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Fig. 6. Baseflow from the four watersheds, expressed as a 365-d moving average. Each date is plotted as the average baseflow during the prior 365 d, removing seasonal variation from the record. Four drought periods, indicated by upward-pointing arrows, each showed a slower recovery of baseflow from the conventionally tilled watersheds (W1, W2) than the conservation watersheds (W3, W4).

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