Articles | Volume 23, issue 3
https://doi.org/10.5194/hess-23-1263-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-23-1263-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
07 Mar 2019
Research article |
| 07 Mar 2019
| 07 Mar 2019
Hydrological trade-offs due to different land covers and land uses in the Brazilian Cerrado
Department of Hydraulics and Sanitation, São Carlos School of
Engineering (EESC), University of São Paulo (USP), CxP. 359, São
Carlos, SP, 13566-590, Brazil
Edson Wendland
Department of Hydraulics and Sanitation, São Carlos School of
Engineering (EESC), University of São Paulo (USP), CxP. 359, São
Carlos, SP, 13566-590, Brazil
Lívia M. P. Rosalem
Department of Hydraulics and Sanitation, São Carlos School of
Engineering (EESC), University of São Paulo (USP), CxP. 359, São
Carlos, SP, 13566-590, Brazil
Cristian Youlton
Department of Hydraulics and Sanitation, São Carlos School of
Engineering (EESC), University of São Paulo (USP), CxP. 359, São
Carlos, SP, 13566-590, Brazil
Paulo T. S. Oliveira
Federal University of Mato Grosso do Sul, CxP. 549, Campo Grande, MS,
79070-900, Brazil
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We monitored the interception process on an undisturbed savanna forest and applied two interception models to evaluate their performance at different time scales and study their seasonal response. As results, both models performed well at a monthly scale and could represent the seasonal trends observed. However, they presented some limitations to predict the evaporative processes on a daily basis.
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Fabian Maier, Florian Lustenberger, and Ilja van Meerveld
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Anne Hartmann, Markus Weiler, Konrad Greinwald, and Theresa Blume
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Rico Hübner, Thomas Günther, Katja Heller, Ursula Noell, and Arno Kleber
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Lisa Angermann, Conrad Jackisch, Niklas Allroggen, Matthias Sprenger, Erwin Zehe, Jens Tronicke, Markus Weiler, and Theresa Blume
Hydrol. Earth Syst. Sci., 21, 3727–3748, https://doi.org/10.5194/hess-21-3727-2017, https://doi.org/10.5194/hess-21-3727-2017, 2017
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Conrad Jackisch, Lisa Angermann, Niklas Allroggen, Matthias Sprenger, Theresa Blume, Jens Tronicke, and Erwin Zehe
Hydrol. Earth Syst. Sci., 21, 3749–3775, https://doi.org/10.5194/hess-21-3749-2017, https://doi.org/10.5194/hess-21-3749-2017, 2017
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Rapid subsurface flow in structured soils facilitates fast vertical and lateral redistribution of event water. We present its in situ exploration through local measurements and irrigation experiments. Special emphasis is given to a coherent combination of hydrological and geophysical methods. The study highlights that form and function operate as conjugated pairs. Dynamic imaging through time-lapse GPR was key to observing both and to identifying hydrologically relevant structures.
Lukáš Vlček, Kristýna Falátková, and Philipp Schneider
Hydrol. Earth Syst. Sci., 21, 3025–3040, https://doi.org/10.5194/hess-21-3025-2017, https://doi.org/10.5194/hess-21-3025-2017, 2017
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The role of mountain headwater area in hydrological cycle was investigated at two opposite hillslopes covered by mineral and organic soils. Similarities and differences in percolation and preferential flow paths between the hillslopes were identified by sprinkling experiments with Brilliant Blue and Fluorescein. The dye solutions infiltrated into the soil and continued either as lateral subsurface pipe flow (organic soil), or percolated vertically towards the bedrock (mineral soil).
Shabnam Saffarpour, Andrew W. Western, Russell Adams, and Jeffrey J. McDonnell
Hydrol. Earth Syst. Sci., 20, 4525–4545, https://doi.org/10.5194/hess-20-4525-2016, https://doi.org/10.5194/hess-20-4525-2016, 2016
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A variety of threshold mechanisms influence the transfer of rainfall to runoff from catchments. Some of these mechanisms depend on the occurrence of intense rainfall and others depend on the catchment being wet. This article first provides a framework for considering which mechanisms are important in different situations and then uses that framework to examine the behaviour of a catchment in Australia that exhibits a mix of both rainfall intensity and catchment wetness dependent thresholds.
Lyssette E. Muñoz-Villers, Daniel R. Geissert, Friso Holwerda, and Jeffrey J. McDonnell
Hydrol. Earth Syst. Sci., 20, 1621–1635, https://doi.org/10.5194/hess-20-1621-2016, https://doi.org/10.5194/hess-20-1621-2016, 2016
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This study provides an important first step towards a better understanding of the hydrology of tropical montane regions and the factors influencing baseflow mean transit times (MTT). Our MTT estimates ranged between 1.2 and 2.7 years, suggesting deep and long subsurface pathways contributing to sustain dry season flows. Our findings showed that topography and subsurface permeability are the key factors controlling baseflow MTTs. Longest MTTs were found in the cloud forest headwater catchments.
Haimanote K. Bayabil, Tigist Y. Tebebu, Cathelijne R. Stoof, and Tammo S. Steenhuis
Hydrol. Earth Syst. Sci., 20, 875–885, https://doi.org/10.5194/hess-20-875-2016, https://doi.org/10.5194/hess-20-875-2016, 2016
P. T. S. Oliveira, E. Wendland, M. A. Nearing, R. L. Scott, R. Rosolem, and H. R. da Rocha
Hydrol. Earth Syst. Sci., 19, 2899–2910, https://doi.org/10.5194/hess-19-2899-2015, https://doi.org/10.5194/hess-19-2899-2015, 2015
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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.
