2014
DOI: 10.1073/pnas.1317606111
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Toward global mapping of river discharge using satellite images and at-many-stations hydraulic geometry

Abstract: Rivers provide critical water supply for many human societies and ecosystems, yet global knowledge of their flow rates is poor. We show that useful estimates of absolute river discharge (in cubic meters per second) may be derived solely from satellite images, with no ground-based or a priori information whatsoever. The approach works owing to discovery of a characteristic scaling law uniquely fundamental to natural rivers, here termed a river's at-many-stations hydraulic geometry. A first demonstration using L… Show more

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Cited by 285 publications
(314 citation statements)
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References 39 publications
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“…The key areas are (1) improve simulations of the storage and transmission of water in the soil matrix, obtained through (a) implementing the mixed form of Richards' equation [Celia et al, 1990;Maxwell and Miller, 2005] and (b) explicitly representing macropore flow [Beven and Germann, 1982;Weiler, 2005;Nimmo, 2010;Yu et al, 2014]; (2) improve representation of hydraulic gradients throughout the soil-plantatmosphere continuum to improve simulations of root water uptake and evapotranspiration [Baldocchi and Meyers, 1998;Mackay et al, 2003;Bonan et al, 2014]; (3) improve representation of groundwater dynamics across a hierarchy of spatial scales, including improving ''among grid'' and ''within grid'' groundwater representations [Famiglietti and Wood, 1994;Troch et al, 2003;Miguez-Macho et al, 2007]; and (4) improve simulations of streamflow, by explicitly representing stream-aquifer interactions and improving parameterizations of channel/floodplain routing [Qu and Duffy, 2007;Shen and Phanikumar, 2010;MiguezMacho and Fan, 2012a;Pappenberger et al, 2012]. Underpinning all of these areas is the need to improve data sets on geophysical attributes, especially data on bedrock depth and permeability [Tesfa et al, 2009;Fan et al, 2015] and data sets on the physical characteristics of rivers [Getirana et al, 2013;Mersel et al, 2013;Gleason and Smith, 2014].…”
Section: Opportunities To Improve the Representation Of Hydrologic Prmentioning
confidence: 99%
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“…The key areas are (1) improve simulations of the storage and transmission of water in the soil matrix, obtained through (a) implementing the mixed form of Richards' equation [Celia et al, 1990;Maxwell and Miller, 2005] and (b) explicitly representing macropore flow [Beven and Germann, 1982;Weiler, 2005;Nimmo, 2010;Yu et al, 2014]; (2) improve representation of hydraulic gradients throughout the soil-plantatmosphere continuum to improve simulations of root water uptake and evapotranspiration [Baldocchi and Meyers, 1998;Mackay et al, 2003;Bonan et al, 2014]; (3) improve representation of groundwater dynamics across a hierarchy of spatial scales, including improving ''among grid'' and ''within grid'' groundwater representations [Famiglietti and Wood, 1994;Troch et al, 2003;Miguez-Macho et al, 2007]; and (4) improve simulations of streamflow, by explicitly representing stream-aquifer interactions and improving parameterizations of channel/floodplain routing [Qu and Duffy, 2007;Shen and Phanikumar, 2010;MiguezMacho and Fan, 2012a;Pappenberger et al, 2012]. Underpinning all of these areas is the need to improve data sets on geophysical attributes, especially data on bedrock depth and permeability [Tesfa et al, 2009;Fan et al, 2015] and data sets on the physical characteristics of rivers [Getirana et al, 2013;Mersel et al, 2013;Gleason and Smith, 2014].…”
Section: Opportunities To Improve the Representation Of Hydrologic Prmentioning
confidence: 99%
“…Globally-available, 1/88 resolution river flow direction, accumulation and slope hydrography datasets, e.g., HydroSHEDS [Lehner et al, 2008] and DRT [Wu et al, 2012], have emerged. Remote-sensing data sets and the application of scaling laws provides global estimates of recharge [Gleason and Smith, 2014] and water depths [Mersel et al, 2013]. The next generation remote-sensing products (e.g., the Surface Water and Ocean Topography, SWOT, expected to launch in 2020) will further expand our ability to characterize stream geometries and discharges [e.g., Getirana et al, 2013;Pavelsky et al, 2014;Pedinotti et al, 2014;Allen and Pavelsky, 2015].…”
Section: 1002/2015wr017096mentioning
confidence: 99%
“…WSS and inundated area) and even stream flow in the future, i.e. by SWOT (Bates et al, 2014;Gleason and Smith, 2014;Paiva et al, 2015), can be applied to determine the weights w i using Eq. (3).…”
Section: Discrete Form Of the Water Balance Modelmentioning
confidence: 99%
“…Leopold and Maddock (1953) present two interpretations of HG including at-a-station hydraulic geometry (AHG) which describes how channel form adjusts to changes in the instantaneous discharge at a channel cross-section, and downstream hydraulic geometry (DHG) which describes how channel form varies in the along-stream direction with discharge of a common frequency such as the mean annual discharge. Gleason (2015) provides a review of HG studies and notes that several "Non-Leopoldian" HG relationships have also been developed including At-Many-Station HG (AMHG) introduced by Gleason and Smith (2014) which characterizes the longitudinal variability in AHG exponents and coefficients, and reach-average hydraulic geometry (RHG) first introduced by Jowett (1998) which uses reach-averaged flow attributes instead of cross-sectional data. For this study, Platte hydraulic model outputs are utilized to study the relationship between BR channel form with a changing hydrograph of the September 2013 highflow event.…”
Section: Hydraulic Geometry Analysismentioning
confidence: 99%