极地研究 ›› 1992, Vol. 3 ›› Issue (1-English): 25-30.
Ma Yimin
Ma Yimin
摘要:
A new simulation method for solving dynamic equations for stationary katabatic wind is suggested by the assumption that the turbulent exchange coefficient is a function of height and the effect of the cold sloping surface is a multinomial function of height. Calculated wind profiles agree with observational data at Mizuho Station, Antarctica.