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Short-term desalination of Pulicat lagoon (Southeast India) due to the 2015 extreme flood event: insights from Land-Ocean Interactions in Coastal Zone (LOICZ) models

机译:由于2015年极端洪水事件:沿海地区(Loicz)型号的土地 - 海洋互动洞察力,普里特泻湖(东南印度)的短期脱盐

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Abstract IntroductionWe investigated the magnitude and duration of desalination of Pulicat—a coastal lagoon ecosystem connected to the Bay of Bengal on the South-eastern coast of India—during the 2015 South India flood event which was a period of high-magnitude precipitation and riverine flooding.MethodsWe estimated freshwater runoff into the lagoon using flow accumulation models for a period of 55?days (November 1 to December 25, 2015) using daily gridded precipitation data from the Global Precipitation Measurement and a digital elevation model. Using the estimates of freshwater runoff, direct precipitation and observed salinities, we simulated water and salinity fluxes of the lagoon using the Land-Ocean Interactions in the Coastal Zone model. Further, we also used Monte Carlo simulation to estimate the uncertainty in system salinity, the residual salinity at the boundary and the freshwater residence times in the lagoon.ResultsWe estimated that a high volume (~?760?×?10sup6/sup?msup3/sup) of relatively low salinity waters (residual salinity?=?23.47?psu) had been exported from the lagoon to the Bay of Bengal during the period which is likely to have caused a strong dip in the daily salinity profile of the coastal sea. We contend that the lagoon experienced ~?40% desalination due to the 2015 event with a freshwater residence time of 18.5?days.ConclusionsThe study highlighted the short-term, high-magnitude desalination undergone by Pulicat lagoon during the 2015 South India floods. Considering the high residual and exchange volumes obtained from the study, we conclude that Pulicat could be a major exporter of relatively low salinity waters to the Bay of Bengal during monsoons.
机译:摘要介绍介绍普拉特 - 一艘沿海泻湖生态系统的额度和持续时间 - 沿海泻湖与印度东南海岸的孟加拉湾 - 在2015年南印度洪水事件期间,这是一项高级别降水和河流洪水.Methodswe使用流量累积模型估计淡水径流,使用来自全球降水测量的日常网格降水数据和数字高程模型(2015年11月1日至2015年11月25日)。利用淡水径流,直接降水和观察到的盐度估算,我们使用沿海地区模型的陆地互动模拟泻湖的水和盐分通量。此外,我们还使用了Monte Carlo模拟来估计系统盐度的不确定性,边界的残留盐度和淡水停留时间在Lagoon.Resultwe估计大容量(〜?760?×10 6 6 < / sup>?m 3 )相对低的盐水(剩余盐度?=?23.47?PSU)从泻湖到孟加拉湾的泻湖,可能导致了一个在沿海海的日常盐度剖面中强烈倾斜。我们争夺泻湖经历了〜40%的海水淡化,由于2015年的淡水停留时间为18.5?天。学习突出了2015年南印度洪水普鲁特泻湖的短期,高幅度脱盐。考虑到从研究中获得的高剩余和交换量,我们得出结论,普利特可以是季风在季风的孟加拉湾的相对低盐度水域的主要出口国。

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