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Satellite observations of middle atmosphere–thermosphere vertical coupling by gravity waves

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Figure

Figure 1. Response function for the Savitzky–Golay filter with awindow size of 11 data points.
Figure 2. Global maps of GWMF derived from SABER observations (1st–7th rows) and ARDF derived from GOCE observations (lastrow) for boreal summer
Figure 3. Latitude–altitude cross section of Pearson correlation coefficients between SABER GWMF and GOCE ARDF for boreal summer.
Figure 4. Same as Fig. 2 but for austral summer.
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