SCIENTIFIC ABSTRACT SHULEYKIN, V.V. - SHULEYKIN, V.V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001550130001-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 9, 2001
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ISAKOV, I.S., prof., admiral flota v otstavke, o tv. red. ;--SHULE,TKIN, V.V.,
skademik, inzb.-kapitan 1 ranga, zamostitel' otv.red. po II to,mu-i-,
DE14111, L.A., dotsent, kand.geograf.nauk, inzh.-kcapitan I ranga,
glavnyy red.: ABANIKIII, P.S., admiral, red.; VIZE, T.Yu., red.;
GF,ILkSII,DV. I.P.. red.: GLIHKOV. Ye.G., inzh.-kontr-admiral. red.;
DROZI)OV, O.A., prof., doktor geograf.nank, red.; ZOZULTA, F.V..
vitse-admiral, red.; PAVIOVSKIY. Ya.N., akademik, general-layte-
rant meditsinakoy nluzhby, red.; POGOSYAII, Kh.P., prof., doktor
geograf.naiik, red.; RUWVITS, L.F., doktor geograf.nauk, rod.:
SKORODU14)V, L.A., kontr-admiral, red.; SHIRSHOV, P.P.. akademik,
red. [deceased]; BASHILOV. G.Ya., inzh.-kapitan 2 ranga, uchenyy
sekretar'; SEREGIN, M.P., kapitau I ranga, red.kart: RYABCHIKOV.
S.T., podpolkovnik, red.kart; YEGORIYEEVA, A.V., kand.geograf.nauk.
red.k-art; AVERIYANOVA, P.S., kand.geograf.nauk, red.kart; BUGORKOVA,
O.S., red.kart; GAPOITOVA, A.A., red.kart; DMITRIYEVA, T.V., red.kart;
DOTSENKO, Ye.I., red.kart; KON-MOVA, L.G., red.kart; KOWIOVA, Te.:N.,
red.kart; LUKABOVA, L.S., red.kart; SMIRNOVA,.V.G., kand.geograf.Pauk.
red.kart; CHWHULINA, Ye.P., red.kart; SHKOLINIKOV, A.M., red.kart;
GRINIKO, A.M., tekhn.red.; IVAMVA, M.A., tekhn.red.; ~VROZOVA, A.F.,
tekhn.red.
[Marine atlas] K)rskoi atlas. Otv.red.I.S.Isakov. Glav.red. L.A.
Demin. Izd. Morskogo -nnerallnogo shtaba. Vol.2 [Physical geography]
r~
Fiziko-geograficheskii. Zamestitell otv.red. Do II torTu T.T. Shulei-
kin. 1953. 76 maps. (MIRA 12:1)
1. Russia (1923- U.S.S.R.) Voyenno-morskoye ministerstvo. 2. Chlen-
korrespondent Akademii nauk SSSR (for Vize, Gerasimov).
(ocean--maps) (Harbors-Maps)

. ~. " - .. -L.. , , .
I:- jqL4,1-u,.+ rif. -,n a :;'r) '-7
--1331 ZI-5 . 1. . - . - P f ~ : e s '17 --"-76 olf : V Otldelonii fiziko-
nauk.
Vest-nik A-kade:rii SSSR, 23(12): 75-77, 1~53.

D141TRIYEV, A.A.,- SHIJIXYXIN, V.L, aXademik.
Passage of long waves through an obstacle with partial reflection and given
reflection coefficient. Dokl.AN SSSR 90 no.4:509-512 Je 153. (W-RA 6:5 )
1. Akademiya Nauk SSSR (for Shaleykin). (waves)

DMITRIM.-A.A.; BOIICHKOVSKAYA, T.V.; SHUIJAMIN, V.V., akademik.
Concerning wave turbulence. DAL All SSSR 91 no-1:31-33 Jl '53.
(W,RA 6:6)
1. Akademiya nauk SSSR (for Shuleykin). (Turbulence)

LINZYKIN, P.S., SHULEYKIN, V.V., akademik.
Distribution of salinity in shallow sea water. Dokl. AN =R 91 no.1:71-
73 Jl '53. (MI-RA 6:6)
1. Akademiya nauk SSSR (for Shuleykin). 2. Gosudarstvenny okeanografiche-
skiy institut. (sea water)

BIBIKOV. D.N.; SHMMN, V.V. 9 akademik.
-i'!~ -,
On the problem of ice conditions in non-completely freezing water
currents. Dok1.AN S35R 91 nb.4:799-801 A6 '53- (MLEA 6:8)
1. Akademlya naulic SM (for Shaleykin).
(Ice on rivers. lakes'. qtc.)_

Sffn =17M., V. V.
Uz SR/~;eonhysics - Wind Energy
53
"How tha Energy of a Wind is Transfered to a Wave," Acad V. V. Shuleykin, Marine
Hydrophys Inst. Acad Sci USSR
DAN SSSR, Vol 91, No 5. PP 1079-1082
Derives the f.,)rmula f or the ei)ergy Wy transf Ered by a wind to a wave ner unit surface
of the seR in unit time; namely WV D-h &aIIV-c)2-, where h is wave height, n a coefficient
2 T
de-oeadin-- on steeDness h//\ of waves (AWave length). T the period of the waves, S. the
density of 91r, V 'the velocity of the waves. c a constant. Also obtains an exDression
for the coefficient, eta, of utilization. by man of wave energy (e.g. finds eta-9 to 54%).
Prest-nti~d 19 A.-pr 53.
266T75

KITKIN. P.A.; SHULEYKIN,,V.V., akademik.
Effect of wind on the water inuss in small inland basins. Dokl.AN SSSR 91
no.05:1325-1328 Ag '53. (MI-RA 6:8)
1..Wcademiya naak SSSR (for Shuleykin). 2. Morskoy gidrofi-.ichel3kiy institut
Ak-adejaii nauk SSSR. (Hydrodynamics) (Winds)

KOLESNIKOV, A.G.; SHULMIN, V.V., akademik.
Variations of water temDerature in reservoirs in wintertime. Dok-I.AN SSSR
92 no.1:37-40 S '53. (MLR4 6:8)
1. Akademiya nauk SSSR (for Shuleykin). 2. Morskiy gidrofizicheskiy institut
Akademii nauk SSSR (for Kolesnikov). (Water) (Reservoirs)

,USSR/Geophysics waves 1 Sep 53
"A Hydrodynamic Pic.ture of the Transfer of., Energy
From Wind to Wave,l-~Acad V. V. Shuleykin:,.2.-M'arine Hy-
~drophysics Inst Acad Sci USSR
DAN SSSR, Vol 92, No 1, pp 41-44
~ElplaIined in a previous work (DAN, Vol 91, No 5, 1953)
how the energy of wind is transferred to'a wave. At-
tempts here to obtain directly from the hydrodynamic
eq ~the approk hypothetical relations which are con-
firmed in the previous work. Reveals some new, im-
portant facts. Presented 4 Jul 53.
274T60

KITXIN, P.A.; ~ .. akademik.
On the dynamics of sea and ocean currents. DoIcLAN SSSR 92 no.2:293-296
S '53. (MT-RA 6--8)
1. "ademiya nauk SSSR (for Shuleykin). 2. Morskoy gidrofisicheakiy institut
Akademil nauk SMR (for Xitkin). (Ocean currents)

VOIT, S.S.; SHU13YKIN, V.V., akademik.
Transition of SDherical sound waves from a moving medium into another medium
moving at a different smeed and having other characteristics. Dokl.AN SWR
92 n0-3:491-493 S '53. (MMA 6:9)
1. Akademiya nauk SSSR (for Shuleykin). 2. Morskoy gidrofizicheskiy insti-
tut Akademii nauk SSSR (for Voit). (Fluid mechanics) (Sound waves)

SOKOLOV, A.A.; TXMIOV, I.M.; SHuljqyKl V.V., al-ademik.
q'-
Motion of fast electrons in the magnetic field. Do!cl.AN SSSR 92 no-3:537-540
S '53. - (MIJU 6 - 9 )
1. Akademiya. nauk SSSR (for Shuleykin). 2. Moskovskiy gosudurstvennyy
universitet im. M.V.Lomonosova. (for Sokolov and Ternov).
(Electrons) (Electromagnetism)

IVANEIKO, D.; BRODSKIY, A.; SHULZYKD1, V.V., akadetaik-.
Interaction of gravitation and the vacuum of particles. Dokl.AN SSSR 92
no.4:731-734 0 '53. MRA 6:9)
1. Akademiya nauk SSSR (for Shuleykin). 2. Moskovskiy gosudaretvennvy
universitet im. M.V.Lomonosova (for Ivanenko and Brodskiy).
(Gravitation) (Mesons)

NOZMEV, V.; SHUIJffKIN$ V.V., akademik.
Investigation of the critical conditions of liquid - vapor systems by ultra-
sonic method. Dokl.AN SWR 92 no.6:1145-1148 0 '53. MRA 6:10)
1. Akademiya nauk SSSR (for Shuleykin). 2. 14ookovskiy goaudarstvennyy uni-
versitet im. H.V.Lomonosova (for Nozdrev). .(Gritical point)

