Martha and the Vandellas would have loved it. Metaphorically speaking, the New York Times practically swooned over it. (“An unforgiving heat wave held much of the West in a sweltering embrace over the weekend, tying or breaking temperature records in several cities, grounding flights, sparking forest fires, and contributing to deaths.”)
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It was a “deadly” heat wave, a “record” one that, in headlines everywhere, left the West and later the rest of the country “sweltering,” and that was, again in multiple headlines, “scary.” The fire season that accompanied the “blasting,” “blazing” heat had its own set of “record” headlines -- and all of this was increasingly seen, in another set of headlines, as the “new normal” in the West. Given that 2012 had already set a heat record for the continental U.S., that the 10 hottest years on record in this country have all occurred since 1997, and that the East had its own sweltering version of heat that wouldn’t leave town, this should have been beyond arresting.
In response, the nightly primetime news came up with its own convenient set of new terms to describe all this: “extreme” or “severe” heat. Like “extreme" or "severe" weather, these captured the eyeball-gluing sensationalism of our weather moment without having to mention climate change or global warming. Weather, after all, shouldn’t be “politicized.” But if you’re out in the middle of the parching West like TomDispatch regular William deBuys, who recently headed down the Colorado River, certain grim realities about the planet we’re planning to hand over to our children and grandchildren can’t help but come to mind -- along with a feeling, increasingly shared by those in the sweltering cities, that our particular way of life is in the long run unsustainable. Tom
Never Again EnoughField Notes from a Drying WestSeveral miles from Phantom Ranch, Grand Canyon, Arizona, April 2013 -- Down here, at the bottom of the continent’s most spectacular canyon, the Colorado River growls past our sandy beach in a wet monotone. Our group of 24 is one week into a 225-mile, 18-day voyage on inflatable rafts from Lees Ferry to Diamond Creek. We settle in for the night. Above us, the canyon walls part like a pair of maloccluded jaws, and moonlight streams between them, bright enough to read by.
One remarkable feature of the modern Colorado, the great whitewater rollercoaster that carved the Grand Canyon, is that it is a tidal river. Before heading for our sleeping bags, we need to retie our six boats to allow for the ebb.
These days, the tides of the Colorado are not lunar but Phoenician. Yes, I’m talking about Phoenix, Arizona. On this April night, when the air conditioners in America’s least sustainable city merely hum, Glen Canyon Dam, immediately upstream from the canyon, will run about 6,500 cubic feet of water through its turbines every second.
Tomorrow, as the sun begins its daily broiling of Phoenix, Scottsdale, Mesa, Tempe, and the rest of central Arizona, the engineers at Glen Canyon will crank the dam’s maw wider until it sucks down 11,000 cubic feet per second (cfs). That boost in flow will enable its hydroelectric generators to deliver “peaking power” to several million air conditioners and cooling plants in Phoenix’s Valley of the Sun. And the flow of the river will therefore nearly double.
It takes time for these dam-controlled tidal pulses to travel downstream. Where we are now, just above Zoroaster Rapid, the river is roughly in phase with the dam: low at night, high in the daytime. Head a few days down the river and it will be the reverse.
By mid-summer, temperatures in Phoenix will routinely soar above 110°F, and power demands will rise to monstrous heights, day and night. The dam will respond: 10,000 cfs will gush through the generators by the light of the moon, 18,000 while an implacable sun rules the sky.
Such are the cycles -- driven by heat, comfort, and human necessity -- of the river at the bottom of the continent’s grandest canyon.
The crucial question for Phoenix, for the Colorado, and for the greater part of the American West is this: How long will the water hold out?
Major Powell’s Main Point
Every trip down the river -- and there are more than 1,000 like ours yearly -- partly reenacts the legendary descent of the Colorado by the one-armed explorer and Civil War veteran John Wesley Powell. The Major, as he preferred to be known, plunged into the Great Unknown with 10 companions in 1869. They started out in four boats from Green River, Wyoming, but one of the men walked out early after nearly drowning in the stretch of whitewater that Powell named Disaster Falls, and three died in the desert after the expedition fractured in its final miles. That left Powell and six others to reach the Mormon settlements on the Virgin River in the vicinity of present-day Las Vegas, Nevada.
Powell’s exploits on the Colorado brought him fame and celebrity, which he parlayed into a career that turned out to be controversial and illustrious in equal measure. As geologist, geographer, and ethnologist, Powell became one of the nation’s most influential scientists. He also excelled as an institution-builder, bureaucrat, political in-fighter, and national scold.
Most famously, and in bold opposition to the boomers and boosters then cheerleading America’s westward migration, he warned that the defining characteristic of western lands was their aridity. Settlement of the West, he wrote, would have to respect the limits aridity imposed.
He was half right.
The subsequent story of the West can indeed be read as an unending duel between society’s thirst and the dryness of the land, but in downtown Phoenix, Las Vegas, or Los Angeles you’d hardly know it.
By the middle years of the twentieth century, western Americans had created a kind of miracle in the desert, successfully conjuring abundance from Powell’s aridity. Thanks to reservoirs large and small, and scores of dams including colossi like Hoover and Glen Canyon, as well as more than 1,000 miles of aqueducts and countless pumps, siphons, tunnels, and diversions, the West has by now been thoroughly re-rivered and re-engineered. It has been given the plumbing system of a giant water-delivery machine, and in the process, its liquid resources have been stretched far beyond anything the Major might have imagined.
Today the Colorado River, the most fully harnessed of the West’s great waterways, provides water to some 40 million people and irrigates nearly 5.5 million acres of farmland. It also touches 22 Indian reservations, seven National Wildlife Reservations, and at least 15 units of the National Park System, including the Grand Canyon.
These achievements come at a cost. The Colorado River no longer flows to the sea, and down here in the bowels of the canyon, its diminishment is everywhere in evidence. In many places, the riverbanks wear a tutu of tamarisk trees along their edge. They have been able to dress up, now that the river, constrained from major flooding, no longer rips their clothes off.
The daily hydroelectric tides gradually wash away the sandbars and beaches that natural floods used to build with the river’s silt and bed load (the sands and gravels that roll along its bottom). Nowadays, nearly all that cargo is trapped in Lake Powell, the enormous reservoir behind Glen Canyon Dam. The water the dam releases is clear and cold (drawn from the depths of the lake), which is just the thing for nonnative trout, but bad news for homegrown chubs and suckers, which evolved, quite literally, in the murk of ages past. Some of the canyon’s native fish species have been extirpated from the canyon; others cling to life by a thread, helped by the protection of the Endangered Species Act. In the last few days, we’ve seen more fisheries biologists along the river and its side-streams than we have tourists.
The Shrinking Cornucopia
In the arid lands of the American West, abundance has a troublesome way of leading back again to scarcity. If you have a lot of something, you find a way to use it up -- at least, that’s the history of the “development” of the Colorado Basin.
Until now, the ever-more-complex water delivery systems of that basin have managed to meet the escalating needs of their users. This is true in part because the states of the Upper Basin (Colorado, Wyoming, Utah, and New Mexico) were slower to develop than their downstream cousins. Under the Colorado River Compact of 1922, the Upper and Lower Basins divided the river with the Upper Basin assuring the Lower of an average of 7.5 million acre-feet (maf) of water per year delivered to Lees Ferry Arizona, the dividing point between the two. The Upper Basin would use the rest. Until recently, however, it left a large share of its water in the river, which California, and secondarily Arizona and Nevada, happily put to use. More
