Development and evaluation of an Earth System Model with surface gravity waves

doi:10.1002/jgrc.20327

CORC > 自然资源部第一海洋研究所 > 自然资源部第一海洋研究所 > 业务部门 > 海洋环境与数值模拟研究室

	Development and evaluation of an Earth System Model with surface gravity waves
	Qiao, Fangli; Song, Zhenya; Bao, Ying; Song, Yajuan; Shu, Qi; Huang, Chuanjiang; Zhao, Wei
刊名	JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
	2013-09
卷号	118 期号:9 页码:4514-4524
关键词	Earth System Model surface wave model development
ISSN号	2169-9275
DOI	10.1002/jgrc.20327
英文摘要	The critical role of oceanic surface waves in climate system is attracting more and more attention. We set up an Earth System Model, which is named as the First Institute of Oceanography-Earth System Model (FIO-ESM), composed of a coupled physical climate model and a coupled carbon cycle model. A surface wave model is introduced through including the nonbreaking wave-induced vertical mixing, which can improve the performance of climate model especially in the simulation of upper ocean mixed layer depth in the southern ocean, into the ocean general circulation model. The FIO-ESM is employed to conduct Coupled Model Intercomparison Project Phase 5 (CMIP5) experiments. The historical simulation of FIO-ESM's physical climate model for 1850-2005 shows that the simulated patterns of surface air temperature (SAT), rainfall, and El Nino-Southern Oscillation (ENSO) match those of the observations. Future projections under the four scenarios of RCP2.6, RCP4.5, RCP6.0, and RCP8.5 are also conducted and the global averaged SAT in 2100 would be -0.007 degrees C, 1.10 degrees C, 1.85 degrees C, and 3.92 degrees C higher than that in 2005, respectively. The historical simulation and future projection under RCP8.5 with global carbon cycle show the SAT and atmospheric CO2 concentration are well reproduced in the historical period and the global averaged SAT would increase by 3.90 degrees C in 2100, which is quite similar to the physical climate model's result. Further analysis shows surface wave makes projected SAT in RCP2.6 about 2 degrees C cooler in the Arctic area and 2 degrees C warmer in the southern ocean.
资助项目	National Basic Research Program of China (973 Program)[2010CB950300] ; National Basic Research Program of China (973 Program)[2010CB950500]
WOS研究方向	Oceanography
语种	英语
出版者	AMER GEOPHYSICAL UNION
WOS记录号	WOS:000326230200034
内容类型	期刊论文
源URL	[http://ir.fio.com.cn/handle/2SI8HI0U/3931]
专题	业务部门_海洋环境与数值模拟研究室
作者单位	State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sci & Numer Modeling, Qingdao 266061, Peoples R China
推荐引用方式 GB/T 7714	Qiao, Fangli,Song, Zhenya,Bao, Ying,et al. Development and evaluation of an Earth System Model with surface gravity waves[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2013,118(9):4514-4524.
APA	Qiao, Fangli.,Song, Zhenya.,Bao, Ying.,Song, Yajuan.,Shu, Qi.,...&Zhao, Wei.(2013).Development and evaluation of an Earth System Model with surface gravity waves.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,118(9),4514-4524.
MLA	Qiao, Fangli,et al."Development and evaluation of an Earth System Model with surface gravity waves".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 118.9(2013):4514-4524.