MAKSIMOV, I.V.; SRU=IN, V.V., akademik.
Secular changes of the 11-year cycle of solar activity. Dokl.AN SSSR 92
no.6:1149-1152 0 '53. 1 (MLRA 6:10)
1. Akademiya nauk SSSR (for Shuleykin). 2. Institut okeanologii Akademii
nauk SSSR (for Maksimov). (Sun Bpota)

LAIMMAII, D.L.; YUDIII, M.I.; SHUMMIN. V.V., akademik.
,V~,
Transformation of the lowest layer of the air under the Influence of the under-
lying surface. Dokl.AN SSSR 93 no.2:249-252 N 153. (KIRA 6:10)
1. Akademiya nauk SSSR (for Shuleykin). (Atmosphere)

SHULBUIN, V.V., akademik.
Wave destruction in shallow waters. DokI.AN 33SR 93 no..3:463-466 N '53.
(KMA 6: 11 )
1. Morskoy gidrofislabeekiy institut Akademii nsuk SSSR. (Tidal waves)

,SRO A 4z Y/f-/N,
USSR/Geo~hysics Shore wave action
Card 1/1
Author : Shuleykin, V. V.
Title : The breakup of waves under the action of shoals
Periodical : Izv- AN SSSR, Ser. geofiz. 1, 65-76, Jan/Feb 1954
Abstract : Investigate the distortion of the profile of waves which are propagated on
shoals.. Expresses a hypothesis concerning the dependence of the phase
velocity up on the phase of the oscillations executed by the surface of-the
wave. This hypothesis pro6eeds from the equation of continuity as written
in application to the case of the joint measurables: the depth of the sea
and the ampr1itude of the waves. The hypothesis is suggested also by the data
of the old investigations that take into consideration the appearance and
development of the second overtone; its results agree well with immediate
observations and experiences.
Institution : Marine Hydrophysics Institute, Academy of Sciences, USSR
Submitted : October 8, 1953

'W_ V. V.
USSR/Geop4y'lics - Book review FD 389
Card 1/1
Author : Shuleykin, V. V., Academician
Title : Morskoy atlas, tom II - Fizikogeograficheskiy (Marine Atlas, Vo3-
ume II - Physicogeographic], edited by Prof. Admiral I. S. Isakov and
L. A. Demin, Docent, Cand. Geog. Sci., 1953
Periodical : Izv. AN SSSR, Ser. geofiz. 3, 299-301, May/Jun 1954
Abstract : Favorable review. The Atlas contains 4 divisions: A. Most i=ortlant
maritime voyage and expeditions (Russian and Soviet). B. Oceanog-
raphy. C. Climate. D. Terrestrial magnetism, cartography, astronomy.
Contains 75 plates.
Institution :
Submitted

6 ylflA" V. V,
R/Ge6physics Book review
Card 1/1
Author Snezhinskiy, V. A., Engineer-Captain (1st rank), and Yegorov, N. I.,
Engineer-Captain (ist rank)
Title Book review: V. V. Shuleykin, Fizika morya (Physics of the Sea], 3rd
edition, supple`m_ent'e_*d',-_A:&&d Scl USSR Publishing House, 1953, 990 PP,
3,000 copies, 50 rubles
Periodical Izv. AN SSSR, Ser. geofiz. 4. "-1"8-380, Jul/Aug 1954
Abstract Favorable review of 3rd edition. First edition appeared 20 years ago.
Institution
Submitted

I fX_1 TV1V
-t-SW(,_e~ophysics '~- Wind wave -FD-759--
Card 1/1 : Pub 44-7/11
Author : Shuleykin, V. V.
Title : Dynamics of wind waves and of dead surges
Periodical : Izv- AN SSSR, Ser. geofiz., 451-481, Sep-Oct 1954
Abstract : Describes a new experimental method for investingating wind waves and
dead surges in so-called storm basin - a circular basin of very large
diameter in which are created wind waves of 10 meter wavelength and
1 meter height under the action of air currents up to 19 M/sec. The
birth, growth, and damping of the waves are recorded photographically
on a paper strip. Seven references, all USSR, including "Formation
of sea waves by wind," P. L. Kapitsa, DAN SSSR, 64, No 4, 1949.
Institution : Marine Hydrophysics Institute, Acad. Sci. USSR
Submitted : June 11, 1954
At - sy

SHUISYKIN, V,V., akademik.
- 1l'- ;';"
~,: - Int.ernai mechanism of wave formation caused by wind power. Dokl.
AN SSSR 94 no.4i677-680 F '54. (MLRA 7:2)
1. Morskoy gidrofizicheskiy Institut Akademii nauk SSSR.
(Wind power) (waves)

SRUL&YKIN, V.V., akadeinik.
Origin of steady stagnant surges. Dokl.AN SSSR 95 no-3:509-512
Mr '54. (KTRA 7:3)
1. Morskoy gidrofizicheskiy institut Akademii nauk SSSR.
(Wind power) (Waves)

SHULEYKIN, V.V.. akademik.
Physical causes of wave crest tapering. Dokl.AK SSSR 9.4, no.5,:987-990
AP '54. (HLRA 7:4)
1. Morskoy gidrofisicheakiy institut Akademii nauk SSSR.
(Waves)

USSR/Cueonhysics Dynwidc oceano,-Iraphy
Card 1/1
Pub. 22 16/47
Authors
Title
Periodical :
Abstract Z
Institution
Submitted
Shuleykin, V. V., Academician
The out'low, of a st-rell from a, stormy zone ofadeep sea
Dok. AN SS3R 9911, 57 66, Noy:l~, 19541- 1-
Naval Hydrophysical Institute ofthe Acad. of Ses..of~the,USSR

r1

SHUjayKIN, V,V., akademik.
D:ev;el.opment of wind-produced waves on a shallow sea. Dokl.AN
sm 1o4 no.2:215-218 S 155. (MLRA 9:2)
I.Morskoy gidrofisichaskiy institut Akademii nauk SSSR-
(Waves)

SHUIRYKIN, V.Y., akademik.
Aquations for wixd-produced wave fields on shallow waters. Dokl.
AN SSSR 104 is-3:397-400 8 155. (KLRA 9:2)
1.Xorskey glokofizicheskiy institut Akademii mauk SSSR.
(Waves)

VOYT,S.S.; SHULEYKII4,V.V.. akademik, redaktor; KLYAUS,Ye.M., redaktor;
redaktor
[What are tides) Chto takoe prilivy. Mosl-va, Izd-vo -Akqdemii nauk
SSSR, 1956. 101 p. (MI.PA 9:2)
(Tides)

SHULEYKIN V.V.- ALEKSEYEV, D.M., redaktor izdatel'stva; SHEVCHENKO, G.N.,
t~~-'
tsrkki-C~eskiy redaktor.
[The theory of ocean waves] Teorita morskikh voln. Moskva, Izd-vo
Akademii nauk SSSR, 1956. 141 P. (Akademiia nauk SSSR. Morskoi
gidrofizichaskil Inetitut. Trudy, vol.9) MaL 9:11)
(ocean) (Waves)

T-AZARIIV, P.P.; SHMTKIN, T.V., akademik, redaktor, IMYAGIN, B.T., redaktor;
1w I
YRAIM, G.W.',r9Ztor'; VOLAROVICH, M.P.. professor, redaktor;
YEFIMOV, professor, redaktor; MASLOV, professor, redaktor; XMIN,
A.M., professor, redaktor; KUZNETSOVA, Te.B., redaktor; SHEVC
G.N., tekhnicheakiy redaktor.
(Collection in memory of Academician P.P.Lazarev] Sbornik posvia-
shchannyi pamiati akademika P.P.IazareTa. Moskva, Izd-vo Akademil
nauk SSSR, 1956. 374 P. (MLRA 9:6)
1. Akademiya nauk SSSR. Z.Ghlen-korrespondent AN SSSR (for Derya-
gin). 3.Ghlen-korrespondent AMU (for Frank)
(Physics) (Physiology) (Geophysicsi

SOV/1 24-57-5-5585
Translation from: Referativnyy zhurnal. Mekhanika, 1957, Nr 5, p 68 (USSR)
AUTHOR: Shuleykin, V. V.
-------------------------- -------- --
T IT LE: Theory of Ocean Waves (Teoriya morskikh voln)
PERIODICAL: Tr. Mor. gidrofiz. in-ta AN SSSR. 1956, Vol 9, 143 -Tip, ill.
ABSTRACT: A compendium containing the results obtained by the author mainly in
the wave basin of the Oceanic Hydrophysics Institute, Academy of
Sciences, USSR. The work contains the following chapters: Deriva-
tion of the Classical Relationships for a Deep Sea. Derivation of the
Classical Relationships for a Shallow Sea. Group Velocity of Waves.
Wave Energy. Transfer of Wave Energy. A More Exact Definition
of the Kinematics of Ocean Waves. The Profile and Basic Para-
meters of Ocean Waves. Physical C~Luses of the Sharpening of
Ocean-wave Crests. The Kinematics of the Limiting Steepness of
Waves. The Breaking of Waves Under the Action of Shallows. Gene-
ration of Wind Waves on a Calm Surface. Some Hypotheses on Wave-
energy Growth. Test- installation Setup in a Wave Basin. Wave-
energy Balance and the Increase in the Height of the Waves. Theory
Card 1/2 of the Maintenance of the Waves by the Wind Energy. Theory of the

