
And I believe JFR said in '63 only 1,000cfs were being released, which isn't much....guess even that sustains Grand canyon? And this is all probably much ado about nothing......
On that point, there was a period from May 12 to August 18, 1964 when releases through Glen Canyon Dam were reduced to roughly 1000 cfs, in an effort to raise the elevation of Lake Powell to at least minimum power pool (3490). That effort was successful. During that 3-month period, Lake Powell rose about 90 feet, on some days, 3 feet per day. The lake's volume increased by 3.1 maf in that time.
That sustained low outflow to the Grand Canyon also had its consequences. During that same period, Lake Mead lost 2.2 maf, and dropped by 23 feet. About 15% of its existing live volume disappeared in those 3 months. Fundamentally, it shifted the storage balance between Mead and Powell, although at the time, most of the water storage still remained in Lake Mead. In late August 1964, after the artificially induced increase of Powell's volume, the live storage volume of Powell was about 4.1 maf. In Mead, it was much more--about 12.3. Here's an interesting tidbit: Collectively, the total live storage of 16.4 maf in August 1964 was almost exactly what it is today here in May 2025, with the main difference being that now, the volumes in Mead and Powell are nearly the same (roughly 8 maf each).
Does that matter? If we had the same reservoir balance now as in 1964, would people be concerned? Probably so. At least now, maintaining more volume in Powell allows for adjustments to releases, and allows for better management of power potential between the two reservoirs.
And then there's the constant cry about Powell's evaporative losses. Let's not forget: despite what that video says, the evaporation rate of Mead is substantially higher than that of Powell. Generally speaking (and based on actual data since 2011), Lake Mead loses about 6.5 afy per acre of surface area. For Powell, it's about 4 afy per acre of surface area. Total evaporation goes up for each reservoir as surface area increases. I'm attaching another graphic which shows the evaporative loss as a function of the volume for the two reservoirs. Bottom line, at least from the perspective of evaporation, it's much better to store water in Powell than Mead. And that's intuitive: the area around Lake Mead is just a lot hotter, plain and simple.
One last thing for now, to Rainbowbridge's question: What does 1000 cfs of flow do to the Grand Canyon? Hard to say. It's rarely been that low. Apart from that period in 1964, the only other times the flow was that low in the Grand Canyon were a few dates in the summers of 1934 and 1940. The lowest recorded flow? That was 672 cfs, on 7-19-34. Hard to imagine what that looks like, but I can show you what 1,000 cfs looks like. In June 1964, my family was on a cross country trip that included the Grand Canyon. My dad happened to take a photo from Desert View that included the river flowing through marble canyon at 1,000 cfs. Here's a link to another post that shows this and goes into some narrative detail:
Big runoff and a rising lake have been huge topics this spring, but one of the lingering questions on the minds of some is this: why didn't the BOR release less than the 18,000 cfs in the last couple of months and make the lake rise even more? Well, I'm not going to answer that one in this post, but instead take a different angle on this whole topic.
In recent decades, the normal release pattern through the dam varies, but it's usually somewhere between 8,000 and 18,000 cfs, depending on the season and how big the snowpack was in the spring. There have been years where the runoff was...
