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。
The analysis of 43-year NCEP-NCAR reanalysis data and the station observations reveals the correlation between troposphere temperature variations and the weakening of the Indian summer monsoon circulation.
对43aNCEP/NCAR再分析资料和台站实际观测资料的分析,揭示了对流层温度变化和印度夏季风环流减弱之间的联系。
The interdecadal variation of Indian summer monsoon and the climate shift in North China are analyzed by using of NCEP-NCAR reanalysis data and the stations observations.
利用NCEP/NCAR再分析资料及台站实测资料分析了近几十年印度夏季风的年代际变化特征及我国北方所发生的气候变化,揭示了印度夏季风的减弱与我国北方地区的气候演变具有密切的联系。
Thus, the series of Indian summer monsoon rainfall of the regions mentioned above could be extrapola.
东绒布冰芯净积累量的相对变化幅度大于印度夏季风降水量的变化,表明高海拔地区的降水比低海拔地区具有更高的敏感性。
The Interannual Variability of the Onset of SCS and Indian Summer Monsoon;
南海夏季风与印度夏季风爆发的年际异常
Interannual Variation of Differences in Onset Dates between South China Sea and Indian Summer Monsoons
南海夏季风与印度夏季风爆发早晚的年际差异
RELATIONS BETWEEN EL NINO, INDIAN SUMMER MONSOON AND THE SUMMER RAINFALL IN NORTHERN CHINA
埃尔-尼诺和印度夏季风与我国北方6～9月降水
(3) Influenced by the onset of the Indian summer monsoon, the second jump is found on Pentad 31.3. The onset of the vigorous convection over Indochina Peninsula and its adjacent areas is of very importance to the onset of the Indian summer monsoon.
(3)受印度夏季风爆发影响第二次北跳在第31候发生。
WIND AND TEMPERATURE CHANGES OVER EURASIA DURING THE ACTIVE, BREAK AND WITHDRAWAL TIME PERIODS OF THE INDIAN SUMMER MONSOON OF 1979
1979年印度夏季风活跃、中断和撤退时期欧亚上空风场和温度场的变化
Simulated Structural Changes of Asian Summer Monsoon Circulation in Association with Indian Ocean Dipole SSTAs
亚洲夏季风环流结构与热带印度洋偶极型海温异常
The Indo-Pacific Ocean warm pool and the South China Sea summer monsoon onset
太平洋—印度洋暖池次表层水温与南海夏季风爆发
Possible Impacts of the Tropical Indian Ocean SST Anomaly Modes on the South China Sea Summer Monsoon Onset
热带印度洋海温异常不同模态对南海夏季风爆发的可能影响
Compare with South China Sea, the interseasonal variability of equatorial eastern Indian summer monsoon is more typical than that of SCS in SCS strong summer monsoon years.
相比之下,在南海强夏季风年,赤道东印度洋的季节内振荡比南海的更具典型性。
Relationships between Rainfall Anomalies in Xinjiang Summer and Indian Rainfall
夏季新疆降水异常与印度降水的关系
The Correlation between East Asia Summer Monsoon and Spring Soil-Moisture over China;
中国春季土壤湿度与东亚夏季风的关系
Interannual Variabilities of the Meridional Circulation of East Asian Summer Monsoon and the Atmospheric Response to the SSTA in Indian Ocean;
东亚夏季风经圈环流年际变化与大气对印度洋偶极型海温强迫的响应
Role of Western Pacific Ocean-Indian Ocean-Tibetan Plateau Climate System in the South China Sea Summer Monsoon;
西太平洋—印度洋—青藏高原气候系统在南海夏季风爆发过程中的作用
UPPER OCEAN HYDROGRAPHIC PROPERTIES OF SOUTHEAST INDIAN OCEAN IN AUSTRAL SUMMER, 2003
2003年夏季东南印度洋上层海洋的水文特征
Indian Ocean SSTA influence on atmosphere probable precipitation in northwest China
印度洋SSTA对西北夏季空中可降水量的影响研究
India monsoon and south sea of China monsoon had positive effect on the rainy season onset time in Yunnan.
印度季风与南海季风对云南雨季开始爆发也起着积极的作用。
Experts say environmental degradation, such as deforestation and environmental pollution, will likely magnify the impacts of climate change.
去年，一场冬季寒流和夏季热浪夺走了印度两千多人的生命。
INFLUENCE STUDY ON SPRING INDIAN OCEAN SSTA TO SUMMER EXTREME PRECIPITATION EVENTS OVER THE EASTERN PART OF NORTHWEST CHINA
春季印度洋SSTA对夏季中国西北东部极端降水事件的影响研究