SCIENTIFIC ABSTRACT MONICH, V. K. - MONIN, A. S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001135110018-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 13, 2001
• Sequence Number: 18
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

Molilcl$ V. K.
Moventh session of the. Commission on the: Datemination of the Abasluto
Age of Geological Formations* lxr*AX Kazakh,SSR. Set,geol, no.54108
(62, (Geological time) (KIRL l5r12)

RUMUNTSIVI, Tamm L1eksaadmvu&LMQX_~CF1, T.K., doktor f,-eol.-miner.
nauk,, prof., oty. red.1 NXSTZHOvi-,-r-.1., red.r, IEUDYAKOV, k.G.,
tokhm. red.
.pAV4,-and genetic chamateriatiew-af-the
(Geologr, pttrogra
Rmlikha. deposit inthe Rudnyy M 'ail Goologiia, potrogra.Ma I
genstichaskie oapbannostiftalikhinskogomestorustdoniia na rud-
non Lltae. kljmm~-kta,, r-sd-va Akadlbnk Kazakhakei SSR, 1963.
146 p. (MIRL 16:5)
(AIUL Mbuntainfi-Ud1*&)

NUFLYRATEV, Abdrakhmfut Murlybayevich; V.K., doktor eeologu-
miner. nauk, prof., otr. red.; NFZTEWVA, I.I., red..
KRUDTA-KOV, A.G., tekhn. red.
[Granitoids of the Psleozoic intrusive complexes of the
northwestern petrt of the IAke Balkhash region (:etitral
Kazakhstan)] Granito4dy paleozoiskikh lntruzlvn.-Ikh korrplek-
sov Severo-Zapadnogo Pribnlkhashlis (TSentralln-ri
Kazakhstan). Alna-Atot, Izd-ro AN razakh. SSR, L963. 219 p.
WMA 16:11)
(Falkhash Lake region-AGranita)

MONICH, V.K.; MAMMA, T.B.; MMMIL, T.P.; ITANOV, L.I.
Itleventh session of the Comission on the Datergination of the,
Lbsolute Age of Geological r~ormtlons attached to the Dap&rtment
of Geological and Geograp4eal Sciences of the AcadevW or Sciences
of the U.S.S.R. liv. LK SM. Sar.gsol. 28 no.6tl29-133 Je
163. (KIRA 16 c 8)
(Geological time)

Kepheline rocks of the Virgin Territory an a comprehensive
rast material for the Production of alumin= oride, soda
products and caunt, Ye5t. M razakh. SSR 18 ro.4t23-31
AP t62. (MIRA 16:11)

MONIM, V,,K,I. SEMEIIOV'L,, T.P,
I
Geological time, scale of 1963. Izv. JLK Kazakh. ';SR. Ser. geolo nauk no.
5snO-112 163, (MIRL 17t1)
iornatUnt geologichemkikh natdc AN KazSSRt Llm-Ata, i Kazakholdy, ina-
titut minerallnogo syrlya, JUma-Ata.

HOMIGH, V.K.; STAROV, V.I.; V.D.
Compa.rative 5tUdy of patanislim feldepars fr= the intrusiona
or the UgrAnskaya tnd Kara t4s-Cku I I etAdskaya zones, Trady ]net.
geol.naijk AN Razakh.SSR 7:293-300 16-3.
(KIRA 17:9)

lit A. _1~-j I j II-jr.y. [dece_rts(,,dj; POXHFUKO, A.G.
~*".i ;
ae;o data on the geology of the rubasadyr flassIr Gf alkali rocka.
Izv. All FArakh. Ser. geol. 22 rio.1:57-61 J&-F 165.
(MIRA 18:6)
1. Inatitut geologicheskikh rAuk Im. K.1. Satpayeva, g. Alma-Ata.

