首页> 外文期刊>Journal of great lakes research >Wind Fields over the Great Lakes Measured by the SeaWinds Scatterometer on the QuikSCAT Satellite
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Wind Fields over the Great Lakes Measured by the SeaWinds Scatterometer on the QuikSCAT Satellite

机译:由QuikSCAT卫星上的SeaWinds散射仪测量的大湖上的风场

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摘要

This paper demonstrates the utility of satellite scatterometer measurements for wind retrieval over the Great Lakes on a daily basis. We use data acquired by the SeaWinds Scatterometer on the QuikSCAT (QSCAT) satellite launched in June 1999 to derive wind speeds and directions over the lakes at a resolution of 12.5 km, which is two times finer than the QSCAT standard ocean wind product at a resolution of 25 km. To evaluate QSCAT performance for high-resolution measurements of lake wind vectors, we compare QSCAT results with Great Lakes Coastal Forecasting System (GLCFS) nowcast wind fields and with standard QSCAT measurements of ocean wind vectors. Although the satellite results over the Great Lakes are obtained with an ocean model function, QSCAT and GLCFS wind fields compare well together for low to moderate wind conditions (4-32 knots). For wind speed, the analysis shows a correlation coefficient of 0.71, a bias of 2.6 knots in mean wind speed difference (nowcast wind is lower) with a root-mean-square (rms) deviation of 3.8 knots. For wind direction, the correlation coefficient is 0.94 with a very small value of 1.3°in mean wind direction bias and an rms deviation of 38°for all wind conditions. When excluding the low wind range of 4-12 knots, the rms deviation in wind direction reduces to 22°. Considering QSCAT requirements designed for ocean wind measurements and actual evaluations of QSCAT performance over ocean, results for high-resolution lake wind vectors indicate that QSCAT performs well over the Great Lakes. Moreover, we show that wind fields derived from satellite scatterometer data before, during, and after a large storm in October 1999, with winds stronger than 50 knots, can monitor the storm development over large scales. The satellite results for storm monitoring are consistent with GLCFS nowcast winds and lake buoy measurements. A geophysical model function can be developed specifically for the Great Lakes using long-term data from satellite scatterometers, to derive more accurate wind fields for operational applications as well as scientific studies.
机译:本文演示了每天使用卫星散射仪测量大湖风的实用性。我们使用SeaWinds散射仪在1999年6月发射的QuikSCAT(QSCAT)卫星上获得的数据得出湖泊上的风速和风向,分辨率为12.5 km,这比QSCAT标准海洋风产品的分辨率细两倍。 25公里。为了评估QSCAT在高分辨率湖风矢量测量中的性能,我们将QSCAT结果与大湖沿岸预报系统(GLCFS)临近预报的风场和标准QSCAT海洋风矢量测量结果进行了比较。尽管五大湖的卫星结果是通过海洋模型函数获得的,但对于中低风条件(4-32节),QSCAT和GLCFS风场的效果很好。对于风速,分析显示相关系数为0.71,平均风速差(现浇风偏小)的偏差为2.6节,均方根(rms)偏差为3.8节。对于风向,相关系数为0.94,平均风向偏差很小,值为1.3°,所有风况的均方根偏差为38°。当排除4-12节的低风范围时,风向的rms偏差减小到22°。考虑到为海洋风测量设计的QSCAT要求以及对海洋QSCAT性能的实际评估,高分辨率湖风矢量的结果表明QSCAT在五大湖地区表现良好。此外,我们显示,由卫星散射仪数据得出的风场在1999年10月的大风暴之前,之中和之后(风速大于50节)可以监视大范围的风暴。用于风暴监测的卫星结果与GLCFS临近预报的风和湖浮标的测量结果一致。可以使用卫星散射仪的长期数据专门为五大湖开发地球物理模型功能,以导出更精确的风场,以用于运营应用和科学研究。

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