The effects of convection on the summertime mid-latitude overworld

Dessler, A. E.

doi:https://doi.org/10.5194/acpd-6-8421-2006

Preprints

https://doi.org/10.5194/acpd-6-8421-2006

Preprints

04 Sep 2006

| 04 Sep 2006

Status: this preprint was under review for the journal ACP. A revision for further review has not been submitted.

The effects of convection on the summertime mid-latitude overworld

A. E. Dessler

Abstract. Halogen Occultation Experiment measurements of H₂O 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.

Received: 18 Jul 2006 – Discussion started: 04 Sep 2006

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A. E. Dessler

Status: closed (peer review stopped)

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC S3166: 'Comments on HALOE and Asian Monsoon', Anonymous Referee #1, 18 Sep 2006
RC S3169: 'Comments on HALOE and Asian Monsoon', Anonymous Referee #1, 18 Sep 2006
RC S3675: 'referee comment', Anonymous Referee #2, 10 Oct 2006

Status: closed (peer review stopped)

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC S3166: 'Comments on HALOE and Asian Monsoon', Anonymous Referee #1, 18 Sep 2006
RC S3169: 'Comments on HALOE and Asian Monsoon', Anonymous Referee #1, 18 Sep 2006
RC S3675: 'referee comment', Anonymous Referee #2, 10 Oct 2006

A. E. Dessler

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The effects of convection on the summertime mid-latitude overworld

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