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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Snow scattering signals in ground-based passive microwave radiometer measurements
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Snow scattering signals in ground-based passive microwave radiometer measurements

机译:地面无源微波辐射计测量中的雪散射信号

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This paper investigates the influence of snow microphysical parameters on the enhancement of ground-based passive microwave brightness temperature (TB) measurements. In addition to multispectral passive microwave observations between 20 and 150 GHz, a 35 GHz cloud radar and a 2-D video disdrometer for in situ measurements of snowfall were deployed as part of the "towards an optimal estimation-based snowfall characterization algorithm" campaign in the winter season of 2008-2009 at an Alpine environment located at 2650 m mean sea level. These observations are combined with nearby radiosonde ascents and surface standard meteorological measurements to reconstruct the atmospheric state (i.e., fields of temperature, humidity, snow, and liquid water contents) and are subsequently used as input for a microwave radiative transfer (RT) model. We investigate the sensitivity of the missing information about snow shape and snow particle size distribution (SSD) on the microwave TB measurements using the disdrometer data as a rough constraint. For an extended case study, we found that TBs at 90 and 150 GHz are significantly enhanced because of scattering of surface radiation at snow crystals and that this enhancement is clearly correlated with the radar derived snow water path (SWP < 0.2 kg m~(-2)). RT simulations highlight the strong influence of the vertical distribution of cloud liquid water (liquid water path LWP < 0.1 kg m~(-2)) on the TB, which in extreme cases, can fully obscure the snow scattering signal. TB variations of the same magnitude can also be caused by typical variations in SSD parameters and particle shape similar to results obtained by space-borne studies. Ground-based stations with their infrastructural capabilities in combining active and passive microwave observations have the potential to disentangle the influences of different snow shape, SSD, and SWP in snow retrievals, thus supporting current and future satellite missions.
机译:本文研究了雪的微物理参数对增强地面无源微波亮度温度(TB)测量的影响。除了在20至150 GHz之间进行多光谱无源微波观测外,还部署了35 GHz云雷达和用于降雪原位测量的2-D视频测速仪,作为“迈向基于最优估计的降雪特征算法”活动的一部分2008-2009年冬季,平均海拔2650 m的高山环境。这些观测结果与附近的探空仪上升和地面标准气象测量结果相结合,以重建大气状态(即温度,湿度,降雪和液态水含量的字段),随后被用作微波辐射传输(RT)模型的输入。我们使用微波计数据作为粗略约束,研究了微波TB测量中有关雪形和雪粒径分布(SSD)的缺失信息的敏感性。在扩展的案例研究中,我们发现90和150 GHz的TBs由于雪晶表面辐射的散射而显着增强,并且这种增强与雷达推导出的雪水路径明显相关(SWP <0.2 kg m〜(- 2))。 RT模拟突显了云状液态水的垂直分布(液态水路径LWP <0.1 kg m〜(-2))对结核病的强烈影响,在极端情况下,这可以完全掩盖雪散射信号。同样大小的TB变化也可能是由于SSD参数和颗粒形状的典型变化而引起的,类似于通过太空研究获得的结果。具有结合主动和被动微波观测的基础设施能力的地面站有可能消除积雪形状,SSD和SWP在取雪中的影响,从而支持当前和将来的卫星任务。

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