W--L)POV, G.I. Ideceasedht. Yj~:A~.deceasej)j, f;U' Ll lY, P..T.;
% ".T,-.;- mitit.
bittzillilrSEIVIll I A.F 0 '. Zlill;,,ip A.~.
Intrunian of ToFarsk cr~nplex In Shatskiy District )f crntral
Kazakhatan. Trvdy Innt. geol. nauk AN' razakh. S.".i: 12:43-73
165. rirrf~,. Iv:W,
.., A I I

; v I A - .
STARUO" V.K. [dcrn-a.,~cdj; G"Kh-1, I.I.;
Potasabm feldspar of sone of the different age intri;zicmg.
Trudy Inst. geol. nauk AN Kazakh. 3011.1. 12:108-112 165.
(VILA 11:9)

-1
"t, N t i . , Ke ': -, ! I::. '!I - "i, , . ; -,. I , I , C. . "..
L
;v -~ny r f* & ~.f I' - r !ri c4.tntrr--, part c' I-to
1* . - . - ~ . J 4 1
J. (azakh. 3~-R 12:74-107 '6c.
,j ~.Itx., I. 'A" ru (~ yir'st. gp%. rVil.

t
i " i7 j, ~u, j~~ 11 j c1 ';'k) 1'(V) /%T il~:V
ACC NR# AP0021713 SCURCE CODE: UR/0130/66/000/003/0027/00i7e
Be" vi-sov G. V.
Monid, A. Go,- akovskiy, M. A.; Smolyarenko, D. A
Tkache R7!~Onmj V. 6,j__PWY, P, I.; ftkudin, Pot I~Wrfnsk a, S. A.
Sosipatrov, V. To
A
ORG : now
TITLZ: Production testing of 08'ru cold rolled low carbon steel
SOURCE: Metallurg, no. 3, 1966, 27-28
TOPIC TAGSs lov carbon steel, deoxidation, cold rolling, quality ccatrol 08Yu steel
ABSTRACT: Production testing was carried out on nonaging 08Yu steel shoots at the
Cherepovetsky.06tall Cal Plant hnd the results were compared to the norms set by
901~5-59.Meltin in single-groov*d Martens furnaces of average
eo dat,04was carried out
Capacity y ferromanganese was done in steps--50% in the furnace and 50%
in the Is so introduced in the ladle in quantities of ~10-150 g/T of
steel while full deox!dation was accomplished by the addition of AlVoollets In quanti-
ties of 900-1000 I/T. The chemical composition of 08Yu steel compared favorably with
the standards set by GOST 9045-S9 (experimentally--CcO.04-0.08%, SivO.01%, HnX0.32-
-0.381, S*0.009-0.016%, PsO.01-0.015%, CroO.01-0.03%, HicO.03-0.07%, Cu=0.02-0.07% andf'
Al-0.02-0.05%). Ingots weigIning 14T were hot rolled 15-18.pasres into slabs of
6U.771.24
Ccrd 1/2

ACC NRt AP60,21713
135-1,40 1" thick I and 1070-1.430 mm, width on a 1150 blocio. These *labs, vere; next
cold rolled to ivium of 60% reduction Into sheets of 2.5-a.5 mm thicknosts and 1040~
"-1430 ra width. W-Musaling was done at SSOOC for 10 hre at a heating rate of' 15*/hr
and cooling was, it-60/hr. The final operation was a finishing pass at 1.0-1.3%. reduc-
tion. Tests made on the sheets after- aging at 2000C for, 30 min substpntiated that
the steel was nonagiug. The shosts, performed well in stamping tentsvkhich were run un-
der the stamping conditions used at the Gor1ky Automotive Plant. Uri&. art. has: I
Sus COECt 11114/ SUBK DATEx none
Card 2/2

cp

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POLAND/Mecdeml, Tectmoloor. CheritcaL Vroducts and Their r-9
Applicati,:m GUlicate-1. Glva. CirarAcs. Binders.
Abs Jour : Referat Zhur nmimiym, No 1#, 1957, 12681
Author : Monikovski Edvard
Ti tl-2 Kk-,erlence with Conclusions Derived frcm Acceleratcd
Aging of Concrete at tlc Building Site
Orig Pub DosviaticzerLia I vniocki z przyspleszonego 4ojrz.--dmnim
betonov n% placu budowy. 1.,Lsovn. prz~.,~s!-, 19c"6, 5,
No 7-8, 29-33 (Pollsh)
Abstract For the purpose of spe-,ding up, building opurations it !s
recomwuded to produce thtg structural coppoamt parta di-
rectly at the ttdMInG cite on comdition of careff%a se-
lection of caterlalzj, &Idition of CaC12 (in vinter) aad
heat treat-,wnts at tviporatures up to 750.
card 1/1 - 129 -

- - J~ 11: - ,- 7
~r ' 'I -
-~ v -00 - i, A- .
"
Conclurions and guncralizations conccrninf: tI.e construction of a cixt'am in K.-I-saw.
it. 1. F.13.
(3uLce.,,,i~urt~o izuii-Imera. Vol. 6, No. (1, J,Ime 1~57- 'e~ixszzawa, I o'=d)
.""*~: 11-'onthly Ust of East European Accesstons (EE-U) if% Vol, 6. No. 10, Cctubcr 1957. Uncl.

