地基微波輻射計反演水汽密度廓線精度分析
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Accuracy Analysis of Vapor Density Profiles Measured by GroundBased Microwave Radiometer
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    摘要:

    以探空水汽廓線為標準,對00:00UTC、12:00UTC北京南郊(39.93 °E,116.28 °N)觀測站的微波輻射計水汽廓線與WRF(Weather Research & Forecasting Model)模擬的水汽廓線進行精度分析。結果表明,整體上WRF水汽密度接近探空,但在近地面處微波輻射計的更接近探空;水汽密度偏差在夏季較大冬季較小;微波輻射計的水汽密度在3 km左右偏大,根據北京地區歷史天氣記錄中有中云的天氣較多的信息,推測可能是由于云對微波輻射計反演有影響。06:00UTC和18:00UTC以WRF水汽廓線為參考對微波輻射計的水汽廓線進行精度分析,得到的結果與00:00UTC和12:00UTC的類似。

    Abstract:

    The radiosonde vapor density is used as standards to analysis the accuracy of microwave radiometer and WRF vapor density data, both at 00:00UTC and 12:00UTC. As a whole, the vapor density profile of WRF seems closer to that of radiosonde comparing with the profile measuring by the groundbased microwave radiometer, but not including that near the surface, where it has a larger bias to sounding vapor density. It is also found that the maximum of vapor density deviation is in summer and the minimum is in winter. Besides, the vapor density of microwave radiometer has a small peak at about 3 km, because there exist clouds in the layer of 3 km to 5 km, which influences microwave radiometer’s vapor density retrieving. Using the WRF vapor density data at 06:00UTC and 18:00UTC as standards to assess the retrieving vapor density profile measured by the groundbased microwave radiometer, the similar result can be obtained.

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侯葉葉,劉紅燕,鮑艷松.地基微波輻射計反演水汽密度廓線精度分析[J].氣象科技,2016,44(5):702~709

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  • 收稿日期:2015-08-17
  • 定稿日期:2016-04-08
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  • 在線發布日期: 2016-10-13
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