J. Bechet, J. Duc, M. Jaboyedoff, A. Loye, and N. Mathys
Hydrol. Earth Syst. Sci., 19, 1849–1855, https://doi.org/10.5194/hess-19-1849-2015, https://doi.org/10.5194/hess-19-1849-2015, 2015
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High-resolution three-dimensional point clouds are used to analyse erosion processes at the millimetre scale. The processes analysed here play a role in the closure of cracks. We demonstrated how micro-scale infiltration can influence the degradation of soil surface by inducing downward mass movements that are not reversible. This development will aid in designing future experiments to analyse processes such as swelling, crack closure, micro-landslides, etc.
R. Hübner, K. Heller, T. Günther, and A. Kleber
Hydrol. Earth Syst. Sci., 19, 225–240, https://doi.org/10.5194/hess-19-225-2015, https://doi.org/10.5194/hess-19-225-2015, 2015
T. G. Wilson, C. Cortis, N. Montaldo, and J. D. Albertson
Hydrol. Earth Syst. Sci., 18, 4169–4183, https://doi.org/10.5194/hess-18-4169-2014, https://doi.org/10.5194/hess-18-4169-2014, 2014
P. Schneider, S. Pool, L. Strouhal, and J. Seibert
Hydrol. Earth Syst. Sci., 18, 875–892, https://doi.org/10.5194/hess-18-875-2014, https://doi.org/10.5194/hess-18-875-2014, 2014
S. Popp, D. Altdorff, and P. Dietrich
Hydrol. Earth Syst. Sci., 17, 1297–1307, https://doi.org/10.5194/hess-17-1297-2013, https://doi.org/10.5194/hess-17-1297-2013, 2013
J. Klaus, E. Zehe, M. Elsner, C. Külls, and J. J. McDonnell
Hydrol. Earth Syst. Sci., 17, 103–118, https://doi.org/10.5194/hess-17-103-2013, https://doi.org/10.5194/hess-17-103-2013, 2013
S. Bachmair and M. Weiler
Hydrol. Earth Syst. Sci., 16, 3699–3715, https://doi.org/10.5194/hess-16-3699-2012, https://doi.org/10.5194/hess-16-3699-2012, 2012
F. Tauro, S. Grimaldi, A. Petroselli, M. C. Rulli, and M. Porfiri
Hydrol. Earth Syst. Sci., 16, 2973–2983, https://doi.org/10.5194/hess-16-2973-2012, https://doi.org/10.5194/hess-16-2973-2012, 2012
B. A. Ebel, E. S. Hinckley, and D. A. Martin
Hydrol. Earth Syst. Sci., 16, 1401–1417, https://doi.org/10.5194/hess-16-1401-2012, https://doi.org/10.5194/hess-16-1401-2012, 2012
G. Romanescu, V. Cotiuga, A. Asandulesei, and C. Stoleriu
Hydrol. Earth Syst. Sci., 16, 953–966, https://doi.org/10.5194/hess-16-953-2012, https://doi.org/10.5194/hess-16-953-2012, 2012
J. Garvelmann, C. Külls, and M. Weiler
Hydrol. Earth Syst. Sci., 16, 631–640, https://doi.org/10.5194/hess-16-631-2012, https://doi.org/10.5194/hess-16-631-2012, 2012
B. Zhang, J. L. Tang, Ch. Gao, and H. Zepp
Hydrol. Earth Syst. Sci., 15, 3153–3170, https://doi.org/10.5194/hess-15-3153-2011, https://doi.org/10.5194/hess-15-3153-2011, 2011
M. B. Defersha, S. Quraishi, and A. Melesse
Hydrol. Earth Syst. Sci., 15, 2367–2375, https://doi.org/10.5194/hess-15-2367-2011, https://doi.org/10.5194/hess-15-2367-2011, 2011
T. Y. Tebebu, A. Z. Abiy, A. D. Zegeye, H. E. Dahlke, Z. M. Easton, S. A. Tilahun, A. S. Collick, S. Kidnau, S. Moges, F. Dadgari, and T. S. Steenhuis
Hydrol. Earth Syst. Sci., 14, 2207–2217, https://doi.org/10.5194/hess-14-2207-2010, https://doi.org/10.5194/hess-14-2207-2010, 2010
B. Creutzfeldt, A. Güntner, S. Vorogushyn, and B. Merz
Hydrol. Earth Syst. Sci., 14, 1715–1730, https://doi.org/10.5194/hess-14-1715-2010, https://doi.org/10.5194/hess-14-1715-2010, 2010
X. J. Guan, C. J. Westbrook, and C. Spence
Hydrol. Earth Syst. Sci., 14, 1375–1386, https://doi.org/10.5194/hess-14-1375-2010, https://doi.org/10.5194/hess-14-1375-2010, 2010
X. J. Guan, C. Spence, and C. J. Westbrook
Hydrol. Earth Syst. Sci., 14, 1387–1400, https://doi.org/10.5194/hess-14-1387-2010, https://doi.org/10.5194/hess-14-1387-2010, 2010
E. Zehe, T. Graeff, M. Morgner, A. Bauer, and A. Bronstert
Hydrol. Earth Syst. Sci., 14, 873–889, https://doi.org/10.5194/hess-14-873-2010, https://doi.org/10.5194/hess-14-873-2010, 2010
Cited articles
Adane, Z. A., Nasta, P., Zlotnik, V., and Wedin, D.: Impact of grassland
conversion to forest on groundwater recharge in the Nebraska Sand Hills, J. Hydrol., 15,
171–183, https://doi.org/10.1016/j.ejrh.2018.01.001, 2018.