SOV/IZ4-57-5-5585
Theory of Ocean Waves
Growth of the Wave Length Under the Action of the Vvlind. The Causes of a Steady
Swell. Wave Behavior During a Change in Wind Direction. Reference Determina-
tion of the Action of the Basin Walls. Reference Determination of the Eddy Vis-
cosity. Wave Development From the Upwind Shore to the-Downwind Shore of a
Deep Sea. The Spreading of Swell Away From a Storm Area in a Deep Sea. Devel-
opment of Sea Waves in a Shallow Sea. Analysis of Measurements of Extremely-
large Wind-generated Waves. Rote of the Tangential Force of the Wind in the
Augme.ntation of the Wave Energy. Wave Refraction on a Continental Shelf.
Bibliography: 30 references.
Reviewer's name not given.
Card 2/2

-?CE -S1 LV
905. ODIL N-P
MR XBG~T I ~-E A
eDda acA
jr,

jai tj~ hroque was -,seLf ic photograph U,.e conUnucus
zipec r
i ra,.-v! t~d ca- 10 km at an a I tltud~ al
f "
! I!
T j
:

Lr. 1. E! Gte
L~~ C M
~r hn ian

d
"-w2

71
;:.Z

SHULRYKIN. VA., akndemik.
...... V-"*
Taneential force of the wind as a factor in the energy increment of
waves. Dokl.AY SSSR. 109 no42761-763 Ag 1956. (MIRA 9:10)
1. Morskoy gidrofisicheRkly institut Akademii nauk SSBR.
(Vaves) (Winds)

SRUIZYKIN, V.V., akademik.
Analysis of measurements of the highest wind-induced waves in
the ocean. Dokl.AN SSSR 110 no.1:53-56 S-0 156. (MLU 9:11)
1. Morskoy gidrofizicheakiy institut Akademii nauk SSM.
(waves)

SHUJWjYKDI, V.V., akadomik.
. -
Refined law of wind wave growth in length. M*kIJX SSSR 111 no*2;348-
35 1 N 15 6. -- (KGL~ 16: 1)
1. Morskoy gidrofizicheakiy inrtitut Akmdemii nauk SSSR.
(Wav,

LAZAREV, P.P., akademik; VAVILOV, 6.1. [deceased], akademik, red.;
OREBLI, L.A:,.akRdemik red.; 214 Y tV T. akademik. red,:
red.; TOLAROVIGH,
MYAGIN, B red.; iR!VWV, so asod
83 am
M.P., doktor fiz.-matem.neuk, red.; XOVM, S.S.,,prof., red.;
PRANK, G.K., d-r biolog.nauk, red.; TJWIMOV, V.V., d-r biologich.
nauk, red.; MABLOV, N.M., nauchny7 sotrudnik, red.; GESM , L.V.,
red.izd-va; ZELUKOVA, Te.V., tekhn.red.
[Works] Sochineniia. Moskva, Izd-vo AkRd.nauk SSSR. Vol.l.
1957. 895 P. (MIRA 11:1)
1. Chlen-korrespondent AN SSSR (for Deryngin, Kravkov).
(Pbysics)

. ~/O. it;ra!Iim, I,do I)IMY, Itollshikh
94

CA V 51-6-23/25
AUTHOR: Z, I Perin, Yu. I.
TITLE; Remarks on the Paper of V V. 3hule k~~i~n and P. F.
t s
Shakurov "The Sodium Line in the sorption Spectrum
of Air Above the Sea". (Po povodu stat'i V. V.*
Shuleykina i P. F. Shakurova "Liniya natriya v
spektre pogloshcheniya vozdukha nad morem".)
PERIODICAL: Optika i Spektroskopiya, 1957, Vol. III, I-,Tr. 6,
p.6?2. (USSR)
ABSTRACT: A letter. The present author criticizes the above
paper of V. V. Shuleykin and P. F. Shakurov (Ref.1).
Shuleykin and Shakarov photographed an emission
spectrum of an incandescent lamp after passage through
10 km of air about 50 m above the sea surface. The
beam from the lamp was not parallel and was not
focused on the spectrograph slit. The D-doublet of
Na was not resolved and it is hardly noticeable in
Fig.1 of Ref.l. Shuleykin and Shakurov's paper does
not give the essential experimental details such as
the type of the spectrograph used, its resolving power,
dispersion, parameters of the camera, etc. Their
Card 1/2 calculation of line intensity and derivation of the

51-6-23/25
Remarks on the Paper of V. V. Shuleykin and P. F. Shakurov
"The Sodium Line in'the Absorption Spectrum of Air Above the Sea".
atomic absorption coefficient are both erroneous.
The present author points out also that the purported
estimate of the number of excited Na atoms can only
apply to non-excited atoms in their ground state.
There is 1 Russian reference.
ASSOCIATION: Institute of Atmospheric Physics, Academy of Sciences
of the USSR. (Institut fiziki atmosfery, AN SSSR.)
SUBMITTED:. July 22, 1957-
AVAIIABIE: Library of Congress.
Card 2/2

6'J Z_ '!~- Y' /V- /1L1 V,
AUTkOR:--Shuleykin, V. V. 49-11-7/12
TITLE: Physics of the Sea in the Soviet Union During the Last
Forty Years. (Sovetskaya fizika morya za sorok let)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
1957, No.11, pp. 1366-1383 (USSR)
ABSTRACT: Investigations in the field of physics of the sea are at
present being carried out by the Hydro-physics Institute
of the Sea Ac.Sc. USSR (Morskoy Gidrofizicheskiy Institut
Akademii Nauk SSSR) and also by the State Oceanographic
Institute of the Chief Directorate of the Hydro-meteoro-
logical Services (Gosudarstvennyy Okeanograficheskiy
Institut Glavnogo Upravleniya Gidrometsluzhby), Institute of
Oceanology- of the -Ac.Sc. USSR (Institut Okeanologii AN SSSR)
and others. The author, who is a well known authority on
this subject, reviews Soviet work in this field both pre-
war and post-war and a considerable part of the information
contained in the paper is based on earlier published work
of the author himself. Particular attention is paid to
the experimental work carried out in an artificial storm
basin at the Hydro-physics Institute of the Sea Ac.-Sc., by
the method of A. A. Ivanov (Ref.22); thousands of waves
were photographed and then analysed. Some of the obtained
Card 112

49-11-7/12
Physicb of the Sea in the Soviet Union During the Last Forty Years.
results are described and these led to changes in the
views relating to the kinematics of the wind currents, the
profile of which may differ considereb1y from that of a trochoide.
The author also deals in some detail with hydro-optical
investigations carried out in the Soviet Union. It is
mentioned that of theoretical and practical interest are
also investigations by R. N. Ivanov relating to molecular
films of surface-active substances which are able to
suppress waves; the wave energy is absorbed by friction
between the sea-water and these films which can be
considered as a sort of "two-dimensional gas" which expands
during the passage of the bottom of the wave and becomes
compressed during -the passage of the top of the wave. The
results of Ivanov (Ref.35) have fully confirmed the theory
of scattering of these films and also the theory of the
wind caused drift.
There are 13 figures and 35 Slavic references.
AVAILABLE: Library of Congress.
Card 2/2

SHULEYKIN, V.V.
...................
Problems in present-day theory of sea waves. Geog.sbor. no.12:68-82
'57- (KIRA 11:1)
(waves)

AUT EOR 3"HULEYKIN V.V. PA - 3143
TITLE h in Length of High Wind Waves And the Role of Turbulent Internal
Friction.
(Narastaniye dliny bol_,!,shikh vetravykh voln i roli vnutrennego turbu-
lentnogo treniya -Russian)
PERIODCIAL Doklady Akademii Nank, 1957, Vol 113, Nr 3, pp 56D-5:63 (U.S.6-.RO
Received 6/1957 -Reviewed 7/1J57
ABSTRACT The problems'dealt with in D., 1956, Vol Ill, Nr'2', are fdrmulated with
greater exactness-in order to explain the effect of second ordir WbIch is
due to internal friction. For this purpose energy dispersion is investigated
sep&-ately from the dissipation of the moved mass at*the expense of the
t-drbulent exchange in water. An equation is obtained which differs fr=
that of the aforementioned paper of 1956 only by an additionai term with
the coefficient of the turbulent exchangei(kinematie viscosity), From tkiis
equation it can be seen that the increase ofthe radius R of the devol-
ving are (and therefore also the wavelength A ) is connected not Only with
the velocity of the increase ( and th 'is also with the velocity of the in-
crease of the wave height h), bat also with a new term that depends on
internal turbulent frictioh. It is shown that A and ~,grow according to.a.
parabolic low. Under the influence of the'effect dealt with here.bothin-
creased.by only 20/0 of the value that corresponds to the maximim wave I .
height within one hour. Investigations confirm the fact that the quantity
Card 1/2 r/R may be considered to be constant, that O,which characterizes the en-,

