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Quantifying Indian Ocean Subtropical High-runoff Relationships a Case Study over Campaspe River

机译:量化印度洋副热带高压径流关系-以坎帕斯佩河为例

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El-Nino Southern Oscillation (ENSO) is one of the factors that widely studied with respect to the variability in rainfall and streamflow. However, there are other factors which also influence the climate variability and patterns of the circulation. This study aims to investigate linkage between Indian Ocean High pressure indices and South Pacific high indices with the Campaspe River streamflow. It was found that the zonal movements of the high-pressure system of South Pacific and Indian Ocean largely affect the flow in the river. A regression model was constructed with Indian Ocean high pressure indices and South Pacific indices that explain 42% of the variability in the flow of the River. A Mann Kendall’s tau test was also applied in order to assess the trends in the data. A significant decreasing trend in the streamflow is correlated with the increasing trend in the Indian Ocean high pressure system.
机译:El-Nino南方涛动(ENSO)是关于降雨和流量变化的广泛研究的因素之一。但是,还有其他因素也会影响气候的可变性和循环模式。本研究旨在调查印度洋高压指数和南太平洋高压指数与坎帕斯佩河水流之间的联系。研究发现,南太平洋和印度洋高压系统的地带运动极大地影响了河流的流量。使用印度洋高压指数和南太平洋指数构建了回归模型,该模型解释了河流流量变化的42%。为了评估数据趋势,还应用了Mann Kendall的tau测试。径流的显着下降趋势与印度洋高压系统的上升趋势相关。

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