Mid-Tropospheric Measurements of Global CO2 with the Atmospheric Infrared Sounder (AIRS)
B. Imbiriba1, L. L. Strow1,2,S. DeSouza-Machado1,S. E. Hannon1, P. Schou1
Joint Center for Earth Systems and Technology, University of Maryland Baltimore County1
Department of Physics, University of Maryland Baltimore County2}
The AIRS (Atmospheric Infraread Sounder) Instrument
Hyperspectral Infrared Sounder on the EOS-AQUA platform - 1:30pm polar orbit - operational since Sept. 2002.
Grating spectrometer with 2378 low noise channels
High resolution IR channels $\sim 0.5-2.0\,\wn$ from $650\wn$ to $2665\wn$ ($3.7-15.4\, \um$)
15 Km footprint - very stable - with well characterized radiances.
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Other groups focus in Higher Troposphere
We go to the Mid Trop by using particular channels:
Narrow ``Q branch'' at $791.75\wn$
Broad ``R branch'' around $2400\wn$
Atmospheric state from ECMWF
Land Emmissivity from Borbas/Seemann (http://cimss.ssec.wisc.edu/iremis)
Peak sensitivity around $500\mb$
Calibration with GlobalView
Use NOAA's GlobalView site data set (http://www.esrl.noaa.gov)
Focus on Mid Trop airplane sites - 11 total.
For simpler comparison, take the highest altitude flight only (usually 5000m - 8000m).
For each site:
$\sigma\approx 7\ppm$ - AIRS radiance noise
Uncertainty of mean $\approx 0.02\ppm$ ($10^4$ obs)
Calibration - {\it mean} of all sites
Daytime - $373.22 \ppm$
Nighttime - $373.55 \ppm$
Calibration $\sigma \approx 1.3\ppm$
AIRS Global Time Series - Rates
Data aggregated in $4\mydeg$ boxes.
Observed growth rate of $\approx 2.28\pm 0.07 \mathrm{ppm/year}$