Climate Change Data Portal
DOI | 10.1175/JCLI-D-19-0596.1 |
Global and regional entropy production by radiation estimated from satellite observations | |
Kato S.; Rose F.G. | |
发表日期 | 2020 |
ISSN | 0894-8755 |
起始页码 | 2985 |
结束页码 | 3000 |
卷号 | 33期号:8 |
英文摘要 | Vertical profiles of shortwave and longwave irradiances computed with satellite-derived cloud properties and temperature and humidity profiles from reanalysis are used to estimate entropy production. Entropy production by shortwave radiation is computed by the absorbed irradiance within layers in the atmosphere and by the surface divided by their temperatures. Similarly, entropy production by longwave radiation is computed by emitted irradiance to space from layers in the atmosphere and surface divided by their temperatures. Global annual mean entropy production by shortwave absorption and longwave emission to space are, respectively, 0.852 and 0.928 W m22 K21. With a steady-state assumption, entropy production by irreversible processes within the Earth system is estimated to be 0.076 W m22 K21 and by nonradiative irreversible processes to be 0.049 W m22 K21. Both global annual mean entropy productions by shortwave absorption and longwave emission to space increase with increasing shortwave absorption (i.e., with decreasing the planetary albedo). The increase of entropy production by shortwave absorption is, however, larger than the increase of entropy production by longwave emission to space. The result implies that global annual mean entropy production by irreversible processes decreases with increasing shortwave absorption. Input and output temperatures derived by dividing the absorbed shortwave irradiance and emitted longwave irradiance to space by respective entropy production are, respectively, 282 and 259 K, which give the Carnot efficiency of the Earth system of 8.5%. © 2020 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses). |
英文关键词 | Atmospheric temperature; Statistical mechanics; Entropy production; Input and outputs; Irreversible process; Long-wave emissions; Long-wave radiation; Satellite observations; Short-wave radiation; Temperature and humidities; Entropy; air temperature; cloud; entropy; humidity; longwave radiation; satellite imagery; shortwave radiation; vertical profile |
语种 | 英语 |
来源期刊 | Journal of Climate
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/171354 |
作者单位 | NASA Langley Research Center, Hampton, VA, United States; Science System and Applications, Inc., Hampton, VA, United States |
推荐引用方式 GB/T 7714 | Kato S.,Rose F.G.. Global and regional entropy production by radiation estimated from satellite observations[J],2020,33(8). |
APA | Kato S.,&Rose F.G..(2020).Global and regional entropy production by radiation estimated from satellite observations.Journal of Climate,33(8). |
MLA | Kato S.,et al."Global and regional entropy production by radiation estimated from satellite observations".Journal of Climate 33.8(2020). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Kato S.]的文章 |
[Rose F.G.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Kato S.]的文章 |
[Rose F.G.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Kato S.]的文章 |
[Rose F.G.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。