AUTHOR - SHULEYKIN V.11., Member of the Academy PA - 3o2o
TITLE Some Data Concerning the Kinematics of bea Waves,
(Xeshche o kinem2tike morshikh voln -Russirun )
PERIODICAL Dokiady Akademii Nauk 6SSR. 1957, Vol 113) Nr 5, pp lo43 - lo45
Received 6/1,057 Reviewed 7/1957
ABSTRACT The present -aork shows th,~t the ellipse with the semi-axes a and b (which
in previons works -were cons-idered only as auxiliary curves), have a very
distinct physical significanca. The aq:aations inthe parametrical form
x = R 0 + a sin9 , y = b cos 0 are more correct kinematic equations than
the equations of the trochoids (which serve as first approximation).
First the mo=ntary value of the velocity w of the wave current is express-
ed oy means of a previously derived formula. In the same mamner the nome-
tary value of drive velocity and of the current are expressed. Further,
the momentary value of the horizontal component of the velocity v cos 0 of
th
velocity of a surface particel is considered, The equations for AT, u and
:o
v sG are written down, and by adding the loft sides of these three equa-
tions the momantar- value of the total velocity of the horizontal motion
of the surface particles is obtained. By adding all right sides an expres-
sion, whicb'is suited for the physical inter*pretation of the phenomena, is
obtained: W + u + veos (W rR + 7a)+(wr+w r4 r) Cos
__
-
a
X
if
This total velocity of the horizontal motion is divided into two parts.
Card 1/2 the first consists of a constant current, which, in turn, consists of a

W-ome Data Concerning the Kinematics of Sea Waves. K - 3020
1,wave velocity" a:-4 of a "drive vejocity% The more interestinc. is the -9e-
0
cond or oscillating part of the current., U r2 -u r, 9
X r + I- + -wV cos /7
The brackets contain nothing but the expression for the semiaxis a of the
aforramentioned "auxiliary ellipse". In a system of coordinates moving
with the velocity r4 - in the direction of the waves the ellipse with
+ U
the semiaxes a and b represents the path taken by a particle of water. In
the general case the complicated motion of a particle on the surface can be
divided into two components in the aforementioned system of coordinates
which is moved at the same time. In conclusion several of such cases are
graphically explained.
(with 2 illustrations)
A,bSOCIATION Marine Hydropbysical Instibate of the Academy of Science of the U.S.b.R.
PRsSENTIM BY
SUBMITTLD 24-12-1956
AVAIILABIIPI Library of Congress
Card 2/2

-

R:
U
A
1-Shuleykin V. V., ',Ac&deJdciau
20-548/~4
TITLE: The Profile of the Wind Waves and their Recording
by Means of Bottom Wave Recorders (Profill vetrovykh
voln i yego zapis' na pridonnykh volnografakh).
PERIODICAL: Doklady Akademii Nauk SSSRt 1957, Vol. 115, Nr
Pp. 915-918 (USSR)
KBSTRACT: On the occasion of the downflow of the surface of the
sea to the bottom not only the total amplitudes of
pressure oscillations, but even the "overtones" of
various orders present in a real profile of highly
tapered wind waves are "filtered". The present paper
discusses the quantitative investigation of this
"filtration", the at present existing kinematic con-
ceptions on the wind waves being assumed. The author
obtains the following results: 1.) Comparison of the
values obtained by means of two different methods of
(a2/a ) (a here denotes the coefficients of the
harmoAic analyses of sea waves) again confirms for all
values of a certain argument V, the accuracy of the
CARD 1/~~ basic assumption of the here assumed kinematics of the

3OV-40-58-6-3/12
A U T H 0 R i. ~il ey ~V, Gushchin V. F. --ov ,
I I Pes~! P. I.
TITLE: Oscillations in the Heat Balance of the Atilantwic Ocean
teplovo-o balansa Atlantichesko-o Okeana)
a 0
i1LeRIOD.t._.'A1j: I_zvestiya Akademii NaW--. SSSR, Seriya Geofiziche3kaya,
~~'8 Pir 6, pp '729-740 (USSR)
1~ I
ABSTRACT: Descriptions of n~)riaal investigational methods in-to heat
b_-l:,_-ice nroblems are f.)und in Ref.l. The present article con-
nr ~ U ~L
.3 oscilla`ons in com-oonents of the heat balance and their
oar,s `,_-L tile Atia-atic (from, day to day) in various regions of
I-'-u 7ill be shown that these oscillations exceed
tile corresnond-in..-I, ones avera-ed over a -month. This blurs
'I-jie general Pattern but enables local oscillations (obtained
C~
b7 the shi-) Sedov) -to be considered - the times examined 'Lie
'Det-,"Neen October and December and the latitudes from 500-1602?:N.
Fir.1 :--ives the values of some of the elements which chanc-e
D
da~- to da~f. Curve 1 shows the change in latitude of a
C)
place at -true -midday in October, November and De~enber 10,57,
Curve 2 E;ives -the chan,e in solar hei--ht at culmination,
rlarve 3 -ives the chan-e in temperature of the water surface
L 0 0
and Curve 4 the chanc---e in tenperature o.-;L7 the air. The first
0
points on all these diagrams (11, 12 and 13 Oct) correspond
to the N. Sea. Position coordinates at true noon ... ere cal-
aard 1/12

SOV-49-58-6--3/12
Oscillations in the Heat Balance of the Atlantic Ocep-..
culated by A. F-q. Gil'mutdinov. Actinoinetric and ;ae teo-rc--
lo7ical observati3ns were made by V. F. Gushchin, V. A.
V. F. F'T
Krasnovl P. I. Feskov, I. G. Serebrennikov, Milr-110v ,
V. G. Fedorov ' and D. I. Filippov.
1. Heat inta-ke from direct and diffuse solar radiation.
As in the hydrcr,~.-ra-ohical ship "Taymyr" (Ref.23, a-D-oaratus
was used uhich -oormitted continuous registration of direct
ancl dif-'-us.--- radlation fall'-no, per cm2 of horizontal surface
(Re'L.3). The rn~di~tion receiver (a piranomete- 7 mounted in
;Timlbals or-, ttlle --lizze-r-, mast - out of the shade) was connected
t,~~ a self-r-~c~Di-C-An- -alvanom--ter. Every twenty seconds a
mark was made on a tape which unrolled at 2 cm/hour (driven
by a synchronous electric motor). Examples of these traces
(reduced in scale) are given in Fi-.2. This instrument was
calibrated several times during the voyage by a system due
to Yu. D. Yanishevskiy. The scale is not entirely linear,
being smaller for small deviations than for large. Had the
solar height remained fairly constant, this could have been
Card 2/12

0'OV_Lj 8-6--3/12
Osciila~ions in the Heat Balance of the Atlantic Ocean.
for by -raduatinc, and measurin- the traces with a
0 tD a
ai2imeter. However, the shiD worked at various latitudes
different method was th-erefore necessary. A trapezium
uses constructed: the ordinate axis was read from the scale
divisions of the galvanometer. Straight lines were then
drawn parallel to the abscissa. A millimetre ruler was used
to measure the total length of all segments cut off. The
ti-iie -scale .,,as 1--.nown from the construction of the instrument
a.rid. -the ordinate of each elementary segme-nt was !mown by
-calibration. Thus the result could be obtained. Cu:sve 1
shows the change in diurnal heat sum -per cm- of the
Atlantic surface (at different stages on the voyage). As
can be seen on clear days the heat sum.2 changes (depending
-an latitude5 from 287 to 506 cal/day/cm , althoughl in theo
same region 7 the variation extends from 56 to 506 cal when
cloudy days are included. One of the authors (Ref.1) has
introduced a coefficient of solar ener- utilisation to
Sy
characterise the influence of clouds, This can be found by
calcHlating the -,reatest possible heat sum which can reach
1 cm of a horizontal surface by direct solar radiation in
a perfectly clear sk-j (at a --iven latitude and day of the
u
s were found for latitudes 600-00oIT
Card 3/1;year). Such quantitie U

SOV-11 9-58-6-3/12
Oscillations in the Heat Balance of the Atlantic Ocean
(Refs.!, 2) and 50'-0' (Ref-3). Fig-3 gives part of a
ED
diagram by N. I. Ye-orov for the three months October,
0 10
'~i'oven
I
ber and D~~cember. From this we can obtain a Nh~a
quantity desisril;ed). If the corresVonding, actually mea-
GuLred iaa~;nitude is q , il (= q/q0) is called the utiliza-
tion coefficie:nt, The curve marked 0 in Firr.6 c-ive.- valued;
Q, Q
for q N. I. Yer-orov has compared the change in q with
the c1,,.a-n-e in cloudiness for the Indian Ocean and the Red Sea
ii
Ref.3)~ Fi 1-.4 -ives a similar comparison for the
(Fig.3, CD
-oarts of t-l-e Atlantic investigated (small circles -- points
obtained in Oct-ober; black dots - points obtained in November,
and so.uares - -oints obtained in December) The dotted line
:-iVeS _111. I. Y-,;-0r0V'S rt-:;SLLltS for comparison. As he showed
in Ref.3, a scatter of points is unavoidable since the amount
of cloud, ualikze t'-qe radiation, is not recorded continuously.
A small correction is needed to allow for the fact that q 0
Card 4/12

