Articles | Volume 19, issue 6
https://doi.org/10.5194/hess-19-2899-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-19-2899-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The water balance components of undisturbed tropical woodlands in the Brazilian cerrado
Department of Hydraulics and Sanitary Engineering, University of São Paulo, CxP. 359, São Carlos, SP, 13560-970, Brazil
USDA-ARS, Southwest Watershed Research Center, 2000 E. Allen Rd., Tucson, AZ 85719, USA
E. Wendland
Department of Hydraulics and Sanitary Engineering, University of São Paulo, CxP. 359, São Carlos, SP, 13560-970, Brazil
M. A. Nearing
USDA-ARS, Southwest Watershed Research Center, 2000 E. Allen Rd., Tucson, AZ 85719, USA
R. L. Scott
USDA-ARS, Southwest Watershed Research Center, 2000 E. Allen Rd., Tucson, AZ 85719, USA
R. Rosolem
Queens School of Engineering, University of Bristol, Bristol, UK
H. R. da Rocha
Departamento de Ciências Atmosféricas, IAG, Universidade de São Paulo, Sao Paulo, Brazil
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53 citations as recorded by crossref.
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- Understory and small trees contribute importantly to stemflow of a lower montane cloud forest T. González‐Martínez et al. 10.1002/hyp.11114
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- Soil water repellency in the Brazilian neotropical savanna: first detection, seasonal effect, and influence on infiltrability J. de Lima Oliveira et al. 10.1007/s10661-023-12097-6
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2 citations as recorded by crossref.
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Saved (final revised paper)
Latest update: 13 Dec 2024
Short summary
We determined the main components of the water balance for an undisturbed cerrado.
Evapotranspiration ranged from 1.91 to 2.60mm per day for the dry and wet seasons, respectively. Canopy interception ranged from 4 to 20% and stemflow values were approximately 1% of gross precipitation.
The average runoff coefficient was less than 1%, while cerrado deforestation has the potential to increase that amount up to 20-fold.
The water storage may be estimated by the difference between P and ET.
We determined the main components of the water balance for an undisturbed cerrado....