Evaluation of radiative effects in the structure of planetary waves

Computer Science

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Carbon Dioxide, Ozone, Planetary Waves, Radiation Effects, Pressure Oscillations, Radiative Heat Transfer, Vertical Distribution, Wave Attenuation, Zonal Flow (Meteorology)

Scientific paper

The effect of ozone and carbon dioxide on the vertical structure of planetary pressure waves and on its variations due to zonal circulation changes is estimated. Atmospheric compressibility is taken into account, making it possible to assess the role of radiation effects in the dissipation of planetary waves which is most intense in the upper stratosphere. An analysis is given of the interannual variability of the differences in the mean zonal values of the geopotential between 45 and 70 deg N in January at isobaric surfaces of 500, 300, 50, and 10 hPa.

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