Response of Water Balance Components to Changes in Soil Use and Vegetation Cover Over Three Decades in the Eastern Amazon
Impacts on global water resources may be intensifying due to the growing and differentiated forms of land use and occupation, which influence the water cycle and thus the maintenance of life. In the Amazon, the effect may be even worse, as it is one of the world's most vulnerable regions to the...
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Frontiers Media S.A.
2021-10-01
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Online Access: | https://www.frontiersin.org/articles/10.3389/frwa.2021.749507/full |
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author | Renato Oliveira da Silva-Júnior Pedro Walfir Martins e Souza-Filho Gabriel Negreiros Salomão Alexandra Lima Tavares Jorge Filipe dos Santos Diogo Corrêa Santos Luanna Costa Dias Marcio Sousa da Silva Adayana Maria Queiroz de Melo Carlos Eduardo Aguiar de Souza Costa Edson José Paulino da Rocha |
author_facet | Renato Oliveira da Silva-Júnior Pedro Walfir Martins e Souza-Filho Gabriel Negreiros Salomão Alexandra Lima Tavares Jorge Filipe dos Santos Diogo Corrêa Santos Luanna Costa Dias Marcio Sousa da Silva Adayana Maria Queiroz de Melo Carlos Eduardo Aguiar de Souza Costa Edson José Paulino da Rocha |
author_sort | Renato Oliveira da Silva-Júnior |
collection | DOAJ |
description | Impacts on global water resources may be intensifying due to the growing and differentiated forms of land use and occupation, which influence the water cycle and thus the maintenance of life. In the Amazon, the effect may be even worse, as it is one of the world's most vulnerable regions to these changes. This work aimed to analyze the response of the components of the water balance to changes in land use and cover in the Eastern Amazon over three decades (1980–2013). First, soil texture maps were prepared. These combined with the classes of use in each decade let us estimate the values of storage and variation in storage (ΔS) of water in the soil. The behavior of the components of the water balance [precipitation, potential evapotranspiration, actual evapotranspiration (E), and ΔS] were analyzed according to the Budyko model on the annual scale as a function of the aridity and evaporative indices. For the seasonal scale, a new parameter (y0) was introduced to explicitly represent the additional water available for E, in addition to instantaneous precipitation. The seasonality of the rains and the seasonal dynamics of storage were directly incorporated into the model developed, which allowed us to understand what the dominant control factors of water balance are. In the decade from 2000 to 2009, the remaining forest cover is only 48.91%, while the cover formed by pasture is 50.47%, meaning the water storage capacity in the soil decreased 8.1%. In the 1990s, to 1999, precipitation shows a reduction, probably as a reflection of the very strong events of La Niña and El Niño (1988–1989 and 1997–1998). Observing the sum of the surface area of water bodies in the region and the relationship of forest vs. pasture, it is possible to infer that the elevation in evapotranspiration is more related to the increase in evaporation due to the increase in the pasture area than to the reduction transpiration due to forest loss, reinforcing the hypothesis that evapotranspiration increases with pasture area. |
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last_indexed | 2024-12-19T19:19:34Z |
publishDate | 2021-10-01 |
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spelling | doaj.art-0f53908223714acbb87f90184a9304a72022-12-21T20:09:02ZengFrontiers Media S.A.Frontiers in Water2624-93752021-10-01310.3389/frwa.2021.749507749507Response of Water Balance Components to Changes in Soil Use and Vegetation Cover Over Three Decades in the Eastern AmazonRenato Oliveira da Silva-Júnior0Pedro Walfir Martins e Souza-Filho1Gabriel Negreiros Salomão2Alexandra Lima Tavares3Jorge Filipe dos Santos4Diogo Corrêa Santos5Luanna Costa Dias6Marcio Sousa da Silva7Adayana Maria Queiroz de Melo8Carlos Eduardo Aguiar de Souza Costa9Edson José Paulino da Rocha10Vale Technological Institute for Sustainable Development, Belém, BrazilVale Technological Institute for Sustainable Development, Belém, BrazilVale Technological Institute for Sustainable