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Future wave-climate driven longshore sediment transport along the Indian coast

机译:未来的波浪气候驱动了印度海岸的漫长沉积物运输

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Longshore sediment transport is an important nearshore process that governs coastal erosion/accretion and in turn defines the orientation of coastlines. In this study, we assess the changes in longshore transport rates along the Indian coast due to the potential changes in wave parameters under the RCP4.5 climate scenario. The projected wave climate for two time slices, 'near-term/present' (2011-2040) and 'mid-term/future' (2041-2070) were used to investigate changes in the corresponding sediment transport rates. An empirical model accounting for major wave parameters, longshore current, resulting sediment transport and shoreline evolution was used. It was found that most of the Indian coast exhibited the same drift direction in both time slices, although changes in transport magnitude were present. To give a broad-brush characterisation of the coastline, the shoreline elements were classified as erosive, accretive or stable based on the comparative longshore transport rates of neighbouring elements. Similar characterisations, carried out for both time slices, showed that about 35% of the total coastline would remain unaffected due to the changing wave climate in the future (i.e. there is little to no change); about 20% is expected to 'worsen' (i.e. expected to undergo higher magnitudes of erosion wrt present rate) and 45% to 'improve' (i.e. expected to accrete/reach stability). It was also observed that the net annual transport rates pertaining to the future period are not expected to change significantly with respect to the current scenario. This indicates that the change in longshore transport rates arising from future changes in wave climate as represented by the RCP4.5 climate change scenario will have a broadly neutral effect.
机译:龙岸沉积物运输是一个重要的近岸过程,管辖沿海侵蚀/吸收,又定义了海岸线的方向。在这项研究中,由于RCP4.5气候情景下的波浪参数的潜在变化,我们评估了印度海岸沿海沿海运输率的变化。预计波浪气候为两个时间片,“近期/现在”(2011-2040)和“中期/未来”(2041-2070)用于调查相应沉积物运输率的变化。使用了主要波浪参数,龙底电流,导致沉积物和海岸线演化的实证模型占核算。发现大多数印度海岸在两个时间切片中表现出相同的漂移方向,尽管存在运输幅度的变化。为了给出海岸线的宽刷子表征,基于相邻元素的比较龙底运输速率,海岸线元素被归类为侵蚀,累积或稳定。对于两次切片进行的类似的特征表明,由于未来的波浪气候变化(即,没有变化几乎没有变化,大约35%的海岸线将不受影响。预计大约20%是“恶化”(即预期接受更高的侵蚀WRT率)和45%的“改善”(即预期令人信服/达到稳定)。还观察到,对未来期间的净年度运输率预计不会对目前的情况发生显着变化。这表明RCP4.5气候变化情景所代表的未来波浪气候变化引起的龙岸运输率的变化将具有巨大中立效果。

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