首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Physical processes impacting passive particle dispersal in the Upper Florida Keys
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Physical processes impacting passive particle dispersal in the Upper Florida Keys

机译:影响上佛罗里达礁岛被动粒子扩散的物理过程

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Physical processes affecting the dispersion of passive particles (e.g., coral larvae, pollutants) in the Upper Florida Keys are investigated through in situ observations (acoustic Doppler current profilers and surface drifters) and numerical ocean circulation modeling (horizontal resolution: 800 m, vertical resolution: 0.1-1 m). During the study period in August 2006 (set to coincide with an annual coral spawning event), Lagrangian trajectories in the vicinity of the reef tract indicate that alongshelf advection was mainly poleward and due to the subtidal flow of the Florida Current, while cross-shelf advection was mainly onshore and due to wind-driven currents. Tidal currents resulted in predominantly alongshelf displacements, but did not contribute significantly to net passive particle transport on a weekly timescale. Typical advection distances were of the order of 10 to 50 km for pelagic durations of 1 week, with significant variability linked to geographical location. In contrast, the direction of transport from the offshore reefs remained essentially constant (i.e., potential dispersion pathways were limited). In addition, Lagrangian trajectories and progressive vector diagrams in the vicinity of the reef tract indicate that alongshelf variations in the cross-shelf velocity gradient associated with the FC are relatively weak on an alongshore scale of ca. 50 km. For August 2006, the highest particle concentrations typically occur inshore of the reef tract, thereby suggesting that onshore transport associated with wind-driven currents contributes significantly to the local retention of passive organisms (and other tracers) in the Upper Florida Keys. Overall, the results illustrate the necessity of conducting targeted in situ observations and numerical model predictions to quantify the physical processes affecting reef-scale advection, especially in an effort to understand local retention and dispersion mechanisms for larval marine organisms.
机译:通过现场观测(声学多普勒电流剖面仪和表面漂移器)和海洋环流数值模拟(水平分辨率:800 m,垂直分辨率),研究影响佛罗里达上游群岛中被动粒子(例如,珊瑚幼虫,污染物)扩散的物理过程。 :0.1-1 m)。在2006年8月的研究期间(与每年的珊瑚产卵事件相吻合),礁区附近的拉格朗日轨迹表明,沿岸平流主要是极向性的,这是由于佛罗里达洋流的潮汐流,而跨层平流的平流主要是在陆地上,并且是由风流引起的。潮流造成的主要是沿棚架的位移,但在每周的时间尺度上并没有显着地促进净被动颗粒的运输。典型的平流距离在中上层持续时间为1周的情况下约为10至50 km,与地理位置有关的变化很大。相反,从近海礁石的运输方向基本上保持不变(即潜在的扩散途径受到限制)。另外,礁区附近的拉格朗日轨迹和渐进矢量图表明,与FC相关的跨架速度梯度中的沿架变化在ca的沿岸尺度上相对较弱。 50公里对于2006年8月,最高的颗粒浓度通常发生在珊瑚礁的近岸,从而表明与风流相关的近岸运输对上佛罗里达礁岛的被动生物(和其他示踪物)的局部滞留有很大贡献。总的来说,这些结果说明有必要进行有针对性的现场观察和数值模型预测,以量化影响礁石规模对流的物理过程,特别是在努力了解幼体海洋生物的局部保留和扩散机制方面。

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