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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2021
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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) |
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Great Artesian Basin groundwater storage variation GRACE PCA MLRA rainfall Science Q |
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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 |
_version_ |
1718431662459584512 |