摘要
杭州湾近10年的围垦工程使其岸线向海推进,导致内部潮波动力发生较大变化。本文基于验证后的非结构化网格的长江口-杭州湾-舟山群岛近海潮波动力数值模型,结合Landsat遥感数据,分析了杭州湾近10年的岸线变化,并计算了2005年和2015年两种工况下杭州湾的潮波动力情况。对比发现,2005-2015年之间的围垦工程造成湾内高潮位抬升0.2~0.5 m,南岸庵东浅滩附近潮流减小,湾顶附近余流增幅明显。
The continuous reclamations on Hangzhou Bay(HZB) moved its coastal line forward into the sea, which lead to the changes of tidal dynamics. Base on the unstructured, high bathymetry resolution hydrodynamic model, and Landsat remote sensing data, the article analyze the evolution of its coastline.Then two different scenarios were simulated to hindcast HZB tidal dynamics in 2005 and 2015. The comparisons of results show the reclamation lead to the spring high tide increase about 0.2~0.5m in the middle portion of HZB and its spring current decrease near the Andong tidal flat. The residual current increase a lot near the upper limit of HZB.
引文
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