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Authordc.contributor.authorJordan, Teresa E. 
Authordc.contributor.authorLohman, Rowena B. 
Authordc.contributor.authorTapia, Lorenzo 
Authordc.contributor.authorPfeiffer Jakob, Marco 
Authordc.contributor.authorScott, Chelsea P. 
Authordc.contributor.authorAmundson, Ronald 
Authordc.contributor.authorGodfrey, Linda 
Authordc.contributor.authorRiquelme, Rodrigo 
Admission datedc.date.accessioned2020-05-08T23:07:16Z
Available datedc.date.available2020-05-08T23:07:16Z
Publication datedc.date.issued2020
Cita de ítemdc.identifier.citationRemote Sensing of Environment 237 (2020) 111544es_ES
Identifierdc.identifier.other10.1016/j.rse.2019.111544
Identifierdc.identifier.urihttp://repositorio.uchile.cl/handle/2250/174623
Abstractdc.description.abstractGround-based monitoring and remote sensing of extreme rain events in the hyperarid Atacama Desert, Chile, reveal a complex relationship between precipitation, soil types and interferometric synthetic aperture radar (InSAR) coherence. These integrated analyses allow examination of temporal and spatial variations of the soil moisture response between locations dominated by sulfate soils and those with immature, silicate-mineral soils. The radar dataset captures at least four separate rain events within the 2015-2017 timeframe, two of which were regionally devastating. The lack of vegetation in this region allows us to discriminate between contributions to the InSAR coherence from permanent changes of the landscape (e.g., erosion or deposition) and transient changes associated with soil moisture variability. The spatial distribution and character of the transient InSAR response depends strongly on soil type, and is remarkably repeatable between rain events. The areas that experienced permanent changes included river channels, steep slopes, playas, and sites of anthropogenic activity, such as roads, mines, or telescope construction. Ground-based observations of soil moisture after each event also exhibit a strong dependence on soil type. The observations presented here demonstrate how InSAR data can constrain variations in soil moisture with high spatial resolution over large regions, complementing the higher-sensitivity but sparser field sites and enabling discrimination of inter-event variability and analysis of longer-term changes in soil mineralogy in arid regions.es_ES
Patrocinadordc.description.sponsorshipChile's CONICYT (Comisión Nacional de Investigación Científica y Tecnológica, Chile) Anillo ACT1203 National Aeronautics & Space Administration (NASA) NNX16AK57Ges_ES
Lenguagedc.language.isoenes_ES
Publisherdc.publisherElsevieres_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/*
Sourcedc.sourceRemote Sensing of Environmentes_ES
Keywordsdc.subjectSentineles_ES
Keywordsdc.subjectSoil moisturees_ES
Keywordsdc.subjectRemote sensinges_ES
Keywordsdc.subjectSoilses_ES
Keywordsdc.subjectActive radares_ES
Keywordsdc.subjectInterferometric coherencees_ES
Títulodc.titleSurface materials and landforms as controls on InSAR permanent and transient responses to precipitation events in a hyperarid desert, Chilees_ES
Document typedc.typeArtículo de revistaes_ES
dcterms.accessRightsdcterms.accessRightsAcceso Abierto
Catalogueruchile.catalogadorctces_ES
Indexationuchile.indexArtículo de publicación ISIes_ES


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Attribution-NonCommercial-NoDerivs 3.0 Chile
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 Chile