SOV-10-58-6-3/12
Oscil.11-ations in the Heat Balance of the Atlantic Ocean-,
is defined for direct radiation whilst q includes also
A.ffuse radiation (thus the experimental curve has some points
>1). A com-parison of Ye-orov's material with that in
Wie joresont article indicates that the relation between A
and degree of cloud is universal to a sufficiently close
approximation,
Amount of heat -oenetratin,-, into the water, Previously,
-ant of heat reaching the surface has been con-
nly the amo
._;_-ered~ To consider the amount entering the water it is
I-ecessary to calculate the extent of reflection. One of the
authors has already considered the reflection coefficient of
L
the sea's surface (Ref.1). Sverdrup (Ref.4) has made similar
investigat.i.ons for both direct and diffuse reflection at
varyin- solar heic-hts. On the basis of these calculations.
0 C)
the authors have constructed a diagram of change in reflec~led
energy depending on the hour angle of the Sun. Fi~',5,(a)and
(b), -ives tmio such diagrams - one corresponding -to the
Northern course of the 'Sedov' and -'the other to the Southern.
The scales of the -two diagrams are different, and, in both
cases, the curve for the reflected rays is ten times larger
than the curve for the daily variation of direct and diffuse
Ca-rd 5/1 iadiation. The reflection coefficient reaches high valueS

30V-49-5~3-6-3/12
Oscillatuions in the Heat Balance of the Atlantic Ocean.
0 ~
at small angles - thusoit has dropped from 0.4 at 5 UG
0.12 at 200. After 50 it remains almost constant at 0.03,
As a result, the to~-ql- reflected energy per day changed
little as the 'Sedovl changed from its northerly tc its,
southerly route. By graphical integration the empirical,
forrmula for the amount of reflected heat:
P
Aq = 33 r,~ m cal/day cm7 (1)
vias obtained, -where q is the utilisation coefficient and
i-al coaff!
s an emp-Jr changing by 2011o between the
northerly a-nd ;,--.)u-'--h-or1y routes, but appro:~.dmately equal tc
one. F-i,-.G. curve I gives Aq thus calculated for each
day and, thence, curve 2 which shows the amount of heat
penet-rati-a-- the wate-n.
'7) He a - 1
,,_.-a,, oss by evaooratior- This was the most important
heat loss Ne-to'Tin the regions surveyed. One of the authors
(Ref.1). in experiments in the Indian Ocean, found that the
amount of viatar evaporating/unit time/unit surface area
depended on the humidity deficiency aa-d the wind speed. It"
Card 6/12

SOV-"~-58-6-3/'2
Oscill. _-,ions in 41 U
-he Heat Balance of the Atlantic Ocean,
ertipha-sise' t'nat in determinin- the former, the compressi-
iii-ty of water vapour at the given temperature must be found
I-' -~ ty 0 1 L
"lso the humidi gradient between the surface of -he sea
Can", the m--asurin- point,. Sverdrup (Ref.10, basins his work on
the theory of t=bulent diffusion,confirmed a linear relation-
ship first put forward by V. V. S~_uleykkin. This has been
shivin to .-;-4Lve good results in many cases (Refs.2, 3, 5)~
LI-ing -CA-is relationship, the results obtained in the Atlantic
LD
be e=essed by:
5.85 (e - e )V m.cal/day/cm 2 (2)
W 6 6
-,ere P -lie -Jv -
is the v, -r vapour com,)ressibility at U e__
su_rface tea.,',erature e6 is the coomr.,--ressibility at a heJ_E_,'._:t
of 6 m abo-T;-c- t1le surface (both expressed in millibars); ane
V.- is the wind velocity j_r, m/sec at this hei--Mt. Curvna 5
F~--.G' i ire s the results obtained with this fo-r-ula, As cF't_
be seent Dn sonte days the aiaoimt of Leat lost by evaporation
e.-~ceeded that -,,airied from ~ola:L- radiation, The heat lo2+-
vc-Li-_J'-C fi,Dij 'r:,:30-100 callcr_-.. The loss by evaporation
~'-'Dximately c,)nStant at all !atitudes investi-gated and
2-
L

30V-4
del"end-ld, hasi-cally, upon the wind velocity.
4, Loss in effective radiation,, The n.-~xt factor in
i3 tn- Leat losf, into interplanetary a,.-
p - c
4-
this had to be c lculated from
L -.~ I - - "
in, tor~:Iulae, Ti~!-~ on-e. c'.iosen ,ia--:: due to L'strim (Ref'
--0~069e) -7
qj crT"(0,255 -1 0.322 :r- 10
Using :3ve.-.-,-d.-u-D a r-ra,,,,h (tem.-Oeratu-re of
a
U Z r"i al-~ve nuiaidi-t- as ordinate) (Ro f 4),,
U V S
f nffective radiations
(0~16(1-1 0,19~~-e m.r-E-111-Mitilcm~) suj-,*Iable 11"or in-terpolatioil-,
M, r ':. Tile authors employed th
.-.!~ar Il c-, s e
2
t.-'ar, quant-ity of 11(,:~at lost per cm of
t h A' ic eac-1,- The resultZ are shoan 211 Curve 4-
-,.,a-~! allowed, for bv --L-ae formula.
(4)
CL;aL)
Card

3OV-4- -) - "CS-6-3/12
0 s c iI a_~,D a s heat Balance of the Atlantic Ocea-n.
__1, -o the amount of cloud in upp-eir,
~IH .4) nL corresT)ond t,
"11-
"1e and lx:er layers (in tenths). The values of
d
-:, nd
-hi ~- C are E;ilren by the authors as suggested by N. I.
Yer,orov (R~f.V. The heat loss in effective rad4ation is
Siven in Curv5 5. FiS.6 - it varies between 250 cal and
82 cal/day/cm~. 'As is ex-oected, negative mmccima on this
curve correspond to positive -maxima on Curve 1.
Loss in convective exchange between ocean and atmosDhere.
TI,,~_-.s plays the major part in polar seas, but in middle lati-
tudes, as in the Atlantic, it is relatively small. Much
a,esearch in -this field has been carried out and the most
suitable formula $to use seems to be that of V. S. Samoylenko
(Ref.7): qc = - ty6)V6 m.cal/day/cm 2 (5)
This has been confirmed by the theoretical resea-rches of
P. P. Xuz'min (Ref.8) and A. G. Xolesnilkov (Ref.9). Here
V is the v-,,ind velocity at hei-ht 6 m; is the tempera-
G
U neralure
tu.re of the viater s:='ace and. is -he aJLr tem-
at 6 m. The convective exchange heat loss is given in Fi-.6
Vard 9/12

30V-4 t-)-53-6-3/12
Oscillations in, Heat Balance of the Atlantic Ocear,
,%jurve it varies little from zero. Usuall7
v U h o u Jh
not a-lways,, the air temnerature was lower than the water
teyn,ocratuxe and the greatest heat loss by this mechp-nism
U
ca-aie about when the teraperature difference was greatest and
the velocity highest. Even so the largest value rea.-IhEld
-~ C, C>
65 cal/day/cr,.~~,
6. Overall heat balm-ce. To obtain the overall heat balanc!--
it is Or-ly necessary to add algebraically the Curves 2,
and 6 in FiLr.(':. This Eives Fi-.7. It can be seen that the
balancc durinq -the v,,),7a-e Das predominantly negative
--)osi+:ive val-C. pearj_
r-,.g ononly 18 days ~on 5 of ,-hich Jt
did -rot reach +10 cal/day/cm~-). The negative may-ima are
. u
muc'h biSger than the positive ~largest Pos * tive ~ +-117 cal/
day/=2; lar-est ne-abive, = 566 cal/day/cm The daily
U 0
oscillations are much greater than the variations from
latitude to latitude and from month to month. It is proposed
that Fi,-,.7 can be -aced to glive the teimpeerature distribution
of viater at different depths and at dilpferent times of the
Ca,rd 10/12

SOV-49-58-6-3/12
Oscillations in the Heat Balance of the Atlantic Ocean.
,-.TeaT~ (using the formula due to A. G. Kolesnikov (Ref.10) and
-Ae results of S. V. Dobroklonskiy (Ref.11) and S. G. Bogus-
iavskiy (Ref.12)). The authars divide their results into
tbree headin-s: the first, from 14 - 29 October, with an
0 0
average latitude 37 N; the second, from 30 October to 18
November, with an average latitude 210N; and the lastlofrom
19 November to 8 December, with an average latitude 34 N.
corres onding average heat losses are 116, 53 and 216
y/cm It is interesting to compare these with heat
content observations made at the same time on the Gettysburg
bank ((P = 360321N, X = 11030'W ). 'Rig.8 gives the vertical
temDerature distribution of the water averaged over the day
- Curve 1 for October 22-23 Curve 2 for December 4-5. The
second curve gives a depth k m deeper than the first, owing
to position, but this is unim-oortant since Curve 1 can be
extrapolated. Fig.8 indicates that, for the period October 24-
V
December 4, the average heat loss was 156 cal/cm /day. The
mean heat loss for November was also calculated by taking
0
the arithmetic mean of the e--%cperimental results obtained in
Card 11112

