the
period of time -
when evaporation or condensation can be disregarded, and
the other system
describes the joint variation of temperature and
humidity. Solution of
the formulated problem for the case of various
characteristics of the re-
gime (various values of the coefficients of heat
conduction, various forms
of functions holding true under the boundary conditions,
various make-up
of the differential equations and boundary conditions)
represents great
difficulty even under conditions of numerical integration.
The author proposes a method for solving problems of this
type, the
method consisting of two stages but permitting one to
avoid the indicated
difficulties. For the problem of the dew the author
assumes that the co-
efficients of exchange diring the period from tqe Initial
mgment of time
up to the moment of onset of the dew point and ur ng the
time
1/2

after the onset of the dew point near the earth are
identical. For the problem of
the evaporation the proposed solution is allowed to take into
account the differences
in the quantities of the exchange coefficients during the
course of both periods.
Analysis of the obtained formulas makes it possible to
determine the amount of dew
through the night, which amount turns out ot be larger the
wind velocity.under
otherwise equal conditions, since here the flow of moisture
toward the earth's
surface in-soils than on moist soils. (RZhGeol, No 7, 1955)
SO: Sum No 884., 9 Apr 1956

BERLYAND. M. Ye.
"Daily Variation of Temperature, Turbulent Exchange and
Radiation Balance".
Tr. GL Geofiz. observ., No 48, pp 26-55, 1954
Forms a periodic solution of a system of equations for
temperature,
moisture and the coefficient of turbulent exchange. Application
of the
hypothesis of "Quasistationariness" of a process in the lower
atmosphere
(30-50 m) makes calculated formulas sufficiently simple.
(RZhMekh, No 8, 1955)
SO: Sum No 812, 6 Feb 1956

BIWAND, X.Te.
now. f or.mat.lon. stud evaporation f rou the @oil and the
effect of
these phenomena on the temperature-and moisture of air
layns
near the ground. Truo GGO no,48:65-83 154. (KMA 10: 7)
(Atmosphere) (Dow)

BERLIA1,U), 11 . Ye.
"Method for Prediction of Radiational Fogs"
Trudy GI. geodiz. observ., iio 48, 1954) 64-92
The method is based on the determination of decrease in
temperature
4T at night and evening , which decrease is necessary for
the attainment
of the dew point. This temperature decrement,8T depends
upon the onditions
for beat balance A and upon the temperature distribution
in soil
along the vertical P in the following way:,4T- AM The
author pre-
sents monograms and tables necessary for computations, and
also an approx-
imate method for the determination of the height of the
fog. Conducted
verification of fog forecasts by this method deteffines
the justifiability
of these forecasts, which is equal to 85%. (RZhGeol, No 9,
1955)
SO: Sum-No 845, 7 Mar 56

SOV/124-58-1-856
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr
1, p 114 (USSR)
AUTHOR: Per' -nd,,- ~.Ye.,.-
TITLE: On the Prediction and Control of the Thermal Regime of
the Surface
Air Layer (0 predskazanii i regu
ii * lirovanii teplovogo rezhima
prizemnogo sloya vozdukha)
PERIODICAL: Tr. Ukr. n. -i. gidrometeorol. in-ta, 1955, Nr 3,
pp 64-72
ABSTRACT: A survey of published works by the author on the
heat and moisture
exchange in the surface air layer. A detailed presentation of
all
these results is available in the author's monograph
"Predskazaniye
i regulirovaniye teplovogo rezhima prizemnogo sloya atmosfery"
(."The Prediction and Control of the Thermal Regime of the
Atmos-
pheric Surface Layer", Gidrometeoizdat, 1950).
Ye. M. Dobryshman
Card 1/1

AID P - 3192
Subject s UL"tearoloff
Card IA Pub. 71-a - 19/23
Authors : _!!!!Iya leflacnm, N. A. and Tanisbevskiy, Tu. D.
Title : Kondratlyev, X. Ya, Luchistays, energiya solutea,
(Radiation
energy of the nun) Gidromateoizdat,, 1954. (Book review)
Periodical : kbt. i. gidr.t 5v 63-4t 3/0 1955
Abstract : The book reviewers give a very favorable criticism of
the mnual.
It in conaidered the first good book on actin try to be 6oiql3md
on the basis of extensive research. However., the book offers
some
contradictory and/or erroneous statements Usted by the reviewers.
Institution : WOMA
Submitted i No date
- -7cmAdw% M - 1191, 2. 6 4UI J1

