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Water budget · Lake Buchanan
Up or down? Up. TWDB's daily storage for Lake Buchanan rose 221 acre-feet on Nov 13.
Where the water came from and where it went on Nov 13, the latest day with every figure published. LCRA publishes the dam’s daily release and what flowed in, and TWDB the lake’s daily storage, so all three are measured. The leftover line covers water with no meter (withdrawals, seepage, ungauged creeks) and is inferred from the other lines.
- River inflowmeasured+326 af/day≈ +0.18 in/day on the lake
LCRA River Operations Report, daily averages for Nov 13: Colorado 165 cfs
- Evaporationmodeled−215 af/day≈ −0.12 in/day on the lake
Estimate from long-term averages over 22,127 surveyed acres (TWDB)
- Dam releasemeasured0 af/day≈ 0.00 in/day on the lake
LCRA River Operations Report: Buchanan Dam, daily average for Nov 13
- Everything arriving that we can’t meter (ungauged creeks, springs)inferred+110 af/day≈ +0.06 in/day on the lake
What’s left once the other rows and the storage change are counted
- =Storage changemeasured+221 af/day≈ +0.12 in/day on the lake
TWDB Water Data for Texas daily storage, Nov 13 vs. the day before
The lines above add up to the storage change: what the lake gained or lost. Every measured line is a published daily figure for Nov 13; evaporation is a long-term average.
Where it’s going
- 215 af/day≈ 108 cfsEvaporationmodeled
estimate from long-term averages
The release leg is LCRA's reported average release through Buchanan Dam for Nov 13. The withdrawals line is the budget’s leftover: city intakes, ungauged runoff and estimation error. The lines can overlap, so treat the split as approximate.
River flow toward the lake now
Swipe sideways to follow the river to the lake →
Streamflow at the river gauge (USGS or LCRA, whichever is newer). Labels are gauge readings in cfs. Line width isn’t to scale.
How this is computed
Inflow is the water that reached Lake Buchanan on Nov 13: each gauged river's daily average where it enters the lake, as LCRA River Operations Report publishes them, in acre-feet per day (1 cfs ≈ 1.9835 af/day). Evaporation uses long-term monthly averages for the region over today’s lake surface. That surface area is TWDB’s daily survey where published, otherwise estimated from storage. With no storage reading, evaporation isn’t estimated. Inches on the lake divides each volume by that same surface area, so an inch takes less water when the lake is low and narrow than when it’s full and wide. Storage change is TWDB’s daily storage, compared with the day before. The leftover is what it takes to make the lines add up. It lumps together withdrawals and ungauged runoff, which can’t be split without data the operator doesn’t publish.
All inputs are provisional. This page is an estimate, not an official accounting.