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Properties of inertia-gravity waves in the lowermost stratosphere as observed by the PANSY radar over Syowa Station in the Antarctic

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Figure

Figure 2. Power spectra of the zonalfluctuations obtained using Blackman–Tukey algorithm between 10and 12 km for the year 2013
Figure 3. Example of zonal (u′) and meridional (v′) horizontal windperturbations extracted with cutoff vertical wavelength 4 km andcutoff period 4 h between 28 June and 2 July 2013.
Figure 4. Mean monthly values of f/ ˆω for year 2013
Figure 7. Distribution of vertical wavelengths for summer (a) andwinter (b) season. Grey and black parts of the histogram representthe upward and downward energy propagating IGWs respectively.
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