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The Nonhydrostatic ICosahedral Atmospheric Model for CMIP6 HighResMIP simulations (NICAM16-S): experimental design, model description, and impacts of model updates

机译:CMIP6高次数模拟的非水型ICOSAHEDRAL大气模型(NICAM16-S):模型更新的实验设计,模型描述和影响

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The Nonhydrostatic ICosahedral Atmospheric Model (NICAM), a global model with an icosahedral grid system, has been under development for nearly two decades. This paper describes NICAM16-S, the latest stable version of NICAM (NICAM.16), modified for the Coupled Model Intercomparison Project Phase 6, High Resolution Model Intercomparison Project (HighResMIP). Major updates of NICAM.12, a previous version used for climate simulations, included updates of the cloud microphysics scheme and land surface model, introduction of natural and anthropogenic aerosols and a subgrid-scale orographic gravity wave drag scheme, and improvement of the coupling between the cloud microphysics and the radiation schemes. External forcings were updated to follow the protocol of the HighResMIP. A series of short-term sensitivity experiments were performed to determine and understand the impacts of these various model updates on the simulated mean states. The NICAM16-S simulations demonstrated improvements in the ice water content, high cloud amount, surface air temperature over the Arctic region, location and strength of zonal mean subtropical jet, and shortwave radiation over Africa and South Asia. Some long-standing biases, such as the double intertropical convergence zone and smaller low cloud amount, still exist or are even worse in some cases, suggesting further necessity for understanding their mechanisms, upgrading schemes and parameter settings, and enhancing horizontal and vertical resolutions.
机译:非水型icosahe向量大气模型(NiCAM)是一个具有ICOSaheDral网格系统的全球模型,已经在近二十年的发展中被开发。本文介绍了NiCAM16-S,最新稳定版的NICAM(NICAM.16),修改了耦合型号离读项目阶段6,高分辨率模型离校学项目(HIGHRESMIP)。 Nicam.12的主要更新,用于气候仿真的先前版本,包括云微观物理方案和陆地表面模型的更新,介绍天然和人为气溶胶的介绍以及划分级的地形重力波阻力波动方案,以及改善耦合之间的耦合云微孔和辐射方案。更新外部迫使以遵循高级胶片的协议。进行一系列短期敏感性实验以确定和理解这些各种模型更新对模拟平均状态的影响。 NiCAM16-S仿真在冰水含量,高云量,北极地区的表面空气温度,区域平均亚热带射流的位置和强度,以及非洲和南亚的短波辐射的改善。在某些情况下,一些长期偏差,例如双闭闭趋势和较小的低云量,仍然存在或甚至更差,表明了解其机制,升级方案和参数设置以及增强水平和垂直分辨率的进一步需要。

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