THCH.W10a
MIODIGAW BUDOMOTWO PRZk3ff-SUKE. Vol. T# no. 6, Auc. 1956
wwIXONSKI, 9. Uperionce acquirod in constructing warthousear anc.' fn&ztrial
multismti.mal buildings from prefabricated parts, p, 1,
Vonth4 List of East European Accessions (EW) LC,, Vol Ot no. 4.
April 1959r, Unclass

'71 14 T ~~~ s -
MI0,)ICALr f3fjw(l;ICIWO P121tyraUNE. Vol, Tr no. 9s, Sept. 195.9
MIKOrXII, E. Experie-ce acq-,saired ir constructing warehouses suid ine--,istrial
miltief-ational buildings from prerabricat-~I pa.rtn. Pt. 2j, P. 45.
Yonth4 Ust of Fast airopear Accessions (MU) LC Vol. 8, ro.h.
April 1959, Unclass

HCIBIXWXIt Mrard, up ins. (WanswoL)
Ttalring cowse. of the Iraraw &=ch of' tb* Association of
PblJjh Bmildinit kqineen and Teobnicism at thel Adxlni~
str&tion of rndustrial &dlding of the city of Warsaw.,
Prsogl budovl i bad:aioomk 33: no,6064-365 A161.

MUCUSKI, .EdweLrd (Wars saw%.)
Roor or a workshop ha.U In tht, fo= of & double-ur"d
. . . hanging shell. Przagi budovi I. bud mieozk 23 noogt481-
4"~ W624,

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Me Pwdvbd~tq, wwtb-t, 1. t. NOW-m.

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Rhiw, I MO, AWr~ Uri U-441-
li" -) m -
It AA A" f, that I - rz-&Cts "A. v 'k a
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L . Liz

Tyroglyptddael, insects noxious to'foods and their exertrination, P WSW (PRZEMTSL RCLMY
.1 SMZr*Mr Witratawap Vol. 6,, now 12P Dec. 1954.)
SOt 14onthlr List of East European Accessionss (EEAL), LOCO Vol* h. no* Xq Jan. 1955,

!t)Li.'cTD/Ch(-~iAc-U Tc~hnulogy. Ch,,~;-Acal ;rcNcts ai-,- If
Th(jir U5,~a,.m P-irt ill. Fov~l lmlustry.
Aba Jour t nof Zhur-Rhintyat, Nu 15, 1958f 51944
ta thor t 'giockowakit Elzbietq Ktu"vtrz
List 1 0, -
Tltli~ i Phosphataso Tost for N'ant ane 1(crat Proemats.
0 r it,; V u bi Room, 'I'matu zakl.. hig., 19561 71 Ito 11,
79-88
1.batrnet t Applictttiun of th., alkalina phmphat'-so
(1) titration as na i0icator )f dagree
(sufficion6y) o,' tharval tr~!zatlunt of
noat an,' zmc:at proeucts has boca explaince.,
It was catablisho-O. tli-It no I w ' "Caent
;;, 17"a f-
in tioat product.,; hoatad tc , . 00 positivo
roaction for I ccuV be inc-uecd by b--ctoria),
Or,.rd g 1/2
1w

HT LtZij Uldr ze j I. MOMOWSKI Kazimiera
Hydrolytla decompositioa or phytin. compourAs during the production
of bakery goods. 1. Acta pol. ph&=. 28 no.5r441-444 161.
1. Z ZaklAdu flauki o Srodkach #pozyw*Voh. Akidemii Kodyezn4j v
'Lodzi Kierovnik Zakladut prof. dr K.46uikovaici.
(INOSITOL chem) (BIUAD cha n)

KCNIKM$Kr. K.1 pMAM,,W.; BODZLK, H.
Katination of stathyL bromide residues in rood% treated with this
prepamtion* Cook* hyge 10 no*3tl98405 W, li5e
lo BromatologickT ustar Eek&rske akadomie, v- LAzi a Tysku=te
usta,v7 pro potirani obilnich akudau v Lodmi. 2. X.Monikovskile
addrozat Wz, u1. Kilinskiego 93,

