Now showing items 1-4 of 4
Living planktonic foraminifera during the late summer monsoon period in the Arabian Sea
During the late summer monsoon living planktonic foraminifera were collected in the southeastern Arabian Sea between 3~'N and 15~'N by using six vertical plankton tows. Sixteen species of planktonic foraminifera were ...
Increased particle flux to the deep ocean related to monsoons
(Nature Publishing Group, 1989)
Monsoons cause seasonal reversals in the surface circulation of the northern Indian Ocean. In the Arabian Sea this results in the upwelling of nutrient-rich water along the coasts, making it one of the highly productive ...
Coupling between SW monsoon-related surface and deep ocean processes as discerned from continuous particle flux measurements and correlated satellite data
(American Geophysical Union, 1996)
Particle flux data obtained by time series sediment traps deployed at water depths of approximately 3000 m in the western, central, and eastern Arabian Sea since 1986 were compared with wind speeds derived from measurements ...
A comparative study of vertical stabilities in the Arabian sea and Bay of Bengal
(India Meteorological Department, 1981)
Stabilities in the upper 300 m in the Arabian Sea and the Bay of Bengal are computed and presented seasonwise. The water column in the Bay of Bengal is more strongly stratified than that in the Arabian Sea. These studies ...