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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >No evidence for solar absorption anomaly by marine water clouds through collocated aircraft radiation measurements
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No evidence for solar absorption anomaly by marine water clouds through collocated aircraft radiation measurements

机译:通过并置的飞机辐射测量,没有证据表明海洋水云会吸收太阳光

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摘要

No observational evidence was found for the so-called anomalous solar absorption by maritime water clouds through collocated aircraft measurements taken during the Japanese Cloud-Climate Study (JACCS) program. The aircraft experiment has been carried out by using two aircraft equipped with various instruments fur wintertime stratocumulus clouds over an area centered at (29 degrees N, 129 degrees E) in the East China Sea. Here we have carefully analyzed solar absorption by the water stratocumulus clouds observed on February 2, 1998. The visible-band net fluxes measured above and below the cloud layer were almost the same within measurement accuracy; this means no substantial absorption in the visible spectral region, On the other hand, there were significant differences as between the near-infrared-band net fluxes measured above and much as 50-80 W m(-2) between the near-infrared-band net fluxes measured above and below the cloud layer; this difference corresponds to absorptance of 6-10% of the total-band solar irradiance above the cloud layer, Without cloud particles, water vapor absorption was estimated to be about 4% of the total-band irradiance for the layer. Distributions along the night legs of the measured visible-band and near-infrared-band absorptance were in phase in their positions with zero mean visible-band absorptance. The measured radiation budget averaged over long distances along the flight legs for the inhomogeneous cloud layers agreed well with theoretical counterparts calculated for plane-parallel, homogeneous cloud models based on the observed microphysical parameters. [References: 29]
机译:在日本的云气候研究(JACCS)计划期间,通过并置飞机测量,没有发现观测到的证据证明海上水云对太阳的吸收异常。该飞机实验是通过在东海以29度N,129度E为中心的两架装有各种仪器的冬季平层积云进行的飞机上进行的。在这里,我们仔细分析了1998年2月2日观测到的层状积云对太阳的吸收。在云层之上和之下测得的可见带净通量在测量精度范围内几乎是相同的。这意味着在可见光谱范围内没有实质性的吸收。另一方面,上述测量的近红外净通量与近红外光谱之间的高达50-80 W m(-2)之间存在显着差异。在云层上方和下方测得的带净通量;该差异对应于云层上方总波段太阳辐照度的6-10%的吸收率。如果没有云颗粒,则估计水蒸气吸收约为该层总波段辐照度的4%。沿测得的可见光带吸收率和近红外光带吸收率的夜间腿部分布在它们的位置同相,平均可见光带吸收率为零。对于不均匀的云层,沿着飞行腿在长距离上测得的平均辐射预算与基于观测到的微物理参数为平面平行,均匀的云模型计算的理论对应物非常吻合。 [参考:29]

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