Development, Belém, BrazilClimatempo (StormGeo), São Paulo, BrazilVale Technological Institute for Sustainable Development, Belém, BrazilVale Technological Institute for Sustainable Development, Belém, BrazilMineral Resources Research Company—Geological Survey of Brazil, Belém, BrazilVale Technological Institute for Sustainable Development, Belém, BrazilVale Technological Institute for Sustainable Development, Belém, BrazilVale Technological Institute for Sustainable Development, Belém, BrazilGeosciences Institute, Federal University of Pará, Belém, BrazilImpacts on global water resources may be intensifying due to the growing and differentiated forms of land use and occupation, which influence the water cycle and thus the maintenance of life. In the Amazon, the effect may be even worse, as it is one of the world's most vulnerable regions to these changes. This work aimed to analyze the response of the components of the water balance to changes in land use and cover in the Eastern Amazon over three decades (1980–2013). First, soil texture maps were prepared. These combined with the classes of use in each decade let us estimate the values of storage and variation in storage (ΔS) of water in the soil. The behavior of the components of the water balance [precipitation, potential evapotranspiration, actual evapotranspiration (E), and ΔS] were analyzed according to the Budyko model on the annual scale as a function of the aridity and evaporative indices. For the seasonal scale, a new parameter (y0) was introduced to explicitly represent the additional water available for E, in addition to instantaneous precipitation. The seasonality of the rains and the seasonal dynamics of storage were directly incorporated into the model developed, which allowed us to understand what the dominant control factors of water balance are. In the decade from 2000 to 2009, the remaining forest cover is only 48.91%, while the cover formed by pasture is 50.47%, meaning the water storage capacity in the soil decreased 8.1%. In the 1990s, to 1999, precipitation shows a reduction, probably as a reflection of the very strong events of La Niña and El Niño (1988–1989 and 1997–1998). Observing the sum of the surface area of water bodies in the region and the relationship of forest vs. pasture, it is possible to infer that the elevation in evapotranspiration is more related to the increase in evaporation due to the increase in the pasture area than to the reduction transpiration due to forest loss, reinforcing the hypothesis that evapotranspiration increases with pasture area.https://www.frontiersin.org/articles/10.3389/frwa.2021.749507/fullhydrological responseBudyko modelwater resources managementsoil degradationevapotranspiration |
spellingShingle | Renato Oliveira da Silva-Júnior Pedro Walfir Martins e Souza-Filho Gabriel Negreiros Salomão Alexandra Lima Tavares Jorge Filipe dos Santos Diogo Corrêa Santos Luanna Costa Dias Marcio Sousa da Silva Adayana Maria Queiroz de Melo Carlos Eduardo Aguiar de Souza Costa Edson José Paulino da Rocha Response of Water Balance Components to Changes in Soil Use and Vegetation Cover Over Three Decades in the Eastern Amazon Frontiers in Water hydrological response Budyko model water resources management soil degradation evapotranspiration |
title | Response of Water Balance Components to Changes in Soil Use and Vegetation Cover Over Three Decades in the Eastern Amazon |
title_full | Response of Water Balance Components to Changes in Soil Use and Vegetation Cover Over Three Decades in the Eastern Amazon |
title_fullStr | Response of Water Balance Components to Changes in Soil Use and Vegetation Cover Over Three Decades in the Eastern Amazon |
title_full_unstemmed | Response of Water Balance Components to Changes in Soil Use and Vegetation Cover Over Three Decades in the Eastern Amazon |
title_short | Response of Water Balance Components to Changes in Soil Use and Vegetation Cover Over Three Decades in the Eastern Amazon |
title_sort | response of water balance components to changes in soil use and vegetation cover over three decades in the eastern amazon |
topic | hydrological response Budyko model water resources management soil degradation evapotranspiration |
url | https://www.frontiersin.org/articles/10.3389/frwa.2021.749507/full |
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