California Water: A Taste of Pork

Tomorrow, our Action Governor is going to star at a media event at Friant Dam, near Fresno. He’s using the dam, which impounds the San Joaquin River, as a prop for a ceremony at which he’ll sign an $11.1 billion bond measure that will go onto next November’s ballot. The money’s supposed to go for building new dams and reservoirs and for environmental restoration of the Sacramento-San Joaquin Delta, which has been laid waste by earlier generations’ water schemes.

It’s a big bond. In ordinary times it might be a tough sell. But these are lean, lean times for the state, which is suffering through a staggering series of budget deficits and will have to pay interest of $700 million or $800 million out of its general fund every year once all the water bonds are sold. Schwarzenegger said last week he thinks voters will go for the measure because they’ve recently passed other big infrastructure bonds, such as last year’s $10 billion initiative to finance a California high-speed rail system.

Maybe so. But enter the Associated Press. One of its Sacramento reporters has been leafing through the bond bill. Here’s what she found:

“… Dozens of projects … were injected into the bond bill to secure enough votes to get it passed. The projects will add tens of millions of dollars to the interest taxpayers will have to pay on the bond if voters approve it next year.

“Many of the projects are only peripherally related to the purpose of the legislative package, which is intended to increase California’s water supply and restore the ecologically fragile Sacramento-San Joaquin Delta.

“For example, $30 million was earmarked to the state Department of Parks and Recreation for grants for watershed education facilities. Another $20 million is set aside for the Baldwin Hills Conservancy, which manages land for recreation and wildlife and is the Los Angeles district represented by Assembly Speaker Karen Bass.

“In the final days of negotiations, lawmakers in both chambers padded the bond bill with an additional $1.7 billion, despite previous statements by legislative leaders that the state could not afford such a large bond.”

The AP is following up here on what was widely rumored around the state Capitol when the bond was passed In fact, a reporter asked Schwarzenegger about the add-ins during his a self-congratulatory press conference the governor held after the Legislature acted. Here’s what the governor had to say last week to the suggestion that some of the projects in the bond measure might be “pork”:

QUESTION: Governor, how can voters support this package when you passed it in the middle of the night and the — so the pork, so-called pork, inserted in there including (Inaudible) pulled out?

GOVERNOR: Are you talking about — I don’t know what you’re talking about, because the end package does not have any pork whatsoever, so I don’t know what you’re talking about.

QUESTION: Late in the evening the bill, as it was being drafted, contained — was amended and contained — and these projects were added for various counties and for various projects. So the tab grew from 9 billion to 11 billion. So how can the voters take on something like this at a time when they’re still feeling the pinch and how can they be sure that all the money will be spent well?

GOVERNOR: Well, first of all, as you know, I’m not as interested in the process as in the end result. So throughout the process we went from 8 billion to 12 billion, to 9 billion, to 11 billion, back to 9 billion and back up to 11 billion. So I think this is maybe something interesting for the journalists but it definitely is not as interesting to me. To me always what’s interesting is the result and the result was a great, great package of approximately $11 billion.

One of the things you have to love here is the way Schwarzenegger, reputed to be a hard-headed businessman, so breezily dismisses the appearance of billions of dollars of extra stuff. That’s something that’s only interesting to journalists, he says. And, he may find out very soon, to the people who will have to pay the tab.

Rain on the Roof

Who owns the water that falls on your rooftop? In most of the western United States, it’s not you, and if you try to catch and store that water, you may be interfering with someone else’s water rights. NPR aired a story on the issue this morning, “Water Wars Out West: Keep What You Catch,” about a Colorado law that breaks with the usual legal regime. The law allows water collection by residential property owners who need to dig a well or get their supply trucked in (in other words, if you’re served by what city dwellers think of as a regular water system, it’s still illegal for you to catch and save rainwater and snowmelt in Colorado.)

