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Controls on residence time and exchange in a system of shallow coastal bays

机译:控制浅滩海湾系统中的停留时间和交换

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Patterns of transport and residence time influence the morphology, ecology and biogeochemistry of shallow coastal bay systems in important ways. To better understand the factors controlling residence time and exchange in coastal bays, a three-dimensional finite-volume coastal ocean model was set up and validated with field observations of circulation in a system of 14 shallow coastal bays on the Atlantic coast of the USA (Virginia Coast Reserve). Residence times of neutrally buoyant particles as well as exchange among the bays in the system and between the bays and the ocean were examined with Lagrangian particle tracking. There was orders of magnitude variation in the calculated residence time within most of the bays, ranging from hours in the tidally refreshed (repletion) water near the inlets to days-weeks in the remaining (residual) water away from the inlets. Residence time in the repletion waters was most sensitive to the tidal phase (low vs. high) when particles were released whereas residence time in the residual waters was more sensitive to wind forcing. Wind forcing was found to act as a diffuser that shortens particle residence within the bays; its effect was higher away from the inlets and in relatively confined bays. Median residence time in the bays significantly decreased with an increase in the ratio between open water area and total area (open water plus marsh). Exchange among the bays and capture areas of inlets (Le., exchange between the bays and the ocean) varied considerably but were insensitive to tidal phase of release, wind, and forcing conditions in different years, in contrast to the sensitivity of residence time to these factors. We defined a new quantity, termed shortest-path residence time, calculated as distance from the closest inlet divided by root-mean-square velocity at each point in model domain. A relationship between shortest-path residence time and particle-tracking residence time provides a means of estimating residence time over an entire model domain. (C) 2015 Elsevier Ltd. All rights reserved.
机译:运输和停留时间的模式以重要的方式影响着浅海沿海海湾系统的形态,生态和生物地球化学。为了更好地了解控制沿海海湾居住时间和交换的因素,建立了三维有限体积沿海海洋模型,并通过对美国大西洋沿岸14个浅沿海海湾系统中的环流进行实地观测进行了验证(弗吉尼亚海岸保护区)。用拉格朗日粒子追踪技术检查了中性浮力粒子的停留时间以及系统中各海湾之间以及各海湾与海洋之间的交换。在大多数海湾中,计算得出的停留时间存在数个数量级的变化,范围从进水口附近经过潮汐更新(补充)的水到数小时,到离开进水口的剩余(残留)水在几天至几周不等。当颗粒被释放时,在补给水中的停留时间对潮汐期最敏感(从低到高),而在残留水中的停留时间对风力更敏感。发现强迫风起到扩散器的作用,缩短了海湾中的颗粒停留时间。远离入口和相对狭窄的海湾,其效果更高。随着开放水域面积与总面积(开放水域与沼泽地)之比的增加,海湾中位停留时间显着减少。海湾之间和入口捕获区域之间的交换(例如,海湾与海洋之间的交换)变化很大,但与滞留时间对时间的敏感性形成对比,它们对不同年份的潮汐阶段的释放,风和强迫条件不敏感。这些因素。我们定义了一个新的量,称为最短路径停留时间,计算为距最近入口的距离除以模型域中每个点的均方根速度。最短路径停留时间和粒子跟踪停留时间之间的关系提供了一种估算整个模型域上停留时间的方法。 (C)2015 Elsevier Ltd.保留所有权利。

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