Articles | Volume 20, issue 4
Hydrol. Earth Syst. Sci., 20, 1621–1635, 2016
https://doi.org/10.5194/hess-20-1621-2016
Hydrol. Earth Syst. Sci., 20, 1621–1635, 2016
https://doi.org/10.5194/hess-20-1621-2016

Research article 27 Apr 2016

Research article | 27 Apr 2016

Factors influencing stream baseflow transit times in tropical montane watersheds

Lyssette E. Muñoz-Villers et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (Editor review) (19 Mar 2016) by Fuqiang Tian
AR by Lyssette Munoz Villers on behalf of the Authors (23 Mar 2016)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (11 Apr 2016) by Fuqiang Tian
AR by Lyssette Munoz Villers on behalf of the Authors (11 Apr 2016)  Author's response    Manuscript
ED: Publish as is (12 Apr 2016) by Fuqiang Tian
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Short summary
This study provides an important first step towards a better understanding of the hydrology of tropical montane regions and the factors influencing baseflow mean transit times (MTT). Our MTT estimates ranged between 1.2 and 2.7 years, suggesting deep and long subsurface pathways contributing to sustain dry season flows. Our findings showed that topography and subsurface permeability are the key factors controlling baseflow MTTs. Longest MTTs were found in the cloud forest headwater catchments.