Arctic Mixed-Phase Stratiform Cloud Properties from Multiple Years of Surface-Based Measurements at Two High-Latitude Locations

被引:105
作者
de Boer, Gijs [1 ]
Eloranta, Edwin W. [1 ]
Shupe, Matthew D. [2 ,3 ]
机构
[1] Univ Wisconsin, Dept Atmospher & Ocean Sci, Madison, WI 53706 USA
[2] Univ Colorado, NOAA, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[3] NOAA, Earth Syst Res Lab, Boulder, CO USA
关键词
MODEL SIMULATIONS; WATER-CONTENT; SHEBA; RETRIEVALS; RADAR; MICROPHYSICS; SENSORS; OCEAN; LIDAR;
D O I
10.1175/2009JAS3029.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Macro- and microphysical properties of single-layer stratiform mixed-phase clouds are derived from multiple years of lidar, radar, and radiosonde observations. Measurements were made as part of the Mixed-Phase Arctic Clouds Experiment (MPACE) and the Study of Environmental Arctic Change ( SEARCH) in Barrow, Alaska, and Eureka, Nunavut, Canada, respectively. Single-layer mixed-phase clouds occurred between 4% and 26% of the total time observed, varying with season and location. They had mean cloud-base heights between similar to 700 and 2100 m and thicknesses between similar to 200 and 700 m. Seasonal mean cloud optical depths ranged from 2.2 up. The clouds existed at temperatures of similar to 242-271 K and occurred under different wind conditions, depending on season. Utilizing retrievals from a combination of lidar, radar, and microwave radiometer, mean cloud microphysical properties were derived, with mean liquid effective diameters estimated from 16 to 49 mu m, mean liquid number densities on the order of 10(4)-10(5) L-1, and mean water contents estimated between 0.07 and 0.28 g m(-3). Ice precipitation was shown to have mean ice effective diameters of 50-125 mu m, mean ice number densities on the order of 10 L-1, and mean water contents estimated between 0.012 and 0.031 g m(-3). Mean cloud liquid water paths ranged from 25 to 100 g m(-2). All results are compared to previous studies, and potential retrieval errors are discussed. Additionally, seasonal variation in macro- and microphysical properties was highlighted. Finally, fraction of liquid water to ice mass was shown to decrease with decreasing temperature.
引用
收藏
页码:2874 / 2887
页数:14
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