Riverine sediment response to deforestation in the Amazon basin
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Published:2024-04-29
Issue:2
Volume:12
Page:581-599
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ISSN:2196-632X
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Container-title:Earth Surface Dynamics
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language:en
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Short-container-title:Earth Surf. Dynam.
Author:
Narayanan AnuskaORCID, Cohen SagyORCID, Gardner John R.
Abstract
Abstract. The Amazon experiences thousands of square kilometers of deforestation annually with recent rates increasing to levels unseen since the late 2000s. These increased rates of deforestation within the basin have led to changes in sediment concentration within its river systems, with potential impacts on ecological functioning, freshwater availability, and fluvial and coastal geomorphic processes. The relationship between deforestation and fluvial sediment dynamics in the Amazon has not been extensively studied using a basin-wide, comparative approach primarily due to lack of data. In this study, we utilize a novel remote-sensing-derived sediment concentration dataset to analyze the impact of deforestation from 2001 to 2020 on suspended sediment in large rivers (>50 m wide) across the Amazon River basin. These impacts are studied using a lag-based approach to quantify the spatiotemporal relationships between observed suspended sediment and changes in land cover over time. The results show that large-scale deforestation of the Amazon during the 2001–2020 period are associated with significant changes in sediment concentration in the eastern portion of the basin. In the heavily deforested eastern regions, the hydrogeomorphic response to deforestation occurs relatively rapidly (within a year), whereas the less disturbed western areas exhibit delays of 1 to 2 years before responses are observable. Moreover, we observe that deforestation must be substantial enough to overcome the collective influences of human activities and natural sediment variations to result in a discernible impact on sediment concentration in large rivers. In 69 % of Amazonian major tributary basins with an immediate response, more than 5 % of the basin was deforested during the 2001–2020 period, while in 85 % of basins with lagged responses, less than 5 % of the land was cleared. These findings suggest severe implications for future sediment dynamics across the Amazon if deforestation is to further expand into the basin.
Publisher
Copernicus GmbH
Reference98 articles.
1. Alemohammad, H. and Booth, K.: LandCoverNet: A global benchmark land cover classification training dataset (Version 1), arXiv [preprint], arXiv:2012.03111, https://doi.org/10.48550/ARXIV.2012.03111, 2020. 2. Alewell, C., Borrelli, P., Meusburger, K., and Panagos, P.: Using the USLE: Chances, challenges and limitations of soil erosion modelling, Int. Soil Water Conserv. Res., 7, 203–225, https://doi.org/10.1016/j.iswcr.2019.05.004, 2019. 3. Altenau, E. H., Pavelsky, T. M., Durand, M. T., Yang, X., Frasson, R. P. D. M., and Bendezu, L.; SWOT River Database (SWORD) (Version v1), Zenodo [data set], https://doi.org/10.5281/ZENODO.4917236, 2021. 4. American Academy of Actuaries: Actuaries Climate Index Sample Calculations, https://actuariesclimateindex.org/wp-content/uploads/2016/04/SampleCalcEng.5.18.pdf (last access: 25 April 2024), 2016. 5. Armijos, E., Crave, A., Espinoza, J. C., Filizola, N., Espinoza-Villar, R., Ayes, I., Fonseca, P., Fraizy, P., Gutierrez, O., Vauchel, P., Camenen, B., Martiínez, J. M., Dos Santos, A., Santini, W., Cochonneau, G., and Guyot, J. L.: Rainfall control on Amazon sediment flux: synthesis from 20 years of monitoring, Environ. Res. Commun., 2, 5, https://doi.org/10.1088/2515-7620/ab9003, 2020.
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