American Geophysical Union Become an AGU Member
Subscribe to AGU Journals
AGU Home AGU Publications

Read Full Article (file size: 1958398 bytes)    Cited by

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 109, D09304, doi:10.1029/2003JD004469, 2004

CO2 column averaged mixing ratio from inversion of ground-based solar spectra

Emmanuel Dufour

Laboratoire des Sciences du Climat et de l'Environnement, Commissariat à l'Energie Atomique, Gif sur Yvette, France


François-Marie Bréon

Laboratoire des Sciences du Climat et de l'Environnement, Commissariat à l'Energie Atomique, Gif sur Yvette, France


Philippe Peylin

Laboratoire de Biogéochimie des Milieux Continentaux, INRA Grignon, Thiverval-Grignon, France


Abstract

High resolution sun spectra from the Kitt Peak observatory are used to estimate the column-averaged mixing ratio of carbon dioxide in the atmosphere. Solar absorption lines are apparent on the measured spectra together with the telluric lines. Their discrimination is easy as they are spectrally shifted according to the Earth-Sun relative speed. For the objective of CO2 mixing ratio estimate, a spectral window of size 15 cm−1, with approximately 10 absorption lines, contains most of the necessary information. The window selection is based on the absence of contamination by other gases and solar absorption lines. Favorable spectral windows are found near 1.6 and 2.0 μm. A radiative transfer model is used to reproduce the data and make the inversion. An excellent fit is obtained. The retrieved CO2 mixing ratio agrees with the expected values within a few percents and shows the expected growth rate of 1.5 ppm per year. On the other hand, the observed short-term variability of several ppm is much larger than what is expected from simulations by an atmospheric transport model using optimized fluxes. It appears necessary to correct the CO2 mixing ratio estimates using concomitant measurements of the O2 mixing ratio, which provides a proxy for the dry air optical path. After the correction, the annual cycle of the CO2 content above Kitt Peak is apparent on the retrieved values. The comparison of the inverted mixing ratios with the simulation results indicates an error on the order of 1.5 ppm RMS for the 1.6-μm band and 2.5 ppm RMS for the 2.0-μm band. The uncertainty on the effective airmass due to the long acquisition time of the spectra, with varying solar zenith angle, may be responsible for a large fraction of the error.

Received 18 December 2003; accepted 25 February 2004; published 12 May 2004.

Keywords: atmospheric CO2; spectroscopy; CO2 absorption.

Index Terms: 0322 Atmospheric Composition and Structure: Constituent sources and sinks; 0394 Atmospheric Composition and Structure: Instruments and techniques; 1640 Global Change: Remote sensing; 1610 Global Change: Atmosphere (0315, 0325).


Read Full Article (file size: 1958398 bytes)    Cited by

Citation: Dufour, E., F.-M. Bréon, and P. Peylin (2004), CO2 column averaged mixing ratio from inversion of ground-based solar spectra, J. Geophys. Res., 109, D09304, doi:10.1029/2003JD004469.