The links:

An Act: Concerning Limited Exemptions for Water Collected from Certain Residential Rooftops

Southwest Colorado Water Information Program: Understanding Water Rights

U.S. Bureau of Land Management: Western States Water Laws

NPR: “Water Wars Out West: Keep What You Catch!

And also, for generally interesting reading on water rights questions, Aguanomics, a blog from two UC-Berkeley economists.

Evaporation

When you read California’s daily water-storage reports and pore over the columns of data–for instance, from Lake Shasta, the state’s largest reservoir–you happen across this one: EVAP. It’s a record of how much water escapes the lake by changing state from liquid to gas. We’re schooled very early on in our science education about the hydrologic cycle. You know, the process by which water evaporates from oceans, lakes, rivers, and your scotch on the rocks, is transported into the atmosphere to fall as rain or snow, and then is evaporated and carried into the sky once more. Still, it’s one thing to know that a theoretical process is operating out there in the world somewhere and another to see its monumental workings in a statistical read-out.

Go back to Lake Shasta. I’ve been to the dam that holds it back, and I’ve driven past it dozens of times. It sprawls in an endless series of bays and inlets — old river courses — among the mountains that wall off the northern end of the Central Valley. The lake is usually ringed by a collar of brilliant orange-red soil, the upper margin of which marks the reservoir’s high-water mark. That ring is a sort of drought gauge: the more of it you see, the lower the lake is and, generally, the drier the state is.

One thing I don’t think when I drive past Shasta is that I’m watching a massive machine pumping millions of gallons of water into the sky. But that’s what it is. According to the summary from the Department of Water Resources California Data Exchange Center, yesterday the lake lost about 316 cubic feet of water per second through evaporation. Here’s what that is in household terms:

–A cubic foot of water is 7.48 gallons, so the lake was leaking 2,363.68 gallons into the atmosphere every second; three seconds’ worth at that rate would be more water than we’ve ever used in our Berkeley household in an entire month.

–Every minute, 141,820.8 gallons evaporated. In rough terms, the evaporation rate was 1 acre-foot every two minutes and 15 seconds. That’s a generous annual supply of water for two water-guzzling U.S. household.

–Every hour, 8,509,248 gallons of water — about 26.1 acre-feet — departed the lake. That’s enough to submerge a football field to a depth of 20 feet.

–For the day (and the evaporation rate is a 24-hour average), the lake lost 204,221,952 gallons, or 627 acre-feet. That’s a minor part of the reservoir’s net change for the day–the overall level fell by 7,271 acre-feet, mainly through water released for power generation–and it’s a tiny fraction of the lake’s current storage, about 3.15 million acre-feet.

Last stat for now: the process of evaporation is highly dependent on local weather, just like the grade-school lesson on the water cycle would suggest. When it’s warm, more water evaporates as the surface layer of lake water heats up. When it’s cool, the process slows. For the past month, the highest daily evaporation rate was 362 cubic feet per second, in the midst of a spike of very hot weather. The low point was 14 CFS, during a stretch of cool, rainy weather.

Wind and Water

aqueduct040508.jpg

From the archives: Last spring, Kate and I drove out to Bethany Reservoir, just south of the Sacramento-San Joaquin Delta at one of the key points in the state’s complex water system. The site is also on the lower eastern slopes of the Altamont Pass country, a big wind-generation site. Pondering the state’s water story and how to tell it–do you take the narrative back to Genesis and/or The Big Bang and talk about where water itself comes from, and how long would it take from that point to get to a discussion of a salmon in the river?– I thought of that visit tonight. Here’s a shot of a wind farm virtually on the bank of the Delta-Mendota Canal–part of the federally developed Central Valley Project–just southeast of Bethany. Whatever you happen to think of the way the water systems were built here and the damage they have caused to salmon and other parts of the old California environment–the engineering is never less than impressive and sometimes beautiful.

