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Model comparison for estimating cloud liquid water content and attenuation in tropical region

机译:热带地区云层液态水含量和衰减估算模型比较

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In this paper, comparison and analysis of two cloud models are performed for prediction of cloud liquid water content and cloud attenuation in tropical region. To this aim, one-year (2012) radiosonde data, collected in the tropical country of Singapore, are processed to derive the 0°C/-20°C isothermal heights, calculate cloud liquid water content and then estimate cloud attenuation. Comparing with ITU-R P.840-6 model, our results indicate that the well-known Salonen Uppala (SU) model intends to underestimate the cloud liquid water content and corresponding cloud attenuation in tropical region. In addition, a newly proposed Water Vapor Pressure (WVP) cloud detection model provides relatively large cloud attenuation and shows its feasibility to predict cloud attenuation for tropical region.
机译:本文对两种云模型进行了比较和分析,以预测热带地区云的液态水含量和云的衰减。为了实现这一目标,对在热带国家新加坡收集的一年(2012年)无线电探空仪数据进行处理,得出0°C / -20°C等温高度,计算云层液体水含量,然后估算云层衰减。与ITU-R P.840-6模型相比,我们的结果表明,众所周知的Salonen Uppala(SU)模型意在低估热带地区的云层液态水含量和相应的云层衰减。此外,新提出的水蒸气压(WVP)云探测模型提供了相对较大的云衰减,并显示了预测热带地区云衰减的可行性。

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