Deep convective cloud phenomena in the upper troposphere/lower stratosphere - A new development in cloud science

研究成果: Paper同行評審

摘要

All three phenomena described above are related to the deep convective cloud process near the tropopause. Traditional cloud physics studies are usually confined to lower to middle troposphere, mainly due to the relatively few observational platforms that can reach higher troposphere. Satellite techniques certainly are extremely useful but to interpret the data correctly we will need in-situ measurements and modeling. The properties of clouds associated with these phenomena are poorly understood. Basic cloud microphysical works related to the very low temperature environment are only beginning (e.g., Bailey and Hallett, 2002, 2004; Wang, 2003, 2004, 2005; Mullendore et al., 2005). Potential research works are needed to understand these phenomena and their implications. This represents a new research area in cloud science that requires more studies.

原文English
出版狀態Published - 2006
事件12th Conference on Cloud Physics and 12th Conference on Atmospheric Radiation - Madison, WI, United States
持續時間: 2006 7月 102006 7月 14

Conference

Conference12th Conference on Cloud Physics and 12th Conference on Atmospheric Radiation
國家/地區United States
城市Madison, WI
期間06-07-1006-07-14

All Science Journal Classification (ASJC) codes

  • 電腦網路與通信
  • 環境化學
  • 環境工程
  • 全球和行星變化

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