首页> 外文OA文献 >Performance of the Vaisala RS80A/H and RS90 Humicap Sensors and the Meteolabor “Snow White” Chilled-Mirror Hygrometer in Paramaribo, Suriname
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Performance of the Vaisala RS80A/H and RS90 Humicap Sensors and the Meteolabor “Snow White” Chilled-Mirror Hygrometer in Paramaribo, Suriname

机译:苏里南帕拉马里博的Vaisala RS80A / H和RS90 Humicap传感器和Meteolabor“ Snow White”冷镜湿度计的性能

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摘要

In climate research there is a strong need for accurate observations of water vapor in the upper atmosphere.Radiosoundings provide relative humidity profiles but the accuracy of many routine instruments isnotoriously inadequate in the cold upper troposphere. In this study results from a soundings programexecuted in Paramaribo, Suriname (5.8°N, 55.2°W), are presented. The aim of this program was to comparethe performance of different humidity sensors in the upper troposphere in the Tropics and to test differentbias corrections suggested in the literature. The payload of each sounding consisted of a chilled-mirror“Snow White” sensor from Meteolabor AG, which was used as a reference, and two additional sensors fromVaisala, that is, either the RS80A, the RS80H, or the RS90. In total 37 separate soundings were made.For the RS80A a clear, dry bias of between 4% and 8% RH is found in the lower tropospherecompared to the Snow White observation, confirming the findings in previous studies. A mean dry bias wasfound in the upper troposphere, which could be effectively corrected. The RS80H sensor shows a significantwet bias of 2%–5% in RH in the middle and upper troposphere, which has not been reported before.Comparing observations with RS80H sensors of different ages gives no indication of sensor aging or sensorcontamination. It is therefore concluded that the plastic cover introduced by Vaisala to avoid sensorcontamination is effective. Finally, the RS90 sensor yields a small but significant wet bias of 2%–3% below7-km altitude.The time-lag error correction from Miloshevich et al. was applied to the Vaisala data, which resulted inan increased variability in the relative humidity profile above 9- (RS80A), 8- (RS80H), and 11-km (RS90)altitude, respectively, which is in better agreement with the Snow White data.The averaged Snow White profile is compared with the average profiles of relative humidity from theEuropean Centre for Medium-Range Weather Forecasts (ECMWF). No significant bias is found in eitherthe analyses or the forecasts. The correlation coefficient for the Snow White and ECMWF data between 200and 800 hPa was 0.66 for the 36-h forecast and 0.77 for the analysis.
机译:在气候研究中,迫切需要对高层大气中的水蒸气进行精确观测。放射探测技术可提供相对湿度曲线,但众所周知,许多常规仪器的准确性在寒冷的对流层中不足。在这项研究中,给出了在苏里南帕拉马里博执行的一个测深程序(5.8°N,55.2°W)的结果。该程序的目的是比较热带对流层上不同湿度传感器的性能,并测试文献中建议的不同偏差校正。每种探测的有效载荷均由作为参考的Meteolabor AG的冷镜“白雪公主”传感器和维萨拉的两个附加传感器组成,即RS80A,RS80H或RS90。总共进行了37次单独的测深。对于RS80A,与对白雪皑皑的观测相比,在对流层下部发现了4%至8%RH的清晰,干燥的相对偏差,从而证实了先前研究的发现。在对流层上部发现了平均干偏,可以对其进行有效纠正。 RS80H传感器在对流层中层和高层对流层的RH上显示2%–5%的显着湿偏,这从未有过报道。与不同年龄的RS80H传感器的观察结果相比,没有迹象表明传感器老化或受到污染。因此可以得出结论,维萨拉引入的避免传感器污染的塑料盖是有效的。最后,RS90传感器在7公里以下的高度产生2%–3%的微小但显着的湿偏。来自Miloshevich等人的时滞误差校正。应用于维萨拉数据,导致相对湿度曲线的变化性分别在9-(RS80A),8(RS80H)和11-km(RS90)海拔上增加,这与Snow White更好地吻合欧洲平均距离天气预报中心(ECMWF)将白雪平均轮廓与相对湿度的平均轮廓进行了比较。在分析或预测中均未发现明显偏差。对于36 h的预报,200至800 hPa之间的Snow White和ECMWF数据的相关系数为0.66,分析的相关系数为0.77。

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