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The effect of cloud liquid water on tropospheric temperature retrievals from microwave measurements

机译:液态云水对微波对流层温度反演的影响

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摘要

Microwave radiometry is a suitable technique to measure atmospherictemperature profiles with high temporal resolution during clear sky andcloudy conditions. In this study, we included cloud models in the inversionalgorithm of the microwave radiometer TEMPERA (TEMPErature RAdiometer) todetermine the effect of cloud liquid water on the temperature retrievals. Thecloud models were built based on measurements of cloud base altitude andintegrated liquid water (ILW), all performed at the aerological station(MeteoSwiss) in Payerne (Switzerland). Cloud base altitudes were detectedusing ceilometer measurements while the ILW was measured by a HATPRO(Humidity And Temperature PROfiler) radiometer. To assess the quality of theTEMPERA retrieval when clouds were considered, the resulting temperatureprofiles were compared to 2 years of radiosonde measurements. The TEMPERAinstrument measures radiation at 12 channels in the frequency range from 51to 57 GHz, corresponding to the left wing of the oxygen emission linecomplex. When the full spectral information with all the 12 frequencychannels was used, we found a marked improvement in the temperatureretrievals after including a cloud model. The chosen cloud model influencedthe resulting temperature profile, especially for high clouds and clouds witha large amount of liquid water. Using all 12 channels, however, presentedlarge deviations between different cases, suggesting that additionaluncertainties exist in the lower, more transparent channels. Using lessspectral information with the higher, more opaque channels only also improvedthe temperature profiles when clouds where included, but the influence of thechosen cloud model was less important. We conclude that tropospherictemperature profiles can be optimized by considering clouds in the microwaveretrieval, and that the choice of the cloud model has a direct impact on theresulting temperature profile.
机译:微波辐射法是一种适合的技术,可以在晴朗的天空和多云的条件下以高时间分辨率测量大气温度曲线。在这项研究中,我们将云模型包括在微波辐射计TEMPERA(温度辐射度计)的反演算法中,以确定云状液态水对温度反演的影响。这些云模型是基于对云底高度和综合液态水(ILW)的测量而建立的,所有这些都在瑞士Payerne的气象站(MeteoSwiss)进行。使用云高仪测量来检测云基准高度,而用HATPRO(湿度和温度PROfiler)辐射计测量ILW。为了在考虑云层时评估TEMPERA检索的质量,将得出的温度剖面与2年的无线电探空仪测量值进行了比较。 TEMPERA仪器可测量12个通道的辐射,这些通道的频率范围为51至57 GHz,对应于氧气排放管线复合体的左翼。当使用所有12个频道的全部频谱信息时,在包括云模型后,我们发现温度检索有显着改善。所选的云模型会影响最终的温度曲线,特别是对于高云和大量液态水云而言。但是,使用所有12个通道,在不同情况之间存在较大的偏差,这表明在较低,更透明的通道中还存在其他不确定性。在包含云的情况下,使用具有更高,更多不透明通道的较少光谱信息也只能改善温度分布,但是所选云模型的影响并不那么重要。我们得出结论,对流层温度曲线可以通过考虑微波检索中的云来优化,并且云模型的选择对结果温度曲线有直接影响。

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