Hemispherically asymmetric volcanic forcing of tropical hydroclimate during
the last millennium

Colose, Christopher M.; LeGrande, Allegra N.; Vuille, Mathias

doi:https://doi.org/10.5194/esd-7-681-2016

Articles | Volume 7, issue 3

https://doi.org/10.5194/esd-7-681-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/esd-7-681-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 7, issue 3

Research article

| Highlight paper

|

23 Aug 2016

Research article | Highlight paper |

| 23 Aug 2016

Hemispherically asymmetric volcanic forcing of tropical hydroclimate during the last millennium

Christopher M. Colose, Allegra N. LeGrande, and Mathias Vuille

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Final revised paper (published on 23 Aug 2016)
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Preprint (discussion started on 29 Apr 2016)
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Interactive discussion

Status: closed

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

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RC1: 'Review of Hemispherically asymmetric volcanic forcing of tropical hydroclimate and water isotopologue variability during the last millennium', Anonymous Referee #1, 03 Jun 2016
- AC1: 'Response to Review #1- Chris Colose', Chris Colose, 12 Jul 2016
RC2: 'Review of Hemispherically asymmetric volcanic forcing of tropical hydroclimate and water isotopologue variability during the last millennium by C. M. Colose, A. N. Le Grande and M. Vuille', Anonymous Referee #2, 13 Jun 2016
- AC2: 'Response to review #2', Chris Colose, 12 Jul 2016

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (review by Editor) (14 Jul 2016) by Daniel Kirk-Davidoff

AR by Chris Colose on behalf of the Authors (24 Jul 2016) Author's response Manuscript

ED: Publish as is (02 Aug 2016) by Daniel Kirk-Davidoff

AR by Chris Colose on behalf of the Authors (03 Aug 2016)

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Short summary

A band of intense rainfall exists near the equator known as the intertropical convergence zone, which can migrate in response to climate forcings. Here, we assess such migration in response to volcanic eruptions of varying spatial structure (Northern Hemisphere, Southern Hemisphere, or an eruption fairly symmetric about the equator). We do this using model simulations of the last millennium and link results to energetic constraints and the imprint eruptions may leave behind in past records.