1) basin-wide SSTA variation in the tropical Indian Ocean
热带印度洋全区一致型海温变化
3) the tropical Pacific-Indian Ocean temperature anomaly mode
热带太平洋-印度洋海温异常综合模
4) Indian Ocean SST
印度洋海温
1.
The Teleconnection Characteristics between the Precipitation on the East Side of Tibetan Plateau and Indian Ocean SST;
青藏高原东侧降水与印度洋海温的遥相关特征
2.
Effect of Indian Ocean SSTA on China Temperature Anomaly;
印度洋海温异常与中国气温异常的可能联系
3.
Datasets including precipitation of 35 observational stations of the east side of Tibetan Plateau and the Indian Ocean SST during 50 years(1951-2000) have been used to analysis their teleconnection characteristics by using SVD method.
选取高原东侧近50年(1951-2000)35个观测站降水和同期印度洋海温资料,运用SVD分析方法讨论了其同期与印度洋海温的遥相关关系。
5) Indian Ocean surface temperature
印度洋海温
1.
With the calulation method of Chebyshev Polynomials in irregular grids and stepwise regression,a system of forecast equations between the Indian Ocean surface temperature and the rainfall of rainy season in Yunnan with precipitation anomaly value in Yunnan is set up.
利用不规则格点上的车贝雪夫多项式及逐步回归的计算方法，用云南省降水距平资料建立印度洋海温场与云南省雨季降水场的预报方程，并做了１９９６ 年及１９９７ 年雨季降水预报检验，效果较理想。
6) the South China Sea (SCS)-Eastern Tropical Indian Ocean
南海-热带东印度洋
1.
Numerical experiments based on a low resolution AGCM were developed to investigate the influence of SSTA over the South China Sea (SCS)-Eastern Tropical Indian Ocean on the South China Sea summer Monsoon (SCSM).
用低阶大气环流谱模式就前期冬春季南海-热带东印度洋(10 oN～15 oS, 90～120 o E) 海温异常对南海夏季风的影响进行了数值试验。
补充资料：热带
1.赤道两侧南回归线和北回归线之间的地带称"热带"，也叫"回归带"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条