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Titlebook: Clouds, Chemistry and Climate; Paul J. Crutzen,Veerabhadran Ramanathan Conference proceedings 1996 Springer-Verlag Berlin Heidelberg 1996

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书目名称Clouds, Chemistry and Climate
编辑Paul J. Crutzen,Veerabhadran Ramanathan
视频videohttp://file.papertrans.cn/229/228513/228513.mp4
丛书名称Nato ASI Subseries I:
图书封面Titlebook: Clouds, Chemistry and Climate;  Paul J. Crutzen,Veerabhadran Ramanathan Conference proceedings 1996 Springer-Verlag Berlin Heidelberg 1996
描述The objective of this NATO Advanced Research Workshop was to discuss our current understanding of the role of clouds in climate and chemistry. The range of topics dis­ cussed during the workshop included: modeling of clouds in GCMs; observations of the cloud micro physical properties; the water vapor cycle; troposphere-stratosphere exchange; role of in-cloud transport in tropospheric ozone; regulation of current and paleo climate by clouds; and anthropogenic sulfate aerosols and modification of cloud properties. The essence of the discussions is captured in the accompanying summary by the rapporteurs and the chapters by some of the speakers. The underlying message is that significant progress has been made, resulting in exciting new developments in our perception of the role of clouds in the global system . .. The tropical convective-cirrus cloud systems emerge as a major influence on the climate system. Micro physical processes, such as the rate of precipitation and re evaporation of ice particles, seem to regulate the large scale vertical distribution of water vapor which is the dominant greenhouse gas. Water vapor data collected during the Central Equatorial Pacific Experiment (
出版日期Conference proceedings 1996
关键词Aerosol; Cloud; Clouds; Troposphere; atmosphere; atmospheric chemistry; chemistry; climate; climatology; ozon
版次1
doihttps://doi.org/10.1007/978-3-642-61051-6
isbn_softcover978-3-642-64672-0
isbn_ebook978-3-642-61051-6Series ISSN 1431-7125
issn_series 1431-7125
copyrightSpringer-Verlag Berlin Heidelberg 1996
The information of publication is updating

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Conference proceedings 1996e climate system. Micro physical processes, such as the rate of precipitation and re evaporation of ice particles, seem to regulate the large scale vertical distribution of water vapor which is the dominant greenhouse gas. Water vapor data collected during the Central Equatorial Pacific Experiment (
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Satellite Observations of Upper Tropospheric Aerosols,chniques. Some of the data obtained during these flight programs have recently been published (Clarke, 1993; Pueschel et al., 1994). Another considerable set of data on the upper troposphere is that of Hofmann (1993) who has presented the results of 20 years of balloonborne measurements made by opti
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