Lake Mead: ‘A record-setting moment’

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Bump and update: From Time (Bryan Walsh):

What’s causing Lake Mead to dry up—and what does it mean for the Southwest? The one undeniable cause is simple growth—Las Vegas has grown from 25,000 people in 1950 to some 2 million today. That means more lawns, more laundry, more swimming pools, more car washes—in general, more straws sucking the water out of Lake Mead. And of course Las Vegas isn’t the only area in the Southwest to experience booming growth over the past few decades. From Denver to Phoenix to Los Angeles, the once lightly populated West has exploded, even as farmers in the region draw more water from the system to irrigate the desert.

But the Southwest has also been caught in a devastating drought that has now gone on for more than 10 years, one that has reduced the region’s water supplies even as growth has further stressed them. Drought is a natural phenomenon—especially in the desert, go figure—and there have been varying levels of rainfall in the region just in the 75 years since Lake Mead was first filled. But the scary thing is that the territory might be more vulnerable to drought than it seemed during the 20th century—a time period that may have been unusually wet on a historical scale. A 2007 panel organized by the National Research Council found evidence that mega-droughts had occurred in the Southwest more frequently than had been thought, and that “drought episodes are a recurrent and integral feature of the region’s climate.” The Colorado River Compact—which divides up water supplies for seven U.S. states and parts of Mexico—was drawn up in 1922, based on river flow data going back to the 1890s, a time of unusual wetness. We may have built the Southwest with a false sense of water security.

Then there’s climate change, an X factor for future water supplies. It’s difficult to gauge what impact, if any, global warming may have had on the current drought and on dropping water levels. As always, it’s virtually impossible to filter out climate change as a cause for a natural disaster amid all the noise and static of other factors. But as the recent report from the government U.S. Global Change Research Program shows, the Southwest is already rapidly warming, reducing the spring mountain snowpack that helps feed the rivers of the region. We’re likely to see increasing temperatures in the future, with more frequent drought and increasingly scarce water supplies. Climate change won’t be the only cause behind the drying of the West, but could make a bad situation much, much worse.

From The New York Times (Felicity Barringer):

“It is a record-setting moment,” said Colleen Dwyer, a spokeswoman for the Bureau of Reclamation. She added that slightly more water than usual had been released through Hoover Dam over the weekend because the power marketing agency that sends dam-generated electricity around the Southwest had requested some additional flow.

Lake Mead’s levels are still eight feet above the level at which a shortage is officially declared and limited rationing could go into effect for users in Nevada and Arizona, and well above the levels when the Hoover Dam’s hydroelectric output might be seriously jeopardized.

But Barry Nelson, a senior policy analyst for the Natural Resources Defense Council, said: “This strikes me as such an amazing moment. It’s three-quarters of a century since they filled it. And at the three-quarter-century mark, the world has changed.”

More coverage from the Arizona Republic (Shaun McKinnon):

Not since it was first filling in 1937 has Lake Mead held so little water. The reservoir’s level fell to the historic low shortly before noon on Sunday, eclipsing a previous record from the drought-stricken 1950s. The lake is now just 8 feet above the level that would trigger the first drought restrictions, which would reduce water supplies for Arizona and Nevada. That gap could close by next year – the reservoir fell 10 feet from October 2009 to 2010 – but there are measures in place that would likely delay rationing for one or two years or even longer if a wet winter increased runoff into the river. Most homes and businesses in Arizona likely would not feel the direct effects of the restrictions, which would divert water first from farmers.

But conservation groups say the reservoir’s low levels underscore the risk to the Colorado River. “Everyone needs to know when we turn on the tap, it drains water out of the river and it has ecological consequences,” said Gary Wockner, campaign coordinator for Save the Colorado, a non-profit education group based in Fort Collins, Colo. “We need to try to keep some water in the river and keep it alive.”[…]

The three lower-river states, along with Colorado, New Mexico, Utah and Wyoming on the upper river, approved a drought plan in 2007 that uses Lake Mead water levels to trigger incremental rationing, part of an attempt to avoid widespread shortages. The first trigger is at 1,075 feet above sea level. The reservoir reached elevation 1,083.18 feet around midday Sunday and was at 1,083 feet by Monday afternoon. The previous low level was 1,083.19 feet, set in 1956…Under the 2007 plan, the first trigger would reduce water deliveries to Arizona by a little more than 11 percent, or 320,000 acre-feet, and to Nevada by about 4 percent, or 13,000 acre-feet. Additional reductions would occur if the lake continued to drop.

