Modifications to a rainfall-streamflow model to handle "non-stationarity"

Croke, B. F. W.; Shin, M.-J.

doi:10.5194/piahs-371-29-2015

Articles | Volume 371

https://doi.org/10.5194/piahs-371-29-2015

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

https://doi.org/10.5194/piahs-371-29-2015

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

Articles | Volume 371

12 Jun 2015

| 12 Jun 2015

Modifications to a rainfall-streamflow model to handle "non-stationarity"

B. F. W. Croke and M.-J. Shin

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Month	HTML	PDF	XML	Total
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Oct 2015	15	9	0	24
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Cumulative views and downloads (calculated since 12 Jun 2015)

Month	HTML	PDF	XML	Total
Jun 2015	26	20	1	47
Jul 2015	38	40	0	78
Aug 2015	18	14	0	32
Sep 2015	9	6	0	15
Oct 2015	15	9	0	24
Nov 2015	15	6	0	21
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Apr 2016	4	6	2	12
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Jun 2016	0
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Nov 2025	8	3	0	11

Latest update: 14 Nov 2025

Short summary

Catchment response can be influenced by man’s activities as well as natural forces like climate, and understanding how stream flow is affected by such activities is important in a changing world, particularly in developing countries. Data for the Bani River in Africa show a steady decrease in the groundwater component of stream flow. This paper shows that the decrease appears to be driven by increased water use in the catchment, and has resulted in the river ceasing to flow in the dry season.