PRUE I BOOK EXPIOITATION 782
Beryland, Mark Te"e"vich
Predskazaniye i regulirovaniye teplovogo rewhims, prizennogo
sloys, stwosfery
(Forecasting and Control of Thermal 'Conditions in the
Near-suzface Layei
of the Atmosphere) ImLingrad,, Oidrometeoizdat, 1956. 434 P. %000
copies printed.
Resp. Ed.: Yudin, M.N.; Ed,: Maksizova,, I.G,,# Tech, Ed.:
Braynina,, M.I.
PURPOSE: The book is intended for meteorologists, "Icistap
Instructors,
students,, heat technologists,, agricultural ex"rts., and all
those interested
in the forecasting and control of temperature in the near-surface
layer of
the atmosphere.
COVERAGE: The author discusses basic problems-in the heat balance
of the near-.
surface layer of air, and the associated phenomena of
evaporation., condensation..
radiation currents, and the transformation of air masse*. The
intensity of
turbulence, changes in humidity content, the w1n&,end other
meteorological
elements depend to a very great extent on thermal conditions in
the near-
Card 1/9

Forecasting and Control of Thermal Conditions (Cont.) 782
surface layer. Temperature changes in this layer are
basically determined
by the radiation balance of the adjacent surfacep by
turbulent and. convective
exchanges in the atmosphere, evaporation from and beat
exchange in the soil.
An analysis of the effect of these factors on the
temperature of the air
makes it possible to vork out basic principles in
forecasting and controlling
thermal conditions in the near-surface layer on a physical
basis alone.
Emphasis is placed on underlying principles and on
practical instructions in
forecasting and controlling thermal conditions in the
near-surface le,7er of
air. The material is presented.so that the mathematical
discussions may be
omitted by readers not having the necessary background with
no lose in under-
standing the physical processes involved, the conclusions
reached., or the
practical recommendations made. The author expresses his
than 'ks to M.1. Yudin
of the Main Geophysical Observatory., M.I. Badyko, F.F. ~
Davitay, A.S. Dabov and
others for their assistance, and particularly to M.V.
7,avarina for'her studies
on the transformation of air masses, andP.N, Kraoitkov for
his studies on
methods of counteracting the destructive effects of early
frosts on plant life.
In addition Krasikov collaborated vith the author in
vriting Sections 1, 2 and
6 of Chapter X and Sections 1, 7, and 10 of Chapter X1.
Krasikov alone is
responsible for Section 3 of Chapter X1. The book was
Vpvieved and corrected
by K.Ya. Kondratryev, D.L. Laykhtman, Ye.S, Lyapin and P.N.
Tverskaya.
Card 2/9

Forecasting and Control of Thermal Conditions (Cont.) 782
There are 24 tables; 94 Photographs, diagram and graphs;
and 525 references
of vtdch 384 are Soviet, 80 58 German, and 3 French.
TANZ OF C011TE21TS:
Introduction
3
PART'ONER'
PERIODICIff IN THMNAL COND37I OF THE NM-SMirACE
LAMM OF AIR AND FORE)CASTOG WS TEMPERATURE
Cho I* Nonstationary Variations in Air and Soil
Temperatures
1, Basic principles 3-1
2. General solution of the problaw 19
3. Temperature variations in the layer Inwdiately adjacent
to the
surface of the earth 31
4. Quasi-stationax7 conditions in the near-surface layer
of air.
Simplified solution 3T
5. boundary cases 42
Card 3/9

Forecasting and Control of Thermal Conditions (Cont.) T62
6.
Determining the temperature of the air by the
temperature of the

underlying surface
44
7.
Determining the
temperature of soil and soil under snow by the

temperature
of the air
45
Ch, 11. Radiation Balance of the Underlying
Surface and Radiant Heat

Transfer
48
1,
ft-tal solar radiation
48
2.
Formulas for determining the effective radiation of
the under-

lying surface
58
3.
Effective radiation under clear
skies
70
4.
Evaluating the effect of cloudiness on effective
radiation
T5
5,
Radiant heat transfer
8l'
Ch. M. Diurnal Variations in Temperature, Turbulent
Transfers, and
the Radiant Heat Balance
1. Status of the probltz 8T
2, Diurnal variations in the radiation balance 92
3. Buie equations .97
4. Solving theproblem. vithout aecotmting for the effect
of the
time factor on the transfer coefficient 102
card 4/9

