SCIENTIFIC ABSTRACT GLAGOLEVA, A. - GLAZOV, V.
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SCIENTIFIC ABSTRACT
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InFtitut Orpnniche,,kikh Po;iupr~~duk%ov I Kr!i2i'eley lr-.
K. E. Va:-)shil-va ;!" Auoist
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I I( TO t
FISHES, M.Ta.; GLAG4DLBVA, G.F.
Jupiter in 1951. Biul.VAGO no.18:41-44 '56. (MIJIA 10: 1)
1. Mookovsko7a otdelan17e VSOGOYusnOgO astronomo-jitodeBichaBkoge
obahcheatTa, otdol planet i Lany.
(Jupiter (Planet))
I I ;.
I - ( ~ .1 1 . I ; I-
GIAGOLEVA, I.I.
Aralysis of w.nrclar --ariationa. ~.-~~:-nn.zzhur. 3?
no.4:773-775 JI-AE 161. n-,
1. Glavnay-- astronomichr,~ka~m oboervatoriya AN USSR.
(latitade variat-,on)
FEDOROV, Ye.P. (Fedorov, IS.F.]i GLAGOLEVA, L.I. (fildiolirtwi,
Flattening of latitude obBervatl~.ns. Dop, AN 'Jitz"R no.4:47,11-4'77
162. NIRA 15: 0
1. Glavn,iya astronomicheskaya observ,ituriya All 1"SSR, 2, Chlen-
korrespondent AN USSR (for Fedorcv).
(AfltronomIcn1 geogr-.-phy) fElacti-onic dii~it,,d c~mputern)
Fq4
A~~ASSION KR: AP40408~0
G a
TMEt Analyzing the 4POctlUm of errots of lj:ti0dj
SOURCE As trooomi theiskly: 4 1
0
%-V:
TOPIC TAGS: latitude obse*",aiun-
positl ni.observairj,
:Observation arrorp astronomic
J
ABSTRACT: Analysis of the accurac
Irkutsk and Poltava - ~ y of 1 ilat*tudt yiisii
is not identical with.that I of~ thId toWhii6
between,thelspectral dons
ity
graphically shown in FL I of,Vth~e IZ ... su .V0.6 i'tT
n0. ~
J,atitude variations is describ~d~.&s.4~461vi6g, &W0
putation of standard is
latituoi *aiu 5;~* ~0640
nd 2) the sm,06thiug-~f- thj~jte *411,4
tilse intervals, a
the.latter, the authors use Idi thIeno tho d,
o jdQvtn
as
'.operations affect spectral density
Istandard (average) latitude vaj 6 ut
a c St of b%i
'Card 1/3
ACCESSION NR: AP4040850
of the spectrum, while- the sz~o;thi'ng"
'-danott Sd(w) of devisti
y 0n$ 0 ~-iltftd i
~N
-
values. Usin6 Sd(W) ob,tainod ftm *I sisrvs~' gusif, P
;j 1
0111 ~4ins
of the observational orrora L 0 1 Tag
th
.406
!a
od. The aCCUTacy. of data. ou~: l4titudi; va~iatioitzO
U
p
on, t to*,;
alues S (W) in this region, or g' A Ir ih~ jlidj
mulass
~~
k k z
.6 t
ASSG
C,IATTO.N,.. Glavnaya,.astronq% dbi.~iv
Ak
Ait#u
,
,
a A ad of
UkrSSR (Main Astronomic Obs rvaior*
iipjjtg: J3 i13;,~`.
SUBMITTED: OSJan64: C11,
~SUB' CODE E.S AA NO n'?' S 0 U 00
J,
~T
C,,d 2/1 L
'-'t Al-A ... FLysi-I.,:,,_y (11, vi.,.-A P;Al~ )1.-,jjraL) T
Il.y'ij.'I.rcy r~f '&'rk IT-A
Abq J~)ur Ref Zhur Firl., u-~ 6, 1(1,59, 271-67
A,-Ah--)r I.M. , Zairtayk.), G.A.
Dn,, t -tf re~lag~~ icril
T -1 t L e ry,%rudco r-,1' Skin 1,2rmer,.iturc in Yol-inc Athltjtes After
Orl !~-Il' Aknd. ped. :~-'iuk K'IFSSP, 1958, Ll~
Ahs tract 68 teen-a,e boyg and :Arls (13-18 years) were z--xv.-.Aiie,~.
