Stratospheric Cooling

Stratospheric Cooling is a climatological phenomenon characterized by the long-term decrease in temperature within the stratosphere, primarily distinguished from tropospheric warming by its association with increased radiative heat loss due to rising concentrations of greenhouse gases, particularly carbon dioxide, under conditions of reduced solar absorption and stratospheric ozone depletion.

558

Publications

42.8K

Citations

1.5K

Authors

454

Institutions

Publications per year

2017–2026

116

Authors

1.5K

  1. SS
    Susan Solomon

    National Oceanic and Atmospheric Administration, United States

    18 publications · 2.7K citations

    18

    h-index

  2. WJ
    William J. Randel

    NSF National Center for Atmospheric Research, United States

    18 publications · 2.7K citations

    17

    h-index

  3. KP
    Keith P. Shine

    University of Reading, United Kingdom

    15 publications · 2.4K citations

    15

    h-index

  4. LM
    Lorenzo M. Polvani

    Columbia University, United States

    16 publications · 1.5K citations

    15

    h-index

  5. QF
    Qiang Fu

    University of Washington, United States

    16 publications · 1.8K citations

    15

    h-index

1–5 of 1.5K

Venues

  1. Geophysical Research Letters

    124 publications · 7.8K citations

    48

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 66 publications · 6.2K citations

    43

    h-index

  3. Journal of Climate

    60 publications · 6.2K citations

    37

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 31 publications · 1.7K citations

    26

    h-index

  5. Journal of the Atmospheric Sciences

    35 publications · 2.8K citations

    24

    h-index

1–5