Change in low flows due to catchment management dynamics—Application of a comparative modelling approach

Understanding the natural low flow of a catchment is critical for effective water management policy in semi‐arid and arid lands. The Geba catchment in Ethiopia, forming the headwaters of Tekeze‐Atbara basin was known for its severe land degradation before the recent large scale Soil and Water conser...

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Veröffentlicht in:Hydrological processes 2020-04, Vol.34 (9), p.2101-2116
Hauptverfasser: Gebremicael, Tesfay G., Mohamed, Yasir A., Zaag, Pieter, Hassaballah, Khalid, Hagos, Eyasu Y.
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Sprache:eng
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Zusammenfassung:Understanding the natural low flow of a catchment is critical for effective water management policy in semi‐arid and arid lands. The Geba catchment in Ethiopia, forming the headwaters of Tekeze‐Atbara basin was known for its severe land degradation before the recent large scale Soil and Water conservation (SWC) programs. Such interventions can modify the hydrological processes by changing the partitioning of the incoming rainfall on the land surface. However, the literature lacks studies to quantify the hydrological impacts of these interventions in the semi‐arid catchments of the Nile basin. Statistical test and Indicators of Hydrological Alteration (IHA) were used to identify the trends of streamflow in two comparatives adjacent (one treated with intensive SWC intervention and control with fewer interventions) catchments. A distributed hydrological model was developed to understand the differences in hydrological processes of the two catchments. The statistical and IHA tools showed that the low flow in the treated catchment has significantly increased while considerably decreased in the control catchment. Comparative analysis confirmed that the low flow in the catchment with intensive SWC works was greater than that of the control by >30% while the direct runoff was lower by >120%. This implies a large proportion of the rainfall in the treated catchment is infiltrated and recharge aquifers which subsequently contribute to streamflow during the dry season. The proportion of soil storage was more than double compared to the control catchment. Moreover, hydrological response comparison from pre‐ and post‐intervention showed that a drastic reduction in direct runoff (>84%) has improved the low flow by >55%. This strongly suggests that the ongoing intensive SWC works have significantly improved the low flows while it contributed to the reduction of total streamflow in the catchment. Understanding the response of low flows to catchment management interventions is critical for effective water management policy interventions. A combination of statistical test, Indicators of Hydrological Alteration and paired catchment modelling approach was applied to understand the impacts. Low flow in the catchment has significantly increased following the ongoing intensive Soil and Water Conservation (SWC) implementation programs. The total streamflow has declined significantly after SWC implementations which is attributed to the increase in evapotranspiration and soil storag
ISSN:0885-6087
1099-1085
DOI:10.1002/hyp.13715