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Synchronous Characteristics of Precipitation Extremes in the Yangtze and Murray-Darling River Basins and the Role of ENSO

机译:长江和默里 - 达令河流域降水极端的同步特性及enso的作用

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摘要

The floods caused by the extreme precipitation in the Yangtze River basin (YRB) and Murray-Darling River basin (MDRB), the largest basins in China and Australia, have significant impacts on the society and regional economies. Based on the spatial-temporal analysis of the daily precipitation extremes (DPEs) during 1982-2016, we found that for both basins, the whole-basin-type DPEs have the highest proportion and a synchronous DPE interannual variation characteristic exists in the two basins, with the 3-yr running correlation coefficient of the annual DPE days (DPEDs) reaching almost 0.7 (significant at the 0.01 level). The El Nino-Southern Oscillation (ENSO), which is one of the most significant climate disturbance factors in the world, plays an important role in modulating the variability of the DPEs in the two basins. Singular value decomposition (SVD) analysis revealed that both the YRB and the MDRB's whole-basin-type DPEs are closely coupled with the procedure that the preceding winter eastern Pacific (EP)-type El Nino faded to a central Pacific (CP)-type La Nina. This means that the DPEs in the YRB and MDRB may synchronously occur more frequently when the above process occurs. Owing to the atmosphere-ocean interaction from the east-west dipole sea surface temperature (SST) anomaly pattern, the atmospheric circulation disturbance exhibits a pattern in which the equatorial eastern Pacific region is a mass source anomaly with a higher pressure, drier air, and weaker convection, while the equatorial western Pacific region is a mass sink anomaly with a lower pressure, wetter air, and stronger convection. Moreover, two wave trains that originated from the tropical western Pacific were found to extend to the YRB and MDRB. The interaction between the wave train's interphase dynamics and water vapor transport disturbance results in the ascent conditions and enhanced water vapor transport, which leads to the synchronous occurrence of DPEs in the YRB and MDRB on an interannual scale.
机译:长江流域(YRB)和澳大利亚最大的盆地极端降水引起的洪水,是中国和澳大利亚最大的盆地,对社会和区域经济有重大影响。在1982 - 2016年期间,基于日常降水极值(DPES)的空间 - 时间分析,我们发现对于两个盆地,整个盆型DPE具有最高比例,并且两个盆地中存在同步DPE续变性特性,随着年度DPE天(DPEDS)的3-YR运行相关系数达到近0.7(0.01级显着)。 El Nino-Southern振荡(ENSO)是世界上最重要的气候障碍因素之一,在调制两个盆地中DPE的可变性方面发挥着重要作用。奇异值分解(SVD)分析显示,YRB和MDRB的整个盆型DPE都与前冬季东部太平洋(EP) - 型El Nino褪色为中心(CP)型 - 型--Type的程序密切联系La Nina。这意味着当发生上述过程时,YRB和MDRB中的DPE可以更频繁地发生。由于从东西海偶极海面温度(SST)异常模式的大气 - 海洋互动,大气循环干扰呈现了一种模式,其中赤道东太平洋地区是具有更高压力,干燥空气的质量异常异常对流较弱,而赤道西太平洋地区是一个较低压力,潮湿的空气和更强对流的质量水槽异常。此外,发现了来自热带西太平洋的两次波动列车延伸到YRB和MDRB。波动列车的相互作用和水蒸气运输干扰之间的相互作用导致上升条件和增强的水蒸气运输,这导致YRB和MDRB中的DPE同步发生在际规模上。

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  • 来源
    《Oceanographic Literature Review》 |2021年第6期|1218-1218|共1页
  • 作者

    Y. Gong; T. Jiang; B. Su;

  • 作者单位

    State Key Laboratory of Desert and Oasis Ecology Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences Urumqi 830011 China;

    State Key Laboratory of Desert and Oasis Ecology Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences Urumqi 830011 China;

    State Key Laboratory of Desert and Oasis Ecology Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences Urumqi 830011 China;

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