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Record #180394:

Regional geoid improvement based on surface gravity data / W. Korth, R. Dietrich, G. Reitmayr, V. Damm.

Title: Regional geoid improvement based on surface gravity data / W. Korth, R. Dietrich, G. Reitmayr, V. Damm.
Author(s): Korth, W.
Dietrich, R.
Reitmayr, G.
Damm, V.
Date: 1998.
Publisher: Berlin: Springer
In: Geodesy on the move; gravity, geoid, geodynamics and Antarctica : IAG Scientific Assembly, Rio de Janeiro, Brazil, September 3-9, 1997. (1998.),
Abstract: Computes geoid model for region around Schirmacher Oasis, Antarctica, applying point mass model for disturbing potential T. Absolute level of geoid was verified through comparison with ellipsoidal height of mean sea level determined by tide gauge measurements and GPS. Undulations are rather strong, varying between 13 m and 24 m mainly in North-South direction. East-west striking conspicuous minimum is located around 71°S. Values increase rapidly towards polar plateau in south, with almost circular maximum between 12°E and 14°E.
Notes:

In: Geodesy on the move; gravity, geoid, geodynamics and Antarctica : IAG Scientific Assembly, Rio de Janeiro, Brazil, September 3-9, 1997 / Rene Forsberg, Martine Feissel, Reinhard Dietrich, Convenors and editors.

Keywords: 528 -- Geodesy.
528.223 -- Gravity measurements of geoid.
A -- Geophysical sciences (general).
(*7) -- Antarctic regions.
(*73) -- Dronning Maud Land.
(*733) -- Prinsesse Astrid Kyste.
SPRI record no.: 180394

MARCXML

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035 ## ‡aSPRI-180394
040 ## ‡aUkCU-P‡beng‡eaacr
245 00 ‡aRegional geoid improvement based on surface gravity data /‡cW. Korth, R. Dietrich, G. Reitmayr, V. Damm.
260 ## ‡aBerlin :‡bSpringer,‡c1998.
300 ## ‡ap. 523-528 :‡bill., diags.
500 ## ‡aIn: Geodesy on the move; gravity, geoid, geodynamics and Antarctica : IAG Scientific Assembly, Rio de Janeiro, Brazil, September 3-9, 1997 / Rene Forsberg, Martine Feissel, Reinhard Dietrich, Convenors and editors.
520 3# ‡aComputes geoid model for region around Schirmacher Oasis, Antarctica, applying point mass model for disturbing potential T. Absolute level of geoid was verified through comparison with ellipsoidal height of mean sea level determined by tide gauge measurements and GPS. Undulations are rather strong, varying between 13 m and 24 m mainly in North-South direction. East-west striking conspicuous minimum is located around 71°S. Values increase rapidly towards polar plateau in south, with almost circular maximum between 12°E and 14°E.
650 07 ‡a528 -- Geodesy.‡2udc
650 07 ‡a528.223 -- Gravity measurements of geoid.‡2udc
650 07 ‡aA -- Geophysical sciences (general).‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*73) -- Dronning Maud Land.‡2udc
651 #7 ‡a(*733) -- Prinsesse Astrid Kyste.‡2udc
700 1# ‡aKorth, W.
700 1# ‡aDietrich, R.
700 1# ‡aReitmayr, G.
700 1# ‡aDamm, V.
773 0# ‡7nnam ‡aRene Forsberg, Martine Feissel, Reinhard Dietrich, Convenors and editors. ‡tGeodesy on the move; gravity, geoid, geodynamics and Antarctica : IAG Scientific Assembly, Rio de Janeiro, Brazil, September 3-9, 1997. ‡dBerlin : Springer, 1998. ‡wSPRI-168474
916 ## ‡aHS
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221003 ‡bHS