Land subsidence in the San Joaquin Valley, California, USA, 2007–2014

Rapid land subsidence was recently measured using multiple methods in two areas of the San Joaquin Valley (SJV): between Merced and Fresno (El Nido), and between Fresno and Bakersfield (Pixley). Recent land-use changes and diminished surface-water availability have led to increased groundwater p...

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Main Authors: M. Sneed, J. T. Brandt
Format: Article
Language:English
Published: Copernicus Publications 2015-11-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/372/23/2015/piahs-372-23-2015.pdf
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spelling doaj-74f259a8608f4f73ba87d6264e9f188f2020-11-24T23:16:28ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2015-11-01372232710.5194/piahs-372-23-2015Land subsidence in the San Joaquin Valley, California, USA, 2007–2014M. Sneed0J. T. Brandt1US Geological Survey, 6000 J Street, Placer Hall, Sacramento, CA 95819, USAUS Geological Survey, 6000 J Street, Placer Hall, Sacramento, CA 95819, USARapid land subsidence was recently measured using multiple methods in two areas of the San Joaquin Valley (SJV): between Merced and Fresno (El Nido), and between Fresno and Bakersfield (Pixley). Recent land-use changes and diminished surface-water availability have led to increased groundwater pumping, groundwater-level declines, and land subsidence. Differential land subsidence has reduced the flow capacity of water-conveyance systems in these areas, exacerbating flood hazards and affecting the delivery of irrigation water. <br><br> Vertical land-surface changes during 2007–2014 were determined by using Interferometric Synthetic Aperture Radar (InSAR), Continuous Global Positioning System (CGPS), and extensometer data. Results of the InSAR analysis indicate that about 7600 km<sup>2</sup> subsided 50–540 mm during 2008–2010; CGPS and extensometer data indicate that these rates continued or accelerated through December 2014. The maximum InSAR-measured rate of 270 mm yr<sup>−1</sup> occurred in the El Nido area, and is among the largest rates ever measured in the SJV. In the Pixley area, the maximum InSAR-measured rate during 2008–2010 was 90 mm yr<sup>−1</sup>. Groundwater was an important part of the water supply in both areas, and pumping increased when land use changed or when surface water was less available. This increased pumping caused groundwater-level declines to near or below historical lows during the drought periods 2007–2009 and 2012–present. <br><br> Long-term groundwater-level and land-subsidence monitoring in the SJV is critical for understanding the interconnection of land use, groundwater levels, and subsidence, and evaluating management strategies that help mitigate subsidence hazards to infrastructure while optimizing water supplies.https://www.proc-iahs.net/372/23/2015/piahs-372-23-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Sneed
J. T. Brandt
spellingShingle M. Sneed
J. T. Brandt
Land subsidence in the San Joaquin Valley, California, USA, 2007–2014
Proceedings of the International Association of Hydrological Sciences
author_facet M. Sneed
J. T. Brandt
author_sort M. Sneed
title Land subsidence in the San Joaquin Valley, California, USA, 2007–2014
title_short Land subsidence in the San Joaquin Valley, California, USA, 2007–2014
title_full Land subsidence in the San Joaquin Valley, California, USA, 2007–2014
title_fullStr Land subsidence in the San Joaquin Valley, California, USA, 2007–2014
title_full_unstemmed Land subsidence in the San Joaquin Valley, California, USA, 2007–2014
title_sort land subsidence in the san joaquin valley, california, usa, 2007–2014
publisher Copernicus Publications
series Proceedings of the International Association of Hydrological Sciences
issn 2199-8981
2199-899X
publishDate 2015-11-01
description Rapid land subsidence was recently measured using multiple methods in two areas of the San Joaquin Valley (SJV): between Merced and Fresno (El Nido), and between Fresno and Bakersfield (Pixley). Recent land-use changes and diminished surface-water availability have led to increased groundwater pumping, groundwater-level declines, and land subsidence. Differential land subsidence has reduced the flow capacity of water-conveyance systems in these areas, exacerbating flood hazards and affecting the delivery of irrigation water. <br><br> Vertical land-surface changes during 2007–2014 were determined by using Interferometric Synthetic Aperture Radar (InSAR), Continuous Global Positioning System (CGPS), and extensometer data. Results of the InSAR analysis indicate that about 7600 km<sup>2</sup> subsided 50–540 mm during 2008–2010; CGPS and extensometer data indicate that these rates continued or accelerated through December 2014. The maximum InSAR-measured rate of 270 mm yr<sup>−1</sup> occurred in the El Nido area, and is among the largest rates ever measured in the SJV. In the Pixley area, the maximum InSAR-measured rate during 2008–2010 was 90 mm yr<sup>−1</sup>. Groundwater was an important part of the water supply in both areas, and pumping increased when land use changed or when surface water was less available. This increased pumping caused groundwater-level declines to near or below historical lows during the drought periods 2007–2009 and 2012–present. <br><br> Long-term groundwater-level and land-subsidence monitoring in the SJV is critical for understanding the interconnection of land use, groundwater levels, and subsidence, and evaluating management strategies that help mitigate subsidence hazards to infrastructure while optimizing water supplies.
url https://www.proc-iahs.net/372/23/2015/piahs-372-23-2015.pdf
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