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- 热带西太平洋SSTthe tropical western SST
- 热带西太平洋对风应力的斜压响应THE BAROCLINIC RESPONSE OF WEST TROPICAL PACIFIC TO WIND STRESS
- 热带西太平洋海温距平与Rossby波传播对1993和1994年东亚夏季风异常影响的差异Differences of Influences of Tropical Western Pacific SST Anomaly and Rossby Wave Propagation on East Asian Monsoon in the Summers of 1993 and 1994
- 西west
- 热带西太平洋大气气候基本态与厄尔尼诺期间赤道附近西风异常The role of atmosphere climate basic state in the formation of westerly over the equatorial Pacific
- 赤道东太平洋SST的海-气振子模型Sea-air oscillator model for equatorial eastern Pacific SST
- 西的western
- 赤道东太平洋SST强增温过程特征分析THE FEATURE ANALYSES OF THE SST STRONG INCREASE PROCESSES IN THE EQUATORAL EASTERN PACIFIC
- 副热带西风带subtropical westerlies
- 副热带圈和赤道太平洋SST的海-气振子模型Sea-air oscillator model in subtropical cells and equatorial Pacific SST
- 中纬度北太平洋SST异常与大气环流的关系MIDLATITUDE NORTH PACIFIC SST ANOMALY IN RELATION TO ATMOSPHERIC CIRCULATIONS
- 沿南美洲副热带西海岸的海岸低压:平均结构和演变Coastal Lows along the Subtropical West Coast of South America: Mean Structure and Evolution
- 北及赤道东太平洋SST近半个世纪的长期变化The SST Variations in North and Eastern Equatorial Pacific from 1951 to 1997
- 山东夏季降水与北太平洋SST和大气环流的关系Relationship among Summer Rainfall in Shandong and North Pacific SST and Atmospheric Circulations
- 西太平洋Lamont海山中新世以来富钴结壳成矿环境的演化Evolution of Ore-forming Condition of Co-rich Crusts From Lamont Guyot in the Western Pacific Since the Miocene
- SST暖异常愈强,引起的降水、高低空越赤道气流、北半球副热带西风气流、扰动西侧的反Walker环流及高层东风异常和扰动东侧的顺Walker环流以及高层西风异常也愈强。The greater the SST warm anomaly is, the more intense are the resulting precipitation, the cross equatorial upper and low level streams, the westerlies in the northern hemisphere subtropics, the anti-Walker circulation on the west side of the disturbance and the anomalous upper-level easterlies, and the usual Walker circulation on the east side and the anomalous upper-level westerlies.
- 2002年西太平洋地球物理会议--固体地球物理部分研究进展2002 Western Pacific Geophysical Meeting-- Progress of the Researches on the Solid Earth Physics
- 西太平洋麦哲伦海山铁锰结壳生物地层、生长年代及沉积环境Biostratigraphy, Growth Period and Sedimentary Environment of Ferromanganese Crusts From Magellan Seamounts in the Western Pacific
- 夏季北太平洋SST的主要异常型为赤道东太平洋型(EEP),阿拉斯加湾型(BAL),热带中太平洋(CTP),以及北部北太平洋型(NNP)。The major spatial patterns of the summer time SSTA over the North Pacific are the eastern equatorial Pacific (EEP), the Bay of Alaska (BAL), the central tropical Pacific (CTP), and the northern North Pacific (NNP) patterns.
- 热带西太平洋western tropical Pacific