HR: 14:10h
AN: A33F-03 [Abstracts]
TI: Cirrus Radiative Flux Study at SGP Using Radar/Lidar/AERI Derived Cloud Properties
AU: * Borg, L A
EM: lori.borg@ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AU: Tobin, D
EM: dave.tobin@ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AU: Turner, D D
EM: dturner@ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AU: Holz, R E
EM: reholz@ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AU: DeSlover, D H
EM: deslover@ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AU: Revercomb, H E
EM: hank.revercomb@ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AU: Knuteson, R O
EM: bob.knuteson@ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AU: Moy, L
EM: leslie.moy@ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AU: Eloranta, E
EM: eloranta@lidar.ssec.wisc.edu
AF: Space Science and Engineering Center
University of Wisconsin, Madison, 1225 West Dayton Street, Madison, WI 53706, United States
AB:
The role that clouds play in the Earth's radiative balance represents a major source of uncertainty in
understanding climate and climate change. A large part of this uncertainty lies in the modeling of the cloud, which
requires assumptions and simplifications of the cloud morphology. In this study uniform cirrus cloud events at the
Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site are investigated using various
data sources (including 3 mm and 8 mm radar, lidar, AERI, and combinations thereof) to derive cloud
microphysical and optical properties. The results of a flux closure study are presented where observed top-of-
atmosphere and surface flux measurements are compared with computed fluxes. Computed heating rates are
compared with the ARM Broadband Heating Rate Profile (BBHRP). Results indicate that combinations of
measurement types are needed to accurately characterize thin cirrus. Radar alone can miss significant upper
level cirrus impacting the computed fluxes and heating rates. Vertical distribution of cirrus extinction and particle
size is significantly less important than the total optical depth in computing heating rates.
DE: 0300 ATMOSPHERIC COMPOSITION AND STRUCTURE
DE: 0321 Cloud/radiation interaction
DE: 0360 Radiation: transmission and scattering
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting