Global Sea Floor Topography from Satellite Altimetry and Ship Depth Soundings
- ISSN: 00368075
- DOI: 10.1126/science.277.5334.1956
- PubMed: 2893884
Abstract
A digital bathymetric map of the oceans with a horizontal resolution of 1 to 12 kilometers was derived by combining available depth soundings with high-resolution marine gravity information from the Geosat and ERS-1 spacecraft. Previous global bathymetric maps lacked features such as the 1600-kilometer-long Foundation Seamounts chain in the South Pacific. This map shows relations among the distributions of depth, sea floor area, and sea floor age that do not fit the predictions of deterministic models of subsidence due to lithosphere cooling but may be explained by a stochastic model in which randomly distributed reheating events warm the lithosphere and raise the ocean floor.
Global Sea Floor Topography from Satellite Altimetry and Ship Depth Soundings
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26 October 1996; accepted 28 May 1997
RESEARCH ARTICLE
Global Sea Floor Topography
from Satellite Altimetry and
Ship Depth Soundings
Walter H. F. Smith* and David T. Sandwell
A digital bathymetric map of the oceans with a horizontal resolution of 1 to 12 kilometers
was derived by combining available depth soundings with high-resolution marine gravity
information from the Geosat and ERS-1 spacecraft. Previous global bathymetric maps
lacked features such as the 1600-kilometer-long Foundation Seamounts chain in the
South Pacific. This map shows relations among the distributions of depth, sea floor area,
and sea floor age that do not fit the predictions of deterministic models of subsidence
due to lithosphere cooling but may be explained by a stochastic model in which randomly
distributed reheating events warm the lithosphere and raise the ocean floor.
Knowledge of ocean floor topography data
is essential for understanding physical
oceanography, marine biology, chemistry,
and geology. Currents, tides, mixing, and
upwelling of nutrient-rich water are all in-
fluenced by topography. Seamounts may be
particularly important in mixing and tidal
dissipation (1), and deep water fisheries on
seamount flanks have become economically
significant (2). Seamounts, oceanic pla-
teaus, and other geologic structures associ-
ated with intraplate volcanism, plate
boundary processes, and the cooling and
subsidence of the oceanic lithosphere
should all be manifest in accurate bathy-
metric maps.
Conventional sea floor mapping is a te-
dious process. Ships have measured depth
with single-beam echo sounders since the
W. H. F. Smith is at the National Oceanic and Atmospher-
ic Administration, Code E/OC-2, 1315 East-West High-
way, Silver Spring, MD 20910–3282, USA.
D. T. Sandwell is at the Scripps Institution of Oceanogra-
phy, La Jolla, CA 92093, USA.
*To whom correspondence should be addressed. E-mail:
walter@amos.grdl.noaa.gov
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