Alberton, B., Almeida, J., Helm, R., da S. Torres, R., Menzel, A., and
Morellato, L. P. C.: Using phenological cameras to track the green up in a
cerrado savanna and its on-the-ground validation, Ecol. Inform., 19, 62–70,
https://doi.org/10.1016/j.ecoinf.2013.12.011, 2014.
Alkimim, A., Sparovek, G., and Clarke, K. C.: Converting Brazil's pastures
to cropland: An alternative way to meet sugarcane demand and to spare
forestlands, Appl. Geogr., 62, 75–84, https://doi.org/10.1016/j.apgeog.2015.04.008, 2015.
Allen, R. G., Pereira, L. S., Raes, D., and Smith, M.: Crop
evapotranspiration – Guidelines for computing crop water requirements – FAO
Irrigation and drainage paper 56, FAO – Food and Agriculture Organization of
the United Nations, Rome, 326 pp., 1998.
Alvares, C. A., Stape, J. L., Sentelhas, P. C., Gonçalves, J. L. M., and
Sparovek, G.: Koppen's climate classification map for Brazil, Meteorol. Z., 22,
https://doi.org/10.1127/0941-2948/2013/0507, 711–728, 2014.
Anache, J. A. A., Wendland, E. C., Oliveira, P. T. S., Flanagan, D. C., and
Nearing, M. A.: Runoff and soil erosion plot-scale studies under natural
rainfall: A meta-analysis of the Brazilian experience, Catena, 152, 29–39,
https://doi.org/10.1016/j.catena.2017.01.003, 2017.
Anache, J. A. A., Flanagan, D. C., Srivastava, A., and Wendland, E. C.: Land
use and climate change impacts on runoff and soil erosion at the hillslope
scale in the Brazilian Cerrado, Sci. Total
Environ., 622, 140–151,
https://doi.org/10.1016/j.scitotenv.2017.11.257, 2018.
Anache, J. A. A.: Supplement for: Hydrological trade-offs due to different
land covers and land uses in the Brazilian Cerrado, HydroShare,
https://doi.org/10.4211/hs.a1c032dbb78d48748b673c876c20b21c, (last access:
7 December 2018), 2019.
Archer, D. R. and Fowler, H. J.: Characterising flash flood response to
intense rainfall and impacts using historical information and gauged data in
Britain, J. Flood Risk Manag., 11, 121–133, https://doi.org/10.1111/jfr3.12187, 2018.
Barretto, A. G., Berndes, G., Sparovek, G., and Wirsenius, S.: Agricultural
intensification in Brazil and its effects on land-use patterns: an analysis
of the 1975–2006 period, Global Change Biol., 19, 1804–1815, https://doi.org/10.1111/gcb.12174,
2013.
Bellezoni, R. A., Sharma, D., Villela, A. A., and Pereira Junior, A. O.:
Water-energy-food nexus of sugarcane ethanol production in the state of
Goiás, Brazil: An analysis with regional input-output matrix, Biomass Bioenerg., 115, 108–119, https://doi.org/10.1016/j.biombioe.2018.04.017, 2018.
Beuchle, R., Grecchi, R. C., Shimabukuro, Y. E., Seliger, R., Eva, H. D.,
Sano, E., and Achard, F.: Land cover changes in the Brazilian Cerrado and
Caatinga biomes from 1990 to 2010 based on a systematic remote sensing
sampling approach, Appl. Geogr., 58, 116–127, https://doi.org/10.1016/j.apgeog.2015.01.017,
2015.
Beven, K.: On undermining the science?, Hydrol. Process., 20, 3141–3146,
https://doi.org/10.1002/hyp.6396, 2006.
Bonan, G. B.: Forests and climate change: forcings, feedbacks, and the
climate benefits of forests, Science, 320, 1444–1449,
https://doi.org/10.1126/science.1155121, 2008.
Bouwer, H. and Rice, R. C.: A slug test for determining hydraulic
conductivity of unconfined aquifers with completely or partially penetrating
wells, Water Resour. Res., 12, 423–428, https://doi.org/10.1029/WR012i003p00423, 1976.
Brannstrom, C., Jepson, W., Filippi, A. M., Redo, D., Xu, Z., and Ganesh,
S.: Land change in the Brazilian Savanna (Cerrado), 1986–2002: Comparative
analysis and implications for land-use policy, Land Use Policy, 25, 579–595,
https://doi.org/10.1016/j.landusepol.2007.11.008, 2008.
Burt, T. P. and McDonnell, J. J.: Whither field hydrology?, The need for
discovery science and outrageous hydrological hypotheses, Water Resour. Res.,
51, 5919–5928, https://doi.org/10.1002/2014WR016839, 2015.
Cabral, O. M. R., Rocha, H. R., Gash, J. H., Ligo, M. A. V., Tatsch, J. D.,
Freitas, H. C., and Brasilio, E.: Water use in a sugarcane plantation, GCB
Bioenergy, 4, 555–565, https://doi.org/10.1111/j.1757-1707.2011.01155.x, 2012.
Cabral, O. M. R., da Rocha, H. R., Gash, J. H., Freitas, H. C., and Ligo, M.
A. V.: Water and energy fluxes from a woodland savanna (cerrado) in
southeast Brazil, J. Hydrol., 4, 22–40,
https://doi.org/10.1016/j.ejrh.2015.04.010, 2015.
