2012
DOI: 10.1002/hyp.9611
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Measuring water availability with limited ground data: assessing the feasibility of an entirely remote-sensing-based hydrologic budget of the Rufiji Basin, Tanzania, using TRMM, GRACE, MODIS, SRB, and AIRS

Abstract: This study explores the feasibility of an entirely satellite remote sensing (RS)‐based hydrologic budget model for a ground data‐constrained basin, the Rufiji basin in Tanzania, from the balance of runoff (Q), precipitation (P), storage change (ΔS), and evapotranspiration (ET). P was determined from the Tropical Rainfall Measuring Mission, ΔS from the Gravity Recovery and Climate Experiment, and ET from the Moderate Resolution Imaging Spectroradiometer, the surface radiation budget, and the Atmosphere Infrared… Show more

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Cited by 36 publications
(40 citation statements)
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References 92 publications
(138 reference statements)
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“…The model can be driven entirely with remote sensing and does not include or require calibration, spinup, or initialization. 1 For one class of products, those based on AIRS meteorological data, we substitute daily mean air temperature for daily maximum air temperature (see Armanios and Fisher 2014). We calculated terrestrial ET globally for ice-free land, as defined by Friedl et al (2010).…”
Section: Methodsmentioning
confidence: 99%
“…The model can be driven entirely with remote sensing and does not include or require calibration, spinup, or initialization. 1 For one class of products, those based on AIRS meteorological data, we substitute daily mean air temperature for daily maximum air temperature (see Armanios and Fisher 2014). We calculated terrestrial ET globally for ice-free land, as defined by Friedl et al (2010).…”
Section: Methodsmentioning
confidence: 99%
“…In an effort to explore the relations between the water dynamics and ecosystem processes, several studies (Anyamba, Tucker, & Mahoney, 2002;Armanios & Fisher, 2014;Chen, De Jeu, Liu, Van der Werf, & Dolman, 2014;Davenport & Nicholson, 1993;Deshmukh, 1984;Eklundh, 1998;Nicholson, Davenport, & Malo, 1990;Richard & Poccard, 1998;Shinoda, 1995) have investigated the response of vegetation to P/SM patterns, by examining the spatiotemporal patterns and inter-relations of P/SM and the Normalized Difference Vegetation Index (NDVI) in EA and other sensitive regions of the globe. While spectral vegetation indices, such as NDVI, have been extensively used to analyze spatiotemporal variations in vegetation distribution, their use to quantify vegetation status or behavior is plagued by several shortcomings, such as its high sensitivity to atmospheric influences (cloud, aerosols), constraints due to seasonal decreases in solar illumination, its limitation in monitoring only the top of the canopy (Liu, de Jeu, McCabe, Evans, & van Dijk, 2011), its proneness to saturation in dense canopies (Liu, van Dijk, McCabe, Evans, & Jeu, 2012), and its weak and indirect link with water content (Pettorelli, 2013).…”
Section: Introductionmentioning
confidence: 99%
“…However, in most developing countries, hydrological ground measurements (Btruth^) data are scarce (Swenson and Wahr 2009), and rarely more than one method has been used to estimate recharge. In this context, remote sensing (RS) arises as a potential water-resource management tool to provide information on water-budget components (Oliveira et al 2014;Armanios and Fisher 2014).…”
Section: Introductionmentioning
confidence: 99%