Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-161-2020
https://doi.org/10.5194/cp-16-161-2020
Research article
 | 
22 Jan 2020
Research article |  | 22 Jan 2020

The effect of mountain uplift on eastern boundary currents and upwelling systems

Gerlinde Jung and Matthias Prange

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: Publish subject to minor revisions (review by editor) (20 Sep 2019) by Yannick Donnadieu
AR by Gerlinde Jung on behalf of the Authors (30 Sep 2019)  Author's response    Manuscript
ED: Publish as is (12 Nov 2019) by Yannick Donnadieu
Download
Short summary
All major mountain ranges were uplifted during Earth's history. Previous work showed that African uplift might have influenced upper-ocean cooling in the Benguela region. But the surface ocean cooled also in other upwelling regions during the last 10 million years. We performed a set of model experiments altering topography in major mountain regions to explore the effects on atmosphere and ocean. The simulations show that mountain uplift is important for upper-ocean temperature evolution.