Cabrera, M. C. M., Anache, J. A. A., Youlton, C., and Wendland, E.:
Performance of evaporation estimation methods compared with standard 20
m−2 tank, Rev. Bras. Eng. Agr. Amb., 20, 874–879,
https://doi.org/10.1590/1807-1929/agriambi.v20n10p874-879, 2016.
Canadell, J., Jackson, R. B., Ehleringer, J. B., Mooney, H. A., Sala, O. E.,
and Schulze, E.-D.: Maximum rooting depth of vegetation types at the global
scale, Oecologia, 108, 583–595, https://doi.org/10.1007/bf00329030, 1996.
Christoffersen, B. O., Restrepo-Coupe, N., Arain, M. A., Baker, I. T.,
Cestaro, B. P., Ciais, P., Fisher, J. B., Galbraith, D., Guan, X., Gulden,
L., van den Hurk, B., Ichii, K., Imbuzeiro, H., Jain, A., Levine, N.,
Miguez-Macho, G., Poulter, B., Roberti, D. R., Sakaguchi, K., Sahoo, A.,
Schaefer, K., Shi, M., Verbeeck, H., Yang, Z.-L., Araújo, A. C., Kruijt,
B., Manzi, A. O., da Rocha, H. R., von Randow, C., Muza, M. N., Borak, J.,
Costa, M. H., Gonçalves de Gonçalves, L. G., Zeng, X., and Saleska,
S. R.: Mechanisms of water supply and vegetation demand govern the
seasonality and magnitude of evapotranspiration in Amazonia and Cerrado, Agr.
Forest Meteorol., 191, 33–50, https://doi.org/10.1016/j.agrformet.2014.02.008, 2014.
da Paz, A. R., Collischonn, W., Bravo, J. M., Bates, P. D., and Baugh, C.:
The influence of vertical water balance on modelling Pantanal (Brazil)
spatio-temporal inundation dynamics, Hydrol. Process., 28, 3539–3553,
https://doi.org/10.1002/hyp.9897, 2014.
da Rocha, H. R., Manzi, A. O., Cabral, O. M., Miller, S. D., Goulden, M. L.,
Saleska, S. R., R.-Coupe, N., Wofsy, S. C., Borma, L. S., Artaxo, P.,
Vourlitis, G., Nogueira, J. S., Cardoso, F. L., Nobre, A. D., Kruijt, B.,
Freitas, H. C., von Randow, C., Aguiar, R. G., and Maia, J. F.: Patterns of
water and heat flux across a biome gradient from tropical forest to savanna
in Brazil, J. Geophys. Res., 114, G00B12, https://doi.org/10.1029/2007jg000640, 2009.
Dawes, W., Ali, R., Varma, S., Emelyanova, I., Hodgson, G., and McFarlane, D.:
Modelling the effects of climate and land cover change on groundwater recharge in
south-west Western Australia, Hydrol. Earth Syst. Sci., 16, 2709–2722, https://doi.org/10.5194/hess-16-2709-2012, 2012.
de Almeida, W. S., Panachuki, E., de Oliveira, P. T. S., da Silva Menezes,
R., Sobrinho, T. A., and de Carvalho, D. F.: Effect of soil tillage and
vegetal cover on soil water infiltration, Soil Till. Res., 175, 130–138,
https://doi.org/10.1016/j.still.2017.07.009, 2018.
Dedecek, R. A.: Coberturas permanentes do solo na erosão sob
condições de cerrados, Pesqui. Agropecu. Bras., 24, 483–488, 1989.
Dias, L. C. P., Macedo, M. N., Costa, M. H., Coe, M. T., and Neill, C.:
Effects of land cover change on evapotranspiration and streamflow of small
catchments in the Upper Xingu River Basin, Central Brazil, J. Hydrol., 4, 108–122, https://doi.org/10.1016/j.ejrh.2015.05.010, 2015.
Domínguez, C. G., Pryet, A., García Vera, M., Gonzalez, A.,
Chaumont, C., Tournebize, J., Villacis, M., d'Ozouville, N., and Violette,
S.: Comparison of deep percolation rates below contrasting land covers with
a joint canopy and soil model, J. Hydrol., 532, 65–79,
https://doi.org/10.1016/j.jhydrol.2015.11.022, 2016.
Doorenbos, J., Pruitt, W. O., Aboukhaled, A., Food, and Nations, A. O. o. t.
U.: Guidelines for Predicting Crop Water Requirements, Food and Agriculture
Organization of the United Nations, 1975.
Doorenbos, J., Kassam, A. H., and Bentvelsen, C. I. M.: Yield response to
water, Food and Agriculture Organization of the United Nations, 1979.
Dotterweich, M.: The history of human-induced soil erosion: Geomorphic
legacies, early descriptions and research, and the development of soil
conservation – A global synopsis, Geomorphology, 201, 1–34,
https://doi.org/10.1016/j.geomorph.2013.07.021, 2013.
Finch, J. W.: Estimating direct groundwater recharge using a simple water
balance model – sensitivity to land surface parameters, J. Hydrol., 211,
112–125, https://doi.org/10.1016/S0022-1694(98)00225-X, 1998.
Frank, S., Fürst, C., Witt, A., Koschke, L., and Makeschin, F.: Making
use of the ecosystem services concept in regional planning – trade-offs from
reducing water erosion, Landscape Ecol., 29, 1377–1391,
https://doi.org/10.1007/s10980-014-9992-3, 2014.
Garcia-Montiel, D. C., Coe, M. T., Cruz, M. P., Ferreira, J. N., da Silva,
E. M., and Davidson, E. A.: Estimating seasonal changes in volumetric soil
water content at landscape scales in a savanna ecosystem using
two-dimensional resistivity profiling, Earth Interact., 12, 1–25,
https://doi.org/10.1175/2007ei238.1, 2008.
