首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Assessment of marine boundary layer cloud simulations in the CAM with CLUBB and updated microphysics scheme based on ARM observations from the Azores
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Assessment of marine boundary layer cloud simulations in the CAM with CLUBB and updated microphysics scheme based on ARM observations from the Azores

机译:基于CLUBB的CAM中海洋边界层云模拟的评估以及基于亚速尔群岛ARM观测结果的最新微物理方案

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To assess marine boundary layer (MBL) cloud simulations in three versions of the Community Atmosphere Model (CAM), three sets of short-term global hindcasts are performed and compared to Atmospheric Radiation Measurement Program (ARM) observations on Graciosa Island in the Azores from June 2009 to December 2010. The three versions consist of CAM5.3 with default schemes (CAM5.3), CAM5.3 with Cloud Layers Unified By Binormals (CLUBB-MG1), and CAM5.3 with CLUBB and updated microphysics scheme (CLUBB-MG2). Our results show that relative to CAM5.3 default schemes, simulations with CLUBB better represent MBL cloud base height, the height of the major cloud layer, and the daily cloud cover variability. CLUBB also better simulates the relationship of cloud fraction to cloud liquid water path (LWP) most likely due to CLUBB's consistent treatment of these variables through a probability distribution function (PDF) approach. Subcloud evaporation of precipitation is substantially enhanced in simulations with CLUBB-MG2 and is more realistic based on the limited observational estimate. Despite these improvements, all model versions underestimate MBL cloud cover. CLUBB-MG2 reduces biases in in-cloud LWP (clouds are not too bright) but there are still too few of MBL clouds due to an underestimate in the frequency of overcast scenes. Thus, combining CLUBB with MG2 scheme better simulates MBL cloud processes, but because biases remain in MBL cloud cover CLUBB-MG2 does not improve the simulation of the surface shortwave cloud radiative effect (CRE_(SW)).
机译:为了评估三种版本的社区大气模型(CAM)中的海洋边界层(MBL)云模拟,执行了三组短期全球后预报并将其与亚速尔群岛上亚速尔群岛的Graciosa岛上的大气辐射测量程序(ARM)观测结果进行了比较。 2009年6月至2010年12月。这三个版本包括具有默认方案的CAM5.3(CAM5.3),具有由双态统一统一的云层的CAM5.3(CLUBB-MG1)和具有CLUBB和更新的微物理学方案(CLUBB)的CAM5.3。 -MG2)。我们的结果表明,相对于CAM5.3默认方案,使用CLUBB进行的模拟可以更好地表示MBL云底高度,主要云层的高度和每日云量的变化。由于CLUBB通过概率分布函数(PDF)方法对这些变量的一致处理,CLUBB还可以更好地模拟云分数与云液态水路径(LWP)的关系。在使用CLUBB-MG2进行的模拟中,降水的亚云蒸发大大增强,基于有限的观测估计,这种蒸发更加现实。尽管进行了这些改进,但是所有模型版本都低估了MBL云覆盖率。 CLUBB-MG2减少了云内LWP(云不太亮)中的偏差,但是由于低估了阴暗场景的频率,MBL云仍然很少。因此,将CLUBB与MG2方案结合可以更好地模拟MBL云过程,但是由于MBL云覆盖中仍然存在偏差,因此CLUBB-MG2不能改善表面短波云辐射效应(CRE_(SW))的模拟。

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