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Analytical Study of Monsoon Rainfall South Mahanadi Delta and Chilika Lagoon, Odisha

机译:奥马萨南马哈纳迪三角洲和奇利卡泻湖季风降雨的分析研究

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The rainfall has become anomalous today along Odisha coast, India. The southern distributaries, Daya and Bhargovi in Mahanadi delta join the sea via Chilika lagoon. The lagoon stands variations in geomorphology, ecology and biodiversity for changes in precipitation and threshold flushing flow. The abnormal rainfall has caused high floods during 2001, 2003, 2006, 2008, 2011 and 2014. Year 2000 was the minimum discharge year of the millennium. Chilika Lagoon, largest in Asia receives 61% of inland flow from Mahanadi system. The tourist, flora and aqua catch decreased remarkably 1995-2000 for lagoon?s reduced salinity, siltation and biodiversity. As engineering intervention, a new inlet dredged, few barrages and cuts constructed upstream in the river system. The anomaly in monsoon precipitation has trimmed down the threshold flushing flow to maintain salinity. Hence frequency analysis and prediction of rainfall at a desired recurrence interval became univocal. As post studies of hydrology to the engineering interferences, the frequency analysis of rainfall has been done after verifying the outliers, goodness of fit with handful recorded data. A suitable probability distribution pattern has been selected and PDF function used to predict monsoon rainfall against various recurrence periods. Out of L-moment, PWM methods available, Log Pearson type III method is found the best and realistic for rainfall analysis. Attempt has been made in this paper to predict annual monsoon rainfall of the delta and lagoon for 10000 years at different return periods.
机译:今天,印度奥里萨邦沿海的降雨已变得异常。 Mahanadi三角洲的南部分水厂Daya和Bhargovi经由Chilika泻湖而入海。泻湖的地貌,生态和生物多样性因降水和阈值冲洗流量的变化而变化。异常的降雨在2001年,2003年,2006年,2008年,2011年和2014年造成了高洪灾。2000年是本千年的最低排放年。亚洲最大的Chilika泻湖通过Mahanadi系统获得了61%的内陆流量。 1995-2000年,泻湖的盐度,淤积和生物多样性减少,使游客,植物和水产捕捞量明显减少。作为工程干预,河道上游建造了一个新的疏inlet口,几乎没有拦河坝和切口。季风降水异常已减少了冲洗阈值,以保持盐度。因此,频率分析和以期望的重复间隔进行降雨的预测变得明确。作为水文工程对工程干扰的后期研究,对降雨的频率分析是在检验了异常值,与少量记录数据的拟合度后进行的。选择了合适的概率分布模式,并使用PDF函数预测了各个复发周期的季风降雨。在可用的L矩,PWM方法中,Log Pearson III类方法被认为是进行降雨分析的最佳方法。本文已尝试预测不同回报期的三角洲和泻湖10000年的季风降雨。

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