Getirana, A. C. V.: Extreme water deficit in Brazil detected from space, J.
Hydrometeorol., 17, 591–599, https://doi.org/10.1175/JHM-D-15-0096.1, 2015.
Ghimire, C. P., Bruijnzeel, L. A., Lubczynski, M. W., and Bonell, M.:
Negative trade-off between changes in vegetation water use and infiltration
recovery after reforesting degraded pasture land in the Nepalese Lesser Himalaya,
Hydrol. Earth Syst. Sci., 18, 4933–4949, https://doi.org/10.5194/hess-18-4933-2014, 2014.
Giambelluca, T. W., Scholz, F. G., Bucci, S. J., Meinzer, F. C., Goldstein,
G., Hoffmann, W. A., Franco, A. C., and Buchert, M. P.: Evapotranspiration
and energy balance of Brazilian savannas with contrasting tree density, Agr.
Forest Meteorol., 149, 1365–1376, https://doi.org/10.1016/j.agrformet.2009.03.006, 2009.
Gibbs, H. K., Ruesch, A. S., Achard, F., Clayton, M. K., Holmgren, P.,
Ramankutty, N., and Foley, J. A.: Tropical forests were the primary sources
of new agricultural land in the 1980s and 1990s, P. Natl. Acad. Sci. USA, 107,
16732–16737, https://doi.org/10.1073/pnas.0910275107, 2010.
Gómez, D., Melo, D. C. D., Rodrigues, D. B. B., Xavier, A. C., Guido, R.
C., and Wendland, E.: Aquifer Responses to Rainfall through Spectral and
Correlation Analysis, J. Am. Water Resour. As., 54, 1341–1354, https://doi.org/10.1111/1752-1688.12696, 2018.
Gómez, J. A., Nearing, M. A., Giráldez, J. V., and Alberts, E. E.:
Analysis of sources of variability of runoff volume in a 40 plot experiment
using a numerical model, J. Hydrol., 248, 183–197,
https://doi.org/10.1016/S0022-1694(01)00402-4, 2001.
Gomyo, M. and Kuraji, K.: Effect of the litter layer on runoff and
evapotranspiration using the paired watershed method, J. Forest Res.-Jpn., 21,
306–313, https://doi.org/10.1007/s10310-016-0542-5, 2016.
Gouvêa, T. H. and Wendland, E. C.: Influência de
características do solo na variação do nível d água em
região de recarga do Aquífero Guarani, Rev. Bras. Rec. Hid., 16, 55–65,
2011.
Graham, C. B., van Verseveld, W., Barnard, H. R., and McDonnell, J. J.:
Estimating the deep seepage component of the hillslope and catchment water
balance within a measurement uncertainty framework, Hydrol. Process., 24,
3631–3647, https://doi.org/10.1002/hyp.7788, 2010.
Grecchi, R. C., Gwyn, Q. H. J., Bénié, G. B., Formaggio, A. R., and
Fahl, F. C.: Land use and land cover changes in the Brazilian Cerrado: A
multidisciplinary approach to assess the impacts of agricultural expansion,
Appl. Geogr., 55, 300–312, https://doi.org/10.1016/j.apgeog.2014.09.014, 2014.
Guarenghi, M. M. and Walter, A.: Assessing potential impacts of sugarcane
production on water resources: A case study in Brazil, Biofuel. Bioprod. Bior., 10, 699–709, https://doi.org/10.1002/bbb.1680, 2016.
Han, D., Currell, M. J., Cao, G., and Hall, B.: Alterations to groundwater
recharge due to anthropogenic landscape change, J. Hydrol., 554, 545–557,
https://doi.org/10.1016/j.jhydrol.2017.09.018, 2017.
Hernandes, T. A. D., Scarpare, F. V., and Seabra, J. E. A.: Assessment of
the recent land use change dynamics related to sugarcane expansion and the
associated effects on water resources availability, J. Clean Prod., 197,
1328–1341, https://doi.org/10.1016/j.jclepro.2018.06.297, 2018a.
Hernandes, T. A. D., Scarpare, F. V., and Seabra, J. E. A.: Assessment of
impacts on basin stream flow derived from medium-term sugarcane expansion
scenarios in Brazil, Agr. Ecosyst. Environ., 259, 11–18,
https://doi.org/10.1016/j.agee.2018.02.026, 2018b.
Kakatkar, R., Gnanaseelan, C., Deepa, J. S., Chowdary, J., and Parekh, A.:
Role of ocean-atmosphere interactions in modulating the 2016 La Niña
like pattern over the tropical Pacific, Dynam. Atmos. Oceans, 83, 100–110,
https://doi.org/10.1016/j.dynatmoce.2018.07.003, 2018.
Klink, C. A. and Machado, R. B.: Conservation of the Brazilian Cerrado,
Conserv Biol, 19, 707–713, https://doi.org/10.1111/j.1523-1739.2005.00702.x, 2005.
Krishnaswamy, J., Bonell, M., Venkatesh, B., Purandara, B. K., Rakesh, K.
N., Lele, S., Kiran, M. C., Reddy, V., and Badiger, S.: The groundwater
recharge response and hydrologic services of tropical humid forest
ecosystems to use and reforestation: Support for the
“infiltration-evapotranspiration trade-off hypothesis”, J. Hydrol., 498,
191–209, https://doi.org/10.1016/j.jhydrol.2013.06.034, 2013.
