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DOI | 10.1007/s00382-018-4528-1 |
Seasonal climatic effects and feedbacks of anthropogenic heat release due to global energy consumption with CAM5 | |
Chen, Bing1,2,3; Wu, C.2,5; Liu, X.2; Chen, L.4; Wu, Jian1; Yang, H.6; Luo, Tao7; Wu, Xue5; Jiang, Yiquan8; Jiang, Lei9; Brown, H. Y.2; Lu, Z.2; Fan, W.1; Lin, G.2; Sun, Bo9; Wu, M.2 | |
发表日期 | 2019 |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
卷号 | 52期号:11页码:6377-6390 |
英文摘要 | Anthropogenic heat release (AHR) is the heat generated in global energy consumption, which has not been considered in global climate models generally. The global high-resolution AHR from 1992 to 2013, which is estimated by using the Defense Meteorological Satellite Program (DMSP)/Operational Linescan System (OLS) satellite data, is implemented into the Community Atmosphere Model version 5 (CAM5). The seasonal climatic effects and possible feedbacks of AHR are examined in this study. The modeling results show that AHR increases the global annual mean surface temperature and land surface temperature by 0.02 +/- 0.01K (1 sigma uncertainty) and 0.05 +/- 0.02K (1 sigma uncertainty), respectively. The global climatic effect of AHR varies with season: with a stronger climatic effect in the boreal winter leading to global mean land surface temperature increases by 0.10 +/- 0.01K (1 sigma uncertainty). In the selected regions (40 degrees N-60 degrees N, 0 degrees E-45 degrees E) of Central and Western Europe the average surface temperature increases by 0.46K in the boreal summer, and in the selected regions (45 degrees N-75 degrees N, 30 degrees E-140 degrees E) of northern Eurasia the average surface temperature increases by 0.83K in the boreal winter. AHR changes the height and thermodynamic structure of the global planetary boundary layer, as well as the stability of the lower troposphere, which affects the global atmospheric circulation and low cloud fraction. In addition, at the surface both the shortwave radiation flux in the boreal summer and the down-welling longwave flux in the boreal winter change significantly, as a result of the change in low clouds caused by the effect of AHR. This study suggests a possible new mechanism of AHR effect on global climate through changing the global low-cloud fraction, which is crucial for global energy balance, by modifying the thermodynamic structure and stability of the lower troposphere. Thus this study improves our understanding of the global climate change caused by human activities. |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源期刊 | CLIMATE DYNAMICS
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/98833 |
作者单位 | 1.Yunnan Univ, Key Lab Atmospher Environm & Proc Boundary Layer, Dept Atmospher Sci, Kunming 650091, Yunnan, Peoples R China; 2.Univ Wyoming, Dept Atmospher Sci, Laramie, WY 82071 USA; 3.Tsinghua Univ, Minist Educ, Key Lab Earth Syst Modeling, Beijing 100084, Peoples R China; 4.Chinese Acad Sci, State Key Lab Remote Sensing Sci, Inst Remote Sensing & Digital Earth, Beijing 100101, Peoples R China; 5.Chinese Acad Sci, Inst Atmospher Phys, Beijing 100029, Peoples R China; 6.Univ Leeds, Sch Earth & Environm, ICAS, Leeds LS2 9JTV, W Yorkshire, England; 7.Chinese Acad Sci, Hefei Inst Phys Sci, Hefei 230031, Anhui, Peoples R China; 8.Nanjing Univ, CMA NJU Joint Lab Climate Predict Studies, Inst Climate & Global Change Res, Sch Atmospher Sci, Nanjing, Jiangsu, Peoples R China; 9.Nanjing Univ Informat Sci & Technol, Nanjing 210044, Jiangsu, Peoples R China |
推荐引用方式 GB/T 7714 | Chen, Bing,Wu, C.,Liu, X.,et al. Seasonal climatic effects and feedbacks of anthropogenic heat release due to global energy consumption with CAM5[J],2019,52(11):6377-6390. |
APA | Chen, Bing.,Wu, C..,Liu, X..,Chen, L..,Wu, Jian.,...&Wu, M..(2019).Seasonal climatic effects and feedbacks of anthropogenic heat release due to global energy consumption with CAM5.CLIMATE DYNAMICS,52(11),6377-6390. |
MLA | Chen, Bing,et al."Seasonal climatic effects and feedbacks of anthropogenic heat release due to global energy consumption with CAM5".CLIMATE DYNAMICS 52.11(2019):6377-6390. |
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