--VZ*FR1t-ZFfEFVSM'- D.Ft-L~;-MNINj7-A.-I~o -
OTypical Schematics of the General Circulation o." the Atmosphere In the
Northern Hemisphere and the Circulation Index," rzvestiy& ldmdemit Uuk SSSF, Serlym
Georiz t cites Mya, fro 6, 1954, PP 562-574.
Tnst. of Geography Lod GeophysicaLl. Inst., AS USSR
Translation K-602# 5 JUL 55

14 N-11 NA ard -I~ H. fK7F--I-VC!
llcnsoma-
Vertical atructure of Monsoons. Net. i. gidrol. no. 6, 1947 (PP - Z? - 30
%I-mnalAtlon of contents available in U-1711~ I Apr 51
M L

00n tha, Theory or Atzospheric Turbul-,nce.ff 'I'lcats
for defTec oll' Cand. Pirryalemathe-rutticil -jet. Sub
11 Yay 49. Moscow Order of tomin Zt-lite U inent
K.; T. Imonosay.
Su=w7 82, 18 Dec 02, Dispertati= E=--Mtad
for, RICTOCII JU agic2ca and EuAn&-_rinr in Zasr-u
La JW From Vacb2rnvaTftEgQ_qT,-m, Jan-Dec 1949.

'FIX i 111 Nkf!
"C'
-tationar,-,- Pattern of tM Distribution of Wincl According to Altitude in the
rnstance of Curvilinear isobars," Meteorology i. Gidrologiyap No. 1, 194.7
Tranal&tiar4i available in U-2392, 22 Sept 522
"A Stationary Model of Wind, Distribution with Respect to Height for thL- Case of
Curvi.lene&r roobars," rt. AN S3SR, Ser. Geograf. i Geeftz., Ycl. 13, ro. 3, PP.
2-,x)-238, 194-3

I i F~j~
- -T, IN, A. -
IT.
NA Stationary Model of Wlxd Distribution with Rerpect to Hei7,1-,t for the 'ase of Cur-
vilinear Isobars"# Is A Nauk S=, Ser Geogr&f 1 Geofizs Tol. 13, 114. 3, pp 22a-238,, I

.... ....
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-1, - a -I L: - t
- u..-i if! ., :3. arA d -1 p L. k
; Zxperimmital D&tO#, lzditelletvo Itiostr Literatur7,
"Hathods of Aralrzin; amcT
~-64, pp, 1990.

~,s m

'i lo

OWNS-
Set SSL
sloji mbdom v poressown &1#4 "Malrbs.. [TwW--ac rtrfmr fix 11-
?Win&
Wteorol4gical Abst. rrDUrALI V-T.S.X 0~00' UP-e4f*4
I 31-1f, 1951. 1 f-0. it ttis, U rqa, DLC-A, (,w*"atatftf t~vii.
vol. 4 No. 2 Me PPMI tht4wT E" InIblak-twt, r-s It w3v &TrIV4~1 (w OnNoved bv kuslkln 6 i"AIA4.
fe- --w !mMj4"'.d "Aut%m art Siven I~ M4 hy" twat tho gnuwl. 14~~ "j%att~.%
Fc-b. 1953 *tb" wirnti.t. %tr 46,wa &A "nsto
bibliography,on Iadi...d- . 11'1~fr Who
'IM6 40 194S fA% (M. tlqk 0,10 ffitifl~A ml M# ut~ km,-to lv-m P4tt,, 11,1',~ i,
Turbulent Exchange CGmvwrk*4 AN& k1111,4.1-81 1. Tortvioact obow y 2. (w%uj #see, Lflalfh~,
U. 1. 11, nbvbhov, A, M, -- 4 A

,- r
-i, Li., F. .J. .
"The variation of pressire in the Barotropic at lasrhore." News of the kade-qy- of Science
of the V3Mr 1952 Geophysical Seri--a.
SO: S=m&ry-0-69903r 29 July 1954.

