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Cloud climatology at the Southern Great Plains and the layer structure, drizzle, and atmospheric modes of continental stratus

2007; American Geophysical Union; Volume: 112; Issue: D9 Linguagem: Inglês

10.1029/2006jd007307

2156-2202

Pavlos Kollias, George Tselioudis, Bruce A. Albrecht,

Atmospheric Ozone and Climate

Long‐term (6.5 years) cloud observations from the Atmospheric Radiation Measurements (ARM) program Southern Great Plains (SGP) climate research facility in Oklahoma are used to develop detailed cloud climatology. Clouds are classified with respect to their altitude (low, middle, and high), vertical development, and the presence of multilayer clouds. Single‐layered cirrus, middle or low clouds were observed a total of 23% of the time the MilliMeter Cloud Radar (MMCR) was operating, and multilayer clouds were observed 20.5% of the time. Boundary layer clouds exhibit the strongest seasonal variability because of continental stratus associated with midlatitude frontal systems. Cirrus clouds are the most frequently observed cloud type and exhibit strong seasonal variability in cloud base height (higher cloud base during the summer months) and relatively constant cloud fraction. The majority of middle‐level clouds are shallow with vertical extent less than 1 km. No strong seasonal cycle in the fractional coverage of multilayer clouds is observed. Continental stratus clouds exhibit strong seasonal variability with maximum occurrence during the cold seasons. Nondrizzling stratus clouds exhibit a bimodal seasonal variability with maximum occurrences in the fall and spring, while drizzling stratus occur most frequently in the winter. Thermodynamic and dynamic variables from soundings and the European Centre for Medium‐Range Weather Forecasts Model (ECMWF) analyses at the SGP site illustrate an interesting coupling between strong large‐scale forcing and the formation of single‐layered (no other cloud layer is present) continental stratus clouds. Single‐layered stratus clouds (drizzling and nondrizzling) exhibit a strong correlation with positive ω at 500 mbar and strong northerly flow.