As the phytoplanktons consume carbon dioxide, they significantly influence the global
carbon cycle and thus, the global temperature by modifying sea surface temperature …

Using a one‐dimensional turbulent closure model, we investigate the physical mechanisms
governing the seasonal evolution of mixed‐layer depth (MLD) and sea surface temperature …

The west coast of India and the adjoining eastern Arabian Sea (EAS) is one of the high
rainfall zones of Indian summer monsoon. The summer monsoon rainfall in this region is …

Though the deep mixed layers (MLs) that form in the northeastern Arabian Sea (NEAS)
during the winter monsoon (November–February) have been attributed to convective mixing …

The time series of temperature, salinity, chlorophyll-a, particle scattering at 700nm, and
dissolved oxygen obtained from Argo floats deployed in the southeastern Arabian Sea (AS) …

The high-salinity water masses that originate in the North Indian Ocean are Arabian Sea
High-Salinity Water (ASHSW), Persian Gulf Water (PGW), and Red Sea Water (RSW) …

With unprecedented rate of development in the countries surrounding the gulfs of the
Arabian Sea, there has been a rapid warming of these gulfs. In this regard, using Advanced …

The formation mechanisms of the barrier layer (BL) and its seasonal variability in the
Arabian Sea (AS) are studied using a comprehensive dataset of temperature and salinity …

The intense winter phytoplankton bloom during November–February in the northeastern
Arabian Sea (NEAS) was thought, until recently, to be controlled only by a convective …

The Shallow Overturning Circulation in the Indian Ocean in: Journal of Physical Oceanography
Volume 48 Issue 2 (2018) Jump to Content Jump to Main Navigation Logo Logo Logo Logo …