-5e-2-1/30
0,
1
AUTHORSr .,,.Kvsy-uk, G.A., Galf tsoTf- L.P. IverorLcva M.I., lies' halleryakovT
Yu*A#
TITLEt. At the XIt4 General Assembi-Y in Toronto of the International Union
of- (;eodday and. Geophysies (IUCKO"Na XI general: noy assambleye
mezhdunarodnogo soyuza f@,eoaezii i geoftz;iki (IUGG) v Toronto)
PERIDDICALt Izvestiya Akademii nauk SSSR Seriya geograficheskayal 1956,
Nr 21 pp 3-8 (USSR)
ABSTRACT t The XIth General Assembly of the International Uhimof Geodesy
ancI._Geqj9Wsics-,ccnvmecI in Tom-tor from 3. to 14- Ileptember.
1957. The USSR was representedby a delegation consisting of
54 scientists heale& by Academician I.P..Bard!-n. The Soviet
geographers G.A. Avayuk, A.P. Ga;C9tsovj M,I, Iveronova and Yu.A.
Meshcheryakov participated for the first time! in a meating of the
Union. The conference was divideclinto various. sections dealing
with special- fields. The conference hear& the! following Savie/-
:raportas The Geodesiats M.S. MolodenskiY7 A-A- Izoto7, Yv-.D.
Bulanzhe :a6a, M.I. Sinyagina OR-79e--aMhievements of Soviet
science in the.geodesy, V.7. Belous*v, V.A. Wagnitskiy, Ye.A.
L@-ubimolvaj : V.I. Keylis-Borok.and. Yu.V. Rezrichenkc on seismo-
logical problems.and questioaa concerning the physical structure
card 1/3 of the Earthla deposits; G.A. Avsyuk on glacial research work
10-58-2-1/30
At the x1th General Assembly In Tozoato of@thq,jmternjtjonaj Union of Geo&sy
and, GeqpWsias _(IUGG)
carried out in the USSR; A.M. Obukhov a 0..
nd A.$ iin on meters
logical questions, especially diffusion and convection. Special
attention was paid to the reports@of the Sovi.et scientists R.I.
Sinyaginays, and Yu.A. Meshch6ryakov on the study of present
movements of
-theSarth.crust in the European part of the USSR.
N.I..Budyko dealt with the distribut@on of the
components of the
thermal balance of the Earthis surface. Thieci report met with'
especially great interest since only:the USSR has succeeded in
preparing monthly charts on the components of' the thermal balance
all over the worli, and what is even more important, in solving
the problem of.determining the evaporation taking place or. the
surface of dry laA'd. Ye.P. Tolstik explorer of polar regions
reported on Soviet research -in the Arctic and Antarctic Zones
within the Internati oniLl -Geophysical Year. Ine to the Soviet
achievements in all these fields of science V.V. Belouso@,: Corm-
Card 2/3 Ocndi4 Member of: the ASOSSR j was elected Vice-President of 4- 11 e
Turkinat if. 1. Candidate of
Technical Sciences,
TITLE:' Answerine@,Lettsra tolth6 Editor
na, voprogy,ohitateley)
PERIODICAL: _Geocteziys i Kartografi-at 19589 1Tr 3, P@. 71-72 (USSR)
ABBTRAGT:, question: in the article by W. I. Yurkina uThe Theory of the Earth's
Shape:iri Foreign Gountries" in ... Teo(ieziya i Kartografiyaj
Hr 7 the method of the analytical continuation of
the gravity anomalies, Isuggested by- A. K. Valovichko, was
not illustrated..
Answert in paragraph 11 of-the book by jjj@_ S. Moloclenskiy
"The Fundamental Problems of Geodetical
("Trudy TsNIIGAiK Mr. 42, 1945) it was prove& that
according to the measurements performed at the earth's
surface it is not possible to determine the elements of
the inner gravitational field. The values of gravity
within the attractive mass cannot be determined either
without using the data on the distribution of density
card 1/2 within the earth. The content of this paragraph entirely
Answering Letters to the Editor 6-58-3-12/16
disproves the considerations made by A. K. ifalovichko
on the possibility of a. determination of the geoict. A
detailed analysis of thia'methoct was given in the article
by 7. A. Kiazivanor (1956). Here,: too, the way for the
determination of the gdoicl, as suggested by malovichko,
is refuted. The proof by iiolo&enskiy and the conclusion
by Kuzivanov are here illustrated with the aid of an
example. There are 1 figure and 2 references, which
are Soviet.
AVAILABLEx Library ofCongreas
1. Gravity--Determination
ff olodens' n @Hemb er Academy of Nciences,
Correupondi
SR
TIT !Z', Present-Day in the, Doteri-An!:Aion of the 'Jincpe alf the
Earth. Sovrer"GnIly-'e zadachi izuehenlya figury Zcm1i)
i kIrtorraff-yal
195a, Yr T, PP., 3-5 053R)
AB5TRACT, -l'ilelps Concerning the investigation of global shepe and
tize extorna. gra,@ritatlonal field of the earth are inseparabl@r
ch uther. Th-ree ra.ngce.of problems carl be
ea
11S't!@,tic geodes-y". which is c nfiried to
t@ia @,,_.-nuhint_oa of mc-e and more accurare and detailed "re-
@-da- -pe of the globe and of
c . i on z o@ tqs prezent sh@_
e nelic geodeny", whicl.-L 'Ll
P"i'aV-LTc;t_iOh&1 f!
@he alteratl-ons. of the Ehv@pe of the globa
o f' t C: ;-r a v i t a t i o n a 1 f i e 1 d - 3j jy n am i c; e, -a o d e, Sy h i c h
dculs: v@ith the causes for 1!i-c-se alteratioau Ln,1 @:,ith th@@
explun;7,tion of the obuerved nrlomulies of Krr..mitation by the
partieulkiir features of.the at -ucture and of ac: developmen',
Card of t1w earth's crust of thze earth as
YA%rtb
xe.-, @m t - rob lem j r,
_C
a,7CkL, 8,tC. L
_Ur f U t r
tne
z.-ravin'--f tric map C'f @',Tc 11*,;`,;@
i t
e 11 f -n LZ n, e, .1 1@ c@ o@, r, t,
0 plumb, lin@ V-_
a f@ ron om, a 1 o r. c t h,--. 7: i ob @,rises ;a-," I., r@ 7 to intornrete
m e t r c @t I d t 3 t r,)n om c f maaasn-, nirnt, t.jn the
re
V.,
advantae:e of or. I!,!r in," ividual coints are
to be d@termzlned Irl tth@ pl,-mn, i_iin6@ m@,,zst di-1-c +1- be obtained,
But tiLen tile t@rf@vimatr_icr-i Lmethod :,ill @%=Iit to -UrIterpolate
Une plumib 7@ qevi@t4r;n.,2 -.-,-;,.h hijh @-ccl=c@,-. "-'hua t'.,e ram@-om
c
erro-- in 'ha astronomical t1i,2
catlon of indivIduad Pcjint5 u- n be covr.@ctc-d. 2) in thi@
odi-icatJon of the i@n@4a' o' the ce:itri';;,- 1 f-c-
case a m
must be tuL-en into. account . @3 omc t lmen -it iS al-zo receszzz@v
to tak- int. 0 ConZ:.4 derat_,'on the mod-ification of the attrac"Icr,
of external masces and of the. te-j (CI-le
to polc shl' v." t Three et@se cla ought to be that inguishc-Ci
are di scu _,;oed , A f:@,-? @luec i& I