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Evaluation of Wind Vectors Observed by QuikSCAT/SeaWinds Using Ocean Buoy Data

机译:使用海洋浮标数据评估QuikSCAT / SeaWinds观测到的风向

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Wind vectors observed by the QuikSCAT/SeaWinds satellite mission are validated by comparing with wind and wave data from ocean buoys. Effects of oceanographic and atmospheric environment on scatterometer measurements are also assessed using the buoy data. Three versions of QuikSCAT/SeaWinds wind data were collocated with buoy observations operated by the National Data Buoy Center (NDBC), Tropical Atmosphere Ocean (TAO), and Pilot Research Moored Array in the Tropical Atlantic (PIRATA) projects, and the Japan Meteorological Agency (JMA). Only buoys located offshore and in deep water were analyzed. The temporal and spatial differences between the QuikSCAT/SeaWinds and buoy observations were limited to less than 30 min and 25 km. The buoy wind speeds were converted to equivalent neutral winds at a height of 10 m above the sea surface. The comparisons show that the wind speeds and directions observed by QuikSCAT/SeaWinds agree well with the buoy data. The root-mean-squared differences of the wind speed and direction for the standard wind data products are 1.01 m s~(-1) and 23°, respectively, while no significant dependencies on the wind speed or cross-track cell location are discernible. In addition, the dependencies of wind speed residuals on oceanographic and atmospheric parameters observed by buoys are examined using the collocated data. A weak positive correlation of the wind speed residuals with the significant wave height is found, while dependencies on the sea surface temperature or atmospheric stability are not physically significant.
机译:通过与来自海洋浮标的风浪数据进行比较,验证了QuikSCAT / SeaWinds卫星任务观测到的风向。还使用浮标数据评估了海洋和大气环境对散射仪测量的影响。将三个版本的QuikSCAT / SeaWinds风数据与国家数据浮标中心(NDBC),热带大气(TAO)和热带大西洋试点系泊阵列(PIRATA)项目以及日本气象厅的浮标观测并置(JMA)。仅对位于近海和深水中的浮标进行了分析。 QuikSCAT / SeaWinds和浮标观测之间的时空差异仅限于少于30分钟和25 km。浮标风速被转换为海平面以上10 m处的等效中性风。比较表明,QuikSCAT / SeaWinds观测到的风速和风向与浮标数据非常吻合。标准风数据产品的风速和风向的均方根差分别为1.01 m s〜(-1)和23°,而对风速或跨轨单元位置没有明显的依存关系。此外,使用并置数据检查了风速残差对浮标观测到的海洋和大气参数的依赖性。发现风速残差与明显的波高之间存在弱的正相关,而对海面温度或大气稳定性的依赖性在物理上并不重要。

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