The aqueducts move water through a combination of gentle flow and brute force: huge quantities of water are lifted from pumping stations to artificial lakes like Bethany. Then gravity takes over, and the water flows down the manmade rivers to the next set of pumps, maybe 60 or 100 miles away, and the process is repeated. (One of the more surreal sights in the state is along Interstate 5 as the highway climbs the Tehachapi Mountains. The aqueduct runs along the highway, and the water is pumped up nearly 2,000 feet through a pair of above-ground tunnels.) One beauty in the aqueducts is the way they follow the contours along the border of the Coast Range hills to the west and the great valley to the east. The engineers had to work with and respect the lay of the land here.

(Here’s the satellite view, with the hills in their full-on golden summer hue. The image shows Bethany Reservoir. The water comes in from a channel at the northwest corner, having been pumped out of the Sacramento River to a holding basin called Clifton Court Forebay. The California Aqueduct flows out to the south and east (below and to the right). Drag the map to follow the course of the aqueduct. In this image, the California Aqueduct is on the left and the Delta-Mendota Canal is to the right.)


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Watching Water

I’ve become preoccupied the last two or three months with the level of water in California’s reservoirs. If you’re inclined to, here’s where you can join in the fun: The state Department of Water Resources’ California Data Exchange Center. The cliche to describe a collection of information like this is “treasure trove.” For example, here’s one report that I’ve taken to taking a look at just about every morning: The Sacramento/San Joaquin Daily Reservoir Storage Summary. It’s a quick look at about three dozen state’s biggest storage facilities: how much water they’re holding, how many acre feet have flowed in or out in the past day, and–especially interesting–how much water they hold compared both to the average for this date and to the amount held a year ago.

There’s a story in the numbers, though I’m still puzzling out what it is. For instance, the state’s current drought is not a drought everywhere. Although rainfall and the mountain snowpack are generally below average, some reservoirs hold more than average for this time of year and much more than they did a year ago (which was an even worse year, precipitation-wise). But the numbers are just one dimension of a complicated picture. All that water has a lot of work to do. We count on it not just for irrigating the Central Valley farms and bringing drinking and lawn water to the citiies and suburbs, but for providing electricity, too. And in recent decades, the state and federal water managers have even been made conscious of another function the water might perform: preserving wildlife–especially the once-magnificent salmon runs in the Sacramento and San Joaquin watersheds.

Big Bathtub II: ‘Wasted’

The state periodically produces a document called the California Water Plan. It has been coming out in one form or other regularly or irregularly since 1930. It's part catalogue of the state's water resources, part status report on climate, rivers and the plumbing system that eases the thirst of farms and cities, and–as I read it–part marketing brochure for our biggest water customer, agriculture, and for new dams and reservoirs to secure its water supplies. That last aspect may seem odd, but I was struck by how the draft for the next water plan sings the praises of farmers' efficiency in using every last drop of water they get. It ought to be noted that California agriculture gets about four gallons out of five of the water impounded in the state's reservoirs.

The California Department of Water Resources offers a set of summary statistics on the state's natural water supply. In an average year, the state gets about 200 million acre feet of water in rain, snow, and river flows from other states (the latter is mostly by way of the Colorado River, long a major source of water for Southern California).

Of that 200 million acre feet–probably enough water to keep China going for a year if you could save every thimbleful–100 million or 120 million just sort of goes away. It evaporates, gets sucked up by redwood trees and crabgrass and some crops, or keeps natural marshes marshy. Of the remaining 80 million to 100 million acre feet, about half is captured for urban and agricultural uses. And the final portion, sometimes a quarter or more of all water that nature provides this dry place, flows down the great valley rivers, the Sacramento and San Joaquin, and out the coastal streams and bays to the Pacific. The state website describes this outflow as necessary "in part to meet environmental requirements." It sounds responsible of us. Almost altruistic.

