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Volume 9, issue 20
Atmos. Chem. Phys., 9, 7973–7995, 2009
https://doi.org/10.5194/acp-9-7973-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 9, 7973–7995, 2009
https://doi.org/10.5194/acp-9-7973-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  23 Oct 2009

23 Oct 2009

Properties of the average distribution of equatorial Kelvin waves investigated with the GROGRAT ray tracer

M. Ern1, H.-K. Cho2, P. Preusse1, and S. D. Eckermann3 M. Ern et al.
  • 1Institute of Chemistry and Dynamics of the Geosphere (ICG-1), Forschungszentrum Jülich, Jülich, Germany
  • 2Department of Atmospheric Sciences, Yonsei University, Seoul, Korea
  • 3E.O. Hulburt Center, Naval Research Laboratory, Washington D.C., USA

Abstract. Kelvin waves excited by tropospheric convection are considered to be one of the main drivers of the stratospheric quasi-biennial oscillation (QBO). In this paper we combine several measured data sets with the Gravity wave Regional Or Global RAy Tracer (GROGRAT) in order to study the forcing and vertical propagation of Kelvin waves. Launch distributions for the ray tracer at tropospheric altitudes are deduced from space-time spectra of European Centre for Medium-Range Weather Forecasts (ECMWF) operational analyses, as well as outgoing longwave radiation (OLR) and rainfall data measured by the Tropical Rainfall Measuring Mission (TRMM) satellite. The resulting stratospheric Kelvin wave spectra are compared to ECMWF operational analyses and temperature measurements of the Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) satellite instrument. Questions addressed are: the relative importance of source variability versus wind modulation, the relative importance of radiative and turbulent damping versus wave breaking, and the minimum altitude where freely propagating waves dominate the spectrum.

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