The teiqerature -I~f thp skin was with thin
~)f thel'L,,o-electric cauri,~ of Vdgh,-kuk's
At zhe saEie tine, te~.n-erat-,we of axilla was determinea.
fti- for Short di Stances 'ICC, 4--,e T.'. the
I~ian,
_,e of skin temperat~~re passed throu,,ji +w.-) phanses:
L, the ber
,~i.int:iG it decreased, and then iocreased.
Card 1/2
163 -
LIBEiiMAN, Yo.A.; TSOFMA, L.M.; GLAGOENA, I-A-1,
Abnormally large resting and action pOtCntDIl:3 Of f,he muscle
fibers of a crab in potassim.-free, solutiorm, BLofizika 6
no.3:373-37/, 161. (KL-A 11,-.6)
1. Institut biologichaskoy fiziki A' SSSR, Moo'I'va.
(1.,'USGU4. (TI,!CTFtOPI~T310Ja;V/
.1
GIAGOLLINA, 1.141.; LIBEWIAN, Ye.A.
Study-LiL~ the, "quantum" nature oC miniature potc!-nUals in the end
plate of myoneural junction of a froR4 Biofizika 0' no-4:459-463 161.
(MIRA 14: 7)
1. Institut bloloj;ichoakoy f.Lzikl tal "r RI ~~)rfle7fn.
(1-1ECTROPHYSIOW.,Y) (GHQLIIP.;)
LILIERIIAII, Ye.tl,; TSJFlll',, GDIGOUVA, I.M.
Generati~.n oll the 'Iction potcnLial by riw;cuL--r A'
crustaceans in sulutions coritaindri6 -dxturc!i of and SrCl,-,.
Dok-l.All 6,iih 145 no.4:945-948 Ag 'U. i.-MU 15 :7)
1. liL;titut biolo6--ichet;Voy fizild AN 36.6h, llrod.-.tavleao ..'-.adei:d'.koln
Yu.A.0rlovy,rl.
(LLLCTOFIMIOW~Y) (bJUUUM LFilGT)
GIAGOLEVA, I-M.; LIEERMI, Ye.A. (Movkva)
Hiniatrure potentials of the end plate and their vole im the
neurommacular transmission. Usp.rovr.biol. 55 zio,,1:68-416 JJa-F
163. OIIRA 16:3)
( RONEURAL JIMICTION) (ELECTROPUSIOLOGY)
~;HTFT,tl, I.A.'-, KIPNIS, Yu.B.; PLO'I'llIKOV, T.V.; '~AVIJ)V, PAVLOV, H.3.;
vm~ov' PR")KlJT'AT, R.E.; 61-~U)LPIA, K.I.;
Ye.L.; FEL)OROVA, L.V.; MININ', I.T.
Ar',ificinl carbocyDitp lf-,~.ther. Ko'-h.-ohuv. .1'rom. f')
no.11:32-34 F164. (MIFLA 1":5)
.-, 1, - ,
. I , . . . - .
I
nauchn. rt;o.; IIESI~IAAS7' "I , N . i-;j(l MJZMET UITA , A.,
tekhn. red.
[0-vor-ali aild Ilutolillitioll of prc-dilctioll
PrOC(;L;31.!.9j KL)!-;j'I(A..-waDA mt, k 1'anizatsila i
proizvodstia. :,.oL3kvz-t, 1-',,)~Auvokii rabachii, L')(;3. IF~l p.
(~M'IFIA -17:;2)
T nv ri I i c Al :f~n rol I i 1 4
v C,
Tr-chn-;c,,;!. Sci. .',lib 1 .un n; M-n;
K-Tinin
,urt-mrv 71, e i r i q ro s r; 'F,,r n
I-'or,cc,,: I n Frorri 7-cn, T n- c
IIIEKSANDROV, R,G.; BARBASIIIIIAp Ye.G.; BASIKO, K,P, VAICANIYMI, A.& -, VASILEv-
SKIY, F.F.; GLAGOUNAI L.A.; DIMIDIIII, JI.P,, prof., (1-4-tor t.'%`411n. nauk;
L.S., NOR.01WN, A.[,; U")NETENK0, V,L.; A~'I"!J'1'ILf)Vp Yo.A.;
TRUT31TTM, IN.A.; TUCHYDICH, N.M., FADETEV, A,D,, A!!
