“intentionally created unused apportionment”: gobbledygook for the greater good

There’s a particularly important passage in Matt Jenkins’ new piece on former Las Vegas water manager Pat Mulroy’s leadership on Colorado Basin issues (behind paywall for now, subscribe!) where he describes an example of a convoluted deal to bank Nevada water in an Arizona aquifer:

It was … the first federally sanctioned deal for a water transfer between two states. But Mulroy has only ever spoken about it euphemistically because transfers, even within the Lower Basin, are so politically charged. “Don’t ever call it a transfer,” she scolded during a 2008 interview. “It’s a banking agreement. That thing will disappear on us tomorrow if we call it a transfer.”

She had learned a crucial lesson, however. In the years that followed, Mulroy would — despite her reputation as a woman who didn’t mince words — speak an increasingly convoluted lingua franca that would eventually include enigmas like “intentionally created unused apportionment.” It sounds like gobbledygook, but it was all for a larger end.

“I learned it’s not what you do, it’s what you call it,” Mulroy told me. “You find the right name for it, and you can do anything.”

Palo Verde Irrigation District, Blythe, Calif.

Palo Verde Irrigation District, Blythe, Calif., by John Fleck

In the Colorado River Basin, there is a core network of people representing each of the states and the major water users within the states who understand that the basic problem is this: If each state clings to the water rights volume numbers written down over the years on pieces of paper documenting “the Law of the River,” there won’t be enough water to go around, the reservoirs will empty and the system is at risk of crashing in unexpected and potentially very unpleasant ways. Down this path lies a lack of resilience.

This is a group of varying size and membership that regularly works together on basin-wide problems. After gathering to work out solutions that invariably involve lots of “using less than we though we were entitled to on paper,” each negotiator must sell the deal back home in a political environment motivated almost entirely by domestic concerns. You can’t just say “we’ve gotta use less water,” because then you get things like this:

“If anybody thought we were going to roll over and say, ‘OK, California, you’re in a really bad drought, you get to use the water that we were going to use,’ they’re mistaken,” said James Eklund, director of the Colorado Water Conservation Board.

Eklund knows, or should know, that there are mutually beneficial solutions that involve both Colorado and California (along with everyone else) not using the full allotment of water to which they’re entitled on paper. (Some of the best solutions also involve clever approaches to moving water across state lines. My book will look in detail at a suite of such ideas.) But as Mulroy said, you’ve got to be careful what you call it, because the Eklunds’ of the world gotta make this work back home.

Eklund’s comments were seen (I think correctly) across the basin as playing to the home crowd, while the state of Colorado actually has been a collaborative participant in the search for shared solutions to the basin’s problems.

But if the whole thing blows up, and my optimism about finding solutions to sharing water turns out to have been wrong, it will almost certainly fail because of problems at this boundary between basin-wide realities and the politics of domestic consumption. The scale of water governance requires solutions at the basin-wide scale that must then be implemented back home one river diversion and water district at a time, where the political system at the state and local level incentivizes pounding fists on tables and vowing to fight to save our water from those other people.

See, for example, Eklund.

So the folks working on this problem at a basin level have to structure the deals in such a way that they have a plausible story upon their return to the world of domestic politics. And they also have to invest in what resilience scholars call “social learning“, which is critical to bridging this gap in governance scale.

In the meantime, “intentionally created unused apportionment” may just mean “we used less water than we could’ve, and those other guys got some of what we saved”, but you’ve gotta be careful how you phrase it.

Strategies for Middle Rio Grande water, March 21

My friends at the Middle Rio Grande Water Assembly are gathering Sat., March 21, to discuss strategies for managing water in the face of climate change in the central New Mexico reach of the river:

While there is a Regional Water Plan for the three county-area (Sandoval, Bernalillo and Valencia), it is ten years old. This event is one of our opportunities to review the Plan and determine what changes need to be made so as to ease our way into a changing climate.

9 a.m. to 3 p.m., Dane Smith Hall at the University of New Mexico, it’s free but they’re asking you to register (but the registration page didn’t work for me, so I may just crash the party uninvited).

Geomorphology of a fake lake

I’m fascinated by the geomorphic traces left by the rise and fall of Lake Mead – human scale (egret scale?) shoreline terraces. This is on the northern bank above Boulder Harbor. The bird, shown for scale (I don’t have a rock hammer, it’s a great egret, so quite large), hangs out there because of the fisher people.

Old shorelines, Lake Mead, February 2015, by John Fleck

Old shorelines, Lake Mead, February 2015, by John Fleck

Lake Mead “bathtub ring”

Lake Mead bathtub ring, by John Fleck, February 2015

Lake Mead bathtub ring, by John Fleck, February 2015

One of the members of my brain trust was speculating idly the other day about how different the Colorado River dialogue might be if the hydro-geo-chemistry of the bathtub ring was different – if the dropping water didn’t leave a white mark, letting you see how much Lake Mead has dropped, letting people like me take a picture to put on my blog.

Standing atop Hoover Dam last week, I heard one of the Bureau of Reclamation tour guides emerge from the elevators, pointing out the bathtub ring and saying:

I don’t think as long as I live I will ever see it get to the top again.

I’m sure he or she does not speak for the Bureau and the Secretary of the Interior on this sensitive point.

Rio Grande forecast improves, but that’s not saying much

update, Thursday, 3/5: Final March 1 forecast numbers are in, unchanged for those in the preliminary quoted below.

previously: It says something about the drought on New Mexico’s Rio Grande in recent years that a forecast of 67 percent of average runoff into Elephant Butte Reservoir is good news.