AUTHOR: Shuleykin V.-- -- BOV/49-58-9-14/14
TITLE: G. U. Sverdrup (Commemorative iiote) (Garal'd Ul'rik
Sverdrup. K godovshchine so dnya smerti)
PERIOXCAL: Izvestiya Akademii ,,'auk SSSR, Seriya Geofizicheskaya,
1958, lir 9, PP 1151 - 1152 (USSR)
ABSTRACT: Commemorative note on the occasion of the first anniversary
of the death of this vorwegian scientist.
Card 1/1

AUTHOR: Shuleykin, V.V., Academician (Moscow) SOV-26-58-10-12/51
TITLE: Some of the Research 'Uork of the Oceanographic Ship "Sedov"
(Nekotoryye issledovaniya na okeanograficheskom sudne "Sedov")
PERIODICAL: Priroda, 1958, Nr 10, PP 5o'-67 (USSR)
ABSTRACT: Some of the research rork carried out on board the "Sedov"
during 10.57 in the Atlantic Ocean is described~ The survey
was carried out at the height of the storm season in the
last three months of the year between Africa and South
Anerica, extending from Cape Verde Islands into the Sargasso
Sea. The heijht and behavior of the waves at different parts
of the sea were studied in relation to the intensity of
storms which had occurred. Geomagnetic studies and research
into the extent of magnetic deviation were made in the
latitude of 160 9 where the deviation is particularly great,
The contributions of L.A. Korneva and A.T. Mironov to geo-
magnetic speculations and research are mentioned. The elec-
tric currents in the ocean were charted at various devths
using special electrodes and it was found that their intensity
decreased with a decrease in depth, achieving a minimum in
the surface layers of the ocean. This agreed with the find-
Card 1/3 ings recorded by Yu.G~ Rvzhkov and G.A. Gubin in the Indian

SOV-26-58-10-12/51
Some of the 10'esearch 7ork of the Oceanographic 'ahip "Sedov"
Ocean in 1,056 on board the "0b"'. From this the author con-
cludes that half the additional magnetic field in the At-
lantic is caused by electric currents in the ocean and the
other half by currents in the upper layers of the ionosphere.
The "Sedov" also studied the thermal balance of the ocean
from day to day, recording by automatic devices the izffli;_x
of the solar energy and the amount of heat lost by vaporiza-
tion. The heat losses were found to exceed the heat re-
ceived from the sun during the pre-winter season, and the
thermal balance varied generally between wide limits. The
wind shifts around capes and peninsulas were also studied.
On the principle that there is a connection bet,.-,reen the
length of a fish's body and the maximum speed it can attain,
it was calculated that a shark has a zop speed of 7.7 m1sec,
whereas its pilot-fish have a top speed of only 2 .7 m/sec.
In movement the pilot-fish keep very close to the shark.
It was found that a shark will produce a friction layer of
water around its body as it moves. If the pilot-fish keep
,vithin this layer they will be "towed" by the shark. If
Card 2/3 inadvertently they tend to stray outside it, strong dynamic

.I -
SOV-26-56-10-12/51
Some of the Reoearch 'Nork of the Oceanographic Ship "Sedov"
forces will tend to draw them back again. Thus, pilot-fish
can accompany the shark at speeds well above their top limit.
There are 4 photos, " maps, 4 graphs, and 1 diagram.
1. Oceanography--Atlantic Ocean
Card 3/3

AUTHOR: Shuleykin, V. V., Academician 2o-3-15/59
TITLE: The Development of Sea Waves from Their Initiation to the
Phase of Maximum Steepness (Razvitiye morskilch voln ot
zarozhdeniya do naibol'shey krutizny)
PERIODICAL: Doklady AN SSSR, 1958, Vol- 116, Nr 3, PP- 472-475 (USSR)
ABSTRACT: This work attempts the description of the principle of the
development of waves in the short initial phase, whereon at
present it is impossible to set up a serious theory. This
is prohibited yet at present by the very difficult analysis
of the small waves. The author studied the kinematics of
the big waves in the presence of a drift-current, which has
taken in already a sufficiently thick water stratum. First
a generalized term for the momentum of the acting forces is
written down. The process of calculation is persecuted step
by step. The change of the steepness of the developing wind-
-waves which is found by this way is here illustrated in a
diagram. The observations in the storm-basin of the Navy
Hydrophysical Institute (Morskoy gidrofizicheskiy institut)
Card 1/2 allowed the discovery of an easily stateable partly

-The Development of Sea Waves from Their Initiation to the 20-3-15/59
Fhase of Maximum Steepness
destruction of the wave tops in the second phase of the
wave formation. The effective dependence of the steepness
of the waves on their length must be expressed by a curve
with flattened breaks. As a comparison in a diagram the
effective chan.-e of steepness of wind-waves with advancing
time is copied on the base of photorecordin.- of waves in a
storm basin. The general character of the curve found in
this way agrees well with the theoretical curve. There are
2 figures and 7 references, 6 of which are Slavic.
SUBMITTED: September 2, 1957
AVAILABLE: Library of Congress
Card 2/2

AUTHOR: Shuleykin, V. V.,Member of the Academy 2o-119-2-17/6o
TITLE: Telluric Currents in the Ocean and Magnetic Declination
(Telluricheskiye toki v okeane i maL-nitnoye skloneniye)
PERIODICAL: Dok)-ady Akademii Nauk SSR, 1958, Vol 119, Nr 2,
pr 257 - 26o (USSR)
ABSTRACT: In 1956 Yu. G. Byzhkov and F. A. Gubin (aboard the
Diesel-electric saip Ob?) discovered a strong increase of the
density of telluric currents in the depth of the Indian
ocean. Of special interest is the measuring of the density
of telluric currents at various depths in the Atlantic bet-
ween Africa and 8outh America where the distance between the
two continents is smallest. Theauthors Gould also carry out
these measurements in this region and also north of it in the
course of the oceanographic-geophysical expedition of the
ship "Sedov" in the last quarter of 1957. The electrodes and the
measuring method are shortly described. A completely reliable
registration of the potential differences between the elec-
trodes was possible at a latitude of 170051 north and a lon-
Card 1/3 gitude of 310571 west on November 10, 1957. The gradient was

2o-119-2-17/6o
Telluric Currents in the Ocean and Magnetic Declination
about 30 'Millivolt/km in the surface layer and was directed
alo-Ig the meridian from north to south. Also at a depth of
25om the potential gradient has the direction from north
to south and may be about Bo millivolt/km. At such a value
of the potential gradient the densitiv of current at a
depth of '250m must amount to 3.57.lo-4 A/m2. When the elec-
trodes are simultaneously lifted the potential differences
between them decreases according to a simple linear law. When
the straight is continued to the bottom of the ocean the
values of the gradient for greater depths can be extrapolated
and the magnitude of the whole amperage flowing in the in-
vedtigated region of the Atlantic along the meridian can be
estimated. According to this only about 10 Ampere flow through
a "gate" of 1 m width and 5000 m height. According to the
calculations by L. A. Korneva an ampera,,,e of 1"; aMpereB WOUld
be necessary for the explanation of the actually existing
earth-magnetic field. The lacking part of the magnetic field
Card 2/3 strength is obviously to be referred to the currents in the
J.

2o-119-2-17/6o
Telluric Currents in the Ocean and Magnetic Declination
ionosphere. A registration of the telluric currents in the
depth about just as reliable was made aboard the "Sedov"
on November 24, 1957. The stronE increase of the density of
telluric currents in the depth was also proved by the measure-
ments aboard the "Sedov" and aboard the third expedition ship
(Mikhail Lomonosov). This increase according to the depth has to
be explained in detail by a theory to be constructed. At pre-
sent it can only be maintained that the telluric currents in
the ocean depend on the corpuscular emission of the sun. At
the end the author reports shortly on the formation of the
eddy current in the ocean. The author expresses his gratitude
to P. S. Mitrofanovand V. N. Dol,-opolov for their help in the
experiments aboard the expedition ship "Sedov".There is 1 fi-
gure and 6 Soviet references.
SUBMITTED: Januury 15, 1958
Card 3/3

