Fig. 7From: Utility of Slepian basis functions for modeling near-surface and satellite magnetic anomalies of the Australian lithosphereMaps a and b compare at 10 km altitude the respective downward continued CHAMP (i.e., MF7 model from Maus 2010) and upward continued near-surface anomalies with the anomaly differences (Map a − Map b) shown in Map c, whereas Maps d and e contrast at 275 km altitude the respective downward continued CHAMP and upward continued near-surface anomalies with the anomaly differences (Map d − Map e) given in Map f. Included on maps b and e are the respective correlation coefficients between maps a and b, and maps e and d Back to article page