Elephant Butte Reservoir, Aug. 13,2014, by John Fleck

Elephant Butte Reservoir, Aug. 13,2014, by John Fleck

That’s the mid-point of the preliminary forecast sent around to New Mexico water managers and stakeholders today by the Natural Resources Conservation Service. The forecast includes the early March storm, which has pushed snowpack to 87 percent of average in the Rio Grande headwaters of Colorado and near normal in the mountain watersheds of northern New Mexico that feed the river. But as you head south, the numbers drop, and the forecast reflects that.

There’s still a big spread of uncertainty in the forecast, with a lot riding on what happens in March:

  • wet (the 3 in 10 high-flow probability): 92 percent or above
  • mid: 67 percent
  • dry (3 in 10 low flow probability): 41 percent or below
Elephant Butte Reservoir storage, courtesy USBR

Elephant Butte Reservoir storage, courtesy USBR

This is the fifth consecutive March 1 for which the forecast has been below-average bad news at San Marcial, the gauge at the head of Elephant Butte Reservoir, a point I’m calling out here because the greatest drought impact has been on farmers who depend on water from Elephant Butte. After flush years in the ’80s and ’90s, irrigators drained the Butte in the first decade of the 21st century. As I wrote a couple of wrote a couple of years ago in the newspaper:

Yields are already down – 30 percent in the case of onions, one of the valley’s money crops. A drive through the valley shows tiny spring onion plants already stunted by the salt accumulating in the soil beneath them.

As for chile, Shayne Franzoy said the Hatch Valley should have a decent crop this year for the packers, like Bueno Foods in Albuquerque, that depend on their chile. But if drought conditions continue, the future is less certain. “If we don’t have surface water in the Hatch Valley,” Jerry Franzoy said, “it’s gonna die pretty quick.”

That was two years ago. It hasn’t gotten better.

AMACRQ: How do you pronounce “CAP” and “SNWA”?

The latest edition of Inkstain’s infrequent* Ask Me a Colorado River Question feature comes via Paolo Bacigalupi, and it wasn’t quite phrased as a question, but I’m hoping to resurrect the feature.

My answer was that I say, and hear others say “cap” for the Central Arizona Project, but I’ve always stumbled over SNWA and usually just say “Vegas” which seems inadequate. Or sometimes “Southern Nevada,” which also doesn’t quite get the thing done.

What do you, dear readers, do with these two initialisms?

* I think it’s appeared, like, once.

How low can municipal water conservation go?

From Gary Woodard’s work – in Arizona…

an annual drop in per-household demand of more than 2 percent between 2000 and 2013 across Maricopa and Pima counties.

This trend is expected to extend through 2020, as we continue to replace appliances, fixtures, and landscape plants with new, more water-efficient ones; construct new, more water-efficient homes; and participate in water conservation programs offered by municipal providers.

 

April-July Colorado River runoff: 71 percent

February precipitation anomalies, courtesy Western Regional Climate Center

February precipitation anomalies, courtesy Western Regional Climate Center

With a dry February, the chances of a big snowpack and “bonus water” flow in 2015 that might begin to refill Lake Mead and Lake Powell are just about gone.

April-July runoff into Lake Powell, the big reservoir in the Colorado River’s “Upper Basin”, is forecast to be 71 percent of average, according to the Colorado Basin River Forecast Center. There’s still a one in ten chance, if things get wet over the next month, that we could have an average year. But with another lost month, the chances on the wet side of the probability distribution no longer leave much room for enough excess runoff to bail out the river system’s shrinking reservoirs.

On the bad side, the “one in ten” forecast on the dry side, the worst case scenario, is for 48 percent of average.

As you can see from the map to the right, February was wet up in the state of Colorado, but if your interest is in Colorado River runoff, it was not wet in the right places. That blue blob is on the eastern slope and the plains. The high mountains and west slope were drier than normal, which translates into less runoff into Lake Powell.

I’m waiting on more New Mexico numbers (the Rio Grande Basin) and will write a separate post when I get them, but the preliminary numbers in the San Juan headwaters, which provides San Juan-Chama water, are not good. The projected flow at the Navajo/Chromo/Oso measurement point in southern Colorado, a good proxy for overall SJC production, is 58 percent.

(Full disclosure: I foolishly entered into a bet regarding April 1 SJC supply. It’s a complicated bet involving total allocated and in storage on April 1. Suffice to say I have a cost-of-a-dinner incentive to root for more snow. Also, it’s my community’s drinking water supply.)

West’s snowpack improves, still not great

It is testimony to a lousy January and most of February that the spectacular snowstorm I drove home into over the weekend left the key watersheds that provide water to the Rio Grande and Colorado River still behind average for the year. The 9 inches of snow at my house was the most since December 2006, and snow was widespread across northern New Mexico and into Colorado:

Courtesy NRCS

Courtesy NRCS

Two key basins I watch in southern Colorado – the San Juan and the Upper Rio Grande, are still well behind, but have gone from potentially disastrous (below 60 percent) to simply bad (72 and 86 percent respectively). In New Mexico, the Sangre de Cristos and Chama area are both above 90 percent, which is enough to earn green on the map.

The broader measure of interest to the West, the Colorado River Basin, has climbed as a result of the storms, with steady improvement for the last week, but is still well below average for this time of year. We’ll get formal forecasts later in the week, but the automated daily computer runs are projecting runoff above Lake Powell (the broadest measure, averaging across all the watersheds that feed the San Juan, Green and Colorado rivers) of 72 percent of the long term mean.

(Thanks to Kerry Jones at the National Weather Service in Albuquerque for help with the maps.)