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Spatio-temporal variability of drought over northern China and its relationships with Indian-Pacific sea surface temperatures

机译:中国北方干旱的时空变化及其与印度太平洋海表温度的关系

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Monthly precipitation data from 66 rain gauge stations in northern China are analyzed for the period 1976-2011. Variations in droughts and wet spells are described using the standardized precipitation index (SPI). Empirical orthogonal functions and a global wavelet spectral analysis are applied to capture modes of spatio-temporal variability in droughts over northern China. Time series of monthly sea surface temperatures (SST) and the Multivariate El Nino Southern Oscillation Index (MEI) are presented, and cross wavelet and wavelet coherence transforms are carried out to investigate possible mechanisms behind variations in droughts and wet spells. From 1976 onwards, the northern parts of northern China have experienced an increase in the frequency of droughts, while the southern parts of northern China have experienced a decrease in the frequency of droughts. The north-south variability of droughts and wet spells is characterized by interannual timescales of 3.3 years and 7.0-11.0 years. The former timescale is closely related with the MEI, while the latter is closely related with sea surface temperature anomalies (SSTA) over the North Pacific. Most parts of northern China experienced an increase in the frequency of droughts during the periods 1980-2000 and 2004-present, and a decrease in the frequency of droughts during the period 2000-2004. The variability of drought in northern China peaks at timescales of 16.0-32.0 and 3.5-4.0 years. The first of these timescales shows a significant correlation with SSTA over the Indian Ocean. The eastern parts of northern China have experienced a decrease in the frequency of droughts since 1976, while the western parts of northern China have experienced an increase in the frequency of droughts. The east-west variability of droughts and wet spells is characterized by interannual timescales of 3.3-8.0 years, which are related with SSTA over the Indian Ocean warm pool.
机译:分析了中国北方66个雨量计站1976-2011年的月降水量数据。使用标准化降水指数(SPI)来描述干旱和湿季的变化。应用经验正交函数和全局小波谱分析来捕获中国北方干旱时空变化的模式。给出了每月海表温度(SST)和多变量厄尔尼诺南方涛动指数(MEI)的时间序列,并进行了交叉小波和小波相干变换,以研究干旱和湿季变化背后的可能机制。从1976年开始,中国北方的干旱频率增加,而中国北方的干旱频率减少。干旱和湿气季节的南北变化特征是3.3年和7.0-11.0年的年际时标。前者与MEI密切相关,而后者与北太平洋海表温度异常(SSTA)密切相关。在1980-2000年和2004年至今,中国北方大部分地区的干旱频率增加,而在2000-2004年期间,干旱频率减少。中国北方干旱的变异性在16.0-32.0年和3.5-4.0年的时间尺度上达到峰值。这些时标中的第一个显示与印度洋上SSTA的显着相关。自1976年以来,中国北部的东部地区干旱频率有所下降,而中国北部的西部地区干旱频率却有所增加。干旱和湿气季节的东西向变化特征是3.3-8.0年的年际时标,这与印度洋暖池上的SSTA有关。

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