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首页> 外文期刊>Hydrology and Earth System Sciences >Modelling of monsoon rainfall for a mesoscale catchment in North-West India I: Assessment of objective circulation patterns
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Modelling of monsoon rainfall for a mesoscale catchment in North-West India I: Assessment of objective circulation patterns

机译:印度西北中尺度流域季风降雨的模拟I:客观循环模式的评估

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摘要

Within the present study we shed light on the question whether objective circulation patterns (CP) classified from either the 500 HPa or the 700 HPa level may serve as predictors to explain the spatio-temporal variability of monsoon rainfall in the Anas catchment in North West India. To this end we employ a fuzzy ruled based classification approach in combination with a novel objective function as originally proposed by (Stehlik and Brdossy, 2002). After the optimisation we compare the obtained circulation classification schemes for the two pressure levels with respect to their conditional rainfall probabilities and amounts. The classification scheme for the 500 HPa level turns out to be much more suitable to separate dry from wet meteorological conditions during the monsoon season. As is shown during a bootstrap test, the CP conditional rainfall probabilities for the wet and the dry CPs for both pressure levels are highly significant at levels ranging from 95 to 99%. Furthermore, the monthly CP frequencies of the wettest CPs show a significant positive correlation with the variation of the total number of rainy days at the monthly scale. Consistently, the monthly frequencies of the dry CPs exhibit a negative correlation with the number of rainy days at the monthly scale. The present results give clear evidence that the circulation patterns from the 500 HPa level are suitable predictors for explaining spatio- temporal Monsoon variability. A companion paper shows that the CP time series obtained within this study are suitable input into a stochastical rainfall model.
机译:在本研究中,我们阐明了一个问题,即从500 HPa或700 HPa水平分类的客观循环模式(CP)是否可以作为解释印度西北部阿纳斯流域季风降雨时空变化的预测因子。 。为此,我们采用了基于模糊规则的分类方法,并结合了由(Stehlik和Brdossy,2002)最初提出的新目标函数。优化之后,我们比较了两个压力水平的获得的循环分类方案的条件降雨概率和数量。事实证明,对于500 HPa的分类方案,更适合于在季风季节将干气象条件与干气象条件分开。如自举测试中所示,两种压力水平的湿CP和干CP的CP条件降雨概率在95%到99%的范围内都非常显着。此外,最湿CP的每月CP频率与每月尺度上雨天总数的变化呈显着正相关。一致地,干CP的月度频率与月度尺度上的雨天数呈负相关。目前的结果提供了明确的证据,表明500 HPa水平的循环模式是解释时空季风变化的合适预测因子。伴随文件显示,在这项研究中获得的CP时间序列适合作为随机降雨模型的输入。

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