The effects of convection on the summertime mid-latitude overworld
Item
Title (Dublin Core)
The effects of convection on the summertime mid-latitude overworld
Description (Dublin Core)
Halogen Occultation Experiment measurements of H<sub>2</sub>O are used to investigate the influence of mid-latitude convection on the summertime overworld between 30° N and 40° N. We find that most of the convective influence over this latitude range occurs over the Asian monsoon and over North America. Over North America, the effects of convection extend to ~410 K (17.5 km). Over Asia, the effects of convection extend to ~460 K (19 km), about 50 K (1.5 km) higher than over North America.
Creator (Dublin Core)
Dessler, A. E.
Date (Dublin Core)
2018-08-09
Type (Dublin Core)
Text
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
10.5194/acpd-6-8421-2006
https://acp.copernicus.org/preprints/acpd-2006-0208/
Source (Dublin Core)
eISSN: 1680-7324
Language (Dublin Core)
eng
