Articles | Volume 19, issue 8
https://doi.org/10.5194/tc-19-3139-2025
https://doi.org/10.5194/tc-19-3139-2025
Research article
 | 
20 Aug 2025
Research article |  | 20 Aug 2025

Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheet

Laura Carrea, Christopher J. Merchant, Richard I. Woolway, and Niall McCarroll

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Cited articles

Abrams, M., Crippen, R., and Fujisada, H.: ASTER Global Digital Elevation Model (GDEM) and ASTER Global Water Body Dataset (ASTWBD), Remote Sens.-Basel, 12, 1156, https://doi.org/10.3390/rs12071156, 2020. a, b
Anderson, N., Bennike, O., Christoffersen, K., Jeppesen, E., Markager, S., Miller, G., and Renberg, I.: Limnological and palaeolimnological studies of lakes in south-western Greenland, Geology of Greenland Survey Bulletin, 183, 68–74, https://doi.org/10.34194/ggub.v183.5207, 1999. a
Anderson, N., Harriman, R., Ryves, D., and Patrick, S.: Dominant factors controlling variability in the ionic composition of West Greenland lakes, Arct. Antarct. Alp. Res., 33, 418–425, https://doi.org/10.1080/15230430.2001.12003450, 2001. a, b
Anderson, N., Saros, J., Bullard, J., Cahoon, S., McGowan, S., Bagshaw, E., Barry, C., Bindler, R., Burpee, B., Carrivick, J., Fowler, R., Fox, A., Fritz, S., Giles, M., Hamerlick, L., Ingeman-Nielsen, T., Law, A., Mernild, S., Northington, R., Osburn, C., Pla-Rabès, S., Post, E., Telling, J., Stroud, D., Whiteford, E., Yallop, M., and Yde, J.: The Arctic in the twenty-first century: changing biogeochemical linkages across a paraglacial landscape of Greenland, Bioscience, 67, 118–133, https://doi.org/10.1093/biosci/biw158, 2017. a
Benn, D., Warren, C., and Mottram, R.: Calving processes and the dynamics of calving glaciers, Earth-Sci. Rev., 82, 143–179, https://doi.org/10.1016/j.earscirev.2007.02.002, 2007. a
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Short summary
Lakes in Greenland serve as a crucial sentinel of climate change. Satellites can be used to monitor water temperature and ice. Using 28 years of measurements from satellites, we conclude that lakes are overall warmer than previously thought. The lakes connected to the ice sheet are cooler than the rest because of cold glacial meltwater inflow. Changes in water temperature can impact light availability, nutrient cycling, and oxygen levels that are crucial for the lake ecosystem and have an influence on the ice sheet.
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