The spatial and temporal subsidence variability of the east mesa geothermal field, California, USA, and its potential impact on the all American canal system
Authors: Han, J.Y., Forster, R.R., Moser, D.E., Ford, A.L.J., Ramírez-Hernández, J. and Tiampo, K.F.
Journal: International Journal of Remote Sensing
Volume: 32
Issue: 12
Pages: 3427-3449
eISSN: 1366-5901
ISSN: 0143-1161
DOI: 10.1080/01431161003749444
Abstract:The spatiotemporal variability of subsidence around the East Mesa Geothermal Field (EMGF) near the All American Canal (AAC) has been measured using 30 temporally averaged interferograms from 1992 to 2000. Deformation rate maps from two shorter time periods indicated the maximum subsidence rate of the EMGF was reduced from -43 mm year-1 (1992-1997) to -34 mm year-1 (1996-2000) corresponding to decreasing net geothermal water production. The maximum subsidence on the East Highline Canal was -9.5 ± 0.5 and -2.4 ± 0.8 cm for each shorter time period. Interferometric synthetic aperture radar (InSAR) stacking demonstrated its utility in monitoring subsidence of the canal caused by the nearby geothermal plant at regional coverage superior to ground levelling networks. Such data on the subsidence of surface and subsurface hydrodynamics along the US-Mexico border are scarce, and are particularly significant in a zone of present and likely future acute water resource management sensitivity. © 2011 Taylor & Francis.
Source: Scopus
The spatial and temporal subsidence variability of the East Mesa Geothermal Field, California, USA, and its potential impact on the All American Canal System
Authors: Han, J.-Y., Forster, R.R., Moser, D.E., Ford, A.L.J., Ramirez-Hernandez, J. and Tiampo, K.F.
Journal: INTERNATIONAL JOURNAL OF REMOTE SENSING
Volume: 32
Issue: 12
Pages: 3427-3449
eISSN: 1366-5901
ISSN: 0143-1161
DOI: 10.1080/01431161003749444
Source: Web of Science (Lite)
The Spatial and Temporal Subsidence Variability of the East Mesa Geothermal Field, CA, USA and its Potential Impact on the All American Canal System
Authors: Han, J.Y., Forster, R.R., Moser, D.E., Ford, A.L.J., Ramírez-Hernandez, J. and Tiampo, K.F.
Journal: International Journal of Remote Sensing
Volume: 32
Pages: 3427-3449
ISSN: 0143-1161
DOI: 10.1080/01431161003749444
Abstract:The spatiotemporal variability of subsidence around the East Mesa Geothermal Field (EMGF) near the All American Canal (AAC) has been measured using 30 temporally averaged interferograms from 1992 to 2000. Deformation rate maps from two shorter time periods indicated the maximum subsidence rate of the EMGF was reduced from -43 mm year-1 (1992–1997) to -34 mm year-1 (1996–2000) corresponding to decreasing net geothermal water production. The maximum subsidence on the East Highline Canal was -9.5 +/- 0.5 and -2.4 +/- 0.8 cm for each shorter time period. Interferometric synthetic aperture radar (InSAR) stacking demonstrated its utility in monitoring subsidence of the canal caused by the nearby geothermal plant at regional coverage superior to ground levelling networks. Such data on the subsidence of surface and subsurface hydrodynamics along the US–Mexico border are scarce, and are particularly significant in a zone of present and likely future acute water resource management sensitivity.
http://dx.doi.org/10.1080/01431161003749444
Source: Manual
Preferred by: Andrew Ford