Journal metrics

Journal metrics

  • IF value: 4.256 IF 4.256
  • IF 5-year value: 4.819 IF 5-year 4.819
  • CiteScore value: 4.10 CiteScore 4.10
  • SNIP value: 1.412 SNIP 1.412
  • SJR value: 2.023 SJR 2.023
  • IPP value: 3.97 IPP 3.97
  • h5-index value: 58 h5-index 58
  • Scimago H index value: 99 Scimago H index 99
Volume 22, issue 1 | Copyright
Hydrol. Earth Syst. Sci., 22, 179-201, 2018
https://doi.org/10.5194/hess-22-179-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 10 Jan 2018

Research article | 10 Jan 2018

Modelling hydrologic impacts of light absorbing aerosol deposition on snow at the catchment scale

Felix N. Matt et al.
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: Reconsider after major revisions (further review by Editor and Referees) (13 Mar 2017) by Jan Seibert
AR by Felix Matt on behalf of the Authors (26 May 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (30 May 2017) by Jan Seibert
RR by Anonymous Referee #3 (19 Jun 2017)
ED: Reconsider after major revisions (further review by Editor and Referees) (15 Jul 2017) by Jan Seibert
AR by Felix Matt on behalf of the Authors (25 Aug 2017)  Author's response    Manuscript
ED: Reconsider after major revisions (further review by Editor and Referees) (10 Sep 2017) by Jan Seibert
AR by Felix Matt on behalf of the Authors (21 Oct 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (07 Nov 2017) by Jan Seibert
Publications Copernicus
Download
Short summary
Certain particles that have the ability to absorb sunlight deposit onto mountain snow via atmospheric transport mechanisms and then lower the snow's ability to reflect sunlight, which increases snowmelt. Herein we present a model aiming to simulate this effect and model the impacts on the streamflow of a southern Norwegian river. We find a significant difference in streamflow between simulations with and without the effect of light absorbing particles applied, in particular during spring melt.
Certain particles that have the ability to absorb sunlight deposit onto mountain snow via...
Citation
Share