摘要
本文用正压模式计算了大尺度湍流输送项对高度倾向的影响,用的是1956年2月13—22日的资料.在这例子中涡度的湍流输送的项作用与平均输送项大小量级相同.这两项所造成的高度倾向分布颇不相同,并不成简单的此例关系.
A computation of height tendency due to large-scale eddy term is made for a ten-day period Feb.13—22,1956,using barotropic model.It is shown that the contribution due to the eddy transport term■is comparable to that due to the mean transport term■.The distribution of the height tendency due to the eddy term is rather different from that due to the mean transport term and thus they are not connected by any simple relation of proportionality.
作者
顾震潮
KOO CHEN-CHAO(Institute of Geophysics and Meteorology,Academia Sinica)
出处
《气象学报》
1959年第2期191-194,共4页
Acta Meteorologica Sinica