More coverage from the Las Vegas Review-Journal (Henry Brean):

Since drought took hold on the Colorado and its tributaries in 1999, the surface of Lake Mead has plunged almost 130 feet and caused fits for the National Park Service and its marina operators who must extend roads, utilities and other services to reach the shrinking shoreline.

The lake’s decline poses major problems for the Southern Nevada Water Authority, which draws 90 percent of the Las Vegas Valley’s drinking water from intake pipes that will start to shut down should the lake fall another 33 feet. “I’m worried,” authority General Manager Pat Mulroy said. “We’re trying everything we can to keep as much water in Mead as we can.” The prognosis looks bleak. Mulroy said federal climate forecasters are predicting abnormally dry conditions during the next two winters in the mountains that feed the Colorado…

The previous low-water mark for Mead came 54 years ago, on April 26, 1956, when the drought-stricken lake bottomed out at 1,083.19 feet above sea level. According to the Bureau of Reclamation, the lake hit elevation 1,083.18 between 11 a.m. and noon Sunday and continued to fall. By Monday afternoon, it sank below elevation 1,083 as water was released through Hoover Dam to meet orders downstream from cities and farms in California and Arizona. Projections by the U.S. Bureau of Reclamation call for Lake Mead to reach a low point of 1,082.1 on Nov. 2. Then it is expected to rise by about 8 feet through the end of February before starting back down again. Water forecasters expect the lake to hit another record low by May and shrink below elevation 1,077 by September…

Even at its lowest level since it was first filled, Lake Mead remains the largest man-made reservoir in the United States. The falling water level has caused some problems with access, but it has also unveiled new coves and pristine beaches that used to be underwater, Roundtree said.

More coverage from the Voice of San Diego Environment (Rob Davis):

Millions of people — San Diegans included — rely on the reservoir’s water. So what does its drop mean here? In the short term, nothing. It doesn’t have any impact on San Diego’s supply even though we relied on the river for 61 percent of our water in 2009. But it does send a bad signal that the river supplying the Southwest’s lifeblood is continuing to face pressure — a pressure that scientists say is growing as the climate warms. If the lake continues dropping, it will first cause problems for cities in Arizona and Nevada before San Diego. Those states hold lower-priority rights to Colorado River water than California does.

More Colorado River basin coverage here.

La Niña primer

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From the High Country News weblog The Range (Ed Quillen):

For the West, this means it will be wet in the north and dry in the south…

Colorado is in the middle between north and south in the West, so fluctuations on the jet stream will determine how much of the state gets buried in December and January…

In some years, there’s talk of “La Nada” — the nothing, or at least nothing out of the ordinary. El Niños and La Niñas tend to run in three- to seven-year cycles, and if you want to sound technical, you can call it ENSO for “El Niño/La Niña Southern Oscillation.”

La Niña was a hot topic last week when members of the CWCB, water providers and others huddled up at Denver Water to answer the question, “Drought in 2011?”. Below are my notes from the meeting:

Water Year 2010 review

Nolan Doesken kicked things off with a look back at the past year.

A year ago October was wet and snowy but in November everything dried out. Northern Colorado was dry until the spring when the precipitation pattern shifted north. Wind speeds were low over the winter leading to a decline in wind energy production in northeastern Colorado. There was a wet spring and early summer in northeastern Colorado. Also in April there was a series on large dust events in the San Juans. The runoff was fast a furious with sudden warming at the end of May. Colorado experienced a strong but confined monsoon mid-July to around August 15.

He said that yesterday’s precipitation was the, “first widespread event in 2 months.”

Overall, “Most of the state ended up near average for precipitation,” he said, and added that, “This is the first time in history that we have had 3 near average years in a row.”

