Oceanic contribution to the poleward heat flux in the climate system includes two components: the sensible heat flux and the latent heat flux. Although the late
'Mode Water', as a product of air-sea interaction, influences the thermal structure and circulation pattern in npper layer ocean and consequently affect
To ensure the effectiveness of the operation of artificial precipitation enhancement, a potential region for the operation should be determined in advance.As cl
Almost half of the oceanic water columns exhibit double-diffusion. The importance of double-diffusion in global oceans' salt and heat fluxes, water-mass for
Floc breakup dynamics are studied by a sediment transport numerical model in an idealized tidal estuary that has a constant water depth and rapid flocculation o