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COASTAL PROCESSES AND CAUSES OF SHORELINE EROSION AND ACCRETION OF THE BATHTHALANGUNDUWA ISLAND IN SRI LANKA

机译:斯里兰卡巴斯通朗杜瓦岛沿岸侵蚀和海岸线增生的过程

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Baththalangunduwa is an elongated sandy island. It is located in the Portugal Bay extending about 16 km long from north to south, and maximum width is about 680m east to west. Coastal processes mainly erosion, transportation and deposition of the Baththalangunduwa island has been calculated from the period from 1985 to 2017. After analyzing data spatially, erosion can be seen especially in the western flank of the island. The area is faced with waves, swells, storm winds and tides of the Palk Strait during the southwest monsoon period and vice versa accretion can be seen especially in the northern and eastern flanks and along the southern corner during the northeast monsoon period. The waves, wind pattern and tide of the Portugal Bay are responsible for the transportation and deposition in the area. Due to these processes, along the eastern and southern flanks of the island, there form micro landforms such as sandy lobes and hooks, mud flats, sea grass beds, mangrove patches, incomplete small bays and lagoon features. Most of these features are temporal, and limited to a week or a month or a season. According to the results, about 1 km erosion measured from the farthest point to the present coastal line, and total land extent change from 501 ha to 226 ha.
机译:Baththalangunduwa是一个细长的沙滩岛。它位于葡萄牙湾,从北向南延伸约16公里,最大宽度从东至西约680m。从1985年至2017年,计算了Baththalangunduwa岛的沿海过程,主要是侵蚀,运输和沉积。通过空间分析数据,可以发现侵蚀尤其是在该岛的西翼。该地区在西南季风时期面临波克海峡的海浪,海浪,暴风雨和潮汐,反之亦然,尤其是在北部和东部的侧翼以及东北季风时期的南角。葡萄牙湾的波浪,风型和潮汐负责该地区的运输和沉积。由于这些过程,在该岛的东部和南部两侧,形成了微观地形,例如沙状叶和钩,泥滩,海草床,红树林斑块,不完整的小海湾和泻湖特征。这些功能大多数都是暂时性的,并且仅限于一周或一个月或一个季节。根据结果​​,从最远点到目前的海岸线,大约侵蚀了1 km,土地总面积从501公顷变为226公顷。

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