A 25-month database of stratus cloud properties generated from ground-based measurements at the Atmospheric Radiation Measurement Southern Great Plains Site

Journal Article · Sun Feb 27 04:00:00 EST 2000 · Journal of Geophysical Research

DOI:https://doi.org/10.1029/1999JD901159· OSTI ID:20216298

Dong, Xiquan ^[1]; Minnis, Patrick ^[2]; Ackerman, Thomas P ^[3]; Clothiaux, Eugene E ^[4]; Mace, Gerald G ^[1]; Long, Charles N ^[4]; Liljegren, James C ^[5]

---

1. Meteorology Department, University of Utah, Salt Lake City (United States)
2. NASA Langley Research Center, Hampton, Virginia (United States)
3. Pacific Northwest National Laboratory, DOE, Richland, Washington (United States)
4. Department of Meteorology, Pennsylvania State University, University Park (United States)
5. Ames Laboratory, DOE, Ames, Iowa (United States)

A 25-month database of the macrophysical, microphysical, and radiative properties of isolated and overcast low-level stratus clouds has been generated using a newly developed parameterization and surface measurements from the Atmospheric Radiation Measurement central facility in Oklahoma. The database (5-min resolution) includes two parts: measurements and retrievals. The former consist of cloud base and top heights, layer-mean temperature, cloud liquid water path, and solar transmission ratio measured by a ground-based lidar/ceilometer and radar pair, radiosondes, a microwave radiometer, and a standard Eppley precision spectral pyranometer, respectively. The retrievals include the cloud-droplet effective radius and number concentration and broadband shortwave optical depth and cloud and top-of-atmosphere albedos. Stratus without any overlying mid or high-level clouds occurred most frequently during winter and least often during summer. Mean cloud-layer altitudes and geometric thicknesses were higher and greater, respectively, in summer than in winter. Both quantities are positively correlated with the cloud-layer mean temperature. Mean cloud-droplet effective radii range from 8.1 {mu}m in winter to 9.7 {mu}m during summer, while cloud-droplet number concentrations during winter are nearly twice those in summer. Since cloud liquid water paths are almost the same in both seasons, cloud optical depth is higher during the winter, leading to greater cloud albedos and lower cloud transmittances. (c) 2000 American Geophysical Union.

• OSTI ID: 20216298
• Journal Information: Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: D4 Vol. 105; ISSN JGREA2; ISSN 0148-0227
• Country of Publication: United States
• Language: English

Related Subjects

54 ENVIRONMENTAL SCIENCES
CLOUDS
DATA ANALYSIS
DROPLETS
EXPERIMENTAL DATA
HUMIDITY
PHYSICAL PROPERTIES
RADIATION MONITORING
REMOTE SENSING
STRATOSPHERE
TIME-SERIES ANALYSIS