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AGU: Geophysical Research Letters

 

Index Terms

  • Atmospheric Processes: Climate change and variability
  • Atmospheric Processes: Remote sensing

Abstract

AIRS hyper-spectral measurements for climate research: Carbon dioxide and nitrous oxide effects

H. H. Aumann

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

David Gregorich

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Steve Gaiser

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Mid-tropospheric temperature soundings over tropical oceans by the Atmospheric Infrared Sounder, AIRS, using 4.3 micron CO2 R-branch and P-branch channels independently measure about 260 K with one Kelvin semi-annual variability. The difference between the soundings, which cancels seasonal variability, has increased over the past two years by 47 ± 9 mK/year. This trend is explained by the increase of 2.2 ± 0.4 ppmv/year and 0.6 ± 0.2 ppbv/year in the abundance of CO2 and N2O, respectively, which results in a 35 mK/year trend. The ability to achieve closure at this level with only two years of AIRS data is very encouraging for measurements of other trends of atmospheric temperatures relevant to climate research. AIRS covers the 3.7 to 15.4 micron region with spectral resolution of λ/Δλ = 1200. AIRS was launched into a polar 705 km altitude orbit on the EOS Aqua spacecraft on May 4, 2002, and has an expected on-orbit lifetime of seven years.

Received 18 October 2004; accepted 18 January 2005; published 3 March 2005.

Citation: Aumann, H. H., D. Gregorich, and S. Gaiser (2005), AIRS hyper-spectral measurements for climate research: Carbon dioxide and nitrous oxide effects, Geophys. Res. Lett., 32, L05806, doi:10.1029/2004GL021784.

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