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The transpose-AMIP II experiment and its application to the understanding of Southern Ocean cloud biases in climate models.

机译:Transpose-AMIP II实验及其在气候模型中对了解南大洋云偏见的应用。

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摘要

The Transpose-Atmospheric Model Intercomparison Project (AMIP) is an international model intercomparison project in which climate models are run in "weather forecast mode." The Transpose-AMIP II experiment is run alongside phase 5 of the Coupled Model Intercomparison Project (CMIP5) and allows processes operating in climate models to be evaluated, and the origin of climatological biases to be explored, by examining the evolution of the model from a state in which the large-scale dynamics, temperature, and humidity structures are constrained through use of common analyses. The Transpose-AMIP II experimental design is presented. The project requests participants to submit a comprehensive set of diagnostics to enable detailed investigation of the models to be performed. An example of the type of analysis that may be undertaken using these diagnostics is illustrated through a study of the development of cloud biases over the Southern Ocean, a region that is problematic for many models. Several models share a climatological bias for too little reflected shortwave radiation from cloud across the region. This is found to mainly occur behind cold fronts and/or on the leading side of transient ridges and to be associated with more stable lower-tropospheric profiles. Investigation of a case study that is typical of the bias and associated meteorological conditions reveals the models to typically simulate cloud that is too optically and physically thin with an inversion that is too low. The evolution of the models within the first few hours suggests that these conditions are particularly sensitive and a positive feedback can develop between the thinning of the cloud layer and boundary layer structure.
机译:换位大气模型比对项目(AMIP)是一个国际模型比对项目,其中气候模型以“天气预报模式”运行。 Transpose-AMIP II实验与耦合模型比对项目(CMIP5)的第5阶段同时进行,通过检查模型的演变来评估气候模型中的过程,并探讨气候偏差的成因。通过使用常规分析来限制大规模动力学,温度和湿度结构的状态。介绍了Transpose-AMIP II实验设计。该项目要求参与者提交一套全面的诊断程序,以对要执行的模型进行详细调查。通过对南大洋云偏向的发展进行研究,可以说明使用这些诊断程序可以进行的分析类型的一个例子,该地区对许多模型都存在问题。对于整个区域中来自云的反射短波辐射过少,一些模型具有共同的气候偏见。发现这主要发生在冷锋的后方和/或瞬变脊的前侧,并与更稳定的低对流层剖面有关。对典型的偏见和相关气象条件进行案例研究后发现,该模型通常模拟光学和物理上太薄而反演值太低的云。在最初的几个小时内,模型的演变表明这些条件特别敏感,并且在云层变薄和边界层结构之间会产生正反馈。

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