Preprints
https://doi.org/10.5194/egusphere-2026-4439
https://doi.org/10.5194/egusphere-2026-4439
10 Aug 2026
 | 10 Aug 2026
Status: this preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).

Stream connectivity and governing processes in high-mountain wetlands

Anthony C. Ross, Ben C. Howard, Braulio Lahuatte, Paola Fuentes, Bert De Bièvre, Mateo Jerves-Ramirez, Patricio Crespo, Nilton Montoya, Jasper Oshun, Athanasios Paschalis, and Wouter Buytaert

Abstract. High-mountain wetlands (hereafter wetlands) have the potential to store and release large volumes of water. They provide substantial contributions to water supply for highland communities and receiving lowlands and their extended residence times can buffer water demand during drier periods. Despite their hydrological significance, major gaps remain in understanding the connection between wetlands and streams, which prevents us from accurately conceptualising them in models. We used a combination of conservative fluorescent tracing and monitoring of rainfall-runoff and wetland water levels to develop a perceptual model of connectivity between wetlands and streams. The experiments were conducted during the wet or dry season in five study catchments (0.38 km2 – 12.58 km2) from northern Ecuador to southern Peru. Fluorescein was introduced into wetlands and monitored downstream with activated carbon samplers for 5–12 months. Our results suggest travel times from less than 1 week to upwards of 3 ½ months, with one experiment seeing little to no response. Results indicate that wetlands have a stronger hydrological connection to streams in the wet season than in the dry season, where in some cases we observed no connection at all. Multiple peaks in fluorescein concentration from a single injection during the wet season may suggest that the wetlands contribute to streamflow via multiple pathways and processes. The results demonstrate a complex connection between wetlands and streams, controlled by topographic configuration and season, amongst other factors. However, persistent contributions from wetlands to streams observed several months after dye introduction support their significance to downstream, year-round water supply. The results provide improved understanding of wetland-stream connectivity that informs the development of models to address the need for site-specific evidence of wetlands’ influence on water supply and the ability to scale this information in space and time.

Competing interests: At least one of the (co-)authors is a member of the editorial board of Hydrology and Earth System Sciences.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Anthony C. Ross, Ben C. Howard, Braulio Lahuatte, Paola Fuentes, Bert De Bièvre, Mateo Jerves-Ramirez, Patricio Crespo, Nilton Montoya, Jasper Oshun, Athanasios Paschalis, and Wouter Buytaert

Status: open (until 21 Sep 2026)

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Anthony C. Ross, Ben C. Howard, Braulio Lahuatte, Paola Fuentes, Bert De Bièvre, Mateo Jerves-Ramirez, Patricio Crespo, Nilton Montoya, Jasper Oshun, Athanasios Paschalis, and Wouter Buytaert
Anthony C. Ross, Ben C. Howard, Braulio Lahuatte, Paola Fuentes, Bert De Bièvre, Mateo Jerves-Ramirez, Patricio Crespo, Nilton Montoya, Jasper Oshun, Athanasios Paschalis, and Wouter Buytaert
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Latest update: 10 Aug 2026
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Short summary
High-mountain wetlands can secure year-round water for communities, but their connection to streams remains unclear. Using dye tracing across five tropical mountain sites, we tracked water movement over several months. Results show that wetland-to-stream travel times vary from under one week to over three months, depending on season, topography and geology, among other factors. Understanding this complex connectivity is vital for improving streamflow predictions and water supply management.
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