We examine the mean pathways, transit timescales, and transformation of waters flowing
from the Pacific and the marginal seas through the Indian Ocean (IO) on their way toward the …

At suboxic oxygen concentrations, key biogeochemical cycles change and denitrification
becomes the dominant remineralization pathway. Earth system models predict oxygen loss …

Abstract In the Arabian Sea, mesoscale eddies are prominent features of the circulation.
They influence biological activities, tracer transport, and physical and chemical properties of …

Abstract The Persian Gulf feeds a warm and salty outflow in the Gulf of Oman (northern
Arabian Sea). The salt climatological distribution is relatively smooth in the Gulf of Oman …

Changing climatic conditions can shape the strength and extent of the oxygen minimum
zone (OMZ). The presence and variability of the OMZ in the Arabian Sea is of importance to …

The Persian Gulf produces high-salinity water (Persian Gulf Water, PGW hereafter), which
flows into the Sea of Oman via the Strait of Hormuz. Beyond the Strait of Hormuz, the PGW …

Abstract Persian Gulf Water and Red Sea Water are salty and dense waters flowing at
intermediate depths in the Gulf of Oman and the Gulf of Aden, respectively. Their spreading …

We investigate the stability of a composite cyclone representative of Arabian Sea eddies
using a high resolution primitive equation model. We observe that the eddy is unstable with …

Submesoscale coherent vortices (SCVs) are numerous in high‐resolution numerical
simulations, but their observations are scarce. Among the few in situ available …

Coupling a three-dimensional ocean circulation model to an atmospheric model can
significantly improve forecasting of tropical cyclones (TCs). This is particularly true of …