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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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發(fā)表于 2025-3-25 03:29:42 | 只看該作者
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發(fā)表于 2025-3-25 07:53:49 | 只看該作者
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發(fā)表于 2025-3-25 12:02:22 | 只看該作者
Interactions of Radiation and Microphysics in Cirrus, cirrus are extensive in space and time. In addition, they are cold enough to cause a strong greenhouse effect. However, the problem of quantifying their influence on the present climate has remained essentially unresolved and we are even farther from being able to predict their response to a changing climate.
24#
發(fā)表于 2025-3-25 17:08:56 | 只看該作者
https://doi.org/10.1007/978-3-642-61051-6Aerosol; Cloud; Clouds; Troposphere; atmosphere; atmospheric chemistry; chemistry; climate; climatology; ozon
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發(fā)表于 2025-3-25 22:00:18 | 只看該作者
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發(fā)表于 2025-3-26 02:09:22 | 只看該作者
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發(fā)表于 2025-3-26 11:17:31 | 只看該作者
1431-7125 y. 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 clo
29#
發(fā)表于 2025-3-26 14:19:59 | 只看該作者
https://doi.org/10.1007/978-3-531-90201-2 albedo. The condensed water in clouds is also strongly related to atmospheric water vapor content, occurring only where the actual vapor pressure locally approaches its saturation value. For these reasons, understanding the control of atmospheric water vapor is an essential part of understanding climate change.
30#
發(fā)表于 2025-3-26 19:37:14 | 只看該作者
Microphysical and Dynamical Control of Tropospheric Water Vapor, albedo. The condensed water in clouds is also strongly related to atmospheric water vapor content, occurring only where the actual vapor pressure locally approaches its saturation value. For these reasons, understanding the control of atmospheric water vapor is an essential part of understanding climate change.
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