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Variations in the Wave Climate and Sediment Transport Due to Climate Change along the Coast of Vietnam

机译:越南沿海气候变化引起的波浪气候和泥沙输送变化

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This study quantifies the climate change (CC)-driven variations in wave characteristics and the resulting variations in potential longshore sediment transport rate along the ~2000 km mainland coast of Vietnam. Wind fields derived from global circulation models (GCM) for current and future (2041–2060 and 2081–2100) climate conditions are used to force a numerical wave model (MIKE21 SW) to derive the deep water wave climate. The offshore wave climate is translated to nearshore wave conditions using another numerical model (Simulating WAves Nearshore—SWAN) and finally, a sediment transport model (GENEralized model for Simulating Shoreline Change—GENESIS) is used to estimate potential sediment transport for current and future climate conditions. Results indicate that CC effects are substantially different in the northern, central and southern parts of the coast of Vietnam. The 2081–2100 mean significant wave height along the northern coast is estimated to be up to 8 cm lower (relative to 1981–2000), while projections for central and southern coasts of Vietnam indicate slightly higher (increases of up to 5 cm and 7 cm respectively). Wave direction along the northern coast of Vietnam is projected to shift by up to 4° towards the south (clockwise) by 2081–2100 (relative to 1981–2000), up to 6° clockwise along the central coast and by up to 8° anti-clockwise (to the north) along the southern coast. The projected potential longshore sediment transport rates show very substantial and spatially variable future changes in net transport rates along the coast of Vietnam, with increases of up to 0.5 million m 3 /year at some locations (by 2081–2100 relative to 1981–2000), implying major changes in future coastline position and/or orientation. The vicinity of the highly developed city of Da Nang is likely to be particularly subject to coastline changes, with potentially an additional 875,000 m 3 of sand being transported away from the area per year by the turn of the 21st century.
机译:这项研究量化了由气候变化(CC)驱动的波浪特征变化,以及由此导致的越南内陆〜2000 km沿海近岸沉积物输运速度变化。从当前和将来(2041–2060年和2081–2100年)气候条件的全球环流模型(GCM)得出的风场用于强迫数值波模型(MIKE21 SW)得出深水波气候。使用另一个数值模型(近岸模拟波浪)将近海浪气候转换为近岸波浪条件,最后,使用沉积物传输模型(模拟海岸线变化的通用化模型——GENESIS)估算当前和未来气候的潜在沉积物传输条件。结果表明,CC效应在越南海岸的北部,中部和南部部分存在显着差异。 2081–2100年,沿北部海岸的平均显着波高估计降低了8厘米(相对于1981–2000年),而越南中部和南部海岸的预测显示略高(升高了5厘米和7厘米)。预计到2081–2100年(相对于1981–2000年),越南北部海岸的波浪方向向南(顺时针)最多偏移4°,沿中部海岸的波浪方向最多偏移6°,然后最多8°沿南部海岸逆时针方向(向北)。预计的潜在近岸沉积物运移速率显示出越南沿海地区的净运移速率未来变化非常大且在空间上会发生变化,某些地区的净运移速率每年最高可达50万m 3(相对于1981-2000年,到2081-2100年) ,暗示未来海岸线的位置和/或方向发生重大变化。高度发展的岘港市附近可能特别容易受到海岸线变化的影响,到21世纪初,每年有额外的875,000 m 3的沙子被运出该地区。

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