Lamparter, G., Nobrega, R. L. B., Kovacs, K., Amorim, R. S., and Gerold, G.:
Modelling hydrological impacts of agricultural expansion in two
macro-catchments in Southern Amazonia, Brazil, Reg. Environ. Change, 18,
91–103, https://doi.org/10.1007/s10113-016-1015-2, 2016.
Lapola, D. M., Martinelli, L. A., Peres, C. A., Ometto, J. P. H. B.,
Ferreira, M. E., Nobre, C. A., Aguiar, A. P. D., Bustamante, M. M. C.,
Cardoso, M. F., Costa, M. H., Joly, C. A., Leite, C. C., Moutinho, P.,
Sampaio, G., Strassburg, B. B. N., and Vieira, I. C. G.: Pervasive
transition of the Brazilian land-use system, Nat. Clim. Change, 4, 27–35,
https://doi.org/10.1038/nclimate2056, 2013.
Leal, M. R. L. V., Horta Nogueira, L. A., and Cortez, L. A. B.: Land demand
for ethanol production, Appl. Energ., 102, 266–271,
https://doi.org/10.1016/j.apenergy.2012.09.037, 2013.
Leite, M. B., Xavier, R. O., Oliveira, P. T. S., Silva, F. K. G., and Silva
Matos, D. M.: Groundwater depth as a constraint on the woody cover in a
Neotropical Savanna, Plant Soil, 426, 1–15, https://doi.org/10.1007/s11104-018-3599-4, 2018.
Loarie, S. R., Lobell, D. B., Asner, G. P., Mu, Q., and Field, C. B.: Direct
impacts on local climate of sugar-cane expansion in Brazil, Nat. Clim. Change,
1, 105–109, https://doi.org/10.1038/nclimate1067, 2011.
Lucas, M., Oliveira, P. T. S., Melo, D. C. D., and Wendland, E.: Evaluation
of remotely sensed data for estimating recharge to an outcrop zone of the
Guarani Aquifer System (South America), Hydrogeol. J., 23, 961–969,
https://doi.org/10.1007/s10040-015-1246-1, 2015.
Lucas, M. and Wendland, E.: Recharge estimates for various land uses in the
Guarani Aquifer System outcrop area, Hydrolog. Sci. J., 61, 1253–1262,
https://doi.org/10.1080/02626667.2015.1031760, 2015.
Manzione, R. L., Soldera, B. C., and Wendland, E. C.: Groundwater system
response at sites with different agricultural land uses: case of the Guarani
Aquifer outcrop area, Brotas/SP-Brazil, Hydrolog. Sci. J., 62, 28–35,
https://doi.org/10.1080/02626667.2016.1154148, 2017.
Marris, E.: Conservation in Brazil: The forgotten ecosystem, Nature, 437,
944–945, 2005.
Meister, S., Nobrega, R. L. B., Rieger, W., Wolf, R., and Gerold, G.:
Process-based modelling of the impacts of land use change on the water
balance in the Cerrado Biome (Rio das Mortes, Brazil), Erdkunde, 71,
241–266, https://doi.org/10.3112/erdkunde.2017.03.06, 2017.
Melo, D. D. C. D., Scanlon, B. R., Zhang, Z., Wendland, E., and Yin, L.: Reservoir
storage and hydrologic responses to droughts in the Paraná River basin,
south-eastern Brazil, Hydrol. Earth Syst. Sci., 20, 4673–4688, https://doi.org/10.5194/hess-20-4673-2016, 2016.
Montgomery, D. C.: Design and Analysis of Experiments, John Wiley & Sons,
752 pp., 2008.
Mwango, S. B., Msanya, B. M., Mtakwa, P. W., Kimaro, D. N., Deckers, J., and
Poesen, J.: Effectiveness OF Mulching UnderMirabain Controlling Soil
Erosion, Fertility Restoration and Crop Yield in the Usambara Mountains,
Tanzania, Land Degrad. Dev., 27, 1266–1275, https://doi.org/10.1002/ldr.2332, 2016.
Nacinovic, M. G. G., Mahler, C. F., and Avelar, A. D. S.: Soil erosion as a
function of different agricultural land use in Rio de Janeiro, Soil Till.
Res., 144, 164–173, https://doi.org/10.1016/j.still.2014.07.002, 2014.
Nearing, M. A., Govers, G., and Norton, L. D.: Variability in Soil Erosion
Data from Replicated Plots, Soil Sci. Soc. Am. J., 63, 1829–1835,
https://doi.org/10.2136/sssaj1999.6361829x, 1999.
Nobrega, R. L. B., Guzha, A. C., Torres, G. N., Kovacs, K., Lamparter, G.,
Amorim, R. S. S., Couto, E., and Gerold, G.: Effects of conversion of native
cerrado vegetation to pasture on soil hydro-physical properties,
evapotranspiration and streamflow on the Amazonian agricultural frontier,
Plos One, 12, e0179414, https://doi.org/10.1371/journal.pone.0179414, 2017.
Oishi, A. C., Oren, R., Novick, K. A., Palmroth, S., and Katul, G. G.:
Interannual Invariability of Forest Evapotranspiration and Its Consequence
to Water Flow Downstream, Ecosystems, 13, 421–436,
https://doi.org/10.1007/s10021-010-9328-3, 2010.
Oliveira, L. C.: Erosão hídrica e alguns processos hidrológicos
em plantios de pinus, mata e campo nativos e estrada florestal, PhD,
Ciências Agrárias, Universidade do Estado de Santa Catarina, Lages,
SC, 96 pp., 2012.