'IWR/Geophysics - Pressure Variation, Jul/AuS 52
Atmospheric
"*T*ssure Variations in a Barotropic Atmosphere,"
1L.3. MonLa, Inst. Acad Sci USSR
"%t Ak Wauk SSSR, Ser Geof iz" No 4. vp '76-bl-
Studied the stracture of the velocity field in a
Volytropic atm. Determines the vertical component of
the velocity. Az a result of analy-zing the cor.-
wetion betveen, velocity f leld and pressure f ield,
22aT53
the author explains the mcbsnisz governing pressure
variations. Acknowledges helpful ady-ice of A.X.
Obvkhor, who initiated this vork. Submitted 11 Feb 52.

A. S., 0 pw&Wkd"tkb razvW mwkmt WOOPM. tpwwwth" of ae
I &S, UWArwil 1032. 12 rds. MC-The cooprometay nuturt a(
61 Absto
mod thwcjul mejhMi 4 a"t toki ImcWIN are strumd. - 'Ibi rnrarkal a
VOL 4 No, 6 r"rtmnftd ti "Mv~~ clyriamic malpis" (A DA). &WopM In ths uViet U140"
Jurm he
a rvd TAR,., 0) -
spectral density of the te=perature field, criT - spectral
donsity or u i and T . The spes-Wral analysis can be per-
formed experizeatally by mearis of a device (e.g. theraoaae-
mometer) which could express the meteorological data as the
fluctuations of the elect.-ic current, The fro-auency Ak
could be obtained and thus the expressions (59) and (60)
evaluated. The spectral funcill-ious could be calculated from
Sqs.(62). Some results of ttie latter formulae for the low,
medium and high winds arer shown in the table on P 311, where
w - energy of vertical fluctuatioaf q - heat flow,
T friction. The method of apectral analysis can be em-
ployed for the determination of the dispersion, the 2ad
momsat (i.e. spectral function) anti the various other
characteristics suchL as anizotropy of spectral components
Card 8/10

The Structu~re of Turbulence in tLe ktmosphere-
and
du") au (4X)
-~OV/52-5-3-3/13,
or the vertical turbulent flow of the energy q i.e. the
calculation of the 3rd moment of spectral component of the
velocity (Eq.63). The problem of stmsture of the &tzoa-
pheric turbulen--e cannot be solved without considering other
factors such as pressure, turbulent acceleration and cliffu-
sion or the waving flustuations.. The str-acture of the press-
ure field can be expresaed by the formula w4ile the
turbulent acceleration can be found from the formula (65),
The turbulent diffusion can be expressed as the coefficient
A/3(ReP.54) or frou the formula (66) (Refs.56, 59), where
k C
the intensity G of c-incentration ic I'lakea into &,::count.
This concentration car. be defized as the function (67) (Ref.
60). Changes in the ataosp!iere due to turbulence, CGLuae
fluctuations of the amplitude of the acousti7. or electrc-
Card 9/10

The Structure of Turbulence in the Ltmosphere
magnetic waves. The propagation of waves ta these cjrvxutxres
can be calculated froa the. tvxpressions (68) or (69) and (70).
Tha last forraula allows tlie finding of the atatistical
charaateristias O(r) when the characteriatieG q(r) are
known. Then the funztioa of tte refraction coefficient can
be found froa gqs.(71) anI (70~ ThLe correlation between, the
refraction coefficient and the fluctuation of temperature or
humidity can, be calculated similarly (Ref.63). There are 9
figures, I table and 83 references, of which &5 are Soviet.
SUBMITTED: March 28, 1958.
Card 10/10

AUTHOR: Monin, A.. a.
T.1TLE-.---fie Chan-,e of Pressure
darleaiya v baroklinnoy
49-58-4-7/18
in a Baroclinle Atmosphere (Izmeneniya
atmosfere)
PLRIODICAL: lzvestiya kkademit Nauk SSSR, Seriya, Goof izichaskaya,
11,15a3, 1[r 4, pp 497-514 (U.SSR)
L3,37RA"IT: Electronic computers have made it possible to integrate
them h,-drody-namic and thermodyn&mic equations numerically- to
obtain. values for the pressure, temperature and wind.. Attempts
have been made in many countries to simplify the dynamical
equations of the at!aosphere by, the quasigeostrGphia approxi-
nzatLori. TLLis uses the. fact that the pressure gradient and
the Goriolis force almost balance so, that the relative
acceleration of tha air particles is small compared with the
~ortolis acceleration. In. tlits caso~ the win(i is close to,
I
the geostrophic. Vie author reviews the, main progresa in the
theor:r of pressure changes., I... L. Melt put forward the
,Idea of a quasi-geostro-,,-'hic approximation in, 1940. In 194g,
A E., Obuxhov gave a much fuller account connecting the,
1-)rearjure fteld. and them wind field', Obukhov, showet, irt the
stinplest carae of a barotr-,)j,ic atmoophere, that, at the break-