I~OKB, G.F.; "kRTIRM3,
S.L., inch., red., SOKOL-OVA, T.F., tokhn. TiJ,
[Steel --moting; foqndijmen'3 handbook] Stallnoe. 110o; spravochilik
dlia inazterov ~itti,-1090 P-Oizvodstva. No~3k-va, Goi. nauclaw .. teklui. i,-,d-
vo mashinol,,troit. lit-ry, 11?61~ 887 p, (MIRA D,. 8)
(Foualing)
PAZUMOV, Ippolit Mikhaylovich; GRIZBURG, Yevgeniy Grigorlyevich.
Prinimall. uchastiyet GIAGOLEVA, L.A. , kand.tekhm.nauk, doteent;
GRINDERG, L.A., knndjoOin.nauk, dotmit. ATRUTSKAYA, RJ.,
red.izd-va; ISLEMIYEVA, P.G., tekhn.rod.
(Industrial organization in nonferrous metalworking p1tints]
Organizatelia proizvodstva na zavod&kh po obrabotke t.,Tve-Lxqkh
Meta.llov. 2.izd., peror. Monkva, Motallurgizclal, 1962.
540 P. (141RA 15:5)
(Nonferrous mtal industries) (Metalwork)
(Jot:';
'J/ 'J";
'~. I ;
f to;
.
"r0
-- I r, ;- 110
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f-,ta
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.
L
iy pj,c poclava te 1
uiAGI -El,A , -A R:.nd.
D.A.,
d-va ; EL IKM, '..D.,
-
i
l
SAIYAL z
of
.
Kri, A.A., -
L
te organ-izatior. :.-'J p-;tnnA-nf;, of
for the coui,,.;(, in
'.Vchii,cry pl--nts, bornik zadach o kati-:-.it organl,,.- t:;i i i
-..ova, L.A.Glar-olevoi. r.
0'r A
(I~achin-r~ ii,du,,lLij
Gi,AGOLNA, L.A.,
Now .~I"; jxactic,:,-~ in
1 C~~-kova ol h~j 11 jxav l-,: C,;!? Val
GLAGOLENA, L.A.,
nauk I.C"S'll"V
off IA Vil
AUTHOR: Glago"ev.9, 0 2 r~,
14
TITLE. Forms of' ltligraLion of' Ktemt,~rits in Rivers ( -ora.y mj.6n~tsii
eLementov v rechfivkh vod~,kh)
PERIODICAL: Dokla(ly Akademii nEiLlk :333)R, 195b, Vol 1-11, lir 6, ';P 1052 -1055
(U-ISR)
ABSTRACT: The river waleri trarisport iifferent ciubstarices ir. ", forms:
1) au trw and colioid OOLULiOUS, a s mecloini~;al ~:u,;,,ension of
firie-textured ptirticles itfid ~~s ,-.-Irried away coarge
boulders. The qunntitativL ratic,,ibetwoen 1) and are different
ac;:orJixig to the water level con,litiorio ul' tfit-~ r1,1E!r:3 811d arcord-
;jig to tile chorrictor of' th~i iral.ned nren, 1t, io irij)(-,rtant to know
I
the forms of* iri~;ration of' the el~-munts fur t,he problern (,,f :,uu~jy
of reservoirs and waters -,-nd for the of Line
~sm of t~ie process of aeclimentation. Thi-3 pLper j2 a continuation
in detail of trie previous papers which xe:-e itarted by the otde2
sravnitel'noy litolo6ii (.'jeLartment of Couqjarixi~ L[!ho1r,6y. cf the
~3eological Institute, AS U33R. The followlri,;, riVE!r.-i in the catch-
ment area of the Black Sea (Chernoye more' were 1-nvesti,;ated
,Iurin6 floods: Dor., Danube (~Iunay), Fripet (Pripyat';', Kuban',
C3rd 1/1-1 Rion nnd Chorokii. At that tiiEe the riv-.~rs usua-.i tninsFor- -0 -
Forms of M, iera t i on o,' Elem~-,n ts: ir. River ij
80 of the annual boultiers intc the sea. i~~ :.ne xw.-~r samplet;
the frnctions 1) - 5) were .3epal-rited. The whi--h wns
ed thri-'(16h .11ter"i cont,?Imed 1:).k:. true ';0I)ltion Find a
p,i f, of tlie (,n I I o id~i . [n thu courze und !'liw L;u:3p!r.,;ion.3 the to-
