The role of protected and deforested areas in the hydrological processes of Itacaiúnas River Basin, eastern Amazonia.

Abstract To protect indigenous land and avoid the spread of deforestation in the Amazon, state and federal Brazilian agencies recognized several protected areas since the 1990s. However, the importance of these protected areas in the water cycle and the hydrologic connection with surrounding landscapes is little analyzed. In this study, we evaluated the role of preserved and deforested areas in the water balance in the Itacaiúnas River Basin using the MGB hydrological model. We estimated the impacts of land cover changes on evapotranspiration and discharge for four scenarios: Preserved (1984 land cover), Recent (2013 land cover, with 50% deforestation), Hypothetical deforestation of protected areas (70% deforestation) and complete deforestation of protected areas (79% deforestation). We showed that deforestation of the remaining preserved area could be responsible for a decrease of 23% (3.5 km³/year) in water transfer to the atmosphere by evapotranspiration. Furthermore, we showed that each 15% of deforestation occurring between the Preserved and Recent scenarios increased the average discharges by 5.4% (40 m³/s). Additionally, past land cover changes in the headwaters of the Itacaiúnas River Basin caused statistically significant changes in discharges inside the protected areas. This insight is considered important due to the association between increases in discharges and water quality issues. The results suggest that headwater areas of secondary drainages that run into the forested domains should be prioritized for reforestation programs. Likewise, the reforestation of nonprotected areas could be responsible for restoring ecosystem services, including hydrological functions, biodiversity and water quality. Highlights • Hydrologic modeling of an important ungauged river basin of Amazon Biome affected by deforestation. • MGB hydrologic model was used to estimate discharges and evapotranspiration in Itacaiúnas River Basin. • Important feedbacks involving evapotranspiration and discharge processes are affected by land use/land cover changes. • Insights of the streamflow inside the protected areas covered by forests are affected by land cover changes. • Insights on the role of protected areas in the hydrological processes and connection with surrounding landscapes. [ABSTRACT FROM AUTHOR]