Järvinen E, Vochezer P, Möhler O, Schnaiter M
Appl Opt. 2014 Nov 1;53(31):7566-75. doi: 10.1364/AO.53.007566.
Corona-producing cirrus clouds were generated and measured under chamber conditions at the AIDA cloud chamber in Karlsruhe. We were able to measure the scattering properties as well as microphysical properties of these clouds under well-defined laboratory conditions in contrast with previous studies of corona-producing clouds, where the measurements were conducted by means of lidar and in situ aircraft measurements. Our results are in agreement with those of previous studies, confirming that corona-producing cirrus clouds consist of a narrow distribution of small (median D=19-32 μm) and compact ice crystals. We showed that the ice crystals in these clouds are most likely formed in homogeneous freezing processes. As a result of the homogeneous freezing process, the ice crystals grow uniformly in size; furthermore, the majority of the ice crystals have rough surface features.
在卡尔斯鲁厄的AIDA云室的室内条件下生成并测量了产生日冕的卷云。与之前对产生日冕的云的研究相比,我们能够在明确的实验室条件下测量这些云的散射特性以及微物理特性,之前的研究是通过激光雷达和飞机原位测量进行的。我们的结果与之前的研究一致,证实产生日冕的卷云由小的(中值直径D = 19 - 32μm)且致密的冰晶的窄分布组成。我们表明这些云中的冰晶很可能是在均匀冻结过程中形成的。由于均匀冻结过程,冰晶尺寸均匀增长;此外,大多数冰晶具有粗糙的表面特征。