Evaluating functional connectivity in a small agricultural catchment under contrasting flood events by using UAV |
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| Authors: | Aleix Calsamiglia Jorge Gago Julián Garcia-Comendador Josep Fortesa Bernat Adolfo Calvo-Cases Joan Estrany |
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| Institution: | 1. Mediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Palma de Mallorca, Balearic Islands, Spain;2. Institute of Agro-Environmental and Water Economy Research – INAGEA, University of the Balearic Islands, Palma de Mallorca, Balearic Islands, Spain
Biology of Plants under Mediterranean Conditions Research Team, Department of Biology, University of the Balearic Islands, Palma de Mallorca, Balearic Islands, Spain;3. Department of Geography, University of Valencia, Valencia, Spain |
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| Abstract: | Concentrated erosion, a major feature of land degradation, represents a serious problem for soil and water resources management and a threat to ecosystems. Understanding the internal mechanisms (de-)coupling sediment pathways can improve the management and resilience of catchments. In this study, concentrated erosion and deposition forms were mapped accurately through field and aerial unmanned aerial vehicle (UAV) campaigns, in order to assess the evolution of connectivity pathways over a series of three contrasted and consecutive flood events occurring between October 2016 and January 2017 (return period ranging from 0.5 to 25 years) in a small Mediterranean agricultural catchment (Can Revull, Mallorca, Spain; 1.4 km2). In addition, a morphometric index of connectivity (IC) was used to identify the potential trajectories of different concentrated erosion forms and deposition areas. IC predictions were calibrated by identifying the optimal critical thresholds, i.e. those most consistent with field observations after each of the events studied. The results found that the index performed well in predicting the occurrence and the length/area of the different type of landforms, giving kappa (κ) coefficients of variation ranging between 0.21 and 0.92 and linear correlations R2 between 0.33 and 0.72. The type of landform affected the correspondence of IC predictions and field observations, with lower thresholds the greater the magnitude of their associated geomorphic processes. Rainfall magnitude proved to be a very important factor controlling the development of erosion and deposition landforms, with large differences in length/area between the contrasted events. The evolution of the observed trajectories revealed feedback dynamics between the structural and functional connectivity of the catchment, in which morphological changes determined the spatial distribution of the processes’ activity in the successive events and vice versa. © 2020 John Wiley & Sons, Ltd. |
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| Keywords: | soil erosion ephemeral gullies tile drains traditional drainage systems UAV |
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