摘要
该项目受到国家自然科学基金项目和国家基础研究发展规划项目的资助。最新研究成果揭示中国东部舂季土壤湿度与夏季降水有联系。春季,从长江中下游到华北的土壤偏湿,对应着中国夏季东北和长江流域降水偏多,华北和南方降水偏少。
This project is supported by the National Natural Science Foundation of China and the Key Projects of National Basic Theoretical Research. The latest findings reveal that there is significant relationship between spring soil moisture and summer precipitation in the eastern China. The more precipitation in Northeast China and the lower reaches of the Yangtze River and less rainfall over the southern China and North China can be seen when there is a positive anomaly in spring soil moisture over North China and the lower reaches of the Yangtze River (NCYR).