Abstract The Indian Ocean presents two distinct climate regimes. The north Indian Ocean is
dominated by the monsoons, whereas the seasonal reversal is less pronounced in the …

In the coastal ocean zones, satellite altimetry data processing and interpretation poses
specific difficulties, due to the interaction of the radar signal with land topography …

Rivers worldwide are now acting as major transport pathways for plastic pollution and
discharge large quantities of waste into the ocean. Previous oceanographic modelling and …

In response to the Indian Monsoon freshwater forcing, the Bay of Bengal exhibits a very
strong seasonal cycle in sea surface salinity (SSS), especially near the mouths of the …

In this study, we analysed decadal and long-term steric sea level variations over 1966–2007
period in the Indo-Pacific sector, using an ocean general circulation model forced by …

The North Indian Ocean is a very special ocean. It is not connected to the poles, it is tropical,
it has very strong seasonal forcing, with the total reversal of winds and dramatic current …

Monsoon rain and rivers bring large freshwater input to the Northern Bay of Bengal (BoB),
yielding low Sea Surface Salinity (SSS) after the monsoon. The resulting sharp upper-ocean …

Sri Lanka occupies a unique location within the equatorial belt in the northern Indian Ocean,
with the Arabian Sea on its western side and the Bay of Bengal on its eastern side, and …

Time series measurements of temperature and salinity recorded at 8° N, 90° E in the south
central Bay of Bengal from a Research Moored Array for African‐Asian‐Australian Monsoon …

Salinity in the Bay of Bengal is highly heterogeneous, with extremely fresh waters found at
the surface in the Northern part of the basin, and saltier waters at subsurface as well as to …