首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Cross-shore velocity shear, eddies and heterogeneity in water column properties over fringing coral reefs: West Maui, Hawaii
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Cross-shore velocity shear, eddies and heterogeneity in water column properties over fringing coral reefs: West Maui, Hawaii

机译:夏威夷西部毛伊岛上跨岸速度剪切,涡流和水柱属性中的非均质性

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摘要

A multi-day hydrographic Survey cruise was conducted to acquire spatially extensive, but temporally limited, high-resolution, three-dimensional measurement Of Currents, temperature, salinity and turbidity off West Maui in the summer of 2003 to better understand coastal dynamics along a complex island shoreline with coral reefs. These data complement long-term, high-resolution tide, wave, Current, temperature, salinity and turbidity measurements made at a number of fixed locations in the study area starting in 2001. Analyses of these hydrographic data, in conjunction with numerous field observations, evoke the following conceptual model of water and turbidity flux along West Maui. Wave- and wind-driven flows appear to be the primary control oil flow over shallower portions of the reefs while tidal and subtidal currents dominate flow over the outer portions of the reefs and insular shelf. When the direction of these flows counter one another, Which is quite common, they cause a Zone of cross-shore horizontal shear and often form a front, with turbid, lower-salinity water inshore of the front and clear, higher-salinity water offshore of the front. It is not clear whether these zones of high shear and fronts are file cause or the result of the location of the fore reef, but they appear to be correlated alongshore over relatively large horizontal distances (orders of kilometers). When two flows converge or when a single flow is bathymetrically steered, eddies can be generated that, in the absence of large ocean Surface waves. tend to accumulate material. Areas of higher turbidity and lower salinity tend to correlate with regions of poor coral health or the absence of well-developed reefs, Suggesting that the oceanographic processes that concentrate and/or transport nutrients, contaminants, low-salinity water or suspended sediment might strongly influence coral reef ecosystem health and sustainability. Published by Elsevier Ltd.
机译:进行了为期多天的水文调查巡游,以获取2003年夏季西毛伊岛海域的水流,温度,盐度和浊度的空间广泛但时间有限的高分辨率三维测量,以便更好地了解复杂地区的海岸动态岛海岸线与珊瑚礁。这些数据补充了2001年开始在研究区域的多个固定位置进行的长期高分辨率海潮,波浪,水流,温度,盐度和浊度测量结果。结合许多实地观测资料,对这些水文数据进行了分析,唤起了西毛伊岛水和浊度通量的以下概念模型。波浪和风驱动的流动似乎是在礁石较浅部分上方的主要控制油流,而潮流和潮汐流则占礁石和岛架外部的主要流动。当这些水流的方向彼此相反时(这很常见),它们会引起跨海岸水平剪切带,并经常形成前缘,前缘近岸为浑浊的低盐度水,而近海为澄清高盐度的水。的前面。目前尚不清楚这些高剪切带和锋面带是否是成因或前礁位置的结果,但它们似乎在相对较大的水平距离(几千米)内沿岸相关。当两股水流汇合时,或以等深线引导单水流时,在没有大的海洋表面波的情况下会产生涡流。倾向于积累物质。浊度较高和盐度较低的地区往往与珊瑚健康状况不佳或没有发达珊瑚礁的地区有关,这表明集中和/或运输养分,污染物,低盐度水或悬浮沉积物的海洋学过程可能强烈影响珊瑚礁生态系统的健康与可持续性。由Elsevier Ltd.发布

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