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Partial afforestation has uncertain effect on flood frequency and peak discharge at large catchment scales (100-1000 km2), south-central Chile

Lookup NU author(s): Dr James Bathurst, Professor Chris Kilsby

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This is the authors' accepted manuscript of an article that has been published in its final definitive form by Wiley, 2022.

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Abstract

An extensive programme of commercial afforestation in south-central Chile provides a unique opportunity to extend the field-based understanding of forest impact on floods to the large catchment scale (100-1000 km2). Until now, much of that understanding has been limited to small catchments (< 10 km2). Data for an approximately 50-year period are analyzed systematically for four catchments (434-1545 km2) with 18-54% increases in forest cover. For each catchment, the forest impact is quantified by pairing annual maximum flood frequency curves and peak discharge/storm rainfall relationships for the pre- and post-afforestation periods. These periods are themselves defined using land use surveys and cumulative double mass curves for runoff and rainfall. Scaling the frequency curves with a discharge corresponding to mean annual rainfall normalizes for rainfall differences and thus isolates the effect of forest cover. Partial afforestation rates of up to 50%, while markedly affecting annual evapotranspiration and runoff, have less certain effects on peak discharges. Downward shifts in the flood frequency curves occur following afforestation but appear more readily explained by changes in rainfall regime. These changes include a small decline in annual rainfall and a downward shift in some of the frequency curves for the storm rainfall totals corresponding to the annual maximum discharges. Nevertheless, some forest impact cannot be ruled out and the effect of a 100% change in forest cover on flood response remains unknown. The results suggest complexity in large catchment flood response and provide only weak support for afforestation with the sole purpose of reducing flood peaks at the large catchment scale. This is a significant conclusion, given that it challenges the largely uncritical view among the public, governments and development agencies worldwide that forests prevent floods.


Publication metadata

Author(s): Bathurst JC, Hagon H, Hambly Barton F, Iroumé A, Kilbride A, Kilsby C

Publication type: Article

Publication status: Published

Journal: Hydrological Processes

Year: 2022

Volume: 36

Issue: 5

Online publication date: 09/05/2022

Acceptance date: 20/04/2022

Date deposited: 03/05/2022

ISSN (electronic): 1099-1085

Publisher: Wiley

URL: https://doi.org/10.1002/hyp.14585

DOI: 10.1002/hyp.14585

ePrints DOI: 10.57711/0w9e-zz78


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