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A SAR Observation and Numerical Study on Ocean Surface Imprints of Atmospheric Vortex Streets

机译:大气涡街海面印记的SAR观测与数值研究

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摘要

The sea surface imprints of Atmospheric Vortex Street (AVS) off Aleutian Volcanic Islands, Alaska were observed in two RADARSAT-1 Synthetic Aperture Radar (SAR) images separated by about 11 hours. In both images, three pairs of distinctive vortices shedding in the lee side of two volcanic mountains can be clearly seen. The length and width of the vortex street are about 60-70 km and 20 km, respectively. Although the AVS's in the two SAR images have similar shapes, the structure of vortices within the AVS is highly asymmetrical. The sea surface wind speed is estimated from the SAR images with wind direction input from Navy NOGAPS model. In this paper we present a complete MM5 model simulation of the observed AVS. The surface wind simulated from the MM5 model is in good agreement with SAR-derived wind. The vortex shedding rate calculated from the model run is about 1 hour and 50 minutes. Other basic characteristics of the AVS including propagation speed of the vortex, Strouhal and Reynolds numbers favorable for AVS generation are also derived. The wind associated with AVS modifies the cloud structure in the marine atmospheric boundary layer. The AVS cloud pattern is also observed on a MODIS visible band image taken between the two RADARSAT SAR images. An ENVISAT advance SAR image taken 4 hours after the second RADARSAT SAR image shows that the AVS has almost vanished.
机译:在相距约11小时的两个RADARSAT-1合成孔径雷达(SAR)图像中观察到了阿拉斯加阿留申火山岛附近的大气涡街(AVS)的海面印记。在这两个图像中,可以清楚地看到在两个火山山的背风侧散发出的三对独特的涡流。涡街的长度和宽度分别约为60-70公里和20公里。尽管两个SAR图像中的AVS具有相似的形状,但AVS中的涡旋结构高度不对称。根据海军NOGAPS模型输入的风向,根据SAR图像估算海面风速。在本文中,我们介绍了所观察到的AVS的完整MM5模型仿真。 MM5模型模拟的地表风与SAR衍生风非常吻合。根据模型运行计算得出的涡旋脱落速率约为1小时50分钟。还导出了AVS的其他基本特征,包括涡旋的传播速度,有利于AVS生成的斯特劳哈尔数和雷诺数。与AVS相关的风改变了海洋大气边界层中的云结构。在两个RADARSAT SAR图像之间拍摄的MODIS可见波段图像上也可以观察到AVS云模式。在第二张RADARSAT SAR图像后4小时拍摄的ENVISAT提前SAR图像显示,AVS几乎消失了。

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