Turbulent eddies play a critical role in oceanic flows. Direct measurements of turbulent eddy fluxes beneath thesea surface were taken to study the direction of
Monsoon driven water mass exchange between the Bay of Bengal (BoB) and Arabian Sea (AS) is the commonexperience. However, it is not yet firmly confirmed that th
Sea-surface acoustic backscattering measurements at moderate to high frequencies were performed in theshallow water of the south Yellow Sea, using omnidirection