標題: Titlebook: Clouds, Chemistry and Climate; Paul J. Crutzen,Veerabhadran Ramanathan Conference proceedings 1996 Springer-Verlag Berlin Heidelberg 1996 [打印本頁] 作者: supplementary 時間: 2025-3-21 16:20
書目名稱Clouds, Chemistry and Climate影響因子(影響力)
書目名稱Clouds, Chemistry and Climate影響因子(影響力)學科排名
書目名稱Clouds, Chemistry and Climate網(wǎng)絡公開度
書目名稱Clouds, Chemistry and Climate網(wǎng)絡公開度學科排名
書目名稱Clouds, Chemistry and Climate被引頻次
書目名稱Clouds, Chemistry and Climate被引頻次學科排名
書目名稱Clouds, Chemistry and Climate年度引用
書目名稱Clouds, Chemistry and Climate年度引用學科排名
書目名稱Clouds, Chemistry and Climate讀者反饋
書目名稱Clouds, Chemistry and Climate讀者反饋學科排名
作者: –LOUS 時間: 2025-3-21 22:15 作者: Bone-Scan 時間: 2025-3-22 01:57 作者: 梯田 時間: 2025-3-22 05:56 作者: 遺產 時間: 2025-3-22 10:15
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 (作者: Allure 時間: 2025-3-22 14:42 作者: Allure 時間: 2025-3-22 18:19 作者: 難聽的聲音 時間: 2025-3-22 21:34 作者: Legend 時間: 2025-3-23 03:27 作者: 昏睡中 時間: 2025-3-23 06:07
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作者: 人造 時間: 2025-3-23 10:23 作者: chapel 時間: 2025-3-23 15:40
,NATO ARW on Clouds — Session Summaries,The two papers presented in this session focused on the role of dynamics in the water vapor distribution of the tropics and its implications to climate.作者: 尾巴 時間: 2025-3-23 18:47 作者: Cleave 時間: 2025-3-24 00:47 作者: 牢騷 時間: 2025-3-24 04:55 作者: indubitable 時間: 2025-3-24 08:26 作者: 減弱不好 時間: 2025-3-24 11:09
Fazit und weiterer Forschungsbedarf, site above sea level, a.s.l, is 3250 m, Figure 1). One year later, the US Greenland Ice Sheet Project (GISP2) successfully completed a second drilling in the same region at a site located 28 km apart (3208 m a.s.l). These two, more than 3 km long, cores have now been continuously analysed for their作者: Indelible 時間: 2025-3-24 16:10
Schulsozialarbeit am übergang Schule - Berufst of which are inadequately understood. The spatial scales involved in cloud formation range from tenths of micrometers for cloud condensation nuclei to hundreds of kilometers for large-scale dynamics. Most of these processes cannot be resolved by the current generation of climate models with typic作者: opalescence 時間: 2025-3-24 20:43
Soziale Arbeit an Sekundarschulen in Berlin,) are within a narrow range between 300 K and 303 K, and less than 0.01% of the ocean surface has SSTs in excess of 304 K (Figure 1). Furthermore, deep convection is triggered only when SSTs exceed 300 K. In regions of deep convection and warm SST, the reduction of outgoing longwave energy by the at作者: Alpha-Cells 時間: 2025-3-25 00:23 作者: 打算 時間: 2025-3-25 03:29 作者: 凌辱 時間: 2025-3-25 07:53 作者: 胡言亂語 時間: 2025-3-25 12:02
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.作者: 要塞 時間: 2025-3-25 17:08
https://doi.org/10.1007/978-3-642-61051-6Aerosol; Cloud; Clouds; Troposphere; atmosphere; atmospheric chemistry; chemistry; climate; climatology; ozon作者: 行業(yè) 時間: 2025-3-25 22:00 作者: bisphosphonate 時間: 2025-3-26 02:09 作者: 極大的痛苦 時間: 2025-3-26 04:48 作者: Genetics 時間: 2025-3-26 11:17
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作者: 共同生活 時間: 2025-3-26 14:19
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.作者: Incompetent 時間: 2025-3-26 19:37
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.作者: mitral-valve 時間: 2025-3-26 23:09
Soziale Arbeit an Sekundarschulen in Berlin, a runaway warming. . [1991] (hereafter RC) found that the warm ocean is also covered by thick cirrus anvil clouds, which reflect a significant amount of solar energy back to space. They concluded that the anvils produced by deep convection act like a thermostat to regulate the flow of solar energy to the ocean.作者: Connotation 時間: 2025-3-27 03:45 作者: 禁止,切斷 時間: 2025-3-27 08:06
Beziehungsarbeit in Schule und Jugendhilfe,ard transport of stratospheric constituents into the troposphere not only serves as the major sink for some of the constituents involved in stratospheric ozone depletion, but also furnishes reactive species that modify tropospheric chemistry, and provides a source of tropospheric ozone.作者: neutral-posture 時間: 2025-3-27 11:45
Stratosphere-Troposphere Exchange and its role in the budget of tropospheric ozone,ard transport of stratospheric constituents into the troposphere not only serves as the major sink for some of the constituents involved in stratospheric ozone depletion, but also furnishes reactive species that modify tropospheric chemistry, and provides a source of tropospheric ozone.作者: conjunctiva 時間: 2025-3-27 14:29 作者: 我悲傷 時間: 2025-3-27 20:06
Abrupt climatic changes: A global perspective from ice cores,obal perspective through a comparison with the Vostok deuterium record, we briefly summarize why and how these isotopic changes provide a record of the local temperature at the time of formation of the precipitation.作者: FOIL 時間: 2025-3-28 01:42 作者: ANN 時間: 2025-3-28 02:40 作者: 雪崩 時間: 2025-3-28 07:17
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 changi作者: Adulate 時間: 2025-3-28 13:12 作者: 放肆的你 時間: 2025-3-28 17:52 作者: Canary 時間: 2025-3-28 21:19
GCM Studies and Parameterization,st of which are inadequately understood. The spatial scales involved in cloud formation range from tenths of micrometers for cloud condensation nuclei to hundreds of kilometers for large-scale dynamics. Most of these processes cannot be resolved by the current generation of climate models with typic作者: Rheumatologist 時間: 2025-3-29 01:10
The Central Equatorial Pacific Experiment,) are within a narrow range between 300 K and 303 K, and less than 0.01% of the ocean surface has SSTs in excess of 304 K (Figure 1). Furthermore, deep convection is triggered only when SSTs exceed 300 K. In regions of deep convection and warm SST, the reduction of outgoing longwave energy by the at
