摘要
采用 OL R表达方式讨论了 1 998年 7月西太平洋副热带高压明显南落的原因。并指出这种表达方式有助于探讨副热带高压南侧热带对流云团对副热带高压的影响。
The cause of the southward withdraw of the west Pacific subtropical high in July 1998 was discussed by using of the OLR formula.It suggests that this OLR method describing daily behavior of the west Pacific subtropical high is favorable for exploring the effect of strong tropical convective cloud cluster on the subtropical high.
出处
《气象》
CSCD
北大核心
2000年第8期6-9,共4页
Meteorological Monthly
基金
973课题资助
关键词
西太平洋副热带高压
OLR
热带对流云团
west Pacific subtropical high OLR tropical convective cloud cluster
