Articles | Volume 372
https://doi.org/10.5194/piahs-372-29-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/piahs-372-29-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Evaluation of the potential of InSAR time series to study the spatio-temporal evolution of piezometric levels in the Madrid aquifer
M. Béjar-Pizarro
Geohazards InSAR laboratory and Modeling group (InSARlab), Geoscience research department, Geological Survey of Spain (IGME), Alenza 1, 28003 Madrid, Spain
Unidad Asociada de investigación IGME-UA de movimientos del terreno mediante interferometría radar (UNIRAD), Universidad de Alicante, P.O. Box 99, 03080 Alicante, Spain
Grupo Español de Trabajo en Subsidencia del Terreno (SUBTER) from the UNESCO, P.O. Box 99, 03080 Alicante, Spain
P. Ezquerro Martín
Geohazards InSAR laboratory and Modeling group (InSARlab), Geoscience research department, Geological Survey of Spain (IGME), Alenza 1, 28003 Madrid, Spain
Grupo Español de Trabajo en Subsidencia del Terreno (SUBTER) from the UNESCO, P.O. Box 99, 03080 Alicante, Spain
Technical University of Madrid. Laboratorio de Topografía y Geomática, ETSI Caminos, Canales y Puertos C/Profesor Aranguren s/n, 28040 Madrid, Spain
G. Herrera
Geohazards InSAR laboratory and Modeling group (InSARlab), Geoscience research department, Geological Survey of Spain (IGME), Alenza 1, 28003 Madrid, Spain
Unidad Asociada de investigación IGME-UA de movimientos del terreno mediante interferometría radar (UNIRAD), Universidad de Alicante, P.O. Box 99, 03080 Alicante, Spain
Grupo Español de Trabajo en Subsidencia del Terreno (SUBTER) from the UNESCO, P.O. Box 99, 03080 Alicante, Spain
Earth Observation and Geohazards Expert Group (EOEG), EuroGeoSurveys, The Geological Surveys of Europe, 36-38, Rue Joseph II, 1000 Brussels, Belgium
Unidad Asociada de investigación IGME-UA de movimientos del terreno mediante interferometría radar (UNIRAD), Universidad de Alicante, P.O. Box 99, 03080 Alicante, Spain
Grupo Español de Trabajo en Subsidencia del Terreno (SUBTER) from the UNESCO, P.O. Box 99, 03080 Alicante, Spain
Departamento de Ingeniería Civil, Escuela Politécnica Superior, Universidad de Alicante, P.O. Box 99, 03080 Alicante, Spain
C. Guardiola-Albert
Geohazards InSAR laboratory and Modeling group (InSARlab), Geoscience research department, Geological Survey of Spain (IGME), Alenza 1, 28003 Madrid, Spain
Geoscience research department, Geological Survey of Spain (IGME), Alenza 1, 28003 Madrid, Spain
J. M. Ruiz Hernández
Geoscience research department, Geological Survey of Spain (IGME), Alenza 1, 28003 Madrid, Spain
M. Marchamalo Sacristán
Geohazards InSAR laboratory and Modeling group (InSARlab), Geoscience research department, Geological Survey of Spain (IGME), Alenza 1, 28003 Madrid, Spain
Grupo Español de Trabajo en Subsidencia del Terreno (SUBTER) from the UNESCO, P.O. Box 99, 03080 Alicante, Spain
Technical University of Madrid. Laboratorio de Topografía y Geomática, ETSI Caminos, Canales y Puertos C/Profesor Aranguren s/n, 28040 Madrid, Spain
R. Martínez Marín
Grupo Español de Trabajo en Subsidencia del Terreno (SUBTER) from the UNESCO, P.O. Box 99, 03080 Alicante, Spain
Technical University of Madrid. Laboratorio de Topografía y Geomática, ETSI Caminos, Canales y Puertos C/Profesor Aranguren s/n, 28040 Madrid, Spain
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Short summary
We use InSAR time series to infer the temporal evolution of the piezometric level in 19 wells of the Tertiary detritic aquifer of Madrid (TDAM) in the period 1997-2010. Our results suggest that an average elastic storage coefficient Ske of all wells can be used to estimate piezometric level variations in all the points where ground deformation has been measured by InSAR, thus allowing production of piezometric level maps for the different extraction/recovery cycles in the TDAM.
We use InSAR time series to infer the temporal evolution of the piezometric level in 19 wells of...