Impact of large‐scale dynamics on the microphysical properties of midlatitude cirrus

Journal of Geophysical Research D: Atmospheres - Tập 119 Số 7 - Trang 3976-3996 - 2014
Andreas Mühlbauer1, Thomas P. Ackerman2,1, D. Chand3, Glenn S. Diskin4, S. M. Evans2, R. Paul Lawson5, Roger Marchand2
1Joint Institute for the Study of the Atmosphere and Ocean University of Washington Seattle Washington USA
2Department of Atmospheric Sciences University of Washington Washington USA
3Pacific Northwest National Laboratory , Richland, Washington, USA
4NASA, Langley Research Center, Hampton, Virginia, USA
5Spec Inc. Boulder Colorado USA

Tóm tắt

In situ microphysical observations of midlatitude cirrus collected during the Department of Energy Small Particles in Cirrus (SPARTICUS) field campaign are combined with an atmospheric state classification for the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site to understand statistical relationships between cirrus microphysics and the large‐scale meteorology. The atmospheric state classification is informed about the large‐scale meteorology and state of cloudiness at the ARM SGP site by combining ECMWF ERA‐Interim reanalysis data with 14 years of continuous observations from the millimeter‐wavelength cloud radar. Almost half of the cirrus cloud occurrences in the vicinity of the ARM SGP site during SPARTICUS can be explained by three distinct synoptic conditions, namely, upper level ridges, midlatitude cyclones with frontal systems, and subtropical flows. Probability density functions (PDFs) of cirrus microphysical properties such as particle size distributions (PSDs), ice number concentrations, and ice water content (IWC) are examined and exhibit striking differences among the different synoptic regimes. Generally, narrower PSDs with lower IWC but higher ice number concentrations are found in cirrus sampled in upper level ridges, whereas cirrus sampled in subtropical flows, fronts, and aged anvils show broader PSDs with considerably lower ice number concentrations but higher IWC. Despite striking contrasts in the cirrus microphysics for different large‐scale environments, the PDFs of vertical velocity are not different, suggesting that vertical velocity PDFs are a poor predictor for explaining the microphysical variability in cirrus. Instead, cirrus microphysical contrasts may be driven by differences in ice supersaturations or aerosols.

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Journal of Geophysical Research D: Atmospheres

Tập 119 Số 7

3976-3996

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