Forecasting and Control of Thermal Conditions (Cont.) 782
5. Solving the problem by tsIdn into account diwwa
variations in
the coefficient of transfer 105
6. Certain periodicities in diurnal temperature variations
114
7. Diurnal variations in the COOMCient of transfer 119
Ch- 1V- Advance CalLn'latiOn Of 9110101M N191t Temperature
and the
Forecasting of Early Frosts 122
1. Critical plant temperatures and, danger4m early frosts
122
2e Methods of advance calculation of mInImam temperatures
3.31
3., Method of advance calculation of nocturnal cooling and
the
forecasting of early frosts 135
4. Comparison with exPerimentRI data and verification of
method 147
5. Periodicity in watumal cooling 150
6. An"is of empirical rormia 16o
Ch- V. Dew.. Soil Evaporation., and Their Effect on the
Temperature and
Humidity of the Near-surface lever of Air 171
1. Dew formation 171
2. Problem of evaporation and condensation on the
underlying surface 173
Card 5/�

Pbrecaeting and Contral of 19wrmal Conditions (Contj 782
3. Solution of heat-and-moisture transfer problem in cases of
sharp changes in conditions relative to time 177
4. Amount of dew and its effect on tmVerature and hmidity 189
Ch* VI. Aftmee Caleulation of Radiational Fogs 196
1. Conditions for fog formation and present forecasting methods
196
2, Methods of advance calculation of radiational fop 203
PART TWO. THANSPOMMON OF AxRHASM
Ch. VU, Nonstationary TransformtIon of Moving Air Manses

204
1. ~
Statas of the problim
214
2.
Formation of the problemi
2L*
3.
General
solution of the problem
230
4.
Analysis of the general solution
235
5.
Formulation of basic fbroulas
240
6.
computing schem,
252
7.
Ca0arison, with experiumtal. data
256
8e
Analysis of formulas and
periodicity in transformation
260
9.
Relationship between
tmperature fluctuations and, humidity

during transformation
268
Card 6
/9

Forecasting and Control or Thermal Conditions (Cont.) T82
Ch. VIII, Extreme Cases in the Transformation of Air Masses

272
1,
Basic formulas of thermal transformation in nearly
stationary

air manses
2T2
2.
Effect of tha bdUal dletrlbftift
of tagerature
276
3.
Iffeat of diurnal varlatlon In the
radiation balance
2B0
4,
CompAing scheme and caqparlsoa vith
experimental data
281
5,
Stationary transformation of moving
air masses
284
6,
Extent of afflicability of a
quasi-stationary solution &n&

memo of increasing its
accuracy

Ch, 3X, Noustationary Temperature Chanve in a Moving Strewn
of Air 291
1. Nonstationary changes in temperature in the near-surface
layer
of air in the presence of advective beat 292
2. Variation in vind velocity vith altitude 304
3. Diurnal temperature variation in the presence of
adveative heat 307
PART TEM. COW=L 01F TMUWAL CONDITIONS
IN THE ARAR4%WACR IAM OF AIR
Ch, X. Open-air Heating of Plwte Daring Early Frosts 313
1, Pandamental reqairements for methods of fiditing frosts
313
Card. 7/9

Forecasting and Control of Thermal Conditions (Cont.) 782
2. Methods of open-air varning of trees and plants 318
3w Thermal balance of a heater 327
4* Tenwerature field near the source of heat 329
5., Thermal effect of a system of beaters and standards of
fuel
emsumirtion 336
6. Praetical urrangements for open-air beating 342
ft. XI. Using Smoke Screens to Protect Plants From Early
Frosts 347
1. Smoke production methods and factors in the thermal
effect
of a smoke.screen 347
2. Reducing effective earth radiation 358
3* Vapor condensation on dispersed moke particles 362
4, Buie equations 364
5* Solution of the problem 31-0
6, Analysis of the solution r( 8
7, FaTerimental data and praetical conclusions on the
application
of moke screens 380
Card 8/9

Foreceatize amd Control of Thermal Con&kto= (Cont.) 782
8, D.16persion of long vave mue.,ion in wrosols and the selection
of efTeettive amokes 389
9. Grndml P3=t deilrostimz after early fromAus 400
10, Smal" Methods 407
414
AVAnA=: Library of Con&-esx
HK /am
11-25-58
Card 9/9

C.

o

n

0

I

g

t

i

p

5

6.

