DETERMINATION OF THE OCEAN CIRCULATION USING GEOSAT ALTIMETRY

被引：57

作者：

NEREM, RS ^{[1
]}

TAPLEY, BD ^{[1
]}

SHUM, CK ^{[1
]}

机构：

[1] UNIV TEXAS, CTR SPACE RES, AUSTIN, TX 78712 USA

来源：

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS | 1990年 / 95卷 / C3期

关键词：

D O I：

10.1029/JC095iC03p03163

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

A spherical harmonic model of the sea surface topography complete to degree and order 10 and a model of the Earth's geopotential field complete to degree and order 50 have been obtained in a simultaneous solution using Geosat altimeter data and tracking data from 14 different satellites. The sea surface topography model compares well with oceanographic models computed using hydrographic data and ship drift data. Error analysis indicates that the correlation between the geoid and the sea surface topography model is less than 0.2, indicating good separation of the geoid and the sea surface topography at wavelengths of 4000 km or longer. -from Authors

引用

页码：3163 / +

共 66 条

[1] AN EMPIRICAL DETERMINATION OF THE EFFECTS OF SEA STATE BIAS ON SEASAT ALTIMETRY [J].