174396.fig.005a
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174396.fig.005b
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174396.fig.005c
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174396.fig.005d
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Figure 5: Polar motion excitations integrated over the Earth’s north high latitudes (latitudes ) and over the other latitudes (latitudes ) using GRACE solutions and CPC and GLDAS models. Larger discrepancies between the models and GRACE observations come from the north high latitudes estimations.