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Association between the Dynamics of Indian OceanSubtropical High and Winter Time Precipitation andStream Flow: A Case Study Over Acheron RiverCatchment, Victoria

机译:印度洋副热带高压与冬季降水与河流流量之间的联系:以维多利亚州阿彻龙河流域为例

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In this study, we explore the relationships between winter (May-August) Acheron River catchment (ARC), Victoria, Australia, rainfall and streamflow and winter Indian Ocean Subtropical High Pressure (IOSHPS) and Indian Ocean Subtropical High Longitude (IOSHLN) through correlation and regression analysis. Analysis is performed for the period of 1951-2011. It is found that the correlation of IOSHPS with winter ARC rainfall and streamflow are -0.46 and -0.33 respectively and IOSHLN are -0.54 and -0.57 are observed. Dynamics (zonal movements) of IOSHPS analysis showed that east-west shifts of IOSHPS are responsible for the variable amounts of rainfall receive in the ARC that resulted in variable streamflow. Regression analysis suggested IOSH indices describe 38% and 36% variability in rainfall (May-August) and streamflow (May-August) over ARC respectively further investigations showed that southern oscillation index (SOI) and El-Nino southern oscillation (ENSO) have weak association independently as well as combination with IOSHLN than IOSH indices over ARC winter rainfall and streamflow.
机译:在这项研究中,我们通过相关性探索了冬季(5月至8月)阿彻龙河流域(ARC),澳大利亚维多利亚,降雨和流量以及冬季印度洋亚热带高压(IOSHPS)和印度洋亚热带高经度(IOSHLN)之间的关系。和回归分析。对1951-2011年进行了分析。发现IOSHPS与冬季ARC降水和流量的相关性分别为-0.46和-0.33,而IOSHLN的相关性为-0.54和-0.57。 IOSHPS分析的动力学(区域运动)表明,IOSHPS的东西向移动是导致ARC接收到的降雨量变化的原因,从而导致水流的变化。回归分析表明,IOSH指数分别描述了ARC上降雨(5月至8月)和水流(5月至8月)的38%和36%的变化,进一步的研究表明,南方涛动指数(SOI)和El-Nino南方涛动(ENSO)较弱在ARC冬季降雨和水流方面,与IOSHLN的相关性独立,也与IOSHLN的组合高于IOSH的指数。

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