
Originally Posted by
jason
I'll be working on that one this summer. There is a lot of information about when various reaches of the river start to lose water rather than gain it, which indicates that water is reversing into springs. It doesn't tell you what springs specifically or the order in which they went under, but the information allows us to examine environmental controls on reversal events, such as rainfall amount and location and antecedent aquifer levels. Using that data, we see large variability in the amount of water that is lost along sections of the river during floods that occur following wet periods vs dry periods. Generally speaking, flood magnitudes are being decreased due to low aquifer levels and reversals are occurring at lower river stages. Low aquifers mean more storage space for water and more attenuated flood pulses. Flooding on the Suwannee in 2009 was near-record up by Madison, indicating that we should have had near record flooding downstream. Because the aquifer levels were so low, however, the flooding even at Peacock wasn't even close to a record.
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