Oliveira, P. T. S.: Balanço hídrico e erosão do solo em mata
nativa do bioma Cerrado, PhD, Departamento de Hidráulica e Saneamento –
Escola de Engenharia de São Carlos, Universidade de São Paulo,
São Carlos, SP, 2014.
Oliveira, P. T. S., Nearing, M. A., Moran, M. S., Goodrich, D. C., Wendland,
E., and Gupta, H. V.: Trends in water balance components across the
Brazilian Cerrado, Water Resour. Res., 50, 7100–7114, https://doi.org/10.1002/2013WR015202,
2014.
Oliveira, P. T. S., Wendland, E., Nearing, M. A., Scott, R. L., Rosolem, R.,
and da Rocha, H. R.: The water balance components of undisturbed tropical woodlands
in the Brazilian cerrado, Hydrol. Earth Syst. Sci., 19, 2899–2910, https://doi.org/10.5194/hess-19-2899-2015, 2015.
Oliveira, P. T. S., Nearing, M. A., Hawkins, R. H., Stone, J. J., Rodrigues,
D. B. B., Panachuki, E., and Wendland, E.: Curve number estimation from
Brazilian Cerrado rainfall and runoff data, J. Soil Water Conserv., 71,
420–429, https://doi.org/10.2489/jswc.71.5.420, 2016.
Oliveira, P. T. S., Leite, M. B., Mattos, T., Nearing, M. A., Scott, R. L.,
de Oliveira Xavier, R., da Silva Matos, D. M., and Wendland, E.: Groundwater
recharge decrease with increased vegetation density in the Brazilian
cerrado, Ecohydrology, 10, e1759, https://doi.org/10.1002/eco.1759, 2017.
Oliveira, R. S., Bezerra, L., Davidson, E. A., Pinto, F., Klink, C. A.,
Nepstad, D. C., and Moreira, A.: Deep root function in soil water dynamics
in cerrado savannas of central Brazil, Funct. Ecol., 19, 574–581,
https://doi.org/10.1111/j.1365-2435.2005.01003.x, 2005.
Paiva, R. C. D., Collischonn, W., and Buarque, D. C.: Validation of a full
hydrodynamic model for large-scale hydrologic modelling in the Amazon,
Hydrol. Process., 27, 333–346, https://doi.org/10.1002/hyp.8425, 2013.
Pereira, A. R.: The Priestley-Taylor parameter and the decoupling factor
for estimating reference evapotranspiration, Agr. Forest Meteorol., 125,
305–313, https://doi.org/10.1016/j.agrformet.2004.04.002, 2004.
Pimentel, D., Harvey, C., Resosudarmo, P., Sinclair, K., Kurz, D., McNair,
M., Crist, S., Shpritz, L., Fitton, L., and Saffouri, R.: Environmental and
economic costs of soil erosion and conservation benefits, Science, 267,
1117–1122, 1995.
Priestley, C. H. B. and Taylor, R. J.: On the Assessment of Surface Heat
Flux and Evaporation Using Large-Scale Parameters, Mon. Weather Rev., 100,
81–92, https://doi.org/10.1175/1520-0493(1972)1000081:OTAOSH>2.3.CO;2,
1972.
Rawitscher, F.: The Water Economy of the Vegetation of the “Campos
Cerrados” in Southern Brazil, J. Ecol., 36, 237–268, https://doi.org/10.2307/2256669, 1948.
Refsgaard, J. C., van der Sluijs, J. P., Højberg, A. L., and
Vanrolleghem, P. A.: Uncertainty in the environmental modelling process – A
framework and guidance, Environ. Modell. Softw., 22, 1543–1556,
https://doi.org/10.1016/j.envsoft.2007.02.004, 2007.
Reys, P., Camargo, M. G. G., Grombone-Guarantini, M. T., Teixeira, A. P.,
Assis, M. A., and Morellato, L. P. C.: Estrutura e composição
florística de um Cerrado sensu stricto e sua importância para
propostas de restauração ecológica, Hoehnea, 40, 449–464, 2013.
Richards, L. A.: Capillary conduction of liquids through porous mediums,
Physics, 1, 318–333, https://doi.org/10.1063/1.1745010, 1931.
Ritchie, J. T.: Model for predicting evaporation from a row crop with
incomplete cover, Water Resour. Res., 8, 1204–1213, https://doi.org/10.1029/WR008i005p01204,
1972.
Rodrigues, N., Losekann, L., and Silveira Filho, G.: Demand of automotive
fuels in Brazil: Underlying energy demand trend and asymmetric price
response, Energ. Econ., 74, 644–655, https://doi.org/10.1016/j.eneco.2018.07.005, 2018.
Sadeghi, S. H. R., Seghaleh, M. B., and Rangavar, A. S.: Plot sizes
dependency of runoff and sediment yield estimates from a small watershed,
Catena, 102, 55–61, https://doi.org/10.1016/j.catena.2011.01.003, 2013.
Sakai, R. K., Fitzjarrald, D. R., Moraes, O. L. L., Staebler, R. M.,
Acevedo, O. C., Czikowsky, M. J., Silva, R. d., Brait, E., and Miranda, V.:
Land-use change effects on local energy, water, and carbon balances in an
Amazonian agricultural field, Global Change Biol., 10, 895–907,
https://doi.org/10.1111/j.1529-8817.2003.00773.x, 2004.
Saraiva, O. F., Cogo, N. P., and Mielniczuk, J.: Erosividade das chuvas e
perdas por erosão em diferentes manejos de solo e coberturas vegetais,
Pesqui. Agropecu. Bras., 16, 121–128, 1981.