L~1 CO%tent 01 ~'e, 1,~n, P, Ca ~irid C Qrg wa~~l A'emically determined
h e L a i~ e g I fin d 2 num I a I a n d a c f. rum
me t'jind
n 1, i le onli'll, ~k I 1 1 t,'~ ~ .01 L I.:; 111,-- n i. te r '.'iq t u r
'Pii b i ghows ti,,) coi,Lenf, ii~ '!,,j ~;us ~~CmL;ion rav] "n
tile .3olution. rhuo may be oeerl "kint Ul! 4iVi,,J(-(l in-
to (:ruupj-. ai We, 'dn , P, V, Ci- ) Ni il-.ud -";ii :iiainly ;IF,
;U~3',UnJion'.3 wil only j~urtly i,ii olved ~A,,Ae, At-j )r !.; url
tioll: its affluent ~'Z.IpA 'irairis' a JwLulpy nr~a. .~11 :Ails caje Fe,
'~r. ind P iuri:: oo;ubla L-, i c c e x--, 0 . j L -011 p i"P pl :.e s
Cu, Ca, ~,r and Ela. Thazi au inly :i. 8ru L-.~ a-i solutions. The
iri "'Le" miera Le as Licar~ons Les In th, ca s~ copper 1 t J 3 ob-
"iia L ai-30 play a -;ertain part The -~if-
fprences in 'he forui3 of i;~i,:rarian w1uc,:. wi~re favoaled ir. -,tii-q
uonne( ,cLun (,,urffirm )ncc: more ti ie ZleparaLi,)n of 014-t cOmponents o'
"'OUPS UO LC
~i,e r-ve- clutlet ic~ WLIJ by N-Y
Card 213 'Ref 4)- T',-2re ~jrc -1, ti:,Ieg and (~ referer'2(.19, Sre Soviet
Forms of Yigrati'on of Elements in Riverc ~:(Dlli/ 2u-,, 2 1
ASSOCIATION: Geoloticheikiy institut 1,adeudi 118Uk 'JLjR (6eolo,i;ical ln.ititite
AS USSRJ
P HE 3 ENT E D: April -~4, !'~56, by 11-M. -.rakhov, "'A?mLer, AS USSR
SUBMIY-7E D: April 24, 1958
Card 3/5
STRAKHOV, ITikolay Ydkhaylovich; ZALMAITZON, Enma Solanionovapt; GJAIJOLEVA, Yariya
Androyevna; BUSHINSKIY, G.I., Otv.red.; 110S07,
.--R,TFjINA-, ~-",.V,, tolchn.red.
[Studies in the geochomiBtry of uuper Paleozoic sediiionts In humid
zores; facies and geochemical rosearch.1 Ocherki gook-himl.i varkhne-
paleozoiskikh otlozhenii gUTnidnogo tipa; opyt fatsial'no-jTeokhi-nl-
chesl-o,-o iscledovaniia. llosk-.ra, Tzd-vo Akp.(!.iwul- SSM, 1959. 217
(Akad~!-,Aia naul, SSSR. Geologicheskli inatitilt TzLdy, *ao.23).
(Mlll- 12: 11)
(Sediments (Gaolopnf))
GLAGOLEVA, M.A.
Effect of benthonic organim on tho diotribution of olmonto in
recent sediments of the Black S-ba. Dokl. All SSSR 135 no.5:1',,'33-1236
D 160. (MIRA 13:12)
1. Predstavleno akademikom N.M. Strakhovym.
(Black Sea-Sediments (Geology))
(Lamellibranchiata)
GIAGOLEVA, M.A. ,
Characteristics of the distribution of elements iii modern sediments
of the Black Sea. Dokl,.Ali S66R 136 110-1-195-1% Ta 16L
I'kKIRA 14-,Ir')
1. Geologicheakly institut, AN S."SP. Prodstalflenn aka&-imilcom
14, 14~ S trakhovym.
(Black Sea---Sediment3 (Geclogy.'I)
GLAGOLEVA.. M.A.
Effect of the salinity of the basin on the acenanLlatioii of chemical
elements in sediments. Dokl. B SSSR 136 no.2:4-4149,3 161.
0IIU 14: 1)
1. Geologicheskiy institut Akademii nauk SSSR. llredst4ivleno
akademikom N.M. Strakbovym.
(Salinity) (Sodbnonts (Cieialogy))
uL ii
'11C
59 62,k'00/010/0,52/071
of
1OV5
0"Ca,lov, 19611
on Of o., I:..-cc-,i,:
ary ~.,,X :t(~r, ti-ley co-,itaix,
c; - 2 3-- 5 7
'r o
0637-0.oO99, 6.0652-(J.010641
.:0,,ju- 7, 2.