According to Doesken, the summer was the 15th warmest on record, statewide.

Short-term forecast

Triste Huse from the National Weather Service presented the short-term weather outlook. She said we can expect a good storm around Tuesday of next week. She showed a slide of comparing the historical precipitation for the 45 day period between August 1 and October 7. 2010 was the third lowest on record. Her 60 day comparison, ending October 7, had 2010 in first place for dryness. She added that September 2010 was the 7th warmest on record.

Long-term forecast

Klaus Wolter started off his presentation by saying that, “La Nina is on a steam roller.” The Multivariate ENSO Index is at it’s lowest level in 94 years, he said, adding that, “This is quite remarkable,” and, “The system can’t really get any colder.” (ENSO = El Nino Southern Oscillation). He told the group, “If you’re making a bet on the first snowfall,” bet on next Tuesday. His research shows that, “We’ve never really had a dry winter with La Nina.”

He told the water providers that if this La Nina turns out to be a two year event, “You better hope that the first year is not too bad because the second year will get you.” He said, “The odds are better than 50-50 that this will be a large La Nina with a normal, at best October.” He believes that we’ll have a few months above average moisture for winter, “but the runoff season next year will be on the dry side.”

“We are not on a 2002 path at this point,” he said, predicting a near normal winter and a dry spring. If La Nina continues it could be the start of a dry 2012.

Water provider updates

Bob Steger from Denver Water asked each of the water providers present to update the group on current operations and any plans for dealing with the possibility of the D1 drought continuing or worsening. Most providers are in good shape regarding storage. Aurora and Colorado Springs are planning work on Homestake Reservoir in 2012 so they will be drawing it down it prior to the work starting. Denver Water does not plan any extra releases for the next few months – they’re just going to match demand.

The National Science Foundation funds Michigan State University effort to develop a management plan for the Ogallala (High Plains) aquifer

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Here’s the release from Michigan State University (Layne Cameron):

Researchers at Michigan State University are helping shape the future of the High Plains’ water supply.

The Ogallala Aquifer is a vast underground system that spans from South Dakota to Texas with smaller portions in Colorado, New Mexico and Wyoming. It is one of the world’s largest aquifer systems, storing nearly as much water as Lake Erie and Lake Huron combined. Yet this seemingly limitless water supply, a key component supporting the Great Plains’ bountiful agriculture production, is shrinking.

The National Science Foundation has awarded MSU $1.2 million to help shape a course to better manage this important natural resource. The multidisciplinary team of researchers, led by hydrogeologist David Hyndman, will use the four-year grant to develop a sustainability plan based on economic, sociological and geographic issues affecting the aquifer.

“For more than 80 years, the Ogallala Aquifer has been used for irrigation, and the withdrawals far exceed its ability to replenish itself,” said Hyndman, who worked with the Kansas Geological Survey on this project. “We are on an unsustainable course and must make difficult changes if we are to keep using some of the best agricultural land in the country.”

Researchers will review decades of scientific data. They also will study the interactions between the region’s landscape, atmosphere and socioeconomic systems and link this data with climate, hydrology, vegetation and economic models.

The end result will produce predictions and impact assessments covering a range of potential solutions. Community and government leaders will be able to implement the team’s forecasts to adjust land management policies and to make strides toward sustainable water-use practices.

“Navigating a patchwork of state laws, regulations and economics means any change will require complex solutions,” Hyndman said. “And since scientific solutions don’t exist in a vacuum, our plan will also address social and economic variables.”

The MSU research team comprises Jinhua Zhao, associate professor of agricultural economics; Stephen Gasteyer, assistant professor of sociology; Nathan Moore, assistant professor of geography; Shiyuan Zhong, associate professor of geography; Warren Wood, John Hannah Visiting Professor of Integrative Studies; and Anthony Kendall, geological sciences research associate.

The grant is funded through the NSF’s Water Sustainability and Climate program.

More Ogallala aquifer coverage here and here.

