HR: 09:15h
AN: A21B-06 [PDF]
TI: Evaluation of pollutant outflow and CO sources during TRACE-P using model-calculated, aircraft-based,
and MOPITT-derived CO concentrations
AU: * Allen, D J
EM: allen@atmos.umd.edu
AF: Department of Meteorology, University of Maryland
3417 Computer and Space Science Building, College Park, MD 20742-2425 United States
AU: Pickering, K
EM: pickerin@atmos.umd.edu
AF: Department of Meteorology, University of Maryland
3417 Computer and Space Science Building, College Park, MD 20742-2425 United States
AU: Fox-Rabinovitz, M
EM: foxrab@atmos.umd.edu
AF: Department of Meteorology, University of Maryland
3417 Computer and Space Science Building, College Park, MD 20742-2425 United States
AB:
Outflow of CO from Asia during March 2001 was evaluated using data from the TRACE-P mission and the MOPITT instrument in
conjunction with model-calculated CO from the University of Maryland CTM. Comparison of model-calculated CO with aircraft
measurements was encouraging. Temporal and spatial variations in CO were well captured (mean correlation coefficient of
0.78); however, model-calculated mixing ratios were lower than observed especially below 850 hPa where negative biases of ~60
ppbv were seen. "Non-standard" aerosol effects explain a portion of the negative biases. Below 300 hPa, biases between
model-calculated and observed CO distributions were reduced by 6-9 ppbv when OH concentrations were adjusted to take into the
account the effect of aerosols on photolysis- and reaction-rates. Inverse modeling of CO was used to estimate the
corrections to Asian CO emissions suggested by the combination of model simulations and aircraft measurements in the TRACE-P
region. Resulting Asian correction factors were 1.70 $\pm$ 0.36 for fossil fuel/biofuel (ff/bf) emissions and 1.00 $\pm$
0.30 for bb emissions. Resulting ff/bf emissions were 29.6 $\pm$ 6.2 Tg for March 2001 (323 $\pm$ 67 Tg for an entire year).
Resulting bb emissions for March 2001 were 18.1 $\pm$ 5.4 Tg. Comparison of model-calculated CO with MOPITT measurements
supported the results from our inverse modeling study. Without exception, mean March 2001 model-calculated CO profiles in
the TRACE-P region from a simulation with adjusted CO sources were within a standard deviation of mean March 2001
MOPITT-sampled profiles. Finally, sampling biases need to be considered when interpreting low-latitude MOPITT profiles
DE: 0300 ATMOSPHERIC COMPOSITION AND STRUCTURE
DE: 0322 Constituent sources and sinks
DE: 0345 Pollution--urban and regional (0305)
DE: 0365 Troposphere--composition and chemistry
DE: 0368 Troposphere--constituent transport and chemistry
SC: Atmospheric Sciences [A]
MN: 2003 Fall Meeting