Further dynamic analysis reveals the dynamic mechanism for the late occurrence of ASM precipitation in Indian monsoon area and the abrupt occurrence of Indian summer monsoon onset.
通过进一步的诊断,揭示了亚洲夏季风降水在印度季风区出现较晚以及印度夏季风爆发的动力机制。
The Asian summer monsoon trough consists of two major components: the South China Sea (SCS) summer monsoon trough and the Indian summer monsoon trough.
亚洲夏季风槽包括两大重要组成部分,即南海夏季风槽和印度夏季风槽。
He Lifu, Wu Bingyi, Mao Weixing. 2005. The interdecadal variation of Indian summer monsoon and the climate shift in North China [J]. Journal of Tropical Meteorology, 21 (3) : 257-264.
何立富,武炳义,毛卫星。2005。印度夏季风的年代际变化与我国北方的气候跃变[J]。热带气象学报,21 (3):257- 264。
DPV is an objectively and quantificationally indicator, hence an useful climate diagnosis tool to diagnose seasonal transition and the Indian summer monsoon onset.
该变差度可客观定量的诊断季节变化和夏季风建立的时间,是一个好用的气候诊断工具。
Stalagmite record revealed that Indian summer monsoon moved forward rapidly, and climate undulation on a century scale resulted in the change of the solar radiation.
石笋记录揭示印度季风的快速推进或退出(萎缩)以及百年尺度上的气候波动是太阳辐射量变化造成的结果。