Convection and the summertime mid-latitude overworld
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چکیده
Introduction Conclusions References Tables Figures Back Close Full Screen / Esc Abstract Introduction Conclusions References Tables Figures Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion EGU Abstract Halogen Occultation Experiment measurements of H 2 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 5 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.
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