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DOI | 10.1007/s00382-018-4401-2 |
Changes in clouds and atmospheric circulation associated with rapid adjustment induced by increased atmospheric CO2: a multiscale modeling framework study | |
Xu K.-M.; Li Z.; Cheng A.; Hu Y. | |
发表日期 | 2020 |
ISSN | 0930-7575 |
起始页码 | 277 |
结束页码 | 293 |
卷号 | 55 |
英文摘要 | The radiative heating increase due to increased CO2 concentration is the primary source for the rapid adjustment of atmospheric circulation and clouds. In this study, we investigate the rapid adjustment resulting from an instantaneous doubling of CO2 and its physical mechanism using a multiscale modeling framework (MMF). The cloud-resolving model component of this MMF includes a sophisticated third-order turbulence closure and the MMF simulates realistic shallow and deep cloud climatology and boundary layer turbulence. Although the simulated cloud adjustment and its mechanism generally agree with earlier studies with conventional global climate models and another MMF with a lower-order turbulence closure, this MMF simulates an increase in the global-mean shortwave and net cloud radiative cooling and a negative cloud radiative effect change due to cloud adjustment. This result is related to the large increase in low-level clouds over the extratropical and subtropical oceans, resulting from reduced cloud-top entrainment implied from strengthened inversion. The downshift of planetary boundary layer and low-level clouds is generally weaker than that simulated by other models, which is due to reduction of shallow cumulus in the ascending and weak subsidence circulation regimes but to increase of stratocumulus in the strongest subsidence regime. Optically thicker stratocumulus compensates for reduced cooling by shallow cumulus. The reduced strength of all oceanic circulation regimes, which may be contributed by weakened energy transport resulting from water vapor and cloud CO2 masking effects, not only reduces optical depth of convective clouds but also shifts cloud coverage to lands where deep convection is enhanced. © 2018, The Author(s). |
英文关键词 | Cloud radiative effects; CO2 forcing; Low-level clouds; Multiscale modeling framework; Rapid adjustment |
语种 | 英语 |
scopus关键词 | atmospheric circulation; atmospheric convection; boundary layer; carbon dioxide; climate modeling; cloud radiative forcing |
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/145417 |
作者单位 | Science Directorate, NASA Langley Research Center, Mail Stop 420, Hampton, VA 23681, United States; NASA Postdoctoral Program, Universities Space Research Association, Hampton, VA, United States; NOAA EMC/NCEP, College Park, MD, United States |
推荐引用方式 GB/T 7714 | Xu K.-M.,Li Z.,Cheng A.,et al. Changes in clouds and atmospheric circulation associated with rapid adjustment induced by increased atmospheric CO2: a multiscale modeling framework study[J],2020,55. |
APA | Xu K.-M.,Li Z.,Cheng A.,&Hu Y..(2020).Changes in clouds and atmospheric circulation associated with rapid adjustment induced by increased atmospheric CO2: a multiscale modeling framework study.Climate Dynamics,55. |
MLA | Xu K.-M.,et al."Changes in clouds and atmospheric circulation associated with rapid adjustment induced by increased atmospheric CO2: a multiscale modeling framework study".Climate Dynamics 55(2020). |
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