Articles | Volume 23, issue 1
https://doi.org/10.5194/hess-23-405-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-23-405-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Multi-scale temporal variability in meltwater contributions in a tropical glacierized watershed
Leila Saberi
CORRESPONDING AUTHOR
Department of Earth Sciences, University of Minnesota, Twin Cities, Minneapolis, MN 55455, USA
Rachel T. McLaughlin
Department of Earth Sciences, University of Minnesota, Twin Cities, Minneapolis, MN 55455, USA
G.-H. Crystal Ng
Department of Earth Sciences, University of Minnesota, Twin Cities, Minneapolis, MN 55455, USA
Saint Anthony Falls Laboratory, University of Minnesota, Twin Cities, Minneapolis, MN 55414, USA
Jeff La Frenierre
Department of Geography, Gustavus Adolphus College, St. Peter, MN 56082, USA
Andrew D. Wickert
Department of Earth Sciences, University of Minnesota, Twin Cities, Minneapolis, MN 55455, USA
Saint Anthony Falls Laboratory, University of Minnesota, Twin Cities, Minneapolis, MN 55414, USA
Michel Baraer
Construction Engineering, École de Technologie Supérieure, Université du Québec, Montreal, H3C 1K3, Canada
Wei Zhi
Department of Civil and Environmental Engineering, Pennsylvania State University, University Park, PA 16802-1294, USA
Department of Civil and Environmental Engineering, Pennsylvania State University, University Park, PA 16802-1294, USA
Bryan G. Mark
Department of Geography, The Ohio State University, Columbus, OH 43210-1361, USA
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29 citations as recorded by crossref.
- Evolution of runoff components and groundwater discharge under rapid climate warming: Lhasa river basin, Tibetan Plateau Q. He et al. 10.1016/j.jhydrol.2023.130556
- Significant stream chemistry response to temperature variations in a high-elevation mountain watershed W. Zhi et al. 10.1038/s43247-020-00039-w
- Glacier retreat and its impact on groundwater system evolution in the Yarlung Zangbo source region, Tibetan Plateau Q. He et al. 10.1016/j.ejrh.2023.101368
- Glacier Image Velocimetry: an open-source toolbox for easy and rapid calculation of high-resolution glacier velocity fields M. Van Wyk de Vries & A. Wickert 10.5194/tc-15-2115-2021
- Quantitative analysis of recharge sources of different runoff types in the source region of Three River L. Zongjie et al. 10.1016/j.jhydrol.2023.130366
- Increasing rate of 21st century volume loss of the Patagonian Icefields measured from proglacial river discharge M. Van Wyk de Vries et al. 10.1017/jog.2023.9
- Groundwater–glacier meltwater interaction in proglacial aquifers B. Ó Dochartaigh et al. 10.5194/hess-23-4527-2019
- A meta-analysis based review of quantifying the contributions of runoff components to streamflow in glacierized basins Z. He et al. 10.1016/j.jhydrol.2021.126890
- Glacier thickness and ice volume of the Northern Andes M. Van Wyk de Vries et al. 10.1038/s41597-022-01446-8
- Towards a conceptualization of the hydrological processes behind changes of young water fraction with elevation: a focus on mountainous alpine catchments A. Gentile et al. 10.5194/hess-27-2301-2023
- Spatiotemporal Drivers of Hydrochemical Variability in a Tropical Glacierized Watershed in the Andes L. Saberi et al. 10.1029/2020WR028722
- Analysis of the groundwater flow system in a high-altitude headwater region under rapid climate warming: Lhasa River Basin, Tibetan Plateau J. Chen et al. 10.1016/j.ejrh.2021.100871
- Topographic control of glacier changes since the end of the Little Ice Age in the Sierra Nevada de Santa Marta mountains, Colombia J. López-Moreno et al. 10.1016/j.jsames.2020.102803
- Hydrological process controls on streamflow variability in a glacierized headwater basin C. Aubry‐Wake et al. 10.1002/hyp.14731
- Artificial Recharge by Means of Careo Channels Versus Natural Aquifer Recharge in a Semi-Arid, High-Mountain Watershed (Sierra Nevada, Spain) J. Jódar et al. 10.2139/ssrn.3983975
- Automated ablation stakes to constrain temperature-index melt models A. Wickert et al. 10.1017/aog.2024.21
- Análisis bibliométrico de la producción científica sobre fósforo y nitrógeno en ecosistemas acuáticos ecuatorianos en el periodo 2000-2019 indexado en SCOPUS D. Bernal Vera et al. 10.26423/rctu.v10i1.735
- Frontiers in páramo water resources research: A multidisciplinary assessment G. Mosquera et al. 10.1016/j.scitotenv.2023.164373
- Last Glacial Maximum Reconstructions of Rwenzori Mountain Glaciers A. Doughty et al. 10.1029/2022PA004527
- Toward catchment hydro‐biogeochemical theories L. Li et al. 10.1002/wat2.1495
- Watershed Reactive Transport L. Li 10.2138/rmg.2018.85.13
- Open-source Arduino-compatible data loggers designed for field research A. Wickert et al. 10.5194/hess-23-2065-2019
- The dual role of meltwater in buffering river runoff in the Yarlung Zangbo Basin, Tibetan Plateau Y. Feng et al. 10.1016/j.ejrh.2024.101857
- Glacio‐hydrological model calibration and evaluation M. van Tiel et al. 10.1002/wat2.1483
- Cryosphere–groundwater connectivity is a missing link in the mountain water cycle M. van Tiel et al. 10.1038/s44221-024-00277-8
- A review of groundwater in high mountain environments L. Somers & J. McKenzie 10.1002/wat2.1475
- Assessing the Contribution of Glacier Melt to Discharge in the Tropics: The Case of Study of the Antisana Glacier 12 in Ecuador L. Gualco et al. 10.3389/feart.2022.732635
- Subglacial Meltwater Recharge in the Dongkemadi River Basin, Yangtze River Source Region Q. He et al. 10.1111/gwat.13189
- Hydrological connections in a glaciated Andean catchment under permafrost conditions (33°S) S. Pereira et al. 10.1016/j.ejrh.2022.101311
1 citations as recorded by crossref.
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Short summary
The relationship among glacier melt, groundwater, and streamflow remains highly uncertain, especially in tropical glacierized watersheds in response to climate. We implemented a multi-method approach and found that melt contribution varies considerably and may drive streamflow variability at hourly to multi-year timescales, rather than buffer it, as commonly thought. Some of the melt contribution occurs through groundwater pathways, resulting in longer timescale interactions with streamflow.
The relationship among glacier melt, groundwater, and streamflow remains highly uncertain,...