T jpo, 2011, in press he origin of along-shelf pressure gradient in the Middle Atlantic Bight

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(c)

Figure 4. (a) The EOF mode 1 of monthly running-averaged sea-level anomalies at the 12 indicated tide-gauge stations; (b) the principle component 1 (PC1); and (c) the linear regression of the EOF mode 1, where distance is from Wilmington (NC). The estimated sea surface slope is about 4.8

10^-⁸. Tick marks on the PC1 plot show January.

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