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DOI | 10.1175/JCLI-D-20-0204.1 |
Observational evidence that radiative heating modifies the life cycle of tropical anvil clouds | |
Wall C.J.; Norris J.R.; Gasparini B.; Smith W.L.; Thieman M.M.; Sourdeval O. | |
发表日期 | 2021 |
ISSN | 0894-8755 |
起始页码 | 8621 |
结束页码 | 8640 |
卷号 | 33期号:20 |
英文摘要 | A variety of satellite and ground-based observations are used to study how diurnal variations of cloud radiative heating affect the life cycle of anvil clouds over the tropical western Pacific Ocean. High clouds thicker than 2 km experience longwave heating at cloud base, longwave cooling at cloud top, and shortwave heating at cloud top. The shortwave and longwave effects have similar magnitudes during midday, but only the longwave effect is present at night, so high clouds experience a substantial diurnal cycle of radiative heating. Furthermore, anvil clouds are more persistent or laterally expansive during daytime. This cannot be explained by variations of convective intensity or geographic patterns of convection, suggesting that shortwave heating causes anvil clouds to persist longer or spread over a larger area. It is then investigated if shortwave heatingmodifies anvil development by altering turbulence in the cloud. According to one theory, radiative heating drives turbulent overturning within anvil clouds that can be sufficiently vigorous to cause ice nucleation in the updrafts, thereby extending the cloud lifetime. High-frequency air motionand ice-crystalnumber concentration are shown tobe inversely related near cloud top, however. This suggests that turbulence depletes or disperses ice crystals at a faster rate than it nucleates them, so another mechanism must cause the diurnal variation of anvil clouds. It is hypothesized that radiative heating affects anvil development primarily by inducing a mesoscale circulation that offsets gravitational settling of cloud particles. © 2020 American Meteorological Society. All rights reserved. |
英文关键词 | Heat radiation; Ice; Tropics; Turbulence; Convective intensity; Diurnal variation; Geographic pattern; Gravitational settlings; Ground-based observations; Mesoscale circulation; Radiative heating; Tropical Western Pacific; Radiant heating; atmospheric convection; cloud microphysics; convective cloud; diurnal variation; mesoscale meteorology; radiative transfer; Pacific Ocean |
语种 | 英语 |
来源期刊 | Journal of Climate
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/170918 |
作者单位 | Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, United States; Department of Atmospheric Sciences, University of Washington, Seattle, WA, United States; Nasa Langley Research Center, Hampton, VA, United States; Science Systems and Applications, Inc., Hampton, VA, United States; Umr 8518-Laboratoire d'Optique Atmosphérique, University of Lille, Cnrs, Lille, France |
推荐引用方式 GB/T 7714 | Wall C.J.,Norris J.R.,Gasparini B.,et al. Observational evidence that radiative heating modifies the life cycle of tropical anvil clouds[J],2021,33(20). |
APA | Wall C.J.,Norris J.R.,Gasparini B.,Smith W.L.,Thieman M.M.,&Sourdeval O..(2021).Observational evidence that radiative heating modifies the life cycle of tropical anvil clouds.Journal of Climate,33(20). |
MLA | Wall C.J.,et al."Observational evidence that radiative heating modifies the life cycle of tropical anvil clouds".Journal of Climate 33.20(2021). |
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