The COMBLE Campaign: A Study of Marine Boundary Layer Clouds in Arctic Cold-Air Outbreaks

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MARC

Fältnamn	Indikatorer	Metadata
000		04563naa a2200745 4500
001		oai:DiVA.org:su-212224
003		SwePub
008		221205s2022 \| \|\|\|\|\|\|\|\|\|\|\|000 \|\|eng\|
024	7	a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-2122242 URI
024	7	a https://doi.org/10.1175/BAMS-D-21-0044.12 DOI
040		a (SwePub)su
041		a engb eng
042		9 SwePub
072	7	a ref2 swepub-contenttype
072	7	a art2 swepub-publicationtype
100	1	a Geerts, Bart4 aut
245	1 0	a The COMBLE Campaign :b A Study of Marine Boundary Layer Clouds in Arctic Cold-Air Outbreaks
264	1	c 2022
338		a print2 rdacarrier
520		a One of the most intense air mass transformations on Earth happens when cold air flows from frozen surfaces to much warmer open water in cold-air outbreaks (CAOs), a process captured beautifully in satellite imagery. Despite the ubiquity of the CAO cloud regime over high-latitude oceans, we have a rather poor understanding of its properties, its role in energy and water cycles, and its treatment in weather and climate models. The Cold-Air Outbreaks in the Marine Boundary Layer Experiment (COMBLE) was conducted to better understand this regime and its representation in models. COMBLE aimed to examine the relations between surface fluxes, boundary layer structure, aerosol, cloud, and precipitation properties, and mesoscale circulations in marine CAOs. Processes affecting these properties largely fall in a range of scales where boundary layer processes, convection, and precipitation are tightly coupled, which makes accurate representation of the CAO cloud regime in numerical weather prediction and global climate models most challenging. COMBLE deployed an Atmospheric Radiation Measurement Mobile Facility at a coastal site in northern Scandinavia (69°N), with additional instruments on Bear Island (75°N), from December 2019 to May 2020. CAO conditions were experienced 19% (21%) of the time at the main site (on Bear Island). A comprehensive suite of continuous in situ and remote sensing observations of atmospheric conditions, clouds, precipitation, and aerosol were collected. Because of the clouds’ well-defined origin, their shallow depth, and the broad range of observed temperature and aerosol concentrations, the COMBLE dataset provides a powerful modeling testbed for improving the representation of mixed-phase cloud processes in large-eddy simulations and large-scale models.
650	7	a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650	7	a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653		a Arctic
653		a Cold air surges
653		a Marine boundary layer
653		a Cloud water/phase
653		a Cloud resolving models
653		a Aerosol-cloud interaction
700	1	a Giangrande, Scott E.4 aut
700	1	a McFarquhar, Greg M.4 aut
700	1	a Xue, Lulin4 aut
700	1	a Abel, Steven J.4 aut
700	1	a Comstock, Jennifer M.4 aut
700	1	a Crewell, Susanne4 aut
700	1	a DeMott, Paul J.4 aut
700	1	a Ebell, Kerstin4 aut
700	1	a Field, Paul4 aut
700	1	a Hill, Thomas C. J.4 aut
700	1	a Hunzinger, Alexis4 aut
700	1	a Jensen, Michael P.4 aut
700	1	a Johnson, Karen L.4 aut
700	1	a Juliano, Timothy W.4 aut
700	1	a Kollias, Pavlos4 aut
700	1	a Kosovic, Branko4 aut
700	1	a Lackner, Christian4 aut
700	1	a Luke, Ed4 aut
700	1	a Lüpkes, Christof4 aut
700	1	a Matthews, Alyssa A.4 aut
700	1	a Neggers, Roel4 aut
700	1	a Ovchinnikov, Mikhail4 aut
700	1	a Powers, Heath4 aut
700	1	a Shupe, Matthew D.4 aut
700	1	a Spengler, Thomas4 aut
700	1	a Swanson, Benjamin E.4 aut
700	1	a Tjernström, Michael,d 1955-u Stockholms universitet,Meteorologiska institutionen (MISU)4 aut0 (Swepub:su)tjern
700	1	a Theisen, Adam K.4 aut
700	1	a Wales, Nathan A.4 aut
700	1	a Wang, Yonggang4 aut
700	1	a Wendisch, Manfred4 aut
700	1	a Wu, Peng4 aut
710	2	a Stockholms universitetb Meteorologiska institutionen (MISU)4 org
773	0	t Bulletin of The American Meteorological Society - (BAMS)g 103:5, s. E1371-E1389q 103:5<E1371-E1389x 0003-0007x 1520-0477
856	4	u https://doi.org/10.1175/BAMS-D-21-0044.1y Fulltext
856	4 8	u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-212224
856	4 8	u https://doi.org/10.1175/BAMS-D-21-0044.1

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