Evidence for Changes in Arctic Cloud Phase Due to Long-Range Pollution Transport

Q. Coopman*, J. Riedi, D. P. Finch, T. J. Garrett

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

Reduced precipitation rates allow pollution within air parcels from midlatitudes to reach the Arctic without being scavenged. We use satellite and tracer transport model data sets to evaluate the degree of supercooling required for 50% of a chosen ensemble of low-level clouds to be in the ice phase for a given meteorological regime. Our results suggest that smaller cloud droplet effective radii are related to higher required amounts of supercooling but that, overall, pollution plumes from fossil fuel combustion lower the degree of supercooling that is required for freezing by approximately 4 °C. The relationship between anthropogenic plumes and the freezing transition temperature from liquid to ice remains to be explained.

Original languageEnglish
Pages (from-to)10,709-10,718
JournalGeophysical Research Letters
Volume45
Issue number19
Early online date21 Sep 2018
DOIs
Publication statusPublished - 16 Oct 2018

Keywords

  • aerosol-cloud interaction
  • Arctic
  • clouds
  • ice nucleation
  • space-based measurements

Fingerprint

Dive into the research topics of 'Evidence for Changes in Arctic Cloud Phase Due to Long-Range Pollution Transport'. Together they form a unique fingerprint.

Cite this