C) 4C c-'.-, a. .',c o., I- M-'
c G:1C C', 1-~, 1~ 4 01, 0 -c,, ~~c
C,, -.)'trait , S-I~ot in Of its
.1; j-, j-,-C~j '.4,,;trjj)jjtjojj
ls)/o -1/07L
ocl-,c 1., 0 -,-!Z~C:: .,c,. -,C(,; I I".~ 0 7
C C)
rj -,C: C, 7
c 17,1 c 4Z., s
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1 . V."-.IiILIYFI" F. F, , , , , ". m ,
. ; (11~ i(,(H~ -1'. (1.
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2. U63R (6co)
"The CoirioctJ.on PF,L~-oen UrIE, 'A;n~j -n 1 t.ho ~Iiritll,ril ." Prul", .1 ',10),
19 '. 3 . ( i ') -') 4 ~,
9. Moteorologiy--i, No. -1, 1949.
OW Red-cort U-2551, 30 Oct 52.
- - I I I
-VAt " 9~~''- - - --.- -
Ob
GLAGOLEVA, M,G.; SAUSIA3, Ye.l(,! TIUrM. Ya,A.
Prognosis of water taraporat.Lre at the vtouthvoelmrn titiore of
Sakhalin. Trudy T3IP no, 57;'3P... "-I! *~"% OILRA 10:9)
(Sa7,chalin
PHASE I BOOK EXPLOITAT1011 SOV/456.2
Moscow. Tsentr&l'nyy institut, prognozov
'Voprosy morskikh gidrometeorologicheskikh prognozov (Problorn,.zi of
1
ff,yclx-ometeorologic Forecasting) IVscow, Gidrimeteoiz1af- 19179.
09 p. (Series: Its: Trudy, Nyp. 91) Errata slip -fn~vrtrM. 31X copjei~
SponHoring Agencies: Tsentrallnyy institut prognovov; Gla,niciye upra,,-Lenlye
gidrometeorclogicheskoy s.luzhby pri Sovete Kiniatz"'v SMR.
:~,I. (ritle page); A.I. Karn-kash; Ed. (Insldr-. book): M.N.
.P
Tech. Ed.: I.M. Zarkh.
MWOSE; This issue of the Trans&cLions of the Contre-1 Institute of Forecaeting is
int~-nded for scientific and field workers of the Fydrcmeteorolo~jcall Serviit~.
It vill be of interest to All meteorologists, hydrolcig.-Istii, and
COVEW,E: The articles in this collection detil mair-ly with '.he
temperature in the open sea and in coastal Wateri. W'hct~a of
casting of spring ice behavior are aloo anillyzed. Tile of I nvl~!3tiqat i fig
Card 112
Problems of Oceanographic Hy(irometeorologic Forecastinv SOTIIIL~,~--
the possibility of extrapolating the Ci(-Idt) of (Y~,Irfjfk' ard
u0ing
Refer-.nces follov earh arLicle.
TABLE OF CONTENTS;
Belinskiy, N.A., and M.G. Glagoleva. hivestigntIng th-,.~
cf Extrapoiating th,~t Anomaly Fields of Cycl.~)ni,! and
t, R fl_:Iont~ o1' -the
Shapkina, V,F. Fcrecasting the Water Tenrperatur,~ in 0te
Kuroshio, TsAshima, and Primorskoye Dirrents
Sau,skav, Ye. M. Forecasting Spring Z-e Ph-enomenza on tbe -.i--rln~ Sf~~-.
T~utnev, Ya, A. On Methods for Long-Range For~cml:ing of th,:~
for Break-up and Clearing of Ice on the Sea of Ja-oan 5,1
1E'her--vP-f.ev3kaya, 0.1. Calcu.Lations of Water 11-2inperatuzi~
1~iring the Warm Season 64
ILVAIT.ABLE. Libra-ry of Ccngr--sE;
Card 2/2 JA/dwji/r-as
t~, Co -r t.-1 T'-) 1 a C, n o
n oma C', 1,3 d ri i (,, -- P n t i c. ~ r~-: I -) 7 1 i c A ci tv
(i ov n I o, i i s I tr "i t i i-lo:r -triom:iliv
31, 1 YI 0 V 'I
C. o if 1 ?,11 1 C ( U3 S 11
Th!2 !on(,,-
t c- r- for--c tz3 h-;V4!- 11()t PI-D(111~ results.
