ArticleProceedings of the National Academy of Sciences of the United States of America2025
Abrupt transformation of west Greenland lakes following compound climate extremes associated with atmospheric rivers.
Article in Proceedings of the National Academy of Sciences of the United States of America, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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Who cites it
5 citing papers in PubMed.
- Glacier retreat shapes organic nutrient availability across lake succession.Science advances · 2026Article
- Freshwater biodiversity in a rapidly changing Arctic: An expert horizon scan of key research questions.Ambio · 2026Review
- Mercury mobilization and export from the Greenland Ice Sheet using an ice-to-ocean approach.Communications earth & environment · 2026Article
- Contrasting Life History Characteristics Between Riverine and Lacustrine Anadromous Arctic Char (Ecology and evolution · 2025Article
- Permafrost and Freshwater Systems in the Arctic as Tipping Elements of the Climate System.Surveys in geophysics · 2025Review
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Authors and funding
10 authors.
Funding
Abstract
Arctic ecosystems are affected by accelerated warming as well as the intensification of the hydrologic cycle, yet understanding of the impacts of compound climate extremes (e.g., simultaneous extreme heat and rainfall) remains limited, despite their high potential to alter ecosystems. Here, we show that the aquatic ecosystems in historically arid west Greenland have undergone an ecological transformation after a series of atmospheric rivers that simultaneously produced record heat and rainfall hit the region in autumn 2022. We analyzed a unique, long-term lake dataset and found that compound climate extremes pushed Arctic lakes across a tipping point. As terrestrial-aquatic linkages were strengthened, lakes synchronously transformed from "blue" lakes with high transparency and low pelagic primary production to "brown" in less than a year, owing to a large influx of dissolved organic material and metals, with iron concentrations increasing by more than two orders of magnitude. The browning of lake waters reduced light penetration by 50% across lakes. The resulting light limitation altered plankton distributions and community structure, including a major reduction in prokaryotic diversity and an increase in algal groups capable of metabolizing organic carbon sources. As a result, lakes shifted from being summer carbon sinks to sources, with a >350% increase in carbon dioxide flux from lakes to the atmosphere. The remarkably rapid, coherent transformation of these Arctic ecosystems underscores the synergistic and unpredictable impacts of compound extreme events and the importance of their seasonal timing, especially in regions with negative moisture balance.
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