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Evolution of extreme high waters along the east coast of India and at the head of the Bay of Bengal

机译:沿印度东海岸和孟加拉湾上游的极端高水位的演变

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The recent evolution of extreme high waters along the severe cyclone-risk coasts of the Bay of Bengal (the east coast of India and Bangladesh) was assessed using long-term (24-34 years) hourly tide gauge data available from five stations. The highest water levels above mean sea level have the greatest magnitude towards the northern part of the Bay, which decreases towards its south-west. Extreme high waters were observed to result from a combination of moderate, or even small, surges with large tides at these stations in most of the cases. Increasing trends, which are significant, were observed in the extreme high waters at Hiron Point, at the head of the Bay. However, the trends in extremes are slightly lower than its mean sea level trend. For the other stations, Cox's Bazaar, Paradip Visakhapatnam and Chennai, no significant trends were observed. At inter-annual time scales, changes in extreme high waters in the Bay of Bengal were found to be influenced by the El Nino Southern Oscillation and the Indian Ocean Dipole. (C) 2016 Elsevier B.V. All rights reserved.
机译:使用五个站的长期(24-34年)每小时潮汐仪数据评估了孟加拉湾(印度和孟加拉国东海岸)严重气旋危险海岸附近极端高水位的最新演变。高于平均海平面的最高水位在海湾北部最大,而在西南部则下降。在大多数情况下,观察到极端高水位是由这些站的中等甚至小潮高潮组合而成。在海湾头的希隆角(Hiron Point)的极端高水域,观察到了明显的上升趋势。但是,极端趋势略低于其平均海平面趋势。对于其他车站,如考克斯的集市,Paradid Visakhapatnam和钦奈,没有观察到明显的趋势。在每年的时间尺度上,发现孟加拉湾极高水位的变化受厄尔尼诺南部涛动和印度洋偶极子的影响。 (C)2016 Elsevier B.V.保留所有权利。

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