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. 2020 Oct 7;7(10):e2020EA001164. doi: 10.1029/2020EA001164

Figure 7.

ess2649-fig-0007

The retrieved MIGHTI‐A and MIGHTI‐B green line LOS wind error using symmetric airglow assumption (Harding17) and the correction using asymmetric airglow procedure (Wu20). (Top) The same as in Figure 6 (top) but for the green line case; (middle) the same as in Figure 6 (middle) but for 106 km, the highest altitude for which both daytime and nighttime data for the green line are available; (bottom) the same as the middle panels but for an altitude of 97 km, which is the closest altitude to the bottom layer of TIEGCM.