AUTHORS: Shuleykin, V. V., Member, Academy of Sciences 2o-119-5-24/59
TITLE: How the Pilot Fish Manages to Move With the Same Speed as the
Shark (Kak ryba-lotsman dvizhetsya so skorostlyu akuly)
PERIODICAL: Doklady Akademii Nauk SSSR, 1958, Vol- 119, Nr 5,
pp. 929 - 932 (USSR)
ABSTRACT: The short body of the pilot fish ( Naucrates ductor) in fact
is only little suited for its high speed of motion. The length
of a fish body actually is related to the maximum speed of a
fish, as the author showed in a previous work (Reference 1).
During the stay of the expeditionary vessel "Sedov" at one of
the oceanographic stations in the Atlantic a shark of a length
of 185 cm and a pilot fish of a length of 21 cm were caught.
According to the theoretical curve mentioned in the above
qaoted previous work the maximum speed of the shark had to be
770 cm/see and that of the pilot fish 275 cm/sec. According to
L. A. Kovalevskaya (Reference 2) the continuous speed (on long
distances) probably is about the same percentage of the maximum
speed with all fishes. Therefore the pilot fish accompanying the
shark can not swim in a normal way. A photograph made aboard
Card 1/2 the "Sedov" gives the explanation for this apparent paradoxical

How the Pilot Fish Manages to Move With the Same Speed 2o-119-5-24/59
as the Shark
phenomenon: the pilot fish always move very closely to the body
of the sharks, also when these swim only slowly. The pilot fish
keep within the friction layer directly at the surface of the
body of the shark in the case of high speed; this friction layer
reaches in the case of any moving body its maximum value near
the tail. The anthor then gives an approximate calculation for
the thickness of the boundary layer. When the pilot fiah leaves the
friction zone by chance it is immediately taken back into the
friction zone by the enormous ponderomotoric force of attraction
(which occurs in the motion of two fishes with parallel course
in a potential flow). Based on these considerations also the
accompanying of ships by pilot fish over thousands of miles
becomes clear. According to an information by A. N. Svetovidov
received when this work was revised
'~the pilot fish deposits
its spawn on the skin of the shark or at the bottom part of the
ships. Such functions are possible only in the friction boundary
zone. There are 3 figures and 3 references, 3 of which are Soviet.
SUBMITTED; January 7, 1958
Card 2/2

AUTHOR: Shuleykin, V. V., Member, Academy of 2o-119-6-23/56
3cre-nces, USSR--
TITLE: The Characteristic Parameters of the Wind Wave Field in the
Ocean (Kharakteristicheakiye parametry polya vetrovykh voln v
okeane)
PERIODICAL: Doklady Akademii n.auk SSSR, 1958v Vol. 119, Nr 6,
PP- 1138 - 1141 (USSR)
ABSTRACT: The results of the new measurements of the waves in the ocean
were compared with the results of the experiments in the storm
basin of the AS USSR and allow the characterization oi the field
of the storm waves long after the initial states of their deve-
lopment.The possibility of the determination of the field main
parameters resulted. The transmission of the wind energy to the
waves is characterized by the aerodynamic coefficient5( which
depends on the steepness of the waves:~ - r r/R. r denoting
the radius of the trajectory of the surface particles on the
wave and R the socalled rocking radius. On the other side the
dimensionless coefficient W is present in the term for the li-
miting value r.0 for the storm wave in the ocean on the occasion
Card 1 of a given wind velocity V. The coefficient 1C and the coeffi-

The Characteristic Parameters of the Wind Wave Field 2o-119-6-23/56
in -the Ocean
cient k characterizing the turbulent phenomena in the water
during the wave action are substituted in the complete equa-
tion for the balance of the wind waves in an arbifrary distance
x from the coast at which the wind1lows. The author succeeded
in ascertaining the numerical values of k on the base of the
observation of waves which practically have become steady.Then
the author controls his results on the basis of various nume-
rical data. In first approximation one can expect the formation
of steady waves of the height h - 7,5 m. The _ second appro-
ximation is ascertained. On this occasion the author restricts
on the consideration of the variability of the values of T
and (R/r)2. A diagram illustrates in first approximation the
law of the increase of the waves at the coast the wind blows
at. Even after a long (lasting 2 days) storm the waves did not
become steady yet, i.e. their height could still grow by 0,6 m.
The maximum height of a wave most probably is 7,8 to 8 m. A
better accuracy in the analysis of the wave field and in the
determination of the coefficient k at present cannot be obtained.
Card 2 There are 3 figures and 4 references, 4 of which are Soviet.
-7

30) SOV/20-121-06-14/45
AUTHOR: Shuleyk1A,,,Y,,Y,,., Academician
TITLE: The Exact Integral of the Equation of the Field of the Wind
Waves in the Ocean and Its Physical Meaning (Tochnyy integral
uravneniya Dolya vetrovykh voln v okeane i yego fizicheskoye
znacheniye)
PERIODICAL: Doklady Akademii nauk SSSR, 1958, Vol 121, Ur 6, PP 1005-1008
(USSR)
ABSTRACT: Recent investigations carried out by A. N. Tikhonov and A. A.
o
Sama:cskiy (Ref make it possible to draw the following
conclusion: The exact integral of the equation
a -Y, /a -r = 1 - -q - YL 1/2 a -tj1a5is completely determined by
those exact solutions which previously were deduced by the
anthors for the folloviinp: simple conditions:
a) for the distribution of the height of the steady waves
with respect to t 'he various distances ~ from the windward
shore; b) for the increase of the height ~ of the waves
Card 1/3 during the time -r in which the wind acts in a very great

SOV/20-121-6-14/45
The Exact Integral of the Equation of the Field of the Wind Waves in the
Ocean and Its Physical Meaning
(theoretically infinite) distance from thevtndward shore. A
discontinuity line ~ (.r) must exist in a certain plane of
the rectangular system of the coordinates. On the one side
of this discontinuity line the condition a) and on the other
side - the condition b) is satisfied. The motion of this dis-
continuity 6n the surface of the ocean begins on the wind-
ward shore. The corresponding differential equation was in-
tegrated according to the method of Euler (Eyler)-Cauchy
(Koshi). A second and more exact method of solution is based
on the physical significance of the phenomena. Some proper-
ties of these phenomena are discussea in a few lines. On
the whole, the discontinuity line describes the law
of the progressive jaotion of a cerLi(nT)"front" extending
from the windward shore to the open sea. Behind this front
there is a swell which becomes steadyj- Ahead of this front
the height of the waves increases according to I = 1 - e
The exact solution of the above-given equation is shown by
a figure. The real velocity of the motion of the above-men-
tioned "front" first increases quickly, and continues to
Card' 2/3 increase slowly. Finally, the equation dx/dt = 0,625 c was

SOV/2o-121-6-14/45
The Exact Integral of the Equation of the Field of the Wind Waves in the
Ocean and Its Phjsical Meaning
obtained for the real velocity of the "front". There is
f00 V = c where f00 denotes the ratio of the phase velocity
of the highest waves which are possible for the wind velocity
V to this velocity V itself. The author thanks A. If. Tikhonov
for his useful advice to use the new theory of quasilinear
equations. There are 2 fij.-ures and 8 references, 8 of which
are Soviet.
ASSOCIATION: Moakovskiy :,,osudarstvennyy universitet im. M. V. Lomonosova
(Moscow State University imeni LT. V. Lomonosov)
SUBMITTED: April 2B, 1958
'4
Card 3/.~

3(0)
AUT HOR: Shuleykin, It V Academician SOV120-123-6-15150
TITLEP.- The Steepness of Developing Waves at Various Wind Velocities
(Krutizna razvivayushchikhsya voln pri razlichnykh
skorostlyakh vetra)
HERIODICAL: Doklady Akademii nauk SSSR, 1958, Vol 123, Nr 6, PP 1010-1013
(USSR)
LMRACT: The author first in short discusses some earlier papers dealing
with this subject. Observations carried out on the open sea as
well as in an artificial storm basin showed that, in the case of
one and the same wave length, the steepness of waves increases
with increasing wind velocity. Thus, it may be surmised that the
intermediate stage of wave development with wavelengths -)f from
A2to A0 is of importance only at high wind velocities. A2
denotes a certain short wave length and A a certain wave length
0
value. At lower wind velocities the difference becomes
smaller and at a certain given wind velocity it may also become
equal to zero. If wind velocities are still smaller, the value
Card 1/3 ?(o = ;12 may shift towards shorter wave lengths. The present

The Steepness of Developing Waves at Various Wind BOV/20-1 23-6-15/50
Velocities
paper intends to examine these assumptions and to find a precise
explanation of existing conceptions of the very interesting
intermediate stage of the development of waves with lengths of
~2 to A 0 . Experiments were carried out in the storm basin
of the Morskoy gidrofizicheskiy institut (Ocean-Hydrographical
Institute), and the wave profile was photographed immediately
by means of the "Kiyev" photographic camera. Within the field
of vision of this camera there were electric clocks and an
electric seconds counter, by means of which it was possible to
measure the time corresponding to each photograph taken with an
accuracy of 0.01 sec. The 33 series of photographs were sub-
divided into 3 groups corresponding to the wind velocities
V = 7 1 1 m/sec, V = 11 � I m/sec and V = 15 � I m1sec
Evaluation of the results obtained by these measurements showed
the following: The differences in the steepness of rraves having
the same wave length increase with a decrease of the
corresponding wave length. In the course of the development of
waves up to their extreme dimensions (possible on the ocean at
one or the other wind velocity) this difference diminishes
Card 2/3 constantly and vanishes practically in the later stages of the

