More cultivation with lower intensity in the South American Chaco: A double hydrological challenge

Raul Gimenez, Jorge Luis Mercau, Javier Houspanossian, Germán Baldi, Sylvain Kuppel, Esteban G. Jobbágy

Research output: Contribution to conferenceOther

Abstract

As in other semi-arid plains of the world, long-scale deforestation to establish croplands in the South American Chaco may disrupt the regional water balance. As annual crops use less water than the native perennial system, water in excess usually translates into serious degradation processes such as run-off driven erosion, or the onset of groundwater recharge which can develop flooding and dryland salinization. Agriculturally, water excess could be reduced by using more intensive crop systems which consume water exhaustively. We used MODIS imagery (2000-present) from Bandera, Argentina (28.8S 62.2W), a major agricultural cluster in the region, to assess deforestation, to identify the main crop systems, and to analyze the impact of crop expansion and phenological shifts on the regional water balance. Three cover classes (Dry Forest DF, Agriculture AG, and Pastures PA) and five AG crop types were distinguished (winter W, spring Sp,summer S, and late-summer LS single crops, winter/summer DCWS and spring/summer DCSpS double crops). Each season, water use (annual evapotranspiration, ET) for each cover/crop type (10 pixels/class) was computed with a daily water balance based on meteorological data and 2 remote sensing-derived indices: Normalized Difference Vegetation Index, to capture canopy conditions, and Dead Fuel Index to represent mulch cover conditions. Throughout 14 crop seasons AG expanded from 20 to 50% of the study area (1M ha) mostly replacing DF. Also, AG gradually evolved from a more intensive and diversified pattern dominated by DC (45-50%), S (28%) and Sp (16%) systems, to a more water-conservative system dominated by LS (60-80% in the last 3 seasons). Crop type differences in ET (DCWS≈DCSpS≈FG>S>Sp>LS≈W) were stronger in wet years (>1000mm) but nil in dry ones (<550mm). As a result, water excess (precipitation-ET) ranged from 0mm for most crop types in the driest year to >250mm for the less intensive W and LS in wet years. Weighting each cover/crop class by their area, we found that the current expansion and reduced intensity of cultivation has cut regional ET of wet years by 50-100mm (compared to early 2000s land cover/crop pattern in similar weather conditions), generating a growing water excess that is likely contributing to drive the water table rises and more frequent floods observed in this region.
Original languageEnglish
Number of pages1
Publication statusPublished - 17 Dec 2014
Event2014 AGU Fall Meeting - San Francisco, United States
Duration: 15 Dec 201419 Dec 2014

Conference

Conference2014 AGU Fall Meeting
CountryUnited States
CitySan Francisco
Period15/12/1419/12/14

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crop
cover crop
evapotranspiration
water budget
summer
water
deforestation
winter
mulch
dry forest
salinization
NDVI
MODIS
water use
water table
recharge
pasture
pixel
land cover
imagery

Cite this

Gimenez, R., Mercau, J. L., Houspanossian, J., Baldi, G., Kuppel, S., & Jobbágy, E. G. (2014). More cultivation with lower intensity in the South American Chaco: A double hydrological challenge. 2014 AGU Fall Meeting, San Francisco, United States.

More cultivation with lower intensity in the South American Chaco : A double hydrological challenge. / Gimenez, Raul; Mercau, Jorge Luis; Houspanossian, Javier; Baldi, Germán; Kuppel, Sylvain; Jobbágy, Esteban G.

2014. 2014 AGU Fall Meeting, San Francisco, United States.

Research output: Contribution to conferenceOther

Gimenez, R, Mercau, JL, Houspanossian, J, Baldi, G, Kuppel, S & Jobbágy, EG 2014, 'More cultivation with lower intensity in the South American Chaco: A double hydrological challenge' 2014 AGU Fall Meeting, San Francisco, United States, 15/12/14 - 19/12/14, .
Gimenez R, Mercau JL, Houspanossian J, Baldi G, Kuppel S, Jobbágy EG. More cultivation with lower intensity in the South American Chaco: A double hydrological challenge. 2014. 2014 AGU Fall Meeting, San Francisco, United States.
Gimenez, Raul ; Mercau, Jorge Luis ; Houspanossian, Javier ; Baldi, Germán ; Kuppel, Sylvain ; Jobbágy, Esteban G. / More cultivation with lower intensity in the South American Chaco : A double hydrological challenge. 2014 AGU Fall Meeting, San Francisco, United States.1 p.
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title = "More cultivation with lower intensity in the South American Chaco: A double hydrological challenge",
abstract = "As in other semi-arid plains of the world, long-scale deforestation to establish croplands in the South American Chaco may disrupt the regional water balance. As annual crops use less water than the native perennial system, water in excess usually translates into serious degradation processes such as run-off driven erosion, or the onset of groundwater recharge which can develop flooding and dryland salinization. Agriculturally, water excess could be reduced by using more intensive crop systems which consume water exhaustively. We used MODIS imagery (2000-present) from Bandera, Argentina (28.8S 62.2W), a major agricultural cluster in the region, to assess deforestation, to identify the main crop systems, and to analyze the impact of crop expansion and phenological shifts on the regional water balance. Three cover classes (Dry Forest DF, Agriculture AG, and Pastures PA) and five AG crop types were distinguished (winter W, spring Sp,summer S, and late-summer LS single crops, winter/summer DCWS and spring/summer DCSpS double crops). Each season, water use (annual evapotranspiration, ET) for each cover/crop type (10 pixels/class) was computed with a daily water balance based on meteorological data and 2 remote sensing-derived indices: Normalized Difference Vegetation Index, to capture canopy conditions, and Dead Fuel Index to represent mulch cover conditions. Throughout 14 crop seasons AG expanded from 20 to 50{\%} of the study area (1M ha) mostly replacing DF. Also, AG gradually evolved from a more intensive and diversified pattern dominated by DC (45-50{\%}), S (28{\%}) and Sp (16{\%}) systems, to a more water-conservative system dominated by LS (60-80{\%} in the last 3 seasons). Crop type differences in ET (DCWS≈DCSpS≈FG>S>Sp>LS≈W) were stronger in wet years (>1000mm) but nil in dry ones (<550mm). As a result, water excess (precipitation-ET) ranged from 0mm for most crop types in the driest year to >250mm for the less intensive W and LS in wet years. Weighting each cover/crop class by their area, we found that the current expansion and reduced intensity of cultivation has cut regional ET of wet years by 50-100mm (compared to early 2000s land cover/crop pattern in similar weather conditions), generating a growing water excess that is likely contributing to drive the water table rises and more frequent floods observed in this region.",
author = "Raul Gimenez and Mercau, {Jorge Luis} and Javier Houspanossian and Germ{\'a}n Baldi and Sylvain Kuppel and Jobb{\'a}gy, {Esteban G.}",
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AU - Gimenez, Raul

