Category: eBooks

Study of Dynamics of Upper High Salinity Water Mass in the Arabian Sea

The water masses of specific characteristics are formed in different regions of the oceans by the processes occurring at the surface of the oceans due to the ocean-atmosphere interactions at specific locations and sink from the surface to subsurface depths. The water mass distribution is controlled by temperature and salinity. The Arabian Sea is an active region of air-sea interaction processes and plays a major role in driving the monsoon system.