Technical note: A hydrological routing scheme for the Ecosystem Demography model (ED2+R) tested in the Tapajós River basin in the Brazilian Amazon
Land surface models are excellent tools for studying how climate change and land use affect surface hydrology. However, in order to assess the impacts of Earth processes on river flows, simulated changes in runoff need to be routed through the landscape. In this technical note, we describe the i...
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doaj-9aa81c49f39a44a19436d8acc549bafe2020-11-24T23:49:35ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-09-01214629464810.5194/hess-21-4629-2017Technical note: A hydrological routing scheme for the Ecosystem Demography model (ED2+R) tested in the Tapajós River basin in the Brazilian AmazonF. F. Pereira0F. F. Pereira1F. Farinosi2F. Farinosi3F. Farinosi4M. E. Arias5M. E. Arias6E. Lee7E. Lee8E. Lee9J. Briscoe10J. Briscoe11P. R. Moorcroft12Sustainability Science Program, Kennedy School of Government, Harvard University, Cambridge, MA 02138, USAnow at: Department of Renewable Energy Engineering, Federal University of Alagoas, Maceió, AL, BrazilSustainability Science Program, Kennedy School of Government, Harvard University, Cambridge, MA 02138, USACa' Foscari University of Venice, Venice, Italynow at: European Commission, DG Joint Research Centre, Ispra, ItalySustainability Science Program, Kennedy School of Government, Harvard University, Cambridge, MA 02138, USADepartment of Civil and Environmental Engineering, University of South Florida, Tampa, FL 33620, USASustainability Science Program, Kennedy School of Government, Harvard University, Cambridge, MA 02138, USAnow at: Goddard Earth Sciences Technology and Research, Universities Space Research Association, Columbia, MD 21046, USAcurrent address: Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, MD 22071, USASustainability Science Program, Kennedy School of Government, Harvard University, Cambridge, MA 02138, USAdeceased, 12 November 2014Sustainability Science Program, Kennedy School of Government, Harvard University, Cambridge, MA 02138, USALand surface models are excellent tools for studying how climate change and land use affect surface hydrology. However, in order to assess the impacts of Earth processes on river flows, simulated changes in runoff need to be routed through the landscape. In this technical note, we describe the integration of the Ecosystem Demography (ED2) model with a hydrological routing scheme. The purpose of the study was to create a tool capable of incorporating to hydrological predictions the terrestrial ecosystem responses to climate, carbon dioxide, and land-use change, as simulated with terrestrial biosphere models. The resulting ED2+R model calculates the lateral routing of surface and subsurface runoff resulting from the terrestrial biosphere models' vertical water balance in order to determine spatiotemporal patterns of river flows within the simulated region. We evaluated the ED2+R model in the Tapajós, a 476 674 km<sup>2</sup> river basin in the southeastern Amazon, Brazil. The results showed that the integration of ED2 with the lateral routing scheme results in an adequate representation (Nash–Sutcliffe efficiency up to 0.76, Kling–Gupta efficiency up to 0.86, Pearson's <i>R</i> up to 0.88, and volume ratio up to 1.06) of daily to decadal river flow dynamics in the Tapajós. These results are a consistent step forward with respect to the <q>no river representation</q> common among terrestrial biosphere models, such as the initial version of ED2.https://www.hydrol-earth-syst-sci.net/21/4629/2017/hess-21-4629-2017.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
F. F. Pereira F. F. Pereira F. Farinosi F. Farinosi F. Farinosi M. E. Arias M. E. Arias E. Lee E. Lee E. Lee J. Briscoe J. Briscoe P. R. Moorcroft |
spellingShingle |
F. F. Pereira F. F. Pereira F. Farinosi F. Farinosi F. Farinosi M. E. Arias M. E. Arias E. Lee E. Lee E. Lee J. Briscoe J. Briscoe P. R. Moorcroft Technical note: A hydrological routing scheme for the Ecosystem Demography model (ED2+R) tested in the Tapajós River basin in the Brazilian Amazon Hydrology and Earth System Sciences |
author_facet |
F. F. Pereira F. F. Pereira F. Farinosi F. Farinosi F. Farinosi M. E. Arias M. E. Arias E. Lee E. Lee E. Lee J. Briscoe J. Briscoe P. R. Moorcroft |
author_sort |
F. F. Pereira |
title |
Technical note: A hydrological routing scheme for the Ecosystem Demography model (ED2+R) tested in the Tapajós River basin in the Brazilian Amazon |
title_short |
Technical note: A hydrological routing scheme for the Ecosystem Demography model (ED2+R) tested in the Tapajós River basin in the Brazilian Amazon |
title_full |
Technical note: A hydrological routing scheme for the Ecosystem Demography model (ED2+R) tested in the Tapajós River basin in the Brazilian Amazon |
title_fullStr |
Technical note: A hydrological routing scheme for the Ecosystem Demography model (ED2+R) tested in the Tapajós River basin in the Brazilian Amazon |
title_full_unstemmed |
Technical note: A hydrological routing scheme for the Ecosystem Demography model (ED2+R) tested in the Tapajós River basin in the Brazilian Amazon |
title_sort |
technical note: a hydrological routing scheme for the ecosystem demography model (ed2+r) tested in the tapajós river basin in the brazilian amazon |
publisher |
Copernicus Publications |
series |
Hydrology and Earth System Sciences |
issn |
1027-5606 1607-7938 |
publishDate |
2017-09-01 |
description |
Land surface models are excellent tools for studying how
climate change and land use affect surface hydrology. However, in order to
assess the impacts of Earth processes on river flows, simulated changes in
runoff need to be routed through the landscape. In this technical note, we
describe the integration of the Ecosystem Demography (ED2) model with a
hydrological routing scheme. The purpose of the study was to create a tool
capable of incorporating to hydrological predictions the terrestrial
ecosystem responses to climate, carbon dioxide, and land-use change, as
simulated with terrestrial biosphere models. The resulting ED2+R model
calculates the lateral routing of surface and subsurface runoff resulting
from the terrestrial biosphere models' vertical water balance in order to
determine spatiotemporal patterns of river flows within the simulated
region. We evaluated the ED2+R model in the Tapajós, a 476 674 km<sup>2</sup>
river basin in the southeastern Amazon, Brazil. The results showed that the
integration of ED2 with the lateral routing scheme results in an adequate
representation (Nash–Sutcliffe efficiency up to 0.76, Kling–Gupta efficiency
up to 0.86, Pearson's <i>R</i> up to 0.88, and volume ratio up to 1.06) of daily to
decadal river flow dynamics in the Tapajós. These results are a
consistent step forward with respect to the <q>no river representation</q> common
among terrestrial biosphere models, such as the initial version of ED2. |
url |
https://www.hydrol-earth-syst-sci.net/21/4629/2017/hess-21-4629-2017.pdf |
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