AU - Mercau, Jorge Luis

AU - Houspanossian, Javier

AU - Baldi, Germán

AU - Kuppel, Sylvain

AU - Jobbágy, Esteban G.

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Y1 - 2014/12/17

N2 - As in other semi-arid plains of the world, long-scale deforestation to establish croplands in the South American Chaco may disrupt the regional water balance. As annual crops use less water than the native perennial system, water in excess usually translates into serious degradation processes such as run-off driven erosion, or the onset of groundwater recharge which can develop flooding and dryland salinization. Agriculturally, water excess could be reduced by using more intensive crop systems which consume water exhaustively. We used MODIS imagery (2000-present) from Bandera, Argentina (28.8S 62.2W), a major agricultural cluster in the region, to assess deforestation, to identify the main crop systems, and to analyze the impact of crop expansion and phenological shifts on the regional water balance. Three cover classes (Dry Forest DF, Agriculture AG, and Pastures PA) and five AG crop types were distinguished (winter W, spring Sp,summer S, and late-summer LS single crops, winter/summer DCWS and spring/summer DCSpS double crops). Each season, water use (annual evapotranspiration, ET) for each cover/crop type (10 pixels/class) was computed with a daily water balance based on meteorological data and 2 remote sensing-derived indices: Normalized Difference Vegetation Index, to capture canopy conditions, and Dead Fuel Index to represent mulch cover conditions. Throughout 14 crop seasons AG expanded from 20 to 50% of the study area (1M ha) mostly replacing DF. Also, AG gradually evolved from a more intensive and diversified pattern dominated by DC (45-50%), S (28%) and Sp (16%) systems, to a more water-conservative system dominated by LS (60-80% in the last 3 seasons). Crop type differences in ET (DCWS≈DCSpS≈FG>S>Sp>LS≈W) were stronger in wet years (>1000mm) but nil in dry ones (<550mm). As a result, water excess (precipitation-ET) ranged from 0mm for most crop types in the driest year to >250mm for the less intensive W and LS in wet years. Weighting each cover/crop class by their area, we found that the current expansion and reduced intensity of cultivation has cut regional ET of wet years by 50-100mm (compared to early 2000s land cover/crop pattern in similar weather conditions), generating a growing water excess that is likely contributing to drive the water table rises and more frequent floods observed in this region.

AB - As in other semi-arid plains of the world, long-scale deforestation to establish croplands in the South American Chaco may disrupt the regional water balance. As annual crops use less water than the native perennial system, water in excess usually translates into serious degradation processes such as run-off driven erosion, or the onset of groundwater recharge which can develop flooding and dryland salinization. Agriculturally, water excess could be reduced by using more intensive crop systems which consume water exhaustively. We used MODIS imagery (2000-present) from Bandera, Argentina (28.8S 62.2W), a major agricultural cluster in the region, to assess deforestation, to identify the main crop systems, and to analyze the impact of crop expansion and phenological shifts on the regional water balance. Three cover classes (Dry Forest DF, Agriculture AG, and Pastures PA) and five AG crop types were distinguished (winter W, spring Sp,summer S, and late-summer LS single crops, winter/summer DCWS and spring/summer DCSpS double crops). Each season, water use (annual evapotranspiration, ET) for each cover/crop type (10 pixels/class) was computed with a daily water balance based on meteorological data and 2 remote sensing-derived indices: Normalized Difference Vegetation Index, to capture canopy conditions, and Dead Fuel Index to represent mulch cover conditions. Throughout 14 crop seasons AG expanded from 20 to 50% of the study area (1M ha) mostly replacing DF. Also, AG gradually evolved from a more intensive and diversified pattern dominated by DC (45-50%), S (28%) and Sp (16%) systems, to a more water-conservative system dominated by LS (60-80% in the last 3 seasons). Crop type differences in ET (DCWS≈DCSpS≈FG>S>Sp>LS≈W) were stronger in wet years (>1000mm) but nil in dry ones (<550mm). As a result, water excess (precipitation-ET) ranged from 0mm for most crop types in the driest year to >250mm for the less intensive W and LS in wet years. Weighting each cover/crop class by their area, we found that the current expansion and reduced intensity of cultivation has cut regional ET of wet years by 50-100mm (compared to early 2000s land cover/crop pattern in similar weather conditions), generating a growing water excess that is likely contributing to drive the water table rises and more frequent floods observed in this region.

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ER -