Assessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations

The influence of climate change and anthropogenic activities (e.g., water withdrawals) on groundwater basins has gained attention recently across the globe. However, the understanding of hydrological stores (e.g., groundwater storage) in one of the largest and deepest artesian basins, the Great Arte...

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Autores principales: Pankaj R. Kaushik, Christopher E. Ndehedehe, Ryan M. Burrows, Mark R. Noll, Mark J. Kennard
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:9fd8f898d4b94970aa96aa19782d88932021-11-11T18:57:50ZAssessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations10.3390/rs132144582072-4292https://doaj.org/article/9fd8f898d4b94970aa96aa19782d88932021-11-01T00:00:00Zhttps://www.mdpi.com/2072-4292/13/21/4458https://doaj.org/toc/2072-4292The influence of climate change and anthropogenic activities (e.g., water withdrawals) on groundwater basins has gained attention recently across the globe. However, the understanding of hydrological stores (e.g., groundwater storage) in one of the largest and deepest artesian basins, the Great Artesian Basin (GAB) is limited due to the poor distribution of groundwater monitoring bores. In this study, Gravity Recovery and Climate Experiment (GRACE) satellite and ancillary data from observations and models (soil moisture, rainfall, and evapotranspiration (ET)) were used to assess changes in terrestrial water storage and groundwater storage (GWS) variations across the GAB and its sub-basins (Carpentaria, Surat, Western Eromanga, and Central Eromanga). Results show that there is strong relationship of GWS variation with rainfall (r = 0.9) and ET (r = 0.9 to 1) in the Surat and some parts of the Carpentaria sub-basin in the GAB (2002–2017). Using multi-variate methods, we found that variation in GWS is primarily driven by rainfall in the Carpentaria sub-basin. While changes in rainfall account for much of the observed spatio-temporal distribution of water storage changes in Carpentaria and some parts of the Surat sub-basin (r = 0.90 at 0–2 months lag), the relationship of GWS with rainfall and ET in Central Eromanga sub-basin (r = 0.10–0.30 at more than 12 months lag) suggest the effects of human water extraction in the GAB.Pankaj R. KaushikChristopher E. NdehedeheRyan M. BurrowsMark R. NollMark J. KennardMDPI AGarticleGreat Artesian Basingroundwater storage variationGRACEPCAMLRArainfallScienceQENRemote Sensing, Vol 13, Iss 4458, p 4458 (2021)
institution DOAJ
collection DOAJ
language EN
topic Great Artesian Basin
groundwater storage variation
GRACE
PCA
MLRA
rainfall
Science
Q
spellingShingle Great Artesian Basin
groundwater storage variation
GRACE
PCA
MLRA
rainfall
Science
Q
Pankaj R. Kaushik
Christopher E. Ndehedehe
Ryan M. Burrows
Mark R. Noll
Mark J. Kennard
Assessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations
description The influence of climate change and anthropogenic activities (e.g., water withdrawals) on groundwater basins has gained attention recently across the globe. However, the understanding of hydrological stores (e.g., groundwater storage) in one of the largest and deepest artesian basins, the Great Artesian Basin (GAB) is limited due to the poor distribution of groundwater monitoring bores. In this study, Gravity Recovery and Climate Experiment (GRACE) satellite and ancillary data from observations and models (soil moisture, rainfall, and evapotranspiration (ET)) were used to assess changes in terrestrial water storage and groundwater storage (GWS) variations across the GAB and its sub-basins (Carpentaria, Surat, Western Eromanga, and Central Eromanga). Results show that there is strong relationship of GWS variation with rainfall (r = 0.9) and ET (r = 0.9 to 1) in the Surat and some parts of the Carpentaria sub-basin in the GAB (2002–2017). Using multi-variate methods, we found that variation in GWS is primarily driven by rainfall in the Carpentaria sub-basin. While changes in rainfall account for much of the observed spatio-temporal distribution of water storage changes in Carpentaria and some parts of the Surat sub-basin (r = 0.90 at 0–2 months lag), the relationship of GWS with rainfall and ET in Central Eromanga sub-basin (r = 0.10–0.30 at more than 12 months lag) suggest the effects of human water extraction in the GAB.
format article
author Pankaj R. Kaushik
Christopher E. Ndehedehe
Ryan M. Burrows
Mark R. Noll
Mark J. Kennard
author_facet Pankaj R. Kaushik
Christopher E. Ndehedehe
Ryan M. Burrows
Mark R. Noll
Mark J. Kennard
author_sort Pankaj R. Kaushik
title Assessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations
title_short Assessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations
title_full Assessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations
title_fullStr Assessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations
title_full_unstemmed Assessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations
title_sort assessing changes in terrestrial water storage components over the great artesian basin using satellite observations
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/9fd8f898d4b94970aa96aa19782d8893
work_keys_str_mv AT pankajrkaushik assessingchangesinterrestrialwaterstoragecomponentsoverthegreatartesianbasinusingsatelliteobservations
AT christopherendehedehe assessingchangesinterrestrialwaterstoragecomponentsoverthegreatartesianbasinusingsatelliteobservations
AT ryanmburrows assessingchangesinterrestrialwaterstoragecomponentsoverthegreatartesianbasinusingsatelliteobservations
AT markrnoll assessingchangesinterrestrialwaterstoragecomponentsoverthegreatartesianbasinusingsatelliteobservations
AT markjkennard assessingchangesinterrestrialwaterstoragecomponentsoverthegreatartesianbasinusingsatelliteobservations
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