Cryoconite Holes

Cryoconite Holes is a supraglacial hydrological feature consisting of water-filled cylindrical depressions formed on glacier surfaces by the accumulation of cryoconite material, which absorbs solar radiation and enhances localized melt, thereby distinguishing it from other glacial surface features through its biogeochemically active, microclimate-influencing properties.

132

Publications

9.4K

Citations

363

Authors

175

Institutions

Publications per year

2017–2026

48

Authors

363

  1. AM
    Alexandre M. Anesio

    University of Bristol, United Kingdom

    30 publications · 3.3K citations

    28

    h-index

  2. MT
    Martyn Tranter

    University of Bristol, United Kingdom

    27 publications · 2.4K citations

    24

    h-index

  3. BS
    Birgit Sattler

    Universität Innsbruck, Austria

    13 publications · 2K citations

    13

    h-index

  4. AG
    Andrew G. Fountain

    Portland State University, United States

    14 publications · 1.4K citations

    13

    h-index

  5. KZ
    Krzysztof Zawierucha

    Adam Mickiewicz University in Poznań, Poland

    13 publications · 541 citations

    12

    h-index

1–5 of 363

Venues

  1. FEMS Microbiology Ecology

    10 publications · 718 citations

    10

    h-index

  2. Annals of Glaciology

    10 publications · 563 citations

    10

    h-index

  3. Frontiers in Microbiology

    9 publications · 477 citations

    9

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 8 publications · 793 citations

    8

    h-index

  5. Arctic Antarctic and Alpine Research

    6 publications · 751 citations

    6

    h-index

1–5