Effects of snow ratio on annual runoff within the Budyko framework

Zhang, D.; Cong, Z.; Ni, G.; Yang, D.; Hu, S.

doi:https://doi.org/10.5194/hess-19-1977-2015

Articles | Volume 19, issue 4

https://doi.org/10.5194/hess-19-1977-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Catchment co-evolution: space–time patterns and functional...

https://doi.org/10.5194/hess-19-1977-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 19, issue 4

Research article

|

24 Apr 2015

Research article |

| 24 Apr 2015

Effects of snow ratio on annual runoff within the Budyko framework

D. Zhang, Z. Cong, G. Ni, D. Yang, and S. Hu

Download

Final revised paper (published on 24 Apr 2015)
Preprint (discussion started on 22 Jan 2015)

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC C23: 'Review of Effect of snow ratio on annual runoff within Budyko framework', Wouter Berghuijs, 27 Jan 2015
- AC C561: 'Responses to Referee W.R Berghuijs', danwu zhang, 15 Mar 2015
RC C212: 'Review comments on Effects of snow ratio on annual runoff within Budyko framework by Zhang et al.', Anonymous Referee #2, 18 Feb 2015
- AC C562: 'Responses to Anonymous Referee #2', danwu zhang, 15 Mar 2015

Peer-review completion

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

ED: Publish subject to minor revisions (Editor review) (21 Mar 2015) by Dingbao Wang

AR by Danwu Zhang on behalf of the Authors (25 Mar 2015) Author's response Manuscript

ED: Publish as is (29 Mar 2015) by Dingbao Wang

AR by Danwu Zhang on behalf of the Authors (29 Mar 2015)

Short summary

1. Catchments with higher snow ratio tend to have larger runoff index. 2. A modified Budyko method is proposed to illustrate the snow effect on runoff. 3. Snow ratio change has a significant contribution to runoff change, according to historical observations and projected future climate scenarios, especially in northwestern mountainous and northern high-latitude areas of China.