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Offshore winds obtained from a network of wind-profiler radars during HyMeX

机译:HyMeX期间从风廓线雷达网络获得的海上风

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摘要

11 ultra-high-frequency (UHF) and very-high-frequency (VHF) wind-profiler radars were in operation for 13-18 months during the international Hydrological Cycle in Mediterranean Experiment (HyMeX) field campaign, devoted to the study of the atmospheric and marine water cycle in the western Mediterranean basin. These profilers provided vertical profiles of wind vector, turbulence, precipitation and the height of the atmospheric boundary layer and tropopause. The inland three VHF profilers aimed to document the upstream or downstream synoptic flow conditions. Five UHF profilers for lower atmosphere description were deployed along the French Mediterranean coast and Corsica Island. They were used to retrieve the 3D atmospheric wind fields over the basin, by assuming linearity of the fields inside a limited spatial and temporal domain. The objective of this article is to establish to what extent the 3D wind fields derived from the coastline profiler network are representative of the offshore kinematics. This assessment is performed by comparing more than one year of continuous profiler observations during different weather conditions with balloon radiosoundings and in situ aircraft or boundary-layer pressurized balloon measurements.
机译:在国际地中海水文实验周期(HyMeX)野外活动中,有11台超高频(UHF)和超高频(VHF)风廓线雷达投入运行了13-18个月,专门用于研究地中海西部盆地的大气和海洋水循环。这些廓线仪提供了风向,湍流,降水以及大气边界层和对流层顶高度的垂直廓线。内陆的三个VHF剖面仪旨在记录上游或下游天气流动状况。在法国地中海沿岸和科西嘉岛上部署了五台用于描述低层大气的UHF剖面仪。通过假设有限空间和时间域内的场的线性,它们被用来获取盆地上的3D大气风场。本文的目的是确定从海岸线廓线仪网络得出的3D风场在多大程度上代表了海上运动学。通过将不同天气条件下连续一年多的探查器观测与气球无线电探空仪和现场飞机或边界层加压气球测量值进行比较,可以进行此评估。

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