L波段雷達系統不同測風方法計算結果分析
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Result Analysis of Lband Radar Wind Mesurement System in Different Methods
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    摘要:

    根據廣東陽江探空站L波段雷達系統觀測的測風資料分析,測風記錄用綜合探測雷達測風方法與無斜距(或高度替代)測風方法計算的測風量得風層的結果,少數情況下會出現與理論值不相符的現象,兩種測風方法計算的結果,有時會超出高空氣象觀測儀器總體測量準確度要求允許的誤差范圍。在雷達的仰角小于30°時,量得風層的風速小于3 m/s時,兩種測風方法計算量得風層的風速基本相同(誤差在允許范圍內),但風向有的相差較大,超出測量準確度要求允許的誤差范圍。當雷達仰角小于15°,量得風層的風速大于30 m/s時,兩種測風方法計算量得風層的風向比較接近,但量得風層的風速有的卻相差較大,超出測量準確度要求允許的誤差范圍。

    Abstract:

    According to the observations of wind data analysis from Lband radar at Yangjiang radiosonde station of Guangdong, there sometimes appear some cases of inconsistence with the theoretical values if using comprehensive detection radar or no slant distance (or height replacement) wind measurement methods to calculate the results at the wind measurement levels.The results from these two methods in wind measuring are sometimes beyond the permitted error range of upperlevel meteorological observation instruments for overall measurement accuracy. Results show that when the radar elevation angle is less than 30° and the wind speed of the wind measurement level is <3 m/s, the wind speeds calculated from the two kinds of wind methods are almost the same, with the errors within the permitted range, but there are large differences sometimes in wind direction, beyond the allowed error range. When radar elevation angle is less than 15° and the wind speed in the wind measurement level is >30 m/s, the wind directions in the measure wind layer calculated by the two methods are close, but the differences in wind speed in the wind measurement levels are comparatively large, also beyond the allowed error range.

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羅雄光,梁國鋒,楊超. L波段雷達系統不同測風方法計算結果分析[J].氣象科技,2015,43(6):1025~1029

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  • 收稿日期:2014-11-18
  • 定稿日期:2015-02-04
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  • 在線發布日期: 2015-12-29
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