Articles | Volume 15, issue 2
https://doi.org/10.5194/cp-15-449-2019
https://doi.org/10.5194/cp-15-449-2019
Research article
 | 
19 Mar 2019
Research article |  | 19 Mar 2019

The response of tropical precipitation to Earth's precession: the role of energy fluxes and vertical stability

Chetankumar Jalihal, Joyce Helena Catharina Bosmans, Jayaraman Srinivasan, and Arindam Chakraborty

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (29 Nov 2018) by Qiuzhen Yin
AR by Chetankumar Jalihal on behalf of the Authors (22 Dec 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (17 Jan 2019) by Qiuzhen Yin
RR by Anonymous Referee #1 (22 Jan 2019)
ED: Publish subject to minor revisions (review by editor) (18 Feb 2019) by Qiuzhen Yin
AR by Chetankumar Jalihal on behalf of the Authors (20 Feb 2019)  Author's response   Manuscript 
ED: Publish as is (26 Feb 2019) by Qiuzhen Yin
AR by Chetankumar Jalihal on behalf of the Authors (01 Mar 2019)  Manuscript 
Download
Short summary
Insolation is thought to drive monsoons on orbital timescales. We find that insolation can be a trigger for changes in precipitation, but surface energy and vertical stability play an important role too. These feedbacks are found to be dominant over oceans and can even counter the insolation forcing, thus leading to a land–sea differential response in precipitation.