1-e Change of Pressure in a Baroalinic Ltmosphere.
down of geGstrophic conditions, high-velocity, waves are gen-
erated. La a result, the pressure field adapts itnelf to
the velocity,field,, The transfer of velocity vortices seems
to br-- a basic fa,-.tor inthe change of velocity and presqure
with time. The basic resulta for the geostrophic approxima-
tion in a b&roclinic atmosohare were obtained in the USSR
by Obukhov and also, independently by N I. Buleyev and
G, I. Marchuk, They were also derived i~ other countr~.es.
The aUtlLor now gives, the baroclinic work in- detail, start-
ingr with the dynamical equations of the atnospbere in. the
quasi.9tatic. aT,-~proximation. There are many -roblems, (slow
7~,,rnDptic -pro--esses, hicrii frequency perturbation processes,
etc.) in which vertical raotion of the air particleG can. be
reiireaented by' 3tatiC: equations, In the quasi-atatic approx-
i TA a. t i on the vertical velocity of the disturbance infinite.
In thi.G systea a change of coordinatea iia, possible a
non-Gtationary set given by the x- and y-planeG and the iao-
b&ric p-tj.-~Iane. p is, now th,~~ independent variable and tha
new function in the; dynamical equations is the height of
the icobaria surface, i,e., z . z (x, y-, r, 11 t )~ The au-
t1tor gives the equations in this cyste=. They include an
imoortant cocffic!~ent, a2- the b!_Lroclinic parazt.,ter, which
"'ard 2/11

49-53-4-7/18
The. C'han:~-e of Pressure iia a Baxoclinic Ltmosphere.
i considered constant in subacqUent work, (in the troposphere
CE- changes slowly and is approximately equal to 0.1);. The
Coriolis coefficient is taken to be constant. Five equ&t-
ionz are derived- (1) projected motion on 'the x,tand y-
coordinate axes,, (2) the equation of continuity he simple
form. obtained is one of the advantages, of the noa-atationary
coordinate system), ('.') heat flow equation, (4) the hydro-
utaltic equation, and (5) the, Chapeyron. equation. There is a
simple transition in the limiting caae from the baroclinic
to IV-lie barotropic atmosphere.9,. This occura wher. oL - 0 and
t.N. ",r,-nsity and the proanure arc related adiabatically. The
creatf-~-r,t uCc of 'Che non-stationpry coordinated system is the
reduction from aix elauations in u. v, WP P~O Pand T to f3ur
in u~ V; W'(- dp/dt~.. a-nd z . Also, W#' can be easily
eliminated by izitegratinLr the continuity equation with the
boundary conditions w)-%, 0 aa P--)0 and w-)0 as
z--~O . Substitution ia made in the resultant expression
not for z = 0 but for a nearby isobaric surface p P
at litACLt zo The fact that it is impossible to uae thg,
bDundary coaditicn z - 0 (at the Earth's surftce) is the
ua,lor dra-,!,ack of' the stationary meti-Lod. The boundary
3/11

4 9-51EJ-14 -7/18
;`.e ChDT.,ge of Pressure in a Baroclinic A,t::iozphere
eproasion thua obtained, together with the dynamic (with
.vi eliminated) are the basic equations for a. baroclinic
atmosphere . Tlho author next introduces dimensionless quan-
Uttea which Te dependent on P_ characteristic horizontal
length and velocivy. In higbL-frequency perturbati3n. process-
e0l the lenEth used is that Introducedby K. M., Obukhov and.
the velocit;( is that of saund. In synoptic processes, the:
length and the velocity -JIO--/(3ec,, Vie author, in-;
troduces two ratlov expreased in terms of these quantities
c, and P -- c represents the ratio of' the characteristic
relative Vortex motion and the transfer motion and P rep-
reGents the influence of the two-dimensioual compressibility
of the medium (ie., the deformability ~a the horizontal
planel. In synoptic' processes, e -10--L and. ~