Journal cover Journal topic
Climate of the Past An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 3.470 IF 3.470
  • IF 5-year value: 4.009 IF 5-year
    4.009
  • CiteScore value: 3.45 CiteScore
    3.45
  • SNIP value: 1.166 SNIP 1.166
  • IPP value: 3.28 IPP 3.28
  • SJR value: 1.929 SJR 1.929
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 64 Scimago H
    index 64
  • h5-index value: 43 h5-index 43
Volume 11, issue 10
Clim. Past, 11, 1433–1451, 2015
https://doi.org/10.5194/cp-11-1433-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 11, 1433–1451, 2015
https://doi.org/10.5194/cp-11-1433-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Oct 2015

Research article | 21 Oct 2015

Tropical cyclone genesis potential across palaeoclimates

J. H. Koh and C. M. Brierley
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
AR by Chris Brierley on behalf of the Authors (30 Jun 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (13 Jul 2015) by Gerrit Lohmann
RR by Matthew Huber (20 Jul 2015)
RR by Robert Korty (07 Aug 2015)
RR by Timothy Merlis (18 Aug 2015)
ED: Publish subject to minor revisions (review by Editor) (03 Sep 2015) by Gerrit Lohmann
AR by Chris Brierley on behalf of the Authors (23 Sep 2015)  Author's response    Manuscript
ED: Publish as is (27 Sep 2015) by Gerrit Lohmann
Publications Copernicus
Download
Short summary
Here we diagnose simulated changes in large-scale climate variables associated with the formation of tropical cyclones (i.e. hurricanes and typhoons). The cumulative potential for storm formation is pretty constant, despite the climate changes between the Last Glacial Maximum and the warm Pliocene. There are, however, coherent shifts in the relative strength of the storm regions. Little connection appears between the past behaviour in the five models studied and their future projections.
Here we diagnose simulated changes in large-scale climate variables associated with the...
Citation