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Influence of Land Cover and Soil Moisture based Brown Ocean Effect on an Extreme Rainfall Event from a Louisiana Gulf Coast Tropical System

机译:土地覆盖与土壤水分棕海效应对路易斯安那湾海岸热带系统极端降雨事件的影响

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Extreme flooding over southern Louisiana in mid-August of 2016 resulted from an unusual tropical low that formed and intensified over land. We used numerical experiments to highlight the role of the 'Brown Ocean' effect (where saturated soils function similar to a warm ocean surface) on intensification and it's modulation by land cover change. A numerical modeling experiment that successfully captured the flood event (control) was modified to alter moisture availability by converting wetlands to open water, wet croplands, and dry croplands. Storm evolution in the control experiment with wet antecedent soils most resembles tropical lows that form and intensify over oceans. Irrespective of soil moisture conditions, conversion of wetlands to croplands reduced storm intensity, and also, non-saturated soils reduced rain by 20% and caused shorter durations of high intensity wind conditions. Developing agricultural croplands and more so restoring wetlands and not converting them into open water can impede intensification of tropical systems that affect the area.
机译:2016年8月中旬南方路易斯安那州的极端洪水导致了一个不寻常的热带低,在土地上形成和加剧。我们使用了数值实验来突出“棕海”效应(饱和土壤功能与温热海面类似)的作用,并通过陆地覆盖变化调节。修改了成功捕获洪水事件(控制)的数值建模实验,以通过将湿地转换为开放水,湿耕地和干性农田来改变水分可用性。湿法前土壤的对照实验中的风暴演变最类似于热带低点,这些低点形成和加剧海洋。无论土壤湿度条件如何,湿地转化为农田减少风暴强度,而且,非饱和的土壤减少了20%,造成的高强度风能较短。开发农业农作物,更恢复湿地,不将它们转换成开阔水可以阻碍影响该区域的热带系统的强化。

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