1.
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。
2.
The Indian summer monsoon starts in the 32nd pentad (5～10 th of June) and ends in the 49 th pentad (1～5 th of September).
印度季风 6月第 2候建立 ,比南海热带季风晚约 4候 ,持续至 9月第 1候
3.
The characteristics of the Indian monsoon:Evidences from the sedimentary records of Tengchong and Shangri-La over the past 60 ka
从腾冲和香格里拉沉积记录看60ka BP以来的印度季风活动特征
4.
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
5.
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
6.
On The Optimal Eastboud Route Across the North Indian Ocean During Southwest Monsoon
北印度洋西南季风期东行最佳航线论证
7.
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
8.
Seeks: Explodes a gap the Himalaya Mountains to let the Indian Ocean warm wet monsoon blow the Qinghai-Tibet Plain.
牟：把喜马拉雅山炸个缺口让印度洋暖湿季风吹进青藏高原。
9.
UPWELLING ACTIONS IN THE BAY OF BENGAL DURING MARINE ISOTOPE STAGES 2 AND 3: EVIDENCE FOR INDIAN WINTER MONSOON
孟加拉湾深海氧同位素2、3期上升流活动——北印度洋冬季风的实证
10.
(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。
11.
Monsoon rains and poor drainage enable the disease to thrive in many Indian cities.
季风降雨以及排水不畅，使得这种疾病仍在印度的许多城市中肆虐。
12.
Interdecadal Variability of Indian Ocean Monsoon Circulation and Its Relation to Atmosphere Circulation;
印度洋季风环流年代际变化及其与大气环流的关系
13.
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
14.
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
15.
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
16.
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。
17.
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
18.
The Impacts of the Dominating Modes of the SST Interannual Variation in the Tropical Indian Ocean on the Atmospheric Circulation in the Asian Monsoon Region;
热带印度洋海表面温度年际变化主模态对亚洲季风区大气环流的影响