Nature Communications (Jun 2022)
Annual cycle observations of aerosols capable of ice formation in central Arctic clouds
- Jessie M. Creamean,
- Kevin Barry,
- Thomas C. J. Hill,
- Carson Hume,
- Paul J. DeMott,
- Matthew D. Shupe,
- Sandro Dahlke,
- Sascha Willmes,
- Julia Schmale,
- Ivo Beck,
- Clara J. M. Hoppe,
- Allison Fong,
- Emelia Chamberlain,
- Jeff Bowman,
- Randall Scharien,
- Ola Persson
Affiliations
- Jessie M. Creamean
- Department of Atmospheric Science, Colorado State University
- Kevin Barry
- Department of Atmospheric Science, Colorado State University
- Thomas C. J. Hill
- Department of Atmospheric Science, Colorado State University
- Carson Hume
- Department of Atmospheric Science, Colorado State University
- Paul J. DeMott
- Department of Atmospheric Science, Colorado State University
- Matthew D. Shupe
- Cooperative Institute for Research in Environmental Sciences, University of Colorado
- Sandro Dahlke
- Climate Sciences Division, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung
- Sascha Willmes
- Environmental System Analysis and Modeling, Universität Trier
- Julia Schmale
- Extreme Environments Research Laboratory, École Polytechnique Fédérale de Lausanne
- Ivo Beck
- Extreme Environments Research Laboratory, École Polytechnique Fédérale de Lausanne
- Clara J. M. Hoppe
- Biosciences Division, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung
- Allison Fong
- Biosciences Division, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung
- Emelia Chamberlain
- Scripps Institution of Oceanography, University of California
- Jeff Bowman
- Scripps Institution of Oceanography, University of California
- Randall Scharien
- Department of Geography, University of Victoria
- Ola Persson
- Cooperative Institute for Research in Environmental Sciences, University of Colorado
- DOI
- https://doi.org/10.1038/s41467-022-31182-x
- Journal volume & issue
-
Vol. 13,
no. 1
pp. 1 – 12
Abstract
The Arctic is changing faster than anywhere else on Earth. Interactions between clouds and aerosols play a role in these changes. We report how the quantities and origins of aerosols that affect cloud ice formation change over a full sea ice cycle
