摘要
本文利用地球辐射平衡试验(ERBE)和国际卫星云气候计划 (ISCCP)提供的地气系统长波射出辐射(OLR)和云量资料,计算并讨论了我国各 季和年平均云量对地气系统OLR的强迫及其所产生的温室效应。结果表明:我国 各季的 OLR云强迫与总云量、高云量都有较好的相关,且季节变化明显;OLR云 强迫和云温室效应的地理分布受云量和云状的影响较大,它们的年变化一般呈弱 双峰型,峰值在春、夏季出现。
Based on the data of the earth-atmosphere system outgoing longwave radia- tion (OLR) and cloud amount provided by ERBE and ISCCP,the seasonal and annual aver- aged outgoing longwave cloud-atmosphere system in China are investigated. Results show that an obvious correlation exists between the total and high cloudcover and the LWCRF,re- spectively, which has obvious seasonal variations. The geographical distribution of the LWCRF and the clouds greenhouse effect are more affected by cloudcover and cloud types. In general,the annual variation of LWCRF show weak double peak forms,whose peak values are in spring and summer.
出处
《气象科学》
CSCD
北大核心
2001年第1期1-8,共8页
Journal of the Meteorological Sciences
基金
国家攀登B计划项目"青藏高原试验"研究成果