VARIATIONS OF THE SOLID EARTHS CENTER OF MASS DUE TO OCEANIC TIDES

被引:4
作者
BROSCHE, P
WUNSCH, J
机构
[1] Sternwarte der Universität Bonn, Bonn, 5300
关键词
EARTH OCEANS; CENTER OF MASS; TIDES;
D O I
10.1002/asna.2113140206
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Periodic variations in the location of the center of mass of the solid Earth due to ocean tides are derived from the ocean tide model of Seiler (1991). The sum of nine partial tides leads to changes in the coordinates X, Y, Z within a range of 1 cm.
引用
收藏
页码:87 / 90
页数:4
相关论文
共 4 条
[1]  
BROSCHE P, 1982, TIDAL FRICTION EARTH, V2, P175
[2]  
MCCARTHY DD, 1989, IERS3 TECHN NOT
[3]   PERIODIC CHANGES OF THE ANGULAR-MOMENTUM BUDGET DUE TO THE TIDES OF THE WORLD OCEAN [J].
SEILER, U .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1991, 96 (B6) :10287-10300
[4]  
SEILER U, 1989, 29 U HAMB I MEER MIT, P101