Analysing the origin of rain- and subsurface water in seasonal wetlands of north-central Namibia

We investigated the origins of rain- and subsurface waters of north-central Namibia’s seasonal wetlands, which are critical to the region’s water and food security. The region includes the southern part of the Cuvelai system seasonal wetlands (CSSWs) of the Cuvelai Basin, a transboundary river basin...

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Main Authors: Tetsuya Hiyama, Hironari Kanamori, Jack R Kambatuku, Ayumi Kotani, Kazuyoshi Asai, Hiroki Mizuochi, Yuichiro Fujioka, Morio Iijima
Format: Article
Language:English
Published: IOP Publishing 2017-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/aa5bc8
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author Tetsuya Hiyama
Hironari Kanamori
Jack R Kambatuku
Ayumi Kotani
Kazuyoshi Asai
Hiroki Mizuochi
Yuichiro Fujioka
Morio Iijima
author_facet Tetsuya Hiyama
Hironari Kanamori
Jack R Kambatuku
Ayumi Kotani
Kazuyoshi Asai
Hiroki Mizuochi
Yuichiro Fujioka
Morio Iijima
author_sort Tetsuya Hiyama
collection DOAJ
description We investigated the origins of rain- and subsurface waters of north-central Namibia’s seasonal wetlands, which are critical to the region’s water and food security. The region includes the southern part of the Cuvelai system seasonal wetlands (CSSWs) of the Cuvelai Basin, a transboundary river basin covering southern Angola and northern Namibia. We analysed stable water isotopes (SWIs) of hydrogen (HDO) and oxygen (H _2 ^18 O) in rainwater, surface water and shallow groundwater. Rainwater samples were collected during every rainfall event of the rainy season from October 2013 to April 2014. The isotopic ratios of HDO ( δ D) and oxygen H _2 ^18 O ( δ ^18 O) were analysed in each rainwater sample and then used to derive the annual mean value of ( δ D, δ ^18 O) in precipitation weighted by each rainfall volume. Using delta diagrams (plotting δ D vs. δ ^18 O), we showed that the annual mean value was a good indicator for determining the origins of subsurface waters in the CSSWs. To confirm the origins of rainwater and to explain the variations in isotopic ratios, we conducted atmospheric water budget analysis using Tropical Rainfall Measuring Mission (TRMM) multi-satellite precipitation analysis (TMPA) data and ERA-Interim atmospheric reanalysis data. The results showed that around three-fourths of rainwater was derived from recycled water at local–regional scales. Satellite-observed outgoing longwave radiation (OLR) and complementary satellite data from MODerate-resolution Imaging Spectroradiometer (MODIS) and Advanced Microwave Scanning Radiometer (AMSR) series implied that the isotopic ratios in rainwater were affected by evaporation of raindrops falling from convective clouds. Consequently, integrated SWI analysis of rain-, surface and subsurface waters, together with the atmospheric water budget analysis, revealed that shallow groundwater of small wetlands in this region was very likely to be recharged from surface waters originating from local rainfall, which was temporarily pooled in small wetlands. This was also supported by tritium ( ^3 H) counting of the current rain- and subsurface waters in the region. We highly recommend that shallow groundwater not be pumped intensively to conserve surface and subsurface waters, both of which are important water resources in the region.
