![]() However, the rise in springflow and water levels has already begun to recede. It is significant to note that Onion Creek, the largest contributor of recharge to the aquifer, did not flow at all, despite some local significant rainfall in its watershed (a testament to how dry that watershed is).īarton Springs and the Lovelady well have responded (both rising) to the recharge that did occur. For example, Bear Creek only flowed for about 4 hours. ![]() Not enough rain occurred in the contributing watershed of the aquifer, so many of the creeks only flowed temporarily. Rainfall totals of locally over 9 inches produced some good runoff and recharge to the Edwards Aquifer, but it was very short-lived. While the rain temporarily boosted springflow (up 31 cfs) and Lovelady water levels (up 0.4 ft), more rain, and in the contributing watershed, is needed to end the (groundwater) drought. Lovelady Depth to water: 197.2 ft (up nearly 0.4 ft) By comparison, the City of Austin draws for its municipal use about 160,000 acre-feet of water per year.Ĭlick here for a link to the LCRA press release.ĭrought Stage: Critical (yes, we're still in it!)īarton Springs flow: 38 cfs (10-day average estimated at 23 cfs declining quickly-see below)
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