The Steepness of Developing Waves at Various Wind SOV/20-123-6-15/50
Velocities
development of waves. The laws for the development of wind
waves found by the present paper are not only of theoretical
but also of great practical interest, for it is easily possible
to improve the technique of correcting measuring scales, which
was described by V. V. Shuleykin (Ref 5) to perfection.
There are 2 figures and 5 Soviet references,
ISSOCIATION: Moskovskiy gosudarstvennyy universitet im. M. V. Lomonosova
(Moscor, State University imeni M. V. Lomonosov)
SUBLITTED: September 19, 1958
Card 3/3

SHULEYKIN, Vasiliy Vladimirovich;. YEGOROV, N.I., otv.red.; GROSMAN, R.V.,
red.; YASN0GORODSrAYA M M., red.; BRAY-NINA. M.I., tekhn.red.;
FLAUM, M.Ya.' tekhn.r;d.*
[Concise course of marine physics] Kratkii kurs fiziki moria.
Leningrad, Gidrometeor.izd-vo, 1959. 477 P. (MIRA 12:8)
(Oceanography)

SHLWTKIN,..Vl3ailiy,,,Vladimirovich, almdemik; FATNBOYM, I.B., red.;
"-" 'SAVC,HENKo, te.y., tekhn.red.
[Research on the physics of oceans and seas] Fizicheskie issle-
dovaniia okeanov i morei. Moskva, Izd-vo *Znanie.0 1960. 39 P.
(Vaesoiuznoe obshchestvo po rasprostrananiiu politicheskikh i nauch-
nykh znanii. Ser.9, Fizika i khimiia, no.18).
(Oceanography) (MIRA 13:10)

SIRMSYKIN, Y.Y.
19~rdrodynamic resonance in summer monsoon streams. Izv.AN
SSSR.Ser.geofis no.6:828-838 Je 160. (MML 13:6)
1. Moskovskly gosndarstvennyy universitet ime M*7.Lomonosovae
(Monsoons)

SHULEYKIN, V.V.
Calculating possible magnitudes of wind waves in the field
of Atlantic hurricanes. Izv.AN SSSR.Ser.geofiz. no-7:
1013-1021 Jl 16o. (MIRA 13:7)
1. Moskovskiy goeudarstvennyy universitet imeni N.Y.
Lomonosova.
(Hurricanes)

SHULMIN, V.V.
Using the equation of the wind wave field for forecasting purposes.
Trudy Okean kom. 9:18-44 160. (MIRA 14:1)
(Waves)

SHMYKIN, V.V-, akademik; XATS, A.L., kand.geograf.nauk; PMSUN, Kh-F.,
prof.; A3TAMKO, F.D., kand.geograf.nauk
Worldle weather. Znan.sila 35 no.8:4-6 Ag 160.
(MIRA 13:9)
(Neteorolou)

686o8
9000 0
S/02Y60/130/05/017/061
AUTHOR: Academician B013 B014
TITLE: Experimental Verification of the Hypothesis Concerning the
Nature of Magnetic Declination
PERIODICAL: Doklady Akademii nauk SSSR, 1960, Vol 130, Nr 5, PP 1015-1017
(USSR)
ABSTRACT: The author describes the experimental verification of his
hypothesis concerning%agnetic declination in the equatorial
and tropical belt of the Plantic. Of special interest is the
region around the point 1 south latitude and 250 west longi-
tude. According to the author's hypothesis, a distorting magne-
tic field is superimposed on the principal magnetic field of
the Earth (with a.moment directed along the axis of rotation
of the planet). The 1_~tter is caused by%lectric currents in
the ocean and also b ,currents of the ionoU21ere (iHIZE-are
directed along the continents). A simple and reliably record-
ing photoelectric instrument was built which allows to take
distinct pictures of the 127-mm mariner's compass (with a course
pointer) and a small timepiece of the type "Moscow". A positive
r
Card 1/3 substandard motion-picture film is used for this purpose. Fo /

68608
Experimental Verification of the Hypothesis S/020/60/130/05/017/061
Concerning the Nature of Magnetic Declination B013/3014
an additional oheck,the compass course was also read from the
magnetic main compass of the ship during the experiments. With
the help of these separate methods.it was found that 0 magnetic
declination at a depth of about 2000 m is at least 5 lower
compared to the ocean surface. It is assumed that declination
is changed there only by:the field of natural earth currents
in the ocean. The latitude component consistsof two quantities,
i.e., quantity y which is caused by currenta. imL-the ocean, and
a certain quantity Y, which is assumed to.be caused by currents
of the ionosphere. Y is probably constant from the.ocean surface
to a depth of about 2000 m. Natural earth.currentz.in..the ocean
thus constitute about one-third of the latitude~_component of
the field strength of the terrestrial magnetic f1eld. It is
therefore possible to assume that the remaining-t-wo.thirds re-
sult from the portion of currents in the ionosph-ere. The latter
--are related to the distribution of oceans and-con-U-nents on
the Earth. The principal theoretical considers-tions of the
author were confirmed by the experimental results under discus-
sion. The problem to be solved next is the refinement of meth-
Card 2/3 ode for the recording of magnetic declination in the depth of

68608
Experimental Verification of the Hypothesis S/020/60/130/05/017/061
Concerning the Nature of Magnetic Declination B013/BO14
the ocean. It would also be necessary to investigate the part
played by currents in the ionosphere in the development of the
latitude component of the terrestrial magnetic field. The author
thanks the Soviet Navy for their assistance in investigations
on board the expedition ship "Sedov". He further thanks B. R.
Lazarenko and Ye. S. Borisevich for their assistance in Yhe -con-
struction of ajTp-aratusq A. V. Lik-edemonskiy for his supervision
of the melting of a bronze container, and L. F. Vereshchagin
and A. A. Semirchan for testing the container at the Insti
vysokikh davleniy AN SSSR (Institute of High Pressures of the
AS USSR) and for the very careful sealing of flanges. L. A.
Kornev is also mentioned in this paper. There are 3 figures
Soviet references.
SUBMITTED: December 3, 1959
Card 3/3

SEUIXfKIN, V.V., akademik .1
More about wind currents in the sea. Dokl. AN SSSR 134 no.6:1343-
1346 0 160. (MIRA 13:10)
(ocean currents)

21h9h
S/020J61/137/004/018/031
3J/60 (loyl,p-LI) B104/B206
AUTHOR: Shuleykin, V.-V.,Icademician
TITLE: Some peculiarities of the secular changes of the magnetic
field above the ocean
PERIODICAL: Doklady Akademii nauk SSSR, v. 137, no. 4, 1961, 848-851
TEXT: The secular changes of the geomagnetic field can be studied with
the aid of records on the magnetic deviations. In Fig. 1, the magnetic
deviations in Paris (2), London (1) and Rome (3) are graphically shown on
the basis of records dating back to the sixteenth century. Accurate
analyses show that to a purely sinusoidal change of the magnetic deviation,
a weak second harmonic is superimposed. The constant deviations in these
places are: -6.60 (London), -6.00 (Paris) and -2.80 (Rome). On-the basis
of known data, Fleming (Terrestrial Magnetism and-Electricity, 1949, P. 15)
constructed for the latitudes 400N, 00 and 400, deviations for different
longitudes. In a similar manner, the author~constructed the changes of
the deviations in the given time interval (Figi 2). These results are
transferred to the map shown in Fig- 3. The shaded part shows the magnetic
Card 113

131494
S/020/61/137/004/018/031
Some peculiarities of the secular... B104/B206
declinations. For the three latitudes, the full lines give&,the changes
of the mean deviations for the different longitudes, the t;Tee dotted
lines give the changes of the deviation amplitudes. From the further
discussion of the results, in which the author also refers to Bullard et
al (Phil. Trans. Roy. Soc. London. A, 247, 213 (1954)), he concludes the
following: 1) If the electromagnetic field of the Bullard "eddies"
interacts with the low-conductive earth's crust and produces a drift of
the convection cells, this type of interaction with the better conductive
ocean must be considerdd all the more. 2) The dotted lines in Fig. 3
prove an interaction of the electromagnetic field of the cells with the
water. 3) Likewise, the constant deviation above the water is greater
than above the continents, which is also taken as proof for the author's
hypothesis on the decisive role of the oceans in the-formation of the
geomagnetic field- 4) The author concludes that the Bullard convection
cells produce the basic geomagnetic field, the axis of which coincides
with the axis of the rotation of the earth. 5) The interaction of the
electromagnetic field of the cells with the highly conductive water of the
ocean produces "eddies" of the currents in the ocean around the continents.
6) It is possible that the interact ion of the electromagnetic cells with
Card 2

S/020/61/137/004/018/031
Some peculiarities of the secular... B104/B206
the waters of the individual oceans produces in them constant currents,
to which eddy currents are superimposed, which are produced in the ocean
during magnetic storm.' There are 3 figures and 10. references:
8 Soviet-bloc and 2 non-Soviet-bloc.
SUBMITTED: January 11, 1960
0
ISOO 16M \17M 18W
10-
U,
ILI
Card VA