I've run the last week's numbers, with the drawdown from 2/6 to 2/13 of 67,100 af, multiplied by 11 weeks, adjusted upward by 210,944 af to account for sedimentation when trying to find a matching elevation, leading me to 7/11/1965 and a lake elevation of 3,520.81, so 3,520' for lowest level this spring is probably closer than 3,512' elevation. Marina operations at Bullfrog are probably still viable at 3,520', maybe not at 3,510'.Good news, three different ways, for your methodology:
(1) For the week ending 2/7, drawdown was 78,340 af, 5827 af less than your 84 KAF figure. 12 weeks of that makes a 70 KAF difference and makes your minimum storage target 5336 KAF instead of 5266 KAF.
(2) For the last 10 years, average minimum spring elevation has occurred on April 20. 2021 was the outlier, so you had the right idea using May instead of May 25, but the decade average is another 11 days earlier than that. That knocks your 12 week number down to 10.3 weeks, and your target minimum storage up another (78.34 KAF/wk x 1.7 fewer weeks) 133 KAF, to 5469 KAF.
(3) Your method ignores the sedimentation since 1965, which has reduced the reservoir volume. See, for example, http://lakepowell.water-data.com/index2.php?elevation=3530.61, which shows a 211,000 af difference between October 1965 and February 2022 for the exact same reservoir elevation. So instead of looking for 5469 KAF back in 1965, you could adjust your method to look for 5680 KAF, which turns out to correspond to 3518'. That's a whole 6' higher than your calculation. Don't you feel better now?
But if this is a contest, I'll adjust my own guess up a little bit higher to account for some slowdown in the drawdown as we approach the minimum, and I'll guess 3520'.
Release volumes are supposed to be 673 kaf in January, 539 kaf in February, 575 kaf in March, 501 kaf in April, 599 kaf in May, 678 kaf in June, going all of the way up to 858 kaf in August (https://www.usbr.gov/uc/water/crsp/studies/images/PowellRelease.png). Things could get pretty scary in July and August.
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