해무의 발생 및 발달 과정에 미치는 대기-해양 상호작용의 효과

Abstract

Advection and steam fogs over the Yellow Sea are examined with the goal of better understanding its formation and persistence using the mesoscale coupled atmosphere/ocean model. The decrease in the wind speed results in a weakening of turbulence and wind stress. The weakened wind stress limits a decrease of turbulent mixing in the ocean, which increases the SST. The effect of air-sea interaction changes or maintains the atmospheric stability by the variability of air-sea temperature difference and wind speed, which determines the duration and dissipation time of sea fog.