It I.: tilat tla,- of
t
-it U-ii.? cycle--, over
,,iort -eri~)ds, The lyiv~~;ti tion ref-rs to 'h--- between
w-t Ion~,
1.itiida -700 i-st north
irlt 1'; 01,10 , -111 -1 1,11C, p (.1 1o c I seo e n1,2 1 71 rl iin-11 1 19 5 7
The ~eiao Tivi~h-l ~M 39 rectan-les- The
Monthl.-( of nnomalc)-is fields in rcc-t!~rit-zle center
.3 exr,,-~nded -n s-~r ieo 1-,v correla-
f,L(~n oel'fici(mt.-3 fourd ir-mod th,? r-rc-isence ol' w,ves of'
t P-l'..-itiong r pr-1,J cjc, ~ 10 C? - .
TO. ~: 7S
J.qve:~ t. j:- j ()rl )f I -~ ~ ', I I i t,,, f - !j -.1 -~ t, I -, -. ) i . I ".,I:, I-
r~ n o I n 7 1 1 :; L
Tho ~in -I z i "I t' I il -ts ~,nj-y oC month3
";inil " r"' .'7 ;~illllysi'i of
"n t in U,)I-l to
t t t, h in 10 -.ro
6 a I ~v 1,v t~ x ~ r
DO t I. ~111'1 I I t' ro- r..'i i-I "s -I r~ - ;113!1
: , Uo all W-ave
cr,-clz-,s, ~ipro considere-1, in th ni r. -vi-li n p-~rio I
shorter than 2 :roar.,3 . The Ill fl 0 !r1,-) 11 11 V Fl*llj-~~fl c i1190"
I v 1 i It o I' i f f e ron c i 1 ik ro (I u t j on o" t1,,
I ('. i "':~ f,:; Thr, .,)It t h I'v vc r- n--, i -wly (-crili )c'nod by the
n~~! %-)*, conn,!,-4
''f-1 th(! of ntmnsph-ric
I ~ r'-) C, Q ': SS .'11- ~i--: )f v -,f !-,horiler periods, e.g.
litv-~ -voul:l ".E, experi th!~t certain syn-
o7tic situ~.tions 77.- -atm-r. It e i. r c ia r a :t-!-- for -,I-,I,)ut thil~
-4 cn!"!'ll * nn v.
Nerio,l of time rh
fncilitattr~ thp usi! ter, v;~v~i iwriodo. n un t-') more
acclir-te value-i
of
-gh ic ~l - r - Sov i e t
Card
6 OHORS.~ Bulinskiy', 11, A., Glagoleva,, M,. G,,
S/050/60/000/03/~O~"`
BO()7/BOO',!
-.'-'LE. Method of Investigating and Forecasting
Lperiodic Marine Currents~v
PPRIODICAL
AB~3TRACT
Card 1/3
Meteorologiya i gidrologiya, 1960, NT 3, pp 18 - 25 (133SR)
In order to general.Lze data regarding observations of aperindic
current changes, two questions have to be sol-red,. Firat, a me-.:.
must be found for a ti.me and space charactex'iZihtiOn of wind con'li
tions, and secondly, the dependence of currents on the wind must
be determined. In this connection papers by V, Yu. Vize (Ref J)
Ekman,s theory of drift and gradient currents., and the papers
(Refs 5 - 12) are mentioned. The question hero is solved in a
different way, Certain simple wiid fields or fields of atmospht~iL~;
pressure are assumed. These simple fields (patterns) must be chosen.
in such a way as to characterize a concrete field in their totalit,i.
In each individual case it has to be explained, to what extei,1.
tain patterns are contained in concrete fields. Single the pattern-i
remain unchanged, the actual wind (or pressure) fielde may be
pared to one another~ For this purpose it is convenient to
pressure fields in series according to the polynomes by Cheb.-j*i;hFr-
This method is well developed (Ref 1) and offers the possibil-,ty
Method of Investigating and Parecasting Aperiodic S/05o/60/000/03/003/020
Marine, Currents B007/BOO2
of using patterns, Since there are not enough data ort observa-
tions of atmosph9ric pressure with a suffioien't accuracy, an in-
terdepartmental expedition was made in the Black Sen and Azov Sea
In 1958--59 in which the following institutes -took Part., Tsentra.1-
nyy inatitut prognozov (Cent;~al__Jngtitute of '-Ic - c -;,,z'ts)_~
Gosudarstvennyy okeanograficheskiy inotitut (~,:LaLe Institute of'
Ocea ap Y__'__~he3~nog(~ I
Gidrometeorologicheskaya observa to1 ya.
