<i>tran</i>-SAS v1.0: a numerical model to compute catchment-scale hydrologic transport using StorAge Selection functions

Benettin, Paolo; Bertuzzo, Enrico

doi:https://doi.org/10.5194/gmd-11-1627-2018

Articles | Volume 11, issue 4

https://doi.org/10.5194/gmd-11-1627-2018

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

https://doi.org/10.5194/gmd-11-1627-2018

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

Articles | Volume 11, issue 4

Model description paper

|

25 Apr 2018

Model description paper |

| 25 Apr 2018

tran-SAS v1.0: a numerical model to compute catchment-scale hydrologic transport using StorAge Selection functions

Paolo Benettin and Enrico Bertuzzo

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Final revised paper (published on 25 Apr 2018)
Preprint (discussion started on 16 Jan 2018)
Supplement to the preprint

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC1: 'review', Anonymous Referee #1, 21 Feb 2018
- AC1: 'reply to RC1', Paolo Benettin, 15 Mar 2018
RC2: 'Interactive comment on “tran-SAS v1.0: a numerical model to compute catchment-scale hydrologic transport using StorAge Selection functions”, by Paolo Benettin and Enrico Bertuzzo', Anonymous Referee #2, 23 Feb 2018
- AC2: 'reply to RC2', Paolo Benettin, 15 Mar 2018
SC1: 'Code Availability', Lutz Gross, 15 Mar 2018
- AC3: 'reply to comment by Lutz Gross', Paolo Benettin, 15 Mar 2018
RC3: 'review', Anonymous Referee #3, 19 Mar 2018
- AC4: 'reply to RC3', Paolo Benettin, 19 Mar 2018

Peer-review completion

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

AR by Paolo Benettin on behalf of the Authors (21 Mar 2018) Author's response Manuscript

ED: Publish as is (31 Mar 2018) by Jeffrey Neal

Short summary

Solutes introduced in the environment are transported by water to streams and lakes. The tran-SAS package includes a set of codes to model this process for entire watersheds by using the concept of water residence times, i.e. the time that water takes to move through the landscape. Results show that the model is implemented efficiently and it can be used to simulate solute transport in a number of different conditions.