ArticleGeophysical research letters2022
Contribution of Atmospheric Rivers to Antarctic Precipitation.
Article in Geophysical research letters, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
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Who cites it
7 citing papers in PubMed, 70 citations in OpenAlex.
- Article
- Projected and historical amplification of moisture fluxes towards Antarctica by synoptic eddies.NPJ climate and atmospheric science · 2026Article
- Emerging threats to Antarctic conservation.Nature ecology & evolution · 2025Article
- Rising atmospheric moisture escalates the future impact of atmospheric rivers in the Antarctic climate system.Communications earth & environment · 2025Article
- Model performance and surface impacts of atmospheric river events in Antarctica.Discover atmosphere · 2025Article
- Sea level rise from West Antarctic mass loss significantly modified by large snowfall anomalies.Nature communications · 2023Article
- Contribution of Atmospheric Rivers to Antarctic Precipitation.Geophysical research letters · 2022Article
Corrections and comments
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Authors and funding
4 authors at 3 institutions in 2 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Atmospheric rivers (ARs) are efficient mechanisms for transporting atmospheric moisture from low latitudes to the Antarctic Ice Sheet (AIS). While AR events occur infrequently, they can lead to extreme precipitation and surface melt events on the AIS. Here we estimate the contribution of ARs to total Antarctic precipitation, by combining precipitation from atmospheric reanalyses and a polar-specific AR detection algorithm. We show that ARs contribute substantially to Antarctic precipitation, especially in East Antarctica at elevations below 3,000 m. ARs contribute substantially to year-to-year variability in Antarctic precipitation. Our results highlight that ARs are an important component for understanding present and future Antarctic mass balance trends and variability.
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Registered trials
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