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Description and basic evaluation of Beijing Normal University Earth System Model (BNU-ESM) version 1

机译:北京师范大学地球系统模型(BNU-ESM)版本1的描述和基本评估

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摘要

An earth system model has been developed at Beijing Normal University(Beijing Normal University Earth System Model, BNU-ESM); the model is basedon several widely evaluated climate model components and is used to studymechanisms of ocean-atmosphere interactions, natural climate variability andcarbon-climate feedbacks at interannual to interdecadal time scales. In thispaper, the model structure and individual components are described briefly.Further, results for the CMIP5 (Coupled Model Intercomparison Project phase5) pre-industrial control and historical simulations are presented todemonstrate the model's performance in terms of the mean model state and theinternal variability. It is illustrated that BNU-ESM can simulate manyobserved features of the earth climate system, such as the climatologicalannual cycle of surface-air temperature and precipitation, annual cycle oftropical Pacific sea surface temperature (SST), the overall patterns andpositions of cells in global ocean meridional overturning circulation. Forexample, the El Ni?o-Southern Oscillation (ENSO) simulated in BNU-ESMexhibits an irregular oscillation between 2 and 5 years with the seasonalphase locking feature of ENSO. Important biases with regard to observationsare presented and discussed, including warm SST discrepancies in the majorupwelling regions, an equatorward drift of midlatitude westerly wind bands,and tropical precipitation bias over the ocean that is related to the doubleIntertropical Convergence Zone (ITCZ).
机译:北京师范大学已经开发了一个地球系统模型(北京师范大学地球系统模型,BNU-ESM);该模型基于几个被广泛评估的气候模型组成部分,用于研究年际至年代际尺度上海洋与大气相互作用,自然气候变异性和碳-气候反馈的机制。本文简要介绍了模型的结构和各个组成部分。此外,还提出了CMIP5(模型比较项目的第5阶段)工业化前控制和历史模拟的结果,以从模型平均状态和内部可变性方面证明了模型的性能。结果表明,BNU-ESM可以模拟地球气候系统的许多观测特征,如地表空气温度和降水的气候年循环,热带太平洋海表温度(SST)的年循环,全球海洋中细胞的整体模式和位置​​。经络翻转循环。例如,在BNU-ESM中模拟的厄尔尼诺-南方涛动(ENSO)表现出2年到5年之间的不规则振荡,并且具有ENSO的季节性锁相特征。提出并讨论了与观测有关的重要偏差,包括主要上升区的暖海温差异,中纬度西风带的赤道漂移以及与双热带辐合带(ITCZ)有关的海洋上的热带降水偏差。

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