Environmental Chemical Processes Laboratory (ECPL), Department of Chemistry, University of Crete, Heraklion, Greece
Center for the Study of Air Quality and Climate Change (C-STACC), Institute of Chemical Engineering Sciences (ICE-HT), Foundation for Research and Technology – Hellas (FORTH), Patras, Greece
now at: Barcelona Supercomputing Center (BSC), Barcelona, Spain
Center for the Study of Air Quality and Climate Change (C-STACC), Institute of Chemical Engineering Sciences (ICE-HT), Foundation for Research and Technology – Hellas (FORTH), Patras, Greece
Laboratory of Atmospheric Processes and their Impacts (LAPI), School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Federale de Lausanne, Lausanne, Switzerland
Environmental Chemical Processes Laboratory (ECPL), Department of Chemistry, University of Crete, Heraklion, Greece
Center for the Study of Air Quality and Climate Change (C-STACC), Institute of Chemical Engineering Sciences (ICE-HT), Foundation for Research and Technology – Hellas (FORTH), Patras, Greece
Laboratory for Modelling and Observation of the Earth System (LAMOS), Institute of Environmental Physics (IUP), University of Bremen, Bremen, Germany
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Total article views: 2,988 (including HTML, PDF, and XML)
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2,549
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2,988
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Supplement: 165
BibTeX: 57
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846
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291
1,375
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Supplement: 72
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Viewed (geographical distribution)
Total article views: 4,363 (including HTML, PDF, and XML)
Thereof 4,321 with geography defined
and 42 with unknown origin.
Total article views: 2,988 (including HTML, PDF, and XML)
Thereof 2,945 with geography defined
and 43 with unknown origin.
Total article views: 1,375 (including HTML, PDF, and XML)
Thereof 1,375 with geography defined
and 0 with unknown origin.
We show distinct seasonal and geographical patterns in the contributions of mineral dust, marine aerosol, and terrestrial biological particles to ice-nucleating particle (INP) concentrations that lead to atmospheric ice formation, a major source of uncertainty in climate projections. Bioaerosols are the major source of INPs at high temperatures, while mineral dust influences the global INP population at lower temperatures. These particles can satisfactorily reproduce INPs in a climate model.
We show distinct seasonal and geographical patterns in the contributions of mineral dust, marine...
