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Landfall season is critical to the impact of a cyclone on a monsoon-regulated tropical coastal lagoon

机译:登陆季对飓风对季风监管的热带沿海泻湖的影响至关重要

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Cyclones can produce a wide variety of short-term and long-term ecological impacts on coastal lagoons depending on cyclone's physical-meteorological characteristics and the lagoon's geographic, geomorphic, and bathymetric characteristics. Here, we theorized that in monsoon regulated tropical coastal lagoons, another important factor that could determine the impact of a cyclone is the landfall season or time of the year with reference to the monsoon season. We analyzed the impact of two cyclones which made landfall near Chilika, Asia's largest brackish water lagoon in different seasons, Cyclone Fani and Titli before and after the monsoon season. We compared field measured and satellite-derived water quality parameters including nutrient, salinity, water temperature, transparency, Chlorophyll-a (Chl-a), total suspended matter (TSM), and colored dissolved organic matter (CDOM) before and after the cyclones. We found that although both the cyclones were of similar intensities, after their land interaction, their impact on the lagoon's water quality was contrasting. The post-monsoon cyclone produced a substantial increase in total nitrogen (TN) and total phosphorous (TP), a large drop in salinity, CDOM, and Chl-a. In contrast, after the pre-monsoon cyclone, TN and TP did not show any such hike, no substantial change in salinity and CDOM either, and only a slight increase in Chl-a was observed. We found that the controlling factor in determining the impact of a cyclone is the rate and duration of freshwater discharge to the lagoon, which is normally a strong pulse for pre-monsoon and a continued high flow for post-monsoon cyclones. We conclude that the antecedent conditions of the lagoon and the watershed at the time of a cyclone's landfall is a key criterion in determining the impact. The combined use of satellite data and field data was proved critical to capture the overall impact of cyclones on the hydrological characteristics of the monsoon-regulated coastal lagoon.
机译:根据旋风的物理气象特征和泻湖的地理,地貌和碱基,旋风,旋风可以对沿海泻湖产生各种短期和长期生态影响。在这里,我们理论在季风监管的热带沿海泻湖中,另一个可以确定飓风的影响的重要因素是参考季风季节的登陆季节或时间。我们分析了两个旋风的影响,这是在季风季节之前和之后的不同季节,Cyclone Fani和Titli在不同的季节,Cyclone Fani和Titli附近抵消了奇利卡附近的影响。我们比较现场测量和卫星衍生的水质参数,包括营养,盐度,水温,透明度,叶绿素-A(CHL-A),在旋风前后和之后和之后的悬浮物(TSM)和有色溶解有机物(CDOM) 。我们发现,虽然旋风器都具有相似的强度,但在他们的土地互动之后,它们对泻湖的水质的影响是对比的。后季后旋风器产生总氮(TN)和总磷(TP)的大幅增加,盐度大滴,CDOM和CHL-A。相比之下,在季风前旋风内,TN和TP未显示任何此类加息,盐度和CDOM中没有大量变化,并且观察到CHL-A的轻微增加。我们发现确定旋风分离器的影响的控制因子是淡水排放到泻湖的速率和持续时间,这通常是季风前季隆的强脉冲,并且对季风后旋转克隆的持续高流动。我们得出结论,泻湖和流域的前进条件在旋风分离人的土地时是确定影响的关键标准。证明了卫星数据和现场数据的结合使用,以捕获旋风对季风调节沿海泻湖水文特征的整体影响。

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