HR: 1330h
AN: A32B-0144    [PDF]
TI: Simulation of a Stratospheric Intrusion Using the Lagrangian Particle Transport Model FLEXPART, Combined With Observed Surface Impacts Over the United States in Early May 1999
AU: * Reid, S J
EM: sreid@nsf.gov
AF: University of Colorado, Cooperative Institute for Research in Environmental Sciences, Boulder, CO 80309 United States
AU: * Reid, S J
EM: sreid@nsf.gov
AF: National Science Foundation, 4201 Wilson Boulevard, Arlington, VA 22230 United States
AU: Cooper, O R
EM: ocooper@al.noaa.gov
AF: University of Colorado, Cooperative Institute for Research in Environmental Sciences, Boulder, CO 80309 United States
AU: Cooper, O R
EM: ocooper@al.noaa.gov
AF: NOAA Aeronomy Laboratory, 325 Broadway, Boulder, CO 80305 United States
AU: Stohl, A
AF: NOAA Aeronomy Laboratory, 325 Broadway, Boulder, CO 80305 United States
AU: Stohl, A
AF: Technical University of Munich, Am Hochanger 13, D-85354 Freising-Weihenstephan, Munich, 85354 Germany
AU: Langford, A O
EM: langford@al.noaa.gov
AF: NOAA Aeronomy Laboratory, 325 Broadway, Boulder, CO 80305 United States
AU: Wimmers, A
EM: wimmers@ssec.wisc.edu
AF: University of Wisconsin - Madison, Cooperative Institute for Meteorological Satellite Studies, Space Science and Engineering Center 1150 University Avenue, Madison, WI 53706 United States
AU: Trainer, M
EM: mtrainer@al.noaa.gov
AF: NOAA Aeronomy Laboratory, 325 Broadway, Boulder, CO 80305 United States
AB: This paper reports observations and a model simulation of an exceptionally-strong tropopause fold in early May 1999 which impacted the surface of Colorado and the south-central United States. The model simulation was performed using a special version of the Lagrangian particle dispersion model FLEXPART, which revealed the evolution of the fold eastward across the United States during the subsequent week. This intrusion was recorded by the NOAA Fritz Peak (40N, 105W) DIAL ozone lidar on May 6. Its subsequent path has been inferred from high ozone values in the AIRS data network, and using altered water vapor (AWV) imagery, a linear modification of the GOES water vapor channel which depicts specific humidity in the mid- and upper troposphere.
DE: 0300 ATMOSPHERIC COMPOSITION AND STRUCTURE
DE: 0325 Evolution of the atmosphere
DE: 0368 Troposphere--constituent transport and chemistry
SC: Atmospheric Sciences [A]
MN: 2003 Fall Meeting