Articles | Volume 24, issue 1
Hydrol. Earth Syst. Sci., 24, 293–305, 2020
https://doi.org/10.5194/hess-24-293-2020
Hydrol. Earth Syst. Sci., 24, 293–305, 2020
https://doi.org/10.5194/hess-24-293-2020

Research article 21 Jan 2020

Research article | 21 Jan 2020

Spatiotemporal assimilation–interpolation of discharge records through inverse streamflow routing

Colby K. Fisher et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (25 Jun 2019) by Stacey Archfield
AR by Colby Fisher on behalf of the Authors (06 Aug 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (16 Aug 2019) by Stacey Archfield
RR by Anonymous Referee #2 (21 Aug 2019)
RR by Laura Read (15 Sep 2019)
ED: Publish subject to minor revisions (review by editor) (29 Sep 2019) by Stacey Archfield
AR by Colby Fisher on behalf of the Authors (09 Oct 2019)  Author's response    Manuscript
ED: Publish subject to technical corrections (27 Oct 2019) by Stacey Archfield
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Short summary
Poorly monitored river flows in many regions of the world have been hindering our ability to accurately estimate global water usage. In this paper we present a method to derive continuous records of streamflow from a set of in situ gauges. Applying this method to the Ohio River basin, we found that we could reliably generate estimates of streamflow throughout the basin using only a small set of streamflow gauges, which can be useful for global river basins where we do not have good observations.