Lofverstrom Marcus, Fyke Jeremy G, Thayer-Calder Katherine, Muntjewerf Laura, Vizcaino Miren, Sacks William J, Lipscomb William H, Otto-Bliesner Bette L, Bradley Sarah L
Department of Geosciences University of Arizona Tucson AZ USA.
Climate and Global Dynamics Laboratory National Center for Atmospheric Research Boulder CO USA.
J Adv Model Earth Syst. 2020 Aug;12(8):e2019MS001984. doi: 10.1029/2019MS001984. Epub 2020 Aug 22.
Spinning up a highly complex, coupled Earth system model (ESM) is a time consuming and computationally demanding exercise. For models with interactive ice sheet components, this becomes a major challenge, as ice sheets are sensitive to bidirectional feedback processes and equilibrate over glacial timescales of up to many millennia. This work describes and demonstrates a computationally tractable, iterative procedure for spinning up a contemporary, highly complex ESM that includes an interactive ice sheet component. The procedure alternates between a computationally expensive coupled configuration and a computationally cheaper configuration where the atmospheric component is replaced by a data model. By periodically regenerating atmospheric forcing consistent with the coupled system, the data atmosphere remains adequately constrained to ensure that the broader model state evolves realistically. The applicability of the method is demonstrated by spinning up the preindustrial climate in the Community Earth System Model Version 2 (CESM2), coupled to the Community Ice Sheet Model Version 2 (CISM2) over Greenland. The equilibrium climate state is similar to the control climate from a coupled simulation with a prescribed Greenland ice sheet, indicating that the iterative procedure is consistent with a traditional spin-up approach without interactive ice sheets. These results suggest that the iterative method presented here provides a faster and computationally cheaper method for spinning up a highly complex ESM, with or without interactive ice sheet components. The method described here has been used to develop the climate/ice sheet initial conditions for transient, ice sheet-enabled simulations with CESM2-CISM2 in the Coupled Model Intercomparison Project Phase 6 (CMIP6).
运行一个高度复杂的耦合地球系统模型(ESM)是一项耗时且计算要求很高的工作。对于具有交互式冰盖组件的模型来说,这成为一项重大挑战,因为冰盖对双向反馈过程敏感,并且在长达数千年的冰川时间尺度上达到平衡。这项工作描述并展示了一种计算上可行的迭代程序,用于启动一个包含交互式冰盖组件的当代高度复杂的ESM。该程序在计算成本高昂的耦合配置和计算成本较低的配置之间交替,在后者中大气组件被数据模型取代。通过定期重新生成与耦合系统一致的大气强迫,数据大气仍能得到充分约束,以确保更广泛的模型状态能现实地演变。通过在社区地球系统模型版本2(CESM2)中启动工业化前气候,并与格陵兰岛上的社区冰盖模型版本2(CISM2)耦合,证明了该方法的适用性。平衡气候状态与使用规定的格陵兰冰盖进行耦合模拟的控制气候相似,这表明迭代程序与没有交互式冰盖的传统启动方法一致。这些结果表明,这里提出的迭代方法为启动高度复杂的ESM提供了一种更快且计算成本更低的方法,无论是否具有交互式冰盖组件。这里描述的方法已被用于为耦合模式比较计划第6阶段(CMIP6)中使用CESM2 - CISM2进行的具有冰盖的瞬态模拟开发气候/冰盖初始条件。