Horizontal Flux of Biogenic elements through PN Section in April 1994

摘要

The horizontal flux of biogenic elements through PN section in April 1994 was calculated in the present paper using output of the OPYC model, which is a very gener- al global model solving the full primitive equation forced by the atmospheric wind stress, observed heat flux, freshwater flux and cloudiness including a sea ice model both poles with rheology. However, since it is a global model, its resolution is rather coarse, less than 1°× 1°horizontally and only 1 layer on continental shelf and 7 layers in the Okinawa Trough.