The common occurrence of highly supercooled drizzle and rain near the coastal regions of the western United States. Issue 17 (5th September 2013)

• Record Type: Journal Article
• Authors: Rosenfeld, Daniel; Chemke, Rei; DeMott, Paul; Sullivan, Ryan C.; Rasmussen, Roy; McDonough, Frank; Comstock, Jennifer; Schmid, Beat; Tomlinson, Jason; Jonsson, Haflidi; Suski, Kaitlyn; Cazorla, Alberto; Prather, Kimberly
• Is Part Of: Journal of geophysical research. Volume 118:Issue 17(2013)
• Page Start: 9819
• Page End: 9833
• Publication Date: 2013-09-05
• Subjects: Supercooled rain -- Supercooled drizzle -- Cloud aerosol interactions; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/jgrd.50529
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: [1] Highly supercooled rain and drizzle from cloud tops at −12 to −21°C down to the 0° isotherm was documented by aircraft observations in clouds over a wide range of meteorological situations under relatively pristine marine aerosol conditions. The Gulfstream‐1 aircraft during the CalWater campaign in February and early March 2011 measured clouds over the coastal waters of northern California, orographically triggered convective clouds over the foothills of the Sierra Nevada, and orographic layer clouds over Yosemite National Park. Supercooled drizzle in layer clouds near Juneau, Alaska, was measured by the Wyoming King Air as part of a FAA project to study aircraft icing in this region. Low concentrations of cloud condensation nuclei (CCN) were commonly observed in all of these clouds, allowing for the formation of clouds with small concentrations of mostly large drops that coalesced into supercooled drizzle and raindrops. Another common observation was the absence of ice nuclei (IN) and/or ice crystals in measurable concentrations, associated with persistent supercooled drizzle and rain. Average ice crystal concentrations were 0.007 l −1 at the top of convective clouds at −12°C and 0.03 l −1 in the case of layer clouds at −21°C. In combination, these two conditions of low concentrations of CCN and very few IN provide ideal conditions for the formation of highly supercooled drizzle and rain. These results help explain the anomalously high incidences of aircraft icing at cold temperatures in U.S. west coast clouds and highlight the need to include aerosol effects when simulating aircraft icing with cloud models. Key Points: Persistent highly supercooled rain was observed in clouds down to ‐21˚C It occurred in a wide range of convective, orographic and layer arctic clouds The likely cause was dearth of CCN and IN aerosols in pristine marine air masses