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

被引:247
作者
Ji, D. [1 ]
Wang, L. [1 ]
Feng, J. [1 ]
Wu, Q. [1 ]
Cheng, H. [1 ]
Zhang, Q. [1 ]
Yang, J. [2 ]
Dong, W. [2 ]
Dai, Y. [1 ]
Gong, D. [2 ]
Zhang, R. -H. [3 ,4 ]
Wang, X. [4 ]
Liu, J. [5 ]
Moore, J. C. [1 ]
Chen, D. [6 ]
Zhou, M. [7 ]
机构
[1] Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China
[2] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource, Beijing 100875, Peoples R China
[3] Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
[4] Univ Maryland, ESSIC, College Pk, MD 20742 USA
[5] SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY 12222 USA
[6] Natl Parallel Comp Engn Technol Res Ctr, Beijing 100190, Peoples R China
[7] Jiangnan Inst Comp Technol, Wuxi 214083, Peoples R China
基金
中国国家自然科学基金;
关键词
MADDEN-JULIAN OSCILLATION; CONVECTIVE MOMENTUM TRANSPORT; COMMUNITY ATMOSPHERE MODEL; CMIP5 MULTIMODEL ENSEMBLE; COUPLED EQUATORIAL WAVES; STOCHASTIC MIXING MODEL; GLOBAL PRECIPITATION; CLIMATE MODELS; PACIFIC-OCEAN; EL-NINO;
D O I
10.5194/gmd-7-2039-2014
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
An earth system model has been developed at Beijing Normal University (Beijing Normal University Earth System Model, BNU-ESM); the model is based on several widely evaluated climate model components and is used to study mechanisms of ocean-atmosphere interactions, natural climate variability and carbon-climate feedbacks at inter-annual to interdecadal time scales. In this paper, the model structure and individual components are described briefly. Further, results for the CMIP5 (Coupled Model Intercomparison Project phase 5) pre-industrial control and historical simulations are presented to demonstrate the model's performance in terms of the mean model state and the internal variability. It is illustrated that BNU-ESM can simulate many observed features of the earth climate system, such as the climatological annual cycle of surface-air temperature and precipitation, annual cycle of tropical Pacific sea surface temperature (SST), the overall patterns and positions of cells in global ocean meridional overturning circulation. For example, the El Nino-Southern Oscillation (ENSO) simulated in BNU-ESM exhibits an irregular oscillation between 2 and 5 years with the seasonal phase locking feature of ENSO. Important biases with regard to observations are presented and discussed, including warm SST discrepancies in the major upwelling regions, an equatorward drift of midlatitude westerly wind bands, and tropical precipitation bias over the ocean that is related to the double Intertropical Convergence Zone (ITCZ).
引用
收藏
页码:2039 / 2064
页数:26
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