Mapping spatiotemporal variability of wet season surface water processes in the Cuvelai-Etosha Basin, Namibia using stable isotopes

The natural tracers δ<sup>18</sup>O and δ<sup>2</sup>H are essential for tracing hydrological processes by identifying water sources, tracking evaporation loss and floodwater dynamics to enhance water management and flood mitigation strategies. This study employed this approach in the ephemeral, endorheic Cuvelai-Etosha Basin (CEB), spanning northern Namibia and southern Angola, to determine its viability in capturing spatial and temporal hydrological patterns, their timing and interactions during a medium flood condition (2017), and contrasted with a drought year (2014). During the 2017 wet season 219 grab surface water samples were collected from ephemeral waterbodies in four sampling campaigns (February, March, April and May) in addition to a single campaign in May 2014 (63 samples). Samples were analysed for stable isotopes (δ²H and δ<sup>18</sup>O) at the University of Namibia laboratory using an off-axis integrated cavity output spectroscope (Los Gatos, DLT-100). Results for 2017 revealed a compositional range of -13.51 to 12.44 ‰ for δ<sup>18</sup>O and from -100.1 to 50.9 ‰ for δ<sup>2</sup>H. The 2017 samples plot along a low sloping line (δ<sup>2</sup>H = 5.19 δ<sup>18</sup>O - 13.91) indicating the dominance of the evaporation effect. Amount, seasonality, and latitude effects were also identified in the isotopic composition of the <i>iishana</i> water. The surface water loss to evaporation is in the range of 24-42 % from March to April and 39-69 % from March to May. The <i>d-</i>excess decreased from April and remains relatively low in May, which supports observations of evaporation losses. The overall large water losses from the system via evaporation reduces the water availability substantially, and the impact is more pronounced in the western part of the basin than in the eastern. Since evaporative loss begins early, even during the rainy season, proactive technical solutions such as floodwater harvesting need to be planned accordingly to mitigate losses and optimizing water use.

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Publication Details

Journal
Isotopes in Environmental and Health Studies
Published
2025-09-09
DOI
https://doi.org/10.1080/10256016.2025.2538594
Primary Topic
Geophysics and Gravity Measurements
Type
article
Field-Weighted Citation Impact
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article

Mapping spatiotemporal variability of wet season surface water processes in the Cuvelai-Etosha Basin, Namibia using stable isotopes

Kwok Pan Chun, Martin Hipondoka, Josefina Tulimevava Hamutoko, Heike Wanke et al.
Isotopes in Environmental and Health Studies
Geophysics and Gravity Measurements
article

Mapping spatiotemporal variability of wet season surface water processes in the Cuvelai-Etosha Basin, Namibia using stable isotopes

Kwok Pan Chun, Martin Hipondoka, Josefina Tulimevava Hamutoko, Heike Wanke, Tamekeni P. Nantuua, Nyambe Masiye
article en

Abstract

The natural tracers δ<sup>18</sup>O and δ<sup>2</sup>H are essential for tracing hydrological processes by identifying water sources, tracking evaporation loss and floodwater dynamics to enhance water management and flood mitigation strategies. This study employed this approach in the ephemeral, endorheic Cuvelai-Etosha Basin (CEB), spanning northern Namibia and southern Angola, to determine its viability in capturing spatial and temporal hydrological patterns, their timing and interactions during a medium flood condition (2017), and contrasted with a drought year (2014). During the 2017 wet season 219 grab surface water samples were collected from ephemeral waterbodies in four sampling campaigns (February, March, April and May) in addition to a single campaign in May 2014 (63 samples). Samples were analysed for stable isotopes (δ²H and δ<sup>18</sup>O) at the University of Namibia laboratory using an off-axis integrated cavity output spectroscope (Los Gatos, DLT-100). Results for 2017 revealed a compositional range of -13.51 to 12.44 ‰ for δ<sup>18</sup>O and from -100.1 to 50.9 ‰ for δ<sup>2</sup>H. The 2017 samples plot along a low sloping line (δ<sup>2</sup>H = 5.19 δ<sup>18</sup>O - 13.91) indicating the dominance of the evaporation effect. Amount, seasonality, and latitude effects were also identified in the isotopic composition of the <i>iishana</i> water. The surface water loss to evaporation is in the range of 24-42 % from March to April and 39-69 % from March to May. The <i>d-</i>excess decreased from April and remains relatively low in May, which supports observations of evaporation losses. The overall large water losses from the system via evaporation reduces the water availability substantially, and the impact is more pronounced in the western part of the basin than in the eastern. Since evaporative loss begins early, even during the rainy season, proactive technical solutions such as floodwater harvesting need to be planned accordingly to mitigate losses and optimizing water use.

Isotopes in Environmental and Health StudiesVol. 61(6)
University of the West of England (GB), University of Namibia (NA), German University of Technology (OM)
Openalex Percentile: Top 75%
Geophysics and Gravity Measurements
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