Azovakogo morey (Hydrometeorological Observatory of the Black and
Azov Sea), Chernomorskays. eksperimen-fa-F-Raya 1119.110 n0- saledovatel;
skaya stantsiya okeanologii All SSSR (Black Sea Expeiimental and--
Scientific Research Station of Oceanology of the AS-U5�14)i
ellskiy institut
(Arctic and Antarctic Scientific Reeearci IwLUIQ~t, Current8
were observed by means of Alekseyev air vane.o and Roberts radio
air vanes, the distributi.on of water temperaW.re aad salt conten,
in the water was observed in the vertical anii in 50-mile=.sectiont,
every 3-5 days, and the currents were meaaun~d, On the basis ~,f
the data obtained, the observed currents, le-rel fluctuations, and
vertical distribution of the water temperature vrere compared ~0
the distribution of the atmospheric pressure ((ieveloped in aerie=-
Card 213 according to the polynomea by Chebyshev),, Tha currenio were, foand
of lf-,i~stigating and Forecasting Aperiodic
Currentg B007/110n')
to be independent of local winds and there-roi-e deui~]--P
influence of the wind field over the whol-j ef)a,, The cnirrentt:,
the same time showed different conditions at difforent poirti)
of the sea., The invest igat . ions showed that that influen-:e of a 1:or~
crete wind field or a baric field on the dev---lopment of the i-1-1:11
rent has to be investigated separately at ev(--.ry individual poi-
Ae usual, the currents were shown in the form of proje~.tion.':-
The method is given by means of which the relations are obtatned
which ser-e for the calculation of current projections ac.f~oTding
to the given baric field. By means of these relationa. the vel'~7-1,-
ty was calculated for all points chosen for observa-1;,or~i,. Or. tbp
basis of these velocities ', the spatial distribution of ourre~-A~-,
and their changes with time were determined, The to~&Aity of ~ur
Tents .calculated and observed thus yiolded 11 TCgUjjjV pi'4ur Th~-
investigations also showed that the important water tomp,-rai~
changes of the surface layer are conditioned by the state of the
baric field above the sea, There are 2 figures and 11' refereri(~:.'
9 of which are Soviet..
Card 3/3
BELIIISKIY, II.A.; GLAGOLETA, M.G.
Mj,thorl of calculating water tomperstUrf, in t3lrfacF~ IEI~er Of
t4c sea during t~ae warm part of the year. Mrtoer.i p.-Jdrol. no.?:
14-2 1 JI 160. (11IRA 13:7)
(Ocoan tomperature)
BELINSKIY, N.A.,; GLAGOLEVA, M,G,,; S,',RIPTUI,'OVA, L.I.
Calculation of the vertical di.str"L'ontion of wat4t.- t-amperature.
Kiteor., i gidrol, no. 6, 1-A- )4 J e '61~ (MIRA 16-0)
1. TSent.rallnyy In3ttt,W, prognozov, ,I I
(W,itor-
7 Y ,',,A, , , ;~
rJoktor p.~.cgraf.rauk
Yand.f 4 z.-:r.ate:::,nauk
Stud,,ing Uic. stiort-period oscillations of tr(-.! :X
Cyclonic &nd ant"Icyclonic act,iv~ty. eteor,i :-i i,-1-
27 - 31
J. T"Ien,ralInvy institut prop-nozov.
dr-lnf~-,,~:-o- c:,,'ca
-omv-imints. Truti~- TSIP
r!n GE m! ~'r.%
' (."[IRA
39
3
SOURCE CODE: UR/2511(:1/65/000,111;2/0033/0039
AUTHOR: Glagoleva, M. G.
ORG: none
TITLE: Analytical representation of the distribution or hydrometeoro'logical vlementli
based on natural orthogonal components
proj;nozov. Trudy, no. ' 42, 1965. Morskiye prog-'
SOURCE: Moscow. Tsentral'ny institut .1
nozy i ras-~h-e-ty -(Marine forecasts and cal .- culations) ; maLerialy Vsesoyuzn0go soveshcha-'
niya, noyabr' 1963 g., 33-39
TOPIC TAGS: atmospheric circulation, weather forecasting, atrospheric pressure,
ocean dynamics , atmQ,spheric temperature, hydrometeorology
ABSTRACT: A method of establi,5hing natural components for temperature distribution
curves in the upper 200 m seaAayer and the baric fields over the nor-,hern parts of
the Atlantic and Pacific Oceans is described. The equation
P(j,) = B0 t BIXI(-T) ~ B2X(X)
was applied for the forccasting of various hydronieteorologiral conci-tions, where Xj(x)
are the natural components and BI ar,,! the expansion coefficients. The natural c--ripo-.
