Seasonal water storage and release dynamics of bofedal wetlands in the Central Andes

dc.contributor.affiliationPontificia Universidad Católica del Perú. Departamento de Humanidades
dc.contributor.authorRoss, A.C.
dc.contributor.authorMendoza, M.M.
dc.contributor.authorDrenkhan, F.
dc.contributor.authorMontoya, N.
dc.contributor.authorBaiker, J.R.
dc.contributor.authorMacKay, J.D.
dc.contributor.authorHannah, D.M.
dc.contributor.authorBuytaert, W.
dc.date.accessioned2026-03-13T16:59:57Z
dc.date.issued2023
dc.description.abstractTropical high-Andean wetlands, locally known as ‘bofedales’, are key ecosystems sustaining biodiversity, carbon sequestration, water provision and livestock farming. Bofedales' contribution to dry season baseflows and sustaining water quality is crucial for downstream water security. The sensitivity of bofedales to climatic and anthropogenic disturbances is therefore of growing concern for watershed management. This study aims to understand seasonal water storage and release characteristics of bofedales by combining remote sensing analysis and ground-based monitoring for the wet and dry seasons of late 2019 to early 2021, using the glacierised Vilcanota-Urubamba basin (Southern Peru) as a case study. A network of five ultrasound loggers was installed to obtain discharge and water table data from bofedal sites across two headwater catchments. The seasonal extent of bofedales was mapped by applying a supervised machine learning model using Random Forest on imagery from Sentinel-2 and NASADEM. We identified high seasonal variability in bofedal area with a total of 3.5% and 10.6% of each catchment area, respectively, at the end of the dry season (2020), which increased to 15.1% and 16.9%, respectively, at the end of the following wet season (2021). The hydrological observations and bofedal maps were combined into a hydrological conceptual model to estimate the storage and release characteristics of the bofedales, and their contribution to runoff at the catchment scale. Estimated lag times between 1 and 32 days indicate a prolonged bofedal flow contribution throughout the dry season (about 74% of total flow). Thus, our results suggest that bofedales provide substantial contribution to dry season baseflow, water flow regulation and storage. These findings highlight the importance of including bofedales in local water management strategies and adaptation interventions including nature-based solutions that seek to support long-term water security in seasonally dry and rapidly changing Andean catchments.
dc.description.sponsorshipFunding: This study was developed within the framework of the Newton-Paulet Fund based RAHU project which is implemented by CONCYTEC Peru and UKRI (NERC grant no. NE/S013210/1). We thank the Phinaya and Sibina Sallma communities (Pitumarca district, Cusco) for their extensive support of the logger installation and data collection. Loggers were installed with the help of Brigitte Macera, Miguel Vargas and Marcelo Bueno (students of N Montoya). We are grateful to use meteorological data provided from SENAMHI (Sibinacocha Lake station) and SENAMHI in collaboration with UNSAAC and Appalachian State University (Quelccaya Glacier station). We also thank Raquel Ríos and Beatriz Fuentealba from INAIGEM (Peru) for their insightful comments on an earlier manuscript version. J Mackay contributed via the BGS International NC programme ‘Geoscience to tackle Global Environmental Challenges', NERC reference NE/X006255/1. The paper is published by permission of the Director of the British Geological Survey.; Funding text 2: This study was developed within the framework of the Newton-Paulet Fund based RAHU project which is implemented by CONCYTEC Peru and UKRI (NERC grant no. NE/S013210/1). We thank the Phinaya and Sibina Sallma communities (Pitumarca district, Cusco) for their extensive support of the logger installation and data collection. Loggers were installed with the help of Brigitte Macera, Miguel Vargas and Marcelo Bueno (students of N Montoya). We are grateful to use meteorological data provided from SENAMHI (Sibinacocha Lake station) and SENAMHI in collaboration with UNSAAC and Appalachian State University (Quelccaya Glacier station). We also thank Raquel Ríos and Beatriz Fuentealba from INAIGEM (Peru) for their insightful comments on an earlier manuscript version. J Mackay contributed via the BGS International NC programme ‘Geoscience to tackle Global Environmental Challenges', NERC reference NE/X006255/1. The paper is published by permission of the Director of the British Geological Survey.
dc.identifier.doihttps://doi.org/10.1002/hyp.14940
dc.identifier.urihttp://hdl.handle.net/20.500.14657/206496
dc.language.isoeng
dc.publisherJohn Wiley and Sons
dc.relation.ispartofurn:issn:0885-6087
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.sourceHydrological Processes; Vol. 37, Núm. 8 (2023)
dc.subjectEnvironmental science
dc.subjectWetland
dc.subjectHydrology (agriculture)
dc.subjectDry season
dc.subjectWet season
dc.subjectSurface runoff
dc.subjectWater storage
dc.subjectDrainage basin
dc.subjectWater quality
dc.subjectWatershed
dc.subjectWater table
dc.subjectDischarge
dc.subjectEcology
dc.subjectGroundwater
dc.subjectGeography
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.05
dc.titleSeasonal water storage and release dynamics of bofedal wetlands in the Central Andes
dc.typehttp://purl.org/coar/resource_type/c_6501
dc.type.otherArtículo
dc.type.versionhttps://vocabularies.coar-repositories.org/version_types/c_970fb48d4fbd8a85/

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