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Comparing high latitude thermospheric winds from Fabry–Perot interferometer (FPI) and challenging mini satellite payload (CHAMP) accelerometer measurements

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Figure

Table 1. Geographic and geomagnetic AACGM coordinates of the FPI facility related to the KEOPS site in Kiruna (see text).
Figure 1. CHAMP observations over Longyearbyen during solar maximum 2001–2003. Panel (a) shows the average values for all data –ascending (blue) and descending (red), panel (b) shows summer (May–August) averages and panel (c) shows winter (end October–earlyMarch) averages.
Figure 2. CHAMP observations over KEOPS during solar maximum 2001–2003. Panel (a) shows the average values for all data – ascend-ing (blue) and descending (red), panel (b) shows summer (May–August) averages and panel (c) shows winter (end October–early March)averages.
Figure 3. Geometry illustrating the projection of the FPI viewingdirection horizontal wind components onto the CHAMP cross-trackorientation for the ascending and descending tracks.
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