InSAR constraints on soil moisture evolution after the March 2015 extreme precipitation event in Chile

Abstarct Constraints on soil moisture can guide agricultural practices, act as input into weather, flooding and climate models and inform water resource policies. Space-based interferometric synthetic aperture radar (InSAR) observations provide near-global coverage, even in the presence of clouds, o...

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Main Authors: C. P. Scott, R. B. Lohman, T. E. Jordan
Format: Article
Language:English
Published: Nature Publishing Group 2017-07-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-017-05123-4
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spelling doaj-c6f80365c645459ca6d18cdab2c9600b2020-12-08T00:43:01ZengNature Publishing GroupScientific Reports2045-23222017-07-01711910.1038/s41598-017-05123-4InSAR constraints on soil moisture evolution after the March 2015 extreme precipitation event in ChileC. P. Scott0R. B. Lohman1T. E. Jordan2Department of Earth and Atmospheric Sciences, Cornell UniversityDepartment of Earth and Atmospheric Sciences, Cornell UniversityDepartment of Earth and Atmospheric Sciences, Cornell UniversityAbstarct Constraints on soil moisture can guide agricultural practices, act as input into weather, flooding and climate models and inform water resource policies. Space-based interferometric synthetic aperture radar (InSAR) observations provide near-global coverage, even in the presence of clouds, of proxies for soil moisture derived from the amplitude and phase content of radar imagery. We describe results from a 1.5 year-long InSAR time series spanning the March, 2015 extreme precipitation event in the hyperarid Atacama desert of Chile, constraining the immediate increase in soil moisture and drying out over the following months, as well as the response to a later, smaller precipitation event. The inferred temporal evolution of soil moisture is remarkably consistent between independent, overlapping SAR tracks covering a region ~100 km in extent. The unusually large rain event, combined with the extensive spatial and temporal coverage of the SAR dataset, present an unprecedented opportunity to image the time-evolution of soil characteristics over different surface types. Constraints on the timescale of shallow water storage after precipitation events are increasingly valuable as global water resources continue to be stretched to their limits and communities continue to develop in flood-prone areas.https://doi.org/10.1038/s41598-017-05123-4
collection DOAJ
language English
format Article
sources DOAJ
author C. P. Scott
R. B. Lohman
T. E. Jordan
spellingShingle C. P. Scott
R. B. Lohman
T. E. Jordan
InSAR constraints on soil moisture evolution after the March 2015 extreme precipitation event in Chile
Scientific Reports
author_facet C. P. Scott
R. B. Lohman
T. E. Jordan
author_sort C. P. Scott
title InSAR constraints on soil moisture evolution after the March 2015 extreme precipitation event in Chile
title_short InSAR constraints on soil moisture evolution after the March 2015 extreme precipitation event in Chile
title_full InSAR constraints on soil moisture evolution after the March 2015 extreme precipitation event in Chile
title_fullStr InSAR constraints on soil moisture evolution after the March 2015 extreme precipitation event in Chile
title_full_unstemmed InSAR constraints on soil moisture evolution after the March 2015 extreme precipitation event in Chile
title_sort insar constraints on soil moisture evolution after the march 2015 extreme precipitation event in chile
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2017-07-01
description Abstarct Constraints on soil moisture can guide agricultural practices, act as input into weather, flooding and climate models and inform water resource policies. Space-based interferometric synthetic aperture radar (InSAR) observations provide near-global coverage, even in the presence of clouds, of proxies for soil moisture derived from the amplitude and phase content of radar imagery. We describe results from a 1.5 year-long InSAR time series spanning the March, 2015 extreme precipitation event in the hyperarid Atacama desert of Chile, constraining the immediate increase in soil moisture and drying out over the following months, as well as the response to a later, smaller precipitation event. The inferred temporal evolution of soil moisture is remarkably consistent between independent, overlapping SAR tracks covering a region ~100 km in extent. The unusually large rain event, combined with the extensive spatial and temporal coverage of the SAR dataset, present an unprecedented opportunity to image the time-evolution of soil characteristics over different surface types. Constraints on the timescale of shallow water storage after precipitation events are increasingly valuable as global water resources continue to be stretched to their limits and communities continue to develop in flood-prone areas.
url https://doi.org/10.1038/s41598-017-05123-4
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