aft
j~j
f for; lo- fit
ier
t
ir Ir
AL
Hirt i 1

WK-TAND, Mark Tevasyevich; EMMOTO Pavel Nikoloyevich;
DATITAYA, F.F.,
-- -- InMOTA, L.P. ved.; SXMM, A.N., toklm.red.
0 v. d.; 9
fFrost prediction and control] Predsimsanis samorozkoy
i bor'ba
9 nimi. Izd.2.. dop. leningred, Gidrowtoor.izd-vo.
1960. 146 p.
(NMI 14:3)
(Frost protection)

8/04
IY62/000/008/034/073
3, Jrolo 0 Oil 0222
AUTHOR: Berlyand, M.Ye.
TITLEt On the numerical prediction of temperature and moisture
in the.atmospheric layer in the neighborhood of the earth
PERIODICAM Referativnyy zhuinal, Matematika, flo. 8, 1962, 70,
abstract OB320. ("Materialy Sovesh-chaniya Koordinate.komise.
po chis16 metodam,prognozat'. L., Gidrometeoroizdatq 19611
106-112)
TEM In order to carry out a numerical p rediction of temperature
and moisture in the lower atmospheric layera,-tbe system of.equations
for the turbulent heat and motstiire exchange in thi atmospheric
layer
in the neighborhood of the earth is solved. For the.solution of this
system according to-the difference method, the-convergence and
a~ability conditions do not allow to carry out the calculation with a
great timely step. In order to--avoid this diffioultyg it is proposed
to solve the system according to the straight-line method, where the
timely derivatives are replaced by differences. An essential
difficulty
in the appliostion..of the obtained formulas consists in the fact
that
Card 1/2
40

S/044j62/000/008/034/073
On the numerical prediction .40 CIII/C222
the integrals occurring in these formulas must be calculated
which
contain complicated expressions in the~l"olution of the
preceding step.
In order to overcome this difficulty, the solutions of the
preceding
step are presupposed under neglect of the variations caused
by the heiabL
in the last but one step, which essentially simplifies the
calculation
of the mentioned integrals* With the aid of this artificei it
becomes
possible to enlarge essentially the timely step,
Tibstracterls note s Complete tran.slation.1

BFA?LYAIqD,, Mae.
Determining the coefficient of turbulent exchange by the countow
of
smoke issuing from factory smokebtacks. Meteor,i gidrol.
no.6sl3-20
Je 161. (MIRA M+
(Atmoopheric turbulence) (Smoke)

BMUAND ~..Ye.; OLOMATINA., I.I.
Theory of diurnal humidity and air temperature Variations in
the lower atmospheric layer. Trudy GGO no.123:62~-69 161.
(MIM 1/,:8)
(Humidity)
(Mmoopheric temperature)

BERLYANDV M.Ye.1 GRACHEVA,, V.P.
Forecasting night-tim Unperature, Tariations in the
surface air .1d
Trudy GGO no,127t35-47 I&*, . - -.;TL (,. ,,7rr*
(A,Ueepher~e temperature)

BERLYAND, Me.; GRACIILTA, V.P.; FMYEVA~ O.A.
Local prognosis of fog formation, Trudy GGO no,227:57-68
162o
(MIRA .15:7)
(Weather forecasting) (Fog)

N
1 18374-63 EWT(1)/EDS AFFTCASDAM-3 BB
ACCEEWTION ~R: AP3005875 S/0050/63/000/008/GK-5/0010
V,
AUMOR: Berlyands M, Ye.; Onilmlx R. i.; Genikhovich, Ye, L ;
Lozhkina,
TITLE: Contamination cof tba atmosphere by Industrial vwtes under
anomalous
stratification comuticons
idr0l09iYa,, no. 8
WME: Mateorologlya i 9 1963.- 3-10
TOPIC TAGS: aerosol.. aerosol diffusion., atmospberic inversion.,
atmospheric
contam~tiono --temperat=e--exchange-coafncie-n-t~-----------
T
MUMT: The diffusion of USbt and-heM aerosols has en investigated for
the complex case of an anomalously stratified Md=Mbere\ hbove the
level of the
source and for certain related cases, The inversion layer is
characterizc,_~ 'by
veak vertical axchange; the exchange coefficient k2 decrewes sharply
in ttz
intercepting layer mid increases fartbar aloft; ih zormal
stratification k.
increaseu to the top of the surface layer and remains constant above
it. The
dependence of the exchange coefficient on Might Is complex and mist
be de-
termined numerically. The distribution of the aerosol conceetration
is es-
sentially dependent on the k2 profile. When the inversion layer is
considerably
Card 3
13

