Seasonal cycle of sea level and currents along the coast of India

被引：2
|
作者：
Shankar, D [1 ]
机构：
[1] Natl Inst Oceanog, Dona Paula 403004, Goa, India
来源：
CURRENT SCIENCE | 2000年 / 78卷 / 03期
关键词：
D O I：
暂无
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
A framework involving long baroclinic waves, which treats the north Indian Ocean as a single dynamical entity, has been remarkably successful in simulating the low-frequency, large-scale circulation in the ocean. It is, however, unable to simulate the observed seasonal, cycle of sea level along the Indian coast. The reason appears to be the absence of salinity variation in these models. The large inflow of freshwater into the:seas around India forces large changes in salinity, and hence, in coastal sea level.
引用
收藏
页码：279 / 288
页数：10
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