Estimation of Terrestrial Water Storage in the Western United States Using Space-based Gravimetry, Ground-based Sensors, and Model-based Hydrologic Loading
dc.contributor.advisor | Forman, Barton A | en_US |
dc.contributor.author | Yin, Gaohong | en_US |
dc.contributor.department | Civil Engineering | en_US |
dc.contributor.publisher | Digital Repository at the University of Maryland | en_US |
dc.contributor.publisher | University of Maryland (College Park, Md.) | en_US |
dc.date.accessioned | 2020-10-10T05:34:14Z | |
dc.date.available | 2020-10-10T05:34:14Z | |
dc.date.issued | 2020 | en_US |
dc.description.abstract | Accurate estimation of terrestrial water storage (TWS) is critically important for the global hydrologic cycle and the Earth's climate system. The space-based Gravity Recovery and Climate Experiment (GRACE) mission and land surface models (LSMs) have provided valuable information in monitoring TWS changes. In recent years, geodetic measurements from the ground-based Global Positioning System (GPS) network have been increasingly used in hydrologic studies based on the elastic response of the Earth's surface to mass redistribution. All of these techniques have their own strengths and weaknesses in detecting TWS changes due to their unique uncertainties, error characteristics, and spatio-temporal resolutions. This dissertation investigated the potential of improving our knowledge in TWS changes via merging the information provided by ground-based GPS, GRACE, and LSMs. First, the vertical displacements derived from ground-based GPS, GRACE, and NASA Catchment Land Surface Model (Catchment) were compared to analyze the behavior and error characteristics of each data set. Afterwards, the ground-based GPS observations were merged into Catchment using a data assimilation (DA) framework in order to improve the accuracy of TWS estimates and mitigate hydrologic state uncertainty. To the best of our knowledge, this study is the first attempt to assimilate ground-based GPS observations into an advanced land surface model for the purpose of improving TWS estimates. TWS estimates provided by GPS DA were evaluated against GRACE TWS retrievals. GPS DA performance in estimating TWS constituent components (i.e., snow water equivalent and soil moisture) and hydrologic fluxes (i.e., runoff) were also examined using ground-based in situ measurements. GPS DA yielded encouraging results in terms of improving TWS estimates, especially during drought periods. Additionally, the findings suggest a multi-variate assimilation approach to merge both GRACE and ground-based GPS into the LSMs to further improve modeled TWS and its constituent components should be pursued as a new and novel research project. | en_US |
dc.identifier | https://doi.org/10.13016/jqes-ssni | |
dc.identifier.uri | http://hdl.handle.net/1903/26598 | |
dc.language.iso | en | en_US |
dc.subject.pqcontrolled | Hydrologic sciences | en_US |
dc.subject.pqcontrolled | Remote sensing | en_US |
dc.subject.pqcontrolled | Water resources management | en_US |
dc.subject.pquncontrolled | GRACE | en_US |
dc.subject.pquncontrolled | Ground-based GPS | en_US |
dc.subject.pquncontrolled | Land Surface Model | en_US |
dc.subject.pquncontrolled | Surface Deformation | en_US |
dc.subject.pquncontrolled | Terrestrial Water Storage | en_US |
dc.title | Estimation of Terrestrial Water Storage in the Western United States Using Space-based Gravimetry, Ground-based Sensors, and Model-based Hydrologic Loading | en_US |
dc.type | Dissertation | en_US |
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