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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Satellite ocean color observations of stormwater runoff plumes along the San Pedro Shelf (southern California) during 1997-2003
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Satellite ocean color observations of stormwater runoff plumes along the San Pedro Shelf (southern California) during 1997-2003

机译:1997年至2003年期间,圣佩德罗架(加利福尼亚州南部)雨水径流羽流的卫星海洋颜色观测

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Knowledge of freshwater runoff plume dynamics in southern California is important for management of coastal water quality, because river discharge associated with episodic winter rainstorms can be a major source of pollutants and pathogens to coastal waters. The purpose of this study was to analyze the spatio-temporal dynamics of plumes at the San Pedro Shelf in southern California and identify factors influencing the incidence and dispersal patterns of plumes. We used 1.1-km spatial resolution satellite images collected in 1997-2003 by the SeaWiFS optical radiometer. The area of each plume was detected by the backscattering characteristics of surface waters in the vicinity of the mouths of four rivers that discharge to the San Pedro Basin. The rainstorm magnitude was estimated from atmospheric precipitation averaged over the total area of local watersheds. The plume size estimated from the backscattering coefficient nLw555 > 1.3 mW cm(-2) mu m(-1) sr(-1) was highly correlated with the amount of rainwater precipitated over the watershed area and accumulated during the period preceding the plume. The relation between rainstorm and plume area was linear with zero intercept: that means that the minimum rainstorm magnitude under which no plume occurred in the study area was almost zero, and even small precipitation resulted in a plume. The persistence of the plumes was estimated by fitting the coefficients of the model of plume water dissipation to achieve maximum correlation between the plume area and rainstorm: Twenty-five percent of rainwater dissipated daily, which gradually decreased the plume size. The size, alongshore and cross-shelf translocation of the plumes were modulated slightly by the local circulation, forced remotely by the equatorward wind a few hundred km to the south (along the coast of Baja California). The influence of tidal circulation on the plume area was slight and statistically insignificant. (c) 2005 Elsevier Ltd. All rights reserved.
机译:对加利福尼亚南部地区淡水径流羽流动力学的了解对于管理沿海水质非常重要,因为与冬季暴发性暴雨有关的河流排放可能是沿海水域污染物和病原体的主要来源。这项研究的目的是分析加利福尼亚南部圣佩德罗架上的羽流的时空动态,并确定影响羽流发生和扩散模式的因素。我们使用了SeaWiFS光学辐射计在1997-2003年收集的1.1公里空间分辨率卫星图像。通过向圣佩德罗盆地排放的四条河口附近的地表水的反向散射特性,可以检测出每个羽状流的面积。暴雨幅度是根据局部流域总面积上的平均大气降水量估算得出的。根据反向散射系数nLw555> 1.3 mW cm(-2)μm(-1)sr(-1)估算的羽流大小与流域区域上方沉淀并在羽流之前的一段时间内积累的雨水量高度相关。暴雨与羽流面积之间的关系是线性的,截距为零:这意味着在研究区域内没有羽流发生的最小暴雨量级几乎为零,即使很小的降水也会产生羽流。通过拟合羽流耗水模型的系数来估计羽流的持久性,以实现羽流面积与暴雨之间的最大相关性:每天消耗25%的雨水,这逐渐减小了羽流的大小。羽流的大小,沿岸和跨架易位受局部环流的调节,受到向南(北加利福尼亚海岸)数百公里的赤道风的作用而被迫偏远。潮气循环对羽流区域的影响很小,在统计学上不显着。 (c)2005 Elsevier Ltd.保留所有权利。

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