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The response of the middle atmosphere to anthropogenic and natural forcing in the CMIP5 simulations with the MPI-ESM

机译:在mpIp-Esm的CmIp5模拟中,中层大气对人为和自然强迫的响应

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摘要

The ECHAM6 atmospheric general circulation model is the atmosphere component of the Max Planck Institute Earth System Model (MPI-ESM) that is used in the Coupled Model Intercomparison Project Phase 5 (CMIP5) simulations. As ECHAM6 has its uppermost layer centered at 0.01 hPa in the upper mesosphere, these simulations offer the opportunity to study the middle atmosphere climate change and its relation to the troposphere on the basis of a very comprehensive set of state-of-the-art model simulations. The goals of this paper are (a) to introduce those new features of ECHAM6 particularly relevant for the middle atmosphere, including external forcing data, and (b) to evaluate the simulated middle atmosphere and describe the simulated response to natural and anthropogenic forcings. New features in ECHAM6 with respect to ECHAM5 include a new short-wave radiation scheme, the option to vary spectral irradiance independent of total solar irradiance, and a latitude-dependent gravity-wave source strength. The description of external forcing data focuses on solar irradiance and ozone. Stratospheric temperature trends simulated with the MPI-ESM for the last decades of the 20th century agree well with observations. The future projections depend strongly on the scenario. Under the high emission scenario RCP8.5, simulated temperatures are locally lower by more than 20 K than preindustrial values. Many of the simulated patterns of the responses to natural forcings as provided by solar variability, volcanic aerosols, and El Niño-Southern Oscillation, largely agree with the observations. © 2013. American Geophysical Union. All Rights Reserved.
机译:ECHAM6大气总循环模型是马克斯·普朗克研究所地球系统模型(MPI-ESM)的大气成分,该模型在耦合模型比较项目第5阶段(CMIP5)模拟中使用。由于ECHAM6的最上层位于中高层的0.01 hPa,这些模拟为基于非常先进的最新模型研究中层大气气候变化及其与对流层的关系提供了机会模拟。本文的目标是(a)引入ECHAM6的那些与中间大气特别相关的新功能,包括外部强迫数据,以及(b)评估模拟的中间大气并描述模拟的对自然和人为强迫的响应。与ECHAM5相比,ECHAM6的新功能包括新的短波辐射方案,可以独立于总太阳辐照度改变光谱辐照度的选项以及与纬度相关的重力波源强度。外部强迫数据的描述着重于太阳辐照度和臭氧。用MPI-ESM模拟的20世纪最后几十年的平流层温度趋势与观测值非常吻合。未来的预测在很大程度上取决于情景。在高排放情景RCP8.5下,局部模拟温度比工业化前的温度低20 K以上。太阳变化,火山气溶胶和厄尔尼诺-南方涛动提供的许多对自然强迫响应的模拟模式在很大程度上与观测结果一致。 ©2013。美国地球物理联盟。版权所有。

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