The influence of diurnal snowmelt and transpiration  on hillslope throughflow and stream response

Woelber, Brett; Maneta, Marco P.; Harper, Joel; Jencso, Kelsey G.; Gardner, W. Payton; Wilcox, Andrew C.; López-Moreno, Ignacio

doi:https://doi.org/10.5194/hess-22-4295-2018

Articles | Volume 22, issue 8

https://doi.org/10.5194/hess-22-4295-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Assessing impacts and adaptation to global change in water...

https://doi.org/10.5194/hess-22-4295-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 22, issue 8

Research article

|

14 Aug 2018

Research article |

| 14 Aug 2018

The influence of diurnal snowmelt and transpiration on hillslope throughflow and stream response

Brett Woelber, Marco P. Maneta, Joel Harper, Kelsey G. Jencso, W. Payton Gardner, Andrew C. Wilcox, and Ignacio López-Moreno

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Final revised paper (published on 14 Aug 2018)
Preprint (discussion started on 05 Apr 2018)

Interactive discussion

Status: closed

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

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RC1: 'Review', Anonymous Referee #1, 12 May 2018
- AC1: 'Reply to Reviewer 1', Brett Woelber, 24 Jun 2018
RC2: 'Review by reviewer 2', Anonymous Referee #2, 23 May 2018
- AC2: 'Reply to Reviewer 2', Brett Woelber, 24 Jun 2018

Peer-review completion

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

ED: Publish as is (16 Jul 2018) by David Pulido-Velazquez

Short summary

The hydrology of high-elevation headwaters in midlatitudes is typically dominated by snow processes, which are very sensitive to changes in energy inputs at the top of the snowpack. We present a data analyses that reveal how snowmelt and transpiration waves induced by the diurnal solar cycle generate water pressure fluctuations that propagate through the snowpack–hillslope–stream system. Changes in diurnal energy inputs alter these pressure cycles with potential ecohydrological consequences.