On the spatial and temporal variability of ENSO precipitation and drought
teleconnection in mainland Southeast Asia

Räsänen, Timo A.; Lindgren, Ville; Guillaume, Joseph H. A.; Buckley, Brendan M.; Kummu, Matti

doi:https://doi.org/10.5194/cp-12-1889-2016

Articles | Volume 12, issue 9

https://doi.org/10.5194/cp-12-1889-2016

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

https://doi.org/10.5194/cp-12-1889-2016

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

Articles | Volume 12, issue 9

Research article

|

21 Sep 2016

Research article |

| 21 Sep 2016

On the spatial and temporal variability of ENSO precipitation and drought teleconnection in mainland Southeast Asia

Timo A. Räsänen, Ville Lindgren, Joseph H. A. Guillaume, Brendan M. Buckley, and Matti Kummu

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Final revised paper (published on 21 Sep 2016)
Supplement to the final revised paper
Preprint (discussion started on 10 Nov 2015)
Supplement to the preprint

Interactive discussion

Status: closed

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

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- Supplement

RC C2873: 'Referee comments', Anonymous Referee #1, 07 Jan 2016
RC C3247: 'Review', Anonymous Referee #2, 23 Mar 2016
AC C3266: 'Author response to referee comments', T.A. Räsänen, 27 May 2016

Peer-review completion

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

ED: Publish subject to technical corrections (20 Jun 2016) by Dominik Fleitmann

AR by T.A. Räsänen on behalf of the Authors (31 Aug 2016) Author's response Manuscript

Short summary

El Niño-Southern Oscillation (ENSO) is linked to severe droughts and floods in mainland Southeast Asia. This research provides a more accurate and uniform picture of the spatio-temporal effects of ENSO on precipitation (1980–2013) and improves our understanding of long-term (1650–2004) ENSO teleconnection and its variability over the study area. The results reveal not only recognisable spatio-temporal patterns but also a high degree of variability and non-stationarity in the effects of ENSO.