I think you're speaking my language...Great stuff! And great descriptions of 1983--you're right, that was an exceptional spring! And the thing about that 120K cfs is that it happened on July 1, exceptionally late as you know...In 1984, it also hit 120K, but that was at the end of May, a more predictable timing...
In the past 20 years, it did hit 95K cfs in 2011(June 16), and of course it reached 78K this past spring on June 18... but other than that, the only other years over 80K were in 1979, 1986, 1993, 1995, and 1997... but none exceeded 96K in 1995... which is another reason 1983-84 were so exceptional...
...1983 and 1984 were both off the charts in terms of flow, but very different in terms of timing. Both years saw sustained peak inflows of 100K+ cfs, and both hit a peak of over 120K cfs. In 1983, that 100K+ flow lasted 9 days, and in 1984 it lasted 2 weeks!! Wow… In both years, you had sustained inflow of 85K+ cfs lasting roughly a month—5 weeks in the case of 1983! The big difference was that in 1984, the peak happened in the last week of May and first week of June. In 1983, it snuck up on everybody—and the peak flow was delayed until the last week of June and the first week of July.
You're right, if we had another 1983-84 double punch, we'd make some real progress on filling the lake.
Imagine if those two years happened starting this coming spring, with a lake level starting at 3598 in early April... How high would the lake rise? Well, first consider the inflow alone—in both 1983 and ’84 from April 1 to August 31, about 15 MAF entered the lake! In just May through July alone, it was about 12.3 MAF. That’s an incredible amount, roughly the annual flow of the Colorado River system in one spring runoff. In both 1983 and ‘84, the Bureau released over 10 MAF during that time to manage the nearly-full lake.
But what if they had been able to release just the minimum to meet the normal annual release requirement of 8.23-9 MAF? In that scenario, the average daily release is 11-12,000 cfs. To model that, I applied the 9.0 MAF scenario by assuming a daily release of 12,432 cfs during that entire period of April 1-August 31. That results in a total release of about 3.7 MAF during that period. So if you do the math, and subtract that release from the same period 1983-84 inflows of about 15 MAF, you end up with a net inflow of a little over 11 MAF for each year. (The Bureau assumes annual evaporation loss is about 0.4 MAF, which I didn’t account for.)
Here’s what would happen if you added a net 11 MAF in two straight years to Lake Powell assuming a starting point of 3598, which is where we're likely to be by the end of March 2020 (lake volume of 11.6 MAF). That would bring the lake up to 22.6 MAF in volume by the end of summer in the first year, minus evaporation of 0.4 MAF, so about 22.2 MAF. That means you would end up with about a 88-foot rise, ending at 3686 (!!). At that point, the lake would be over 85% full, and higher than the level as where it started in the spring of 1983. So that means a second straight year like the first would be almost exactly like what ended up actually happening in 1983-84—the lake would be full, with massive releases.
That would be great... we can only hope...
Thanks for bringing your voice to this discussion!!