Scanlon, B. R., Reedy, R. C., Stonestrom, D. A., Prudic, D. E., and Dennehy,
K. F.: Impact of land use and land cover change on groundwater recharge and
quality in the southwestern US, Global Change Biol., 11, 1577–1593,
https://doi.org/10.1111/j.1365-2486.2005.01026.x, 2005.
Scott, R. L., Huxman, T. E., Barron-Gafford, G. A., Darrel Jenerette, G.,
Young, J. M., and Hamerlynck, E. P.: When vegetation change alters ecosystem
water availability, Global Change Biol., 20, 2198–2210, https://doi.org/10.1111/gcb.12511, 2014.
Silva, M. A., Silva, M. L. N., Curi, N., Avanzi, J. C., and Leite, F. P.:
Sistemas de manejo em plantios florestais de eucalipto e perdas de solo e
água na região do Vale do Rio Doce, MG, Cienc. Florest., 21, 765–776,
2011.
Soares-Filho, B., Rajão, R., Macedo, M., Carneiro, A., Costa, W., Coe,
M., Rodrigues, H., and Alencar, A.: Cracking Brazil's Forest Code, Science,
344, 363–364, https://doi.org/10.1126/science.1246663, 2014.
Strohmeier, S., Laaha, G., Holzmann, H., and Klik, A.: Magnitude and
Occurrence Probability of Soil Loss: A Risk Analytical Approach for the Plot
Scale For Two Sites in Lower Austria, Land Degrad. Dev., 27, 43–51,
https://doi.org/10.1002/ldr.2354, 2016.
Su, C., Cheng, Z., Wei, W., and Chen, Z.: Assessing groundwater availability
and the response of the groundwater system to intensive exploitation in the
North China Plain by analysis of long-term isotopic tracer data, Hydrogeol. J., 26, 1401–1415, https://doi.org/10.1007/s10040-018-1761-y, 2018.
Tseng, C. L., Alves, M. C., and Crestana, S.: Quantifying physical and
structural soil properties using X-ray microtomography, Geoderma, 318,
78–87, https://doi.org/10.1016/j.geoderma.2017.11.042, 2018.
Villalobos-Vega, R., Salazar, A., Miralles-Wilhelm, F., Haridasan, M.,
Franco, A. C., and Goldstein, G.: Do groundwater dynamics drive spatial
patterns of tree density and diversity in Neotropical savannas?, J. Veg. Sci.,
25, 1465–1473, https://doi.org/10.1111/jvs.12194, 2014.
Vourlitis, G. L., Filho, N. P., Hayashi, M. M. S., de S. Nogueira, J.,
Caseiro, F. T., and Campelo, J. H.: Seasonal variations in the
evapotranspiration of a transitional tropical forest of Mato Grosso, Brazil,
Water Resour. Res., 38, 30–31, https://doi.org/10.1029/2000wr000122, 2002.
Wang, H., Tetzlaff, D., and Soulsby, C.: Modelling the effects of land cover
and climate change on soil water partitioning in a boreal headwater
catchment, J. Hydrol., 558, 520–531, https://doi.org/10.1016/j.jhydrol.2018.02.002, 2018.
Wang, Q. J.: The Genetic Algorithm and Its Application to Calibrating
Conceptual Rainfall-Runoff Models, Water Resour. Res., 27, 2467–2471,
https://doi.org/10.1029/91WR01305, 1991.
Wendland, E., Barreto, C., and Gomes, L. H.: Water balance in the Guarani
Aquifer outcrop zone based on hydrogeologic monitoring, J. Hydrol., 342,
261–269, https://doi.org/10.1016/j.jhydrol.2007.05.033, 2007.
Wendt, R., Alberts, E., and Hjelmfelt, A.: Variability of runoff and soil
loss from fallow experimental plots, Soil Sci. Soc. Am. J., 50, 730–736, 1986.
Wohl, E., Barros, A., Brunsell, N., Chappell, N. A., Coe, M., Giambelluca,
T., Goldsmith, S., Harmon, R., Hendrickx, J. M. H., Juvik, J., McDonnell,
J., and Ogden, F.: The hydrology of the humid tropics, Nat. Clim. Change, 2,
655–662, https://doi.org/10.1038/nclimate1556, 2012.
Youlton, C., Bragion, A. P., and Wendland, E.: Experimental evaluation of
sediment yield in the first year after replacement of pastures by sugarcane,
Cienc. Investig. Agrar., 43, 374–383, https://doi.org/10.4067/S0718-16202016000300005, 2016a.
Youlton, C., Wendland, E., Anache, J. A. A., Poblete-Echeverría, C.,
and Dabney, S.: Changes in erosion and runoff due to replacement of pasture
land with sugarcane crops, Sustainability-Basel, 8, 685, https://doi.org/10.3390/su8070685,
2016b.
Zhao, C., Gao, J. E., Huang, Y., Wang, G., and Xu, Z.: The Contribution of
Astragalus adsurgens Roots and Canopy to Water Erosion Control in the
Water-Wind Crisscrossed Erosion Region of the Loess Plateau, China, Land Degrad. Dev., 28, 265–273, https://doi.org/10.1002/ldr.2508, 2017.
Short summary
We assessed the water balance over 5 years in different land uses typical of the Brazilian Cerrado: tropical woodland, bare land, pasture and sugarcane. Land uses may affect hillslope hydrology and cause trade-offs; the woodland consumes the soil water storage along the dry season, while the agricultural LCLU (pasture and sugarcane) reduces the water consumption in either season, and the aquifer recharge rates may be reduced in forested areas due to increased water demand by the vegetation.
We assessed the water balance over 5 years in different land uses typical of the Brazilian...