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spelling doaj.art-a2409585d8164b66963f65d808535e522023-08-09T14:30:44ZengIOP PublishingEnvironmental Research Letters1748-93262017-01-0112303401210.1088/1748-9326/aa5bc8Analysing the origin of rain- and subsurface water in seasonal wetlands of north-central NamibiaTetsuya Hiyama0Hironari Kanamori1Jack R Kambatuku2Ayumi Kotani3Kazuyoshi Asai4Hiroki Mizuochi5Yuichiro Fujioka6Morio Iijima7Institute for Space-Earth Environmental Research , Nagoya University, Nagoya, Japan; Author to whom any correspondence should be addressed.Institute for Space-Earth Environmental Research , Nagoya University, Nagoya, JapanFaculty of Agriculture and Natural Resources , University of Namibia, Oshakati, NamibiaGraduate School of Bioagricultural Sciences , Nagoya University, Nagoya, JapanGeo-Science Laboratory Co. Ltd , Nagoya, JapanGraduate School of Life and Environmental Sciences , University of Tsukuba, Tsukuba, JapanFrontier Research Institute for Interdisciplinary Sciences , Tohoku University, Sendai, JapanFaculty of Agriculture , Kindai University, Nara, JapanWe investigated the origins of rain- and subsurface waters of north-central Namibia’s seasonal wetlands, which are critical to the region’s water and food security. The region includes the southern part of the Cuvelai system seasonal wetlands (CSSWs) of the Cuvelai Basin, a transboundary river basin covering southern Angola and northern Namibia. We analysed stable water isotopes (SWIs) of hydrogen (HDO) and oxygen (H _2 ^18 O) in rainwater, surface water and shallow groundwater. Rainwater samples were collected during every rainfall event of the rainy season from October 2013 to April 2014. The isotopic ratios of HDO ( δ D) and oxygen H _2 ^18 O ( δ ^18 O) were analysed in each rainwater sample and then used to derive the annual mean value of ( δ D, δ ^18 O) in precipitation weighted by each rainfall volume. Using delta diagrams (plotting δ D vs. δ ^18 O), we showed that the annual mean value was a good indicator for determining the origins of subsurface waters in the CSSWs. To confirm the origins of rainwater and to explain the variations in isotopic ratios, we conducted atmospheric water budget analysis using Tropical Rainfall Measuring Mission (TRMM) multi-satellite precipitation analysis (TMPA) data and ERA-Interim atmospheric reanalysis data. The results showed that around three-fourths of rainwater was derived from recycled water at local–regional scales. Satellite-observed outgoing longwave radiation (OLR) and complementary satellite data from MODerate-resolution Imaging Spectroradiometer (MODIS) and Advanced Microwave Scanning Radiometer (AMSR) series implied that the isotopic ratios in rainwater were affected by evaporation of raindrops falling from convective clouds. Consequently, integrated SWI analysis of rain-, surface and subsurface waters, together with the atmospheric water budget analysis, revealed that shallow groundwater of small wetlands in this region was very likely to be recharged from surface waters originating from local rainfall, which was temporarily pooled in small wetlands. This was also supported by tritium ( ^3 H) counting of the current rain- and subsurface waters in the region. We highly recommend that shallow groundwater not be pumped intensively to conserve surface and subsurface waters, both of which are important water resources in the region.https://doi.org/10.1088/1748-9326/aa5bc8stable water isotopes (SWIs)rainwatersurface watersubsurface wateratmospheric water budgetrecycled water
spellingShingle Tetsuya Hiyama
Hironari Kanamori
Jack R Kambatuku
Ayumi Kotani
Kazuyoshi Asai
Hiroki Mizuochi
Yuichiro Fujioka
Morio Iijima
Analysing the origin of rain- and subsurface water in seasonal wetlands of north-central Namibia
Environmental Research Letters
stable water isotopes (SWIs)
rainwater
surface water
subsurface water
atmospheric water budget
recycled water
title Analysing the origin of rain- and subsurface water in seasonal wetlands of north-central Namibia
title_full Analysing the origin of rain- and subsurface water in seasonal wetlands of north-central Namibia
title_fullStr Analysing the origin of rain- and subsurface water in seasonal wetlands of north-central Namibia
title_full_unstemmed Analysing the origin of rain- and subsurface water in seasonal wetlands of north-central Namibia
title_short Analysing the origin of rain- and subsurface water in seasonal wetlands of north-central Namibia
title_sort analysing the origin of rain and subsurface water in seasonal wetlands of north central namibia
topic stable water isotopes (SWIs)
rainwater
surface water
subsurface water
atmospheric water budget
recycled water
url https://doi.org/10.1088/1748-9326/aa5bc8
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