Planetary Ices

Planetary Ices is a scientific construct referring to the diverse class of volatile compounds, predominantly including water, ammonia, and methane, that condense into solid phases under the low-temperature conditions prevalent on or within planetary bodies, thereby distinguishing it from refractory materials and atmospheric gases in the study of planetary composition and evolution.

681

Publications

46.7K

Citations

2.1K

Authors

661

Institutions

Publications per year

2017–2026

199

Authors

2.1K

  1. RI
    Ralf I. Kaiser

    University of Hawaiʻi at Mānoa, United States

    27 publications · 1.7K citations

    22

    h-index

  2. EF
    E. F. van Dishoeck

    Leiden University, Netherlands

    22 publications · 2.8K citations

    21

    h-index

  3. DP
    D. P. Cruikshank

    Ames Research Center, United States

    25 publications · 2K citations

    19

    h-index

  4. BS
    B. Schmitt

    Centre National de la Recherche Scientifique, France

    18 publications · 1.7K citations

    18

    h-index

  5. WM
    W. M. Grundy

    Lowell Observatory, United States

    21 publications · 1K citations

    17

    h-index

1–5 of 2.1K

Venues

  1. The Astrophysical Journal

    ApJ · 101 publications · 10.2K citations

    52

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 60 publications · 5.6K citations

    40

    h-index

  3. Icarus

    74 publications · 4.9K citations

    39

    h-index

  4. Astronomy and Astrophysics

    58 publications · 3.6K citations

    36

    h-index

  5. Science

    32 publications · 6.2K citations

    29

    h-index

1–5