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卧龙降水稳定同位素与季风活动的关系 被引量:20
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作者 徐振 刘玉虹 +4 位作者 王中生 崔军 徐庆 安树青 刘世荣 《环境科学》 EI CAS CSCD 北大核心 2008年第4期1007-1013,共7页
2003-07-2004-07在四川卧龙自然保护区对逐次降水事件进行采样,分析了降水的稳定同位素特征及其与降水量、气温和风向风速等气象参数的关系.结果表明,4-8月降水的过量氘(d-excess)值为(8.4±7.4)‰,降水由东亚季风带来的大洋水... 2003-07-2004-07在四川卧龙自然保护区对逐次降水事件进行采样,分析了降水的稳定同位素特征及其与降水量、气温和风向风速等气象参数的关系.结果表明,4-8月降水的过量氘(d-excess)值为(8.4±7.4)‰,降水由东亚季风带来的大洋水汽主导;9-10月降水的d-excess值为(-7.4±12.5)‰,降水由南亚季风带来的经过强烈分馏作用的大洋水汽主导;11月-次年3月降水的d-excess值为(12.5±12.1)‰,降水由本地蒸发水汽以及西风环流带来的内陆蒸发水汽主导.季风期降水的δD和δ^18O具降水量效应(r分别为-0.389、-0.380,p〈0.05),次一级是气温影响(p≤0.10).季风期降水的δD、δ^18O与南风指数呈显著负相关(r分别为-0.354、-0.390,p〈0.05),表明降水中的稳定同位素比率对水汽来源与运输过程指示性很强,特别是南亚季风的暴发带来了稳定同位素比率和d-excess值都极低的降水. 展开更多
关键词 降水 氢、氧稳定同位素 过量氘 季风 南风指数 卧龙自然保护区
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Annual and Interannual Variability of Scatterometer Ocean Surface Wind over the South China Sea 被引量:1
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作者 ZHANG Guosheng XU Qing +3 位作者 GONG Zheng CHENG Yongcun WANG Lei JI Qiyan 《Journal of Ocean University of China》 SCIE CAS 2014年第2期191-197,共7页
To investigate the annual and interaunual variability of ocean surface wind over the South China Sea (SCS), the vector empirical orthogonal function (VEOF) method and the Hilbert-Huang transform (HHT) method wer... To investigate the annual and interaunual variability of ocean surface wind over the South China Sea (SCS), the vector empirical orthogonal function (VEOF) method and the Hilbert-Huang transform (HHT) method were employed to analyze a set of combined satellite scatterometer wind data during the period from December 1992 to October 2009. The merged wind data were generated from European Remote Sensing Satellite (ERS)-1/2 Scatterometer, NASA Scatterometer (NSCAT) and NASA's Quick Scatterometer (QuikSCAT) wind products. The first VEOF mode corresponds to a winter-summer mode which accounts for 87.3% of the total variance and represents the East Asian monsoon features. The second mode of VEOF corresponds to a spring-autumn oscil- lation which accounts for 8.3% of the total variance. To analyze the interannual variability, the annual signal was removed from the wind data set and the VEOFs of the residuals were calculated. The temporal mode of the ftrst intcrannual VEOF is correlated with the Southern Oscillation Index (SOI) with a four-month lag. The second temporal interannual VEOF mode is correlated with the SOI with no time lag. The time series of the two interannual VEOFs were decomposed using the HI-IT method and the results also show a correlation between the interannual variability and El Nino-Southern Oscillation (ENSO) events. 展开更多
关键词 ocean surface wind annual and interannual variability SCATTEROMETER South China Sea
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