摘要
A two-dimensional numerical model,which is configured on the basis of Princeton ocean model(POM),is used to study the effect of Stokes production(SP) of the turbulent kinetic energy on a density profile and Ekman transport in an idealized shelf region in summer.The energy input from SP is parameterized and included into the Mellor-Yamada turbulence closure submodel.Results reveal that the intensity of wind-driven upwelling fronts near the sea surface is weakened by the SP-associated turbulent kinetic energy input.The vertical eddy viscosity coefficient in the surface boundary layer is enhanced greatly owing to the impact of SP,which decreases the alongshore velocity and changes the distribution of upwelling.In addition,the SP-induced mixing easily suppresses the strong stratification and significantly increases the depth of the upper mixed layer(ML) under strong winds.
A two-dimensional numerical model,which is configured on the basis of Princeton ocean model(POM),is used to study the effect of Stokes production(SP) of the turbulent kinetic energy on a density profile and Ekman transport in an idealized shelf region in summer.The energy input from SP is parameterized and included into the Mellor-Yamada turbulence closure submodel.Results reveal that the intensity of wind-driven upwelling fronts near the sea surface is weakened by the SP-associated turbulent kinetic energy input.The vertical eddy viscosity coefficient in the surface boundary layer is enhanced greatly owing to the impact of SP,which decreases the alongshore velocity and changes the distribution of upwelling.In addition,the SP-induced mixing easily suppresses the strong stratification and significantly increases the depth of the upper mixed layer(ML) under strong winds.
基金
The National Basic Research Program of China under contract No.2013CB430304
the National Natural Science Foundation of China under contract Nos 41030854
41106005
41176003 and 41206178
the National Science and Technology Support Program of China under contract No.2011BAC03B02-01