Energy policy — hydroelectric: Aspen hydroelectric plant application filed with FERC

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From the Aspen Daily News (Curtis Wackerle):

The city on Friday submitted its draft application for a conduit exemption to the Federal Energy Regulatory Commission (FERC). A conduit exemption would waive the formal FERC licensing process, which would likely include an environmental assessment or environmental impact statement.

The 521-page document explains why city officials believe the project qualifies for the conduit exemption.

It contains a report from Miller Ecological Consultants, which states that a minimum stream flow of 13.3 cubic feet per second (cfs) would be sufficient to maintain a healthy Castle Creek. It also contains intergovernmental agreements regarding stream monitoring and in-stream flows with the Colorado Division of Wildlife (DOW) and the Colorado Water Conservation Board (CWCB). It also includes about a dozen letters that have been filed in opposition to the conduit exemption…

Conduit exemptions are granted for small hydroelectric projects — defined as 15 megawatts or less — that use infrastructure that is not primarily intended for the generation of hydroelectricity. City officials claim that standard is met by a drainline currently under construction from Thomas Reservoir to Castle Creek near the site of the proposed hydro plant. City officials say the 4,000-foot-long drainline, approved in April at a cost of $2.3 million, is a necessary safety feature for Thomas Reservoir, which lacks adequate discharge capacity if there was ever an emergency. But the drainline also would be a “penstock” to feed water from the reservoir into a hydroelectric turbine in the proposed building underneath the Castle Creek Bridge…

A conduit exemption also requires that water used to generate electricity be discharged back into a conduit, into a point of municipal consumption or into a natural body of water if the same amount of water is re-diverted further downstream for municipal purposes. The application, prepared by Boulder law firm Dietze and Davis, states that discharging the water from the hydro plant into Castle Creek sustains an “in-stream flow” water right held by the CWCB. The in-stream flow constitutes a “point of municipal consumption,” according to the application. To come to that conclusion, the application argues that the CWCB is a municipality as defined by FERC. Further, the application cites case law which found that municipal consumption does not necessarily mean physically removing water from a river or stream…

By returning the water to the stream to meet a minimum stream flow requirement, the city and the water conservation board fulfill a municipal purpose, according to the application. The document, while arguing that it meets the discharge requirement, simultaneously asks for a waiver from that provision. “It’s just a belt and suspenders approach,” Kumli said. “We’re being careful to use FERC law in a manner that is fair [and consistent] with the way FERC approves hydroelectric projects.”[…]

Meanwhile, the Aspen City Council is considering whether to grant local land use approval for the hydro plant. Public hearings on the project began this summer, but have been tabled while a group of citizens and Pitkin County’s Healthy Rivers and Streams Board undertakes further study of the project. A group of citizens also is attempting to convene mediation meetings between project opponents — some of whom are considering lawsuits if the hydro plant is approved — and the city.

More hydroelectric coverage here and here.

Pueblo: The Pueblo Board of Water Works is considering a five percent rate hike

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From The Pueblo Chieftain (Chris Woodka):

Water board employees anticipate the 5 percent increase in 2011 largely to cover increased utility costs, which are expected to rise 22 percent to $2.57 million. Other large areas of expenditures include $1.26 million for outside services, up 8 percent; $1.3 million for repairs and maintenance, level; $1.24 million for supplies, level; $1.6 million for new main extension projects; and $870,000 to continue converting meters to an automated reading system. A rehabilitation of the outside and inside of the Hellbeck water tank will cost $400,000. Without using water development money, a rate increase of 8 percent is estimated…

Metered water sales are the largest source of revenue for the water board, and are expected to be about $19.5 million — 3.5 percent below budget — for 2010. Customers continue to use less water as part of a continuing conservation trend. In 2011, $20.5 million in metered sales is projected. The board also is anticipating more than $7.5 million in contract water sales in 2011, including $4.9 million to Xcel’s Comanche plants, $1.58 million from a pair of contracts with Aurora, $812,000 from raw water sales and $360,000 from the Black Hills contract. The budget workshop is scheduled at noon Nov. 9 and the hearing at 2 p.m. Nov. 16 at the Board of Water Works, 319 W. Fourth St.

More Pueblo Board of water works coverage here.