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Closing the terrestrial water budget from satellite remote sensing
by
Ferguson, Craig R.
, McCabe, Matthew F.
, Troy, Tara J.
, Wood, Eric F.
, Sheffield, Justin
in
Budgets
/ Earth sciences
/ Earth, ocean, space
/ Evapotranspiration
/ Exact sciences and technology
/ Hydrologic cycle
/ Hydrology
/ Mississippi
/ Remote sensing
/ River basins
/ Satellites
/ Stream discharge
/ Stream flow
/ Uncertainty
/ Water
/ Water balance
/ Water budget
/ water budgets
/ Water storage
2009
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Closing the terrestrial water budget from satellite remote sensing
by
Ferguson, Craig R.
, McCabe, Matthew F.
, Troy, Tara J.
, Wood, Eric F.
, Sheffield, Justin
in
Budgets
/ Earth sciences
/ Earth, ocean, space
/ Evapotranspiration
/ Exact sciences and technology
/ Hydrologic cycle
/ Hydrology
/ Mississippi
/ Remote sensing
/ River basins
/ Satellites
/ Stream discharge
/ Stream flow
/ Uncertainty
/ Water
/ Water balance
/ Water budget
/ water budgets
/ Water storage
2009
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Do you wish to request the book?
Closing the terrestrial water budget from satellite remote sensing
by
Ferguson, Craig R.
, McCabe, Matthew F.
, Troy, Tara J.
, Wood, Eric F.
, Sheffield, Justin
in
Budgets
/ Earth sciences
/ Earth, ocean, space
/ Evapotranspiration
/ Exact sciences and technology
/ Hydrologic cycle
/ Hydrology
/ Mississippi
/ Remote sensing
/ River basins
/ Satellites
/ Stream discharge
/ Stream flow
/ Uncertainty
/ Water
/ Water balance
/ Water budget
/ water budgets
/ Water storage
2009
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Closing the terrestrial water budget from satellite remote sensing
Journal Article
Closing the terrestrial water budget from satellite remote sensing
2009
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Overview
The increasing availability of remote sensing products for all components of the terrestrial water cycle makes it now possible to evaluate the potential of water balance closure purely from remote sensing sources. We take precipitation (P) from the TMPA and CMORPH products, a Penman‐Monteith based evapotranspiration (E) estimate derived from NASA Aqua satellite data and terrestrial water storage change (ΔS) from the GRACE satellite. Their combined ability to close the water budget is evaluated over the Mississippi River basin for 2003–5 by estimating streamflow (Q) as a residual of the water budget and comparing to streamflow measurements. We find that Q is greatly overestimated due mainly to the high bias in P, especially in the summer. Removal of systematic biases in P reduces the error significantly. However, uncertainties in the individual budget components due to simplifications in process algorithms and input data error are generally larger than the measured streamflow.
Publisher
Blackwell Publishing Ltd,American Geophysical Union,John Wiley & Sons, Inc
Subject
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