nents were found using a method develope(I Ly N. A. Baprov (19SJ). BaIrrov's methD'l
1/2
~109111-66
ACC NR: AT6006572
consists of tabulating d fLITICILiOn Y(x,t), which iz; a solucto'd
ment, for some discrete values of time and space, and applying it for the development
of a system of equations based on equation (1). The solution of the system leadi; to
the evaluation of characteristic numbers and characteristic vectors of' a symmetrica'
matrix. For the evaluation of natural comi ')onents, seine. def.,Aiile temperature v-ilthl!i
were assumed at depths of 0, 10, 25, 50, 75, 100, 150 m. II: is coiicludod that
use of natural components, i. e., the coefficients of expan!-.ioa of baric fields, Fjv-
es better results in forecasting than Chebyshev poly mials. Orig. art. has: 4 Figures,
10 formulas. T
SUB CODE: 04,08/ SUBM DATE: none/ O~T~ REF: 004
af
SOURCL CODL
01~G: nono
U E / 2 5 46 6 / 0 0 0 / 15 6 / 0 0 6 30 () 0 8
11 TL Z' Forecasts of the vertical distribution of water temperatkin;! in the Darents Sea
SOU3CE: '-Moscow. T-,,=,tral'nyy institut
_prognozov. Trudy, no. 156,, '966. :~aschet i
pro~-,noz cle.-,,entov rezhima morya (Observing and forecasting char~lctvristicz; of sea phe-
I'OPIC 7AGS: wo6ther forecasting, occan ayivimIC5, weather st,-~tion
"I -is acco-,-,,:L;i~, to a wez,ic,kk dov~~,Inpt,~d at the Central Insti-
1`0 verification W,
y. laz-;t,,~d b to 8 day:-- t cmp,! ra -
'Uto 0, '-:Otcol'olo~'Y Cnd Jiyoroloi-
tu~-'s llcr-~ ""Casure'd from anchorod wc,iLner ,;"iip-;, w*'-,iJ*Ie curr,--nts 14e:M! mcai;ur,~d by auto-
ma-zic. buoy, rocorders. Water temperatures in the uppei-Taost --tratum of -,Iie sea are con-
zi,olled by the inflow of heat at the sea surface; heat transfer is controlled by the
cur;:,e-,,ts. Calculation of the he-at-balanceIat the sea surface can be made only for the
period of time covered by actual observations. Any extrapolation .`nto the future for
fo-zecasziDg purposes is based on the known heat level. Such calculations involve an
!caialyf,is of change in time in the values of eight coefficients obtained by the solution
of Chebyshev polyzomials representing the pressure field. it is desirable to further
Card 1/2
L 1008!-67
ACC NR, AT60264Li7
verify the correctness of -forecasts by making observations over longer periods of
tim.e. Ermrs in such forecasts stemnied frem temperature variations from station to
5tation and the different locations of measuring instruments. Oril.r. art. has: 3
figures, 1 table, 2 formulas.
SUB CODZ:C-~P8/ SUMH DATE: none/ ORIG REF: 005
CurEi 2/2
USM/Medloix;e Leprosy, Therapy Jan 48
Modlaimie Therapeutics
"The Use of Eye Fluids on Leprous Patients,"
L. 0. Baluyova, M. I. Glagoleva, Leprosy Sector,
lust of Malzitia, Med Paraeltol and Relminthol,
Acad Med Seft USSR, 1 p
'Bov Med" Ho 1
Suggests use of Ve fluids 129 cine of the patho-
genic substances in current'treatment of
leprosy. Discusses eye fluids and methoda for
administering them.
ALOT
3LAGOLEVA, M. N.
Torsuyev, N. A. and Ulagoleva, M. N. "Painful percussion of tne ,one a;s
a symptom in tne- leper," Sbornik naucn. trudov (Rost. n/D gos. in-t),
voi. viii, 1948, p.
KRYLOV. Aleksay Nikolayevich, akademik; GLAGOL9VA, M.14., )tv,~tjj~,vallW
sostavitell ; SMIRNov, v. i. , a,