L 18374-63
ACMMON NR.- AP3005875
higber than tha source., the influence of the layer at short
distances is nc-t
great., even it k2 vithin the inversion layer is extremely m%sll. If
the Uver
boundary ef the Inversion layer approaches the level of the source,
the Wer-
cepting effect increases wopreclably, but can be detected oiLly at a
consider-
able distance -from the source. The anomalous stratification
associated Vith
an inversion layer aloft does not always lead to a significimt
enhancement
of the surface concentration. If the source is sufficiently high
above the
ground and
the intercepting layer Is sufficiently high above the soutce, a
relatively moll intensification of the surface concentration occurs
withir
a zone of several kilometers from the source. If the source is not
high skove
the ground., ani an inversion layer is directly above it., the
intercepting ef-
feet of the inversion layer vi3-'L be highly significant; at
sufficiently gmat
dista=es from the source the surface concentration nay increase by a
factor
of nore t-h- 2. When the source Is within or above the Inverslon
layer., the
penetrqUon of the aerosol itto tba surface layer is elightj, even at
great
distances from the source, Gravitationta settling =at also be
considered
in a study of the propagation of heavy aerosols, This problem is
solved
numerically. In the absence of an iwmrslon., the surface
concentration near
Cord 2/3

Card 3/3
Z' -~ -=77 , . . . 1-1 - . - .1 -- - .. --1-- -

BERLYAND, M.Ye.; ONIKUL, R.I.; GENIKHOVIGH, Ye.L.; LOZFMNA,
V.P.
Pollution of the atmosphere by industrial refuse under the
anomalous
,~ N. conditions of stratificatiah. MeteorA g1drol. no.80-10
Ag 163.
(min 16,1o)
1. Glaynaya goofisichaskaya observatoriya.

KIRYUKEIN, Boris Viktorovich; MUSIKOVP Pavel
Nikolayevich; BERLYAND#
Mark Yevsayevich, otv. red.; VAYTSW, A.I.j, red-;
~.a., red.,- 1VXOVAj G.V., tekhn. red.
[Rain and snow by the will of mn) Dozhd' i aneg po vole
cheloveka. Leningrad, Gidrometeoizdat, 1963.(MI64 P.
IRA 1723)

IBERLYAND, M.Ye.; GENIKHOVICH,.Ye.L..; LOZHKINA,
V.P.; ONIKUL, R.I.
Numerical solution of the turbulent diffusion
equation and
calculation of atmospheric pollution near industrial
enterprises. Trudy GGO no.138.-3-17 163. (NIRA 17:2)

Trudy,,GGO no.13801-37
163. q.-
(MIn 17:2)
1. a; r

BMILYAW,M.Xsj PANFILOVAt G.A.
Forecasting the time of fog dissipation. Trudy GGO no.138i
73-81 163. (MIRA 17t2)

BWWAND -1L7.q,.;-,DUBOVq A.S.
, :,,-,-- - 0 .
Mikhail Isaakovich Wdin; on his 50th birthday.
Meteor. i
gidrol. no.12%55-56 D 163. (MIRA 17:3)

ACCESSION Zv'R-- AT4004714 6/2922/63/007/000/0078/0088
AUTHOR: Berlyand. M. Ye.
TITLE: Allowance iaradvection while forecasting diurnal
temperature,..and humidity
fluctuations in the bou'ndary layer of the atmosphere
!SOIMCE: Vaes. nauchn.'meteorologich. soveshch. Trudy*, v. 7, Nika
prizemnogo
410ye. Leningrad, 1963, 18-68
PIC TAGS: meteorology, forecasting, atmospheric boundary layerY
temperature
~,~`111~uc'tuation, humidity fluctqation, advection, advection
calculation, -diurnal temperature
Awtuation., diurnal humidity fluctuation, synoptic meteorology
ABSTRACT: Computations of local and advective values of
temperature and humidity
are generally arrived at by an application of the results of the
theory of the non-
stationary transformation of air masses. Even as an approximation,
an allowance for
adv6ction considerably increases the correctness 'of forecasting
fogs, the appearance of
dew and the intensity of nighttime Inversions. The formulas for
computing the inter-
diurnal variations in air temperature and humidity are not
applicable to the computation
of the intra-diurnal fluctuations of T and q with allowance for
advection. The latter are
computed by a combination of the results of local forecasting and
the transformation of
C"d 1/8

