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Stationary, oscillating or drifting mantle‐driven geomagnetic flux patches?

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Table 2. Fractional Threshold h f b i for Defining Extreme Points for the Time Averages and the Resulting Coordinates of the Intense Flux Patches at Each Hemisphere a
Table 3. Synthetic Analysis of Time Series a
Figure 8. Field‐flow relationship for three different snapshots in case T 0. (top) The radial field B r is given in units of ffiffiffiffiffiffiffiffiffiffiffiffiffiffi

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