Altimetry, ship gravimetry, and the general circulation of the North Atlantic

Gravity accelerations estimated from satellite altimetric mean sea surfaces (Seasat and Geos-3) are compared to ship gravity measurements. Ship gravity are closer to an estimate based on least squares collocation, orbit perturbations, altimetry and terrestrial gravity than to an estimate based on Fo...

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Main Authors: Zlotnicki, Victor, Marsh, James G.
Format: Other/Unknown Material
Language:unknown
Published: 1989
Subjects:
48
Online Access:http://ntrs.nasa.gov/search.jsp?R=19890066148
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19890066148 2023-05-15T17:27:57+02:00 Altimetry, ship gravimetry, and the general circulation of the North Atlantic Zlotnicki, Victor Marsh, James G. Unclassified, Unlimited, Publicly available Sep 1, 1989 http://ntrs.nasa.gov/search.jsp?R=19890066148 unknown http://ntrs.nasa.gov/search.jsp?R=19890066148 Accession ID: 89A53519 Copyright Other Sources 48 Geophysical Research Letters; 16; 1011-101 1989 ftnasantrs 2012-02-15T18:07:55Z Gravity accelerations estimated from satellite altimetric mean sea surfaces (Seasat and Geos-3) are compared to ship gravity measurements. Ship gravity are closer to an estimate based on least squares collocation, orbit perturbations, altimetry and terrestrial gravity than to an estimate based on Fourier transforms, orbit perturbations and altimetry only. Both altimetric estimates yield a smoothed picture of the geostrophic component of sea surface currents in the North Atlantic when gravity acceleration data from only nine cruises are subtracted from the altimetric gravity. Other/Unknown Material North Atlantic NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic 48
spellingShingle 48
Zlotnicki, Victor
Marsh, James G.
Altimetry, ship gravimetry, and the general circulation of the North Atlantic
topic_facet 48
description Gravity accelerations estimated from satellite altimetric mean sea surfaces (Seasat and Geos-3) are compared to ship gravity measurements. Ship gravity are closer to an estimate based on least squares collocation, orbit perturbations, altimetry and terrestrial gravity than to an estimate based on Fourier transforms, orbit perturbations and altimetry only. Both altimetric estimates yield a smoothed picture of the geostrophic component of sea surface currents in the North Atlantic when gravity acceleration data from only nine cruises are subtracted from the altimetric gravity.
format Other/Unknown Material
author Zlotnicki, Victor
Marsh, James G.
author_facet Zlotnicki, Victor
Marsh, James G.
author_sort Zlotnicki, Victor
title Altimetry, ship gravimetry, and the general circulation of the North Atlantic
title_short Altimetry, ship gravimetry, and the general circulation of the North Atlantic
title_full Altimetry, ship gravimetry, and the general circulation of the North Atlantic
title_fullStr Altimetry, ship gravimetry, and the general circulation of the North Atlantic
title_full_unstemmed Altimetry, ship gravimetry, and the general circulation of the North Atlantic
title_sort altimetry, ship gravimetry, and the general circulation of the north atlantic
publishDate 1989
url http://ntrs.nasa.gov/search.jsp?R=19890066148
op_coverage Unclassified, Unlimited, Publicly available
genre North Atlantic
genre_facet North Atlantic
op_source Other Sources
op_relation http://ntrs.nasa.gov/search.jsp?R=19890066148
Accession ID: 89A53519
op_rights Copyright
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