ACCESSON NR: AT4004714
moving air masses. 7he author first considers the allowance for
advection while fore-
casting nightly changes in air humidity. 7be basic equation is:
-OL.k,'ft +A, (z>Jk).
with the limiting conditions
where z = 0, dq and z h. Limitation of the solution for infinity
and for initial
-izCL-
conditions impose the constraints t = 0 and q2 = q21. Aq is the
moisture advection; Q is
the initial distribution of the moisture in the layer vo h; X 0 + k
z and k2 are the
variable coefficients in the layers z4 h and z;ph. Aq Is some known
getion. The'
problem can then be solved in terms of two items: one satisfies the
homogeneous equations
(1) where Aq =- 0 and also satisfies the hoterogcneous Initial
condition t = 0 and q2 = q21,
standing for hunildity vuriationx In tho 4bactica of advacklon.
71to accond itf3m, 1 14,
satisfies the heterogeneous equations (1) and the homogeneous
Initial conditions. 71ten qI
Card 2/8

ACCESMON NR: AT4004714
r
is the solution of the equation system for Equation (1) with the
limiting conditions z = 0
and dql = 0 and the Initial conditions t = 0 and q2 = 0. Aq' comes
from Aq = Cq + Aq',
dz
where Cq represents the phonic advectioxi and Aq' the advection
conditioned by humidity
variations under the innuqnce of the underlying surface, whereby it
is assumed that Aq
depends on Q2 = average diurnal variations of the humidity
quantity, 'Cq comes from Cq
*h, e x 'rewthe d Ince of the shifting of the air mass, u the
velocity of shifting
er Is'
d Q the diffe Ce of th; h: Midi values between the initial an4 end
points of the
jectory at 850_700 mb. h Aq~~ U -LQ1 Q2 is derived from the
differential
r
dx
eqpations (2) and the limiting conditions (3)
+ a (2)
Cara 3/6

ACCESMN NR: kN004714
Where a = ZI Q, = jP(M); where z -4100 Q2 --0. 0 (9)
zi in the level of the meteorological box, ip(x) a known function
and Qj the deviWon of
tHe average diurnal humidity value from the.humidity'values at the
points x - 0. 7%eql
and Qlvalues are found by a Laplace transformation. The
transformation of the functions
of Equations (1) and (2), and a change of the equation system of
particular derivatives to
ordinary differential equations, yields the following equation:
(4)
q, lip
p' (A,'+
it applies whenever the development of humidity variations remains
stationary during the
preceding period. Its p and pl are converted according to rules of
operational calcula-
tions. . I'he variations of humidity related to phonic advection
are considered. qj = Aqa
is the humidity due to advection. By converting the obtained
representative functions,
the following equations are derived:
Card 4/8

ACCEMON NR: AT4004714
where
F*wmvl-F" ll'-ff
F-F,+F,'.
kj
Fl, 3
+ 2k (5)
F2 2 v ~s r k,
k2 V SOA
eedcy;
r (y)
IA h , (&~,
AOA
dt'
01 #A -At -21- 1; #A) - -
S VIA #A-&
'd
o
c

ACCESSION NR: AT4004714
The cipected humidity near the ground is A Q. The values of wl
(Dal, Da) are indicated.
A table shows the calculations for P and all its components. x
= 1 diurnal period; t,
ki, kil have different values. An analysis of the table u
indicates that with t,
or rather with the size of W
_X_, F increases because Aq remains constant with time. The
longer the time, the greater the humidity changes -conditioned
by advection. A qa ir. the
IRftdary layer Z.< h is independent of height. The influence
of the turbulence variable
.isvelated to k 1. The greater the k, , the smaller F. When x
and t are very large.
R-,r IT U_
-F2 becomes small and q, is determined by Fl. In practice, F2
Is only 20-30% of F,
When x = I diurnal period and t > 10 hours. For F1 increases
also with the size of the
U
relMonship tu and k' , thus increasing the influence of
advection. The author then
Y fl,
considers the allowance for advection while
forecasting'diurnal fluctuations In air
-temperature. In the computation of the allowance for
advection by the local forecasting
o&,temperature in the boundary layer, th6 author uses an
analogous set of equations:
6/8

AccEssioN NFL: ATiOO4714
d
(We+k,Z) --L-0 (O