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首页> 外文期刊>Journal of Advances in Modeling Earth Systems >LMDZ6A: The Atmospheric Component of the IPSL Climate Model With Improved and Better Tuned Physics
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LMDZ6A: The Atmospheric Component of the IPSL Climate Model With Improved and Better Tuned Physics

机译:LMDZ6A:IPSL气候模型的大气成分,具有改进和更好的调谐物理学

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This study presents the version of the LMDZ global atmospheric model used as the atmospheric component of the Institut Pierre Simon Laplace coupled model (IPSL‐CM6A‐LR) to contribute to the 6th phase of the international Coupled Model Intercomparison Project (CMIP6). This LMDZ6A version includes original convective parameterizations that define the LMDZ “New Physics”: a mass flux parameterization of the organized structures of the convective boundary layer, the “thermal plume model,” and a parameterization of the cold pools created by reevaporation of convective rainfall. The vertical velocity associated with thermal plumes and gust fronts of cold pools are used to control the triggering and intensity of deep convection. Because of several shortcomings, the early version 5B of this New Physics was worse than the previous “Standard Physics” version 5A regarding several classical climate metrics. To overcome these deficiencies, version 6A includes new developments: a stochastic triggering of deep convection, a modification of the thermal plume model that allows the representation of stratocumulus and cumulus clouds in a unified framework, an improved parameterization of very stable boundary layers, and the modification of the gravity waves scheme targeting the quasi‐biennal oscillation in the stratosphere. These improvements to the physical content and a more well‐defined tuning strategy led to major improvements in the LMDZ6A version model climatology. Beyond the presentation of this particular model version and documentation of its climatology, the present paper underlines possible methodological pathways toward model improvement that can be shared across modeling groups. Plain Language Summary The improvement of global numerical models is essential for the anticipation of future climate changes. We present significant advances in the physical content of a particular atmospheric model which contributes to the simulations of the Coupled Model Intercomparison project CMIP that feed reports from the IPCC. We document in particular the improvements of the representation through “parameterizations” of convective and cloudy processes. The article emphasizes the importance of strengthening the formalization of the methodology of development and tuning of models, so that new physical ideas can be translated into effective improvement of the climate representation.
机译:本研究介绍了LMDZ全球大气模型的版本,用作Institut Pierre Simon Laplace耦合模型(IPSL-CM6A-LR)的大气成分,以有助于国际耦合模型互通项目的第6阶段(CMIP6)。该LMDZ6A版本包括定义LMDZ“新物理学”的原始对流参数化:对流边界层的有组织结构的质量磁通参数化,“热羽模型”,以及通过Reevapive降雨创建的冷库的参数化。与冷池的热羽毛和阵风前方相关的垂直速度用于控制深对流的触发和强度。由于几个缺点,这种新物理学的早期版本5B比以前的“标准物理”版本5A有关几种古典气候指标。为了克服这些缺陷,版本6a包括新的发展:对深度对流的随机触发,允许在统一的框架中的划分模型和积云表示的热羽云模型的变形例,改进了非常稳定的边界层的参数化,以及重力波方案瞄准平流层中的准生物振荡的重力波方案。这些改善物理内容和更明确的调整策略导致了LMDZ6A版本模型气候学的重大改进。除了介绍这一特殊模型版本和其气候学的文档之外,本文提出了可能在建模组中共享的模型改进的可能方法途径。简单语言摘要全球数值模型的改进对于预期未来的气候变化至关重要。我们对特定大气模型的物理内容提出了显着的进展,这有助于模拟来自IPCC的耦合模型互通项目CMIP的模拟。我们尤其记录通过对流和多云流程的“参数化”的说明改进。本文强调加强发展和调整模式的方法形式化的重要性,使新的物理思想可以转化为有效改善气候代表性。
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