Articles | Volume 18, issue 24
https://doi.org/10.5194/acp-18-18023-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-18023-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Marine and terrestrial influences on ice nucleating particles during continuous springtime measurements in an Arctic oilfield location
Jessie M. Creamean
CORRESPONDING AUTHOR
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, 80309, USA
Physical Sciences Division, National Oceanic and Atmospheric Administration, Boulder, CO, 80305, USA
now at: Department of Atmospheric Science, Colorado State University, Fort Collins, CO, 80521, USA
Rachel M. Kirpes
Department of Chemistry, University of Michigan, Ann Arbor, MI, 48109, USA
Kerri A. Pratt
Department of Chemistry, University of Michigan, Ann Arbor, MI, 48109, USA
Nicholas J. Spada
Air Quality Research Center, University of California, Davis, CA, 95616, USA
Maximilian Maahn
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, 80309, USA
Physical Sciences Division, National Oceanic and Atmospheric Administration, Boulder, CO, 80305, USA
Gijs de Boer
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, 80309, USA
Physical Sciences Division, National Oceanic and Atmospheric Administration, Boulder, CO, 80305, USA
Russell C. Schnell
Global Monitoring Division, National Oceanic and Atmospheric Administration, Boulder, CO, 80305, USA
Swarup China
Environmental and Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, WA, 99352, USA
Data sets
SplitR R. Iannone https://github.com/rich-iannone/SplitR
Short summary
Warm-temperature ice nucleating particles (INPs) were observed during a springtime transition period of the melting of frozen surfaces in Northern Alaska. Such INPs were likely biological and from marine and terrestrial (tundra) sources. Influxes of these efficient INPs may have important implications for Arctic cloud ice formation and, consequently, the surface energy budget.
Warm-temperature ice nucleating particles (INPs) were observed during a springtime transition...
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