Title:
Data assimilation and dynamical downscaling of remotely-sensed precipitation and soil moisture from space

dc.contributor.advisor Bras, Rafael L.
dc.contributor.author Lin, Liao-Fan
dc.contributor.committeeMember Wang, Jingfeng
dc.contributor.committeeMember Georgakakos, Aris
dc.contributor.committeeMember Di Lorenzo, Emanuele
dc.contributor.committeeMember Flores, Alejandro
dc.contributor.department Civil and Environmental Engineering
dc.date.accessioned 2016-05-27T13:12:46Z
dc.date.available 2016-05-27T13:12:46Z
dc.date.created 2016-05
dc.date.issued 2016-04-01
dc.date.submitted May 2016
dc.date.updated 2016-05-27T13:12:46Z
dc.description.abstract Environmental monitoring of Earth from space has provided invaluable information for understanding the land-atmosphere water and energy exchanges. However, the use of satellite observations in hydrologic applications is often limited by coarse space-time resolutions. This study aims to develop a data assimilation system that integrates remotely-sensed precipitation and soil moisture observations into physically-based models to produce fine-scale precipitation, soil moisture, and other relevant hydrometeorological variables. This is particularly useful with the active Global Precipitation Measurement and Soil Moisture Active Passive missions. The system consists of two major components: (1) a framework for dynamic downscaling of satellite precipitation products using the Weather Research and Forecasting (WRF) model with four-dimensional variational data assimilation (4D-Var) and (2) a variational data assimilation system using spatio-temporally varying background error covariance for directly assimilating satellite soil moisture data into the Noah land surface model coupled with the WRF model. The WRF 4D-Var system can effectively assimilate and downscale six-hour precipitation products of a spatial resolution of about 20 km (i.e., those derived from the National Centers for Environmental Prediction Stage IV data and the Tropical Rainfall Measuring Mission (TRMM) 3B42 dataset) to hourly precipitation with a spatial resolution of less than 10 km. The system is able to assimilate and downscale daily soil moisture products at a gridded 36-km resolution obtained from the Soil Moisture and Ocean Salinity (SMOS) mission to produce hourly 4-by-4 km surface soil moisture forecasts with a reduction of mean absolute error by 35% on average. The results from the system with coupled components show that assimilation of the TRMM 3B42 precipitation improves the quality of both downscaled precipitation and soil moisture analyses, while the effect of SMOS soil moisture data assimilation is largely on the soil moisture analyses. The downscaled WRF precipitation, with and without assimilation of TRMM precipitation, was preliminarily tested with a spatially distributed simulation of streamflow using the TIN (Triangular Irregular Network)-based Real-time Integrated Basin Simulator (tRIBS).
dc.description.degree Ph.D.
dc.format.mimetype application/pdf
dc.identifier.uri http://hdl.handle.net/1853/54974
dc.language.iso en_US
dc.publisher Georgia Institute of Technology
dc.subject Precipitation
dc.subject Soil moisture
dc.subject Data assimilation
dc.subject Dynamical downscaling
dc.subject Weather research and forecasting
dc.subject Land-atmosphere interaction
dc.subject Remote sensing
dc.subject Hydrometeorology
dc.subject Hydrology
dc.title Data assimilation and dynamical downscaling of remotely-sensed precipitation and soil moisture from space
dc.type Text
dc.type.genre Dissertation
dspace.entity.type Publication
local.contributor.advisor Bras, Rafael L.
local.contributor.corporatename School of Civil and Environmental Engineering
local.contributor.corporatename College of Engineering
relation.isAdvisorOfPublication 64e45b8f-3df1-4e41-84d2-0cd91b9a0d61
relation.isOrgUnitOfPublication 88639fad-d3ae-4867-9e7a-7c9e6d2ecc7c
relation.isOrgUnitOfPublication 7c022d60-21d5-497c-b552-95e489a06569
thesis.degree.level Doctoral
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