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Circulation Dynamics and Seasonal Variability for the Charlotte Harbor Estuary, Southwest Florida Coast

机译:佛罗里达州西南部夏洛特港口河口的循环动力学和季节性变异

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摘要

A hydrodynamic model was developed and validated for the Charlotte Harbor estuarine system, located in SW Florida, to elucidate freshwater fluxes within the system's various inlets during diverse hydrologic conditions. Fresh water entering the system not only varies seasonally but also, because of regulatory fresh water, releases controlling water levels within an upstream lake. The unnatural freshwater releases have been found to negatively affect the system's ecology, in particular within the Caloosahatchee River portion of the system. Neither the flood nor ebb phase exhibits uniform dominance in flushing the system's four major passes. Boca Grande Pass and Big Carlos Pass were mostly ebb dominant, whereas San Carlos Bay was largely flood dominant; neither phase dominated at Captiva Pass. The similarities and/or contradictions of these results in comparison to former field and modeling results are mainly attributed to the differences between the freshwater sources and environmental forces corresponding to each study that forces a different mass-balance condition over the estuary-bay system and, thereby, at each individual inlet. A Lagrangian particle tracking study revealed particles released within the Peace River during different hydrological conditions were comparably transported regardless of freshwater inputs and predominate wind direction. In contrast, particles released within the Caloosahatchee River were flushed into the Gulf of Mexico within 10 days during a usually wet El Nino, dry(November-April) season period whereas during the summer wet (May-October) season released particles remained in the estuary for a longer period (13 days), ultimately resulting in their further transport into Pine Island Sound and Matlacha Pass. The results also demonstrate the effect of freshwater river inputs and wind on the travel time of the neutrally buoyant particles within the estuarine system. The hydrodynamic and coupled particle tracking model serve as the first step in a forthcoming larval transport modeling study.
机译:为位于SW佛罗里达州的夏洛特港河口系统开发和验证了一种流体动力学模型,在不同的水文条件下阐明了系统各种入口内的淡水通量。淡水进入系统不仅季节性差异,而且由于监管淡水,释放控制上游湖内的水平。已发现不自然的淡水释放对系统的生态产生负面影响,特别是在系统的Caloosahatchee河部分内。洪水和EBB阶段都没有在冲洗系统的四个主要通行证时表现出统一的主导地位。 Boca Grande Pass和Big Carlos Pass大多是EBB主导,而圣卡洛斯湾大部分泛滥;既不在Captiva Pass中占主导地位。与前场和建模结果相比,这些结果的相似性和/或矛盾主要归因于对应于每项研究的淡水来源和环境力之间的差异,这些研究迫使在河口湾系统上迫使不同的质量平衡条件以及因此,在每个单独的入口处。拉格朗日粒子跟踪研究揭示了在不同水文条件下和平河内释放的颗粒,无论淡水输入和偏向风向如何,都是相当运输的。相比之下,在通常湿的El Nino的10天内,在夏天潮湿(4月至4月)季节期间,在10天内冲入墨西哥湾的颗粒,而夏季潮湿(五月)季节释放颗粒仍然存在河口长期(13天),最终导致他们进一步运输到松树岛声音和Matlacha通过。结果还证明了淡水河流输入和风对酯氨基系统内中立浮力颗粒的行程时间的影响。流体动力学和耦合粒子跟踪模型作为即将到来的幼虫传输建模研究的第一步。

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