Paleo-hydrologic reconstruction of 400 years of past flows at a weekly time step for major rivers of Western Canada

Slaughter, Andrew R.; Razavi, Saman

doi:https://doi.org/10.5194/essd-12-231-2020

Articles | Volume 12, issue 1

https://doi.org/10.5194/essd-12-231-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Water, ecosystem, cryosphere, and climate data from the interior...

https://doi.org/10.5194/essd-12-231-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 12, issue 1

Data description paper

|

05 Feb 2020

Data description paper |

| 05 Feb 2020

Paleo-hydrologic reconstruction of 400 years of past flows at a weekly time step for major rivers of Western Canada

Andrew R. Slaughter and Saman Razavi

Download

Final revised paper (published on 05 Feb 2020)
Preprint (discussion started on 17 May 2019)

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC1: 'Paleo-hydrologic reconstruction of 400 years of past flows at a weekly time step for major rivers of Western Canada', Anonymous Referee #1, 11 Oct 2019
- AC1: 'Author response', Andrew Slaughter, 12 Nov 2019
RC2: 'Review comments for “Paleo-hydrologic reconstruction of 400 years of past flows at a weekly time step for major rivers of Western Canada” by Slaughter and Razavi', Anonymous Referee #2, 18 Oct 2019
- AC2: 'Author response', Andrew Slaughter, 12 Nov 2019

Peer-review completion

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

AR by Svenja Lange on behalf of the Authors (18 Dec 2019) Author's response

ED: Publish as is (06 Jan 2020) by Chris DeBeer

Short summary

Water management faces the challenge of non-stationarity in future flows. To extend flow datasets beyond the gauging data, this study presents a method of generating an ensemble of weekly flows from tree-ring reconstructed flows to represent uncertainty that can overcome certain long-standing data challenges with paleo-reconstruction. An ensemble of 500 flow time series were generated for the four sub-basins of the Saskatchewan River basin, Canada, for the period 1600–2001.