摘要
利用5个全球大气海洋海冰模式,模拟了大气中二氧化碳浓度的增加对我国冬季与夏季地面气温、降水率及土壤湿度的影响。结果表明,由于温室效应,我国冬、夏季气温增暖,降水率与土壤湿度也有明显变化。
The changes of the surface air temperature, preeipitation rate and soil moisture in winter and summer seasons in China induced hy doubled CO2 as simulated by five atmospheric GGM /mixed-layor ncean(with ice)madels are. shown.It is clemostrated from five simulations that the temperature is going up in China and precipitation and soil moisture are changing somewhere clue to the green house than the present time.
出处
《气象》
CSCD
北大核心
1989年第3期10-14,共5页
Meteorological Monthly