If you've spent enough time in the San Francisco Bay region, you can name a couple of these "environmental requirements" almost without thinking about them. One is the need for an adequate flow of freshwater to prevent the "intrusion" of saltwater into the Sacramento-San Joaquin Delta. Brackish water threatens farms there, and it also effects residential users, some of whose water is siphoned right out of the Delta channels.

Another environmental factor is fish. The installation of the vast and complex system of dams, reservoirs, canals, pumps and siphons up and down the Central Valley–but especially in the Delta–has proved deadly for the great salmon runs that used to charge in from the Pacific nearly year round. Belatedly, state and federal water and wildlife officials, at the prompting and prodding of politicians, environmentalists and their lawyers, and judges, have seen fit to set aside some of the yearly flows for the good of the salmon and other imperiled species.

But that responsible, almost altruistic-sounding side of the state's water management sometimes lets its guard down. Our governor, remarkable for his knack to say the right thing–and for seeming to never dig in and deliver on that thing–was talking last week about all that must still be done to fix California. One of his pet projects is a $9 billion program of dam, reservoir, and canal construction. When he was making his pitch for it last week, he described the water that flows out to the Pacific as a waste. It's as if he and those of like mind believe that every glassful, every ounce, ought to be put to productive–you know, human–use.

In saying that, the governor gave voice to an old, old sentiment. Fish and wildlife were never a big consideration when the rivers got plumbed. Putting water to work was the chief concern.

In 1919–90 years ago this week, in fact–the California State Irrigation Association published a tract by Lt. Col. Robert Bradford Marshall. He was a veteran of the U.S. Geological Survey who had studied rivers in California and the West and the problem of getting water where it wasn't. His 12-page report was titled "Irrigation of Twelve Million Acres in the Valley of California." The Department of Water Resources acknowledges Marshall's report as the forebear of the present-day California Water Plan by listing it as the earliest iteration of the state's great water schemes. In short, Marshall proposed building a big dam in the northern Sacramento Valley and building a series of great canals to bring water to both farm and city. Thinking about our current governor and the idea that water that flows into the ocean without having done any honest work is a waste, I was struck by the tract's introduction to Marshall's ideas:

"… Back in those early days Col. Marshall wondered why they didn't irrigate in Northern California as they were doing in Colorado, where he had surveyed the year before. And he then as a young man dreamed that dream of EMPIRE BUILDING that every man of vision at one time or another has dreamed when he views California's millions of acres parched and burning in the summer and her millions of acre feet of water pouring into the Pacific in the winter. …"

And here's Marshall himself, describing that free-flowing water and the people who apparently refused to control it:

"The people of California, indifferent to the bountiful gifts that Nature has given them, sit idly by waiting for rain, indefinitely postponing irrigation, and allowing every year millions and millions of dollars in water to pour unused into the seas, when there are hungry thousands in this and in other countries pleading for food and when San Francisco and the Bay Cities, the metropolitan district of California, are begging for water."

In a dry year like this one, you still hear voices begging for water. And the answer we hear from the governor, farm interests, and water officials is now, as it was so long ago, to capture more of the water that falls on us and put it to work.

Big Bathtub I: The Acre Foot

An acre foot is the amount of water it would take to flood an acre to a depth of one foot. An acre is, ballpark number only, a patch of land 100 feet by 400 feet. If you were standing on that patch of land with water about halfway up to your knees — well, you’d be having a direct experience of the acre foot.

An acre foot is 325,000 gallons. If you pay a water bill that shows how much you use, you can figure how long that much water would last you. The rule of thumb, that we journalists borrowed from “water experts” here in California was that an acre foot was enough to supply two average households for a year. That’s for use inside and outside the home for three or four people say, and it comes out to about 460 gallons a day for each household. Of course, there’s a lot of variation. An inner city apartment dweller uses a lot less than someone whose lawn looks like a fairway at Augusta National. Someone in a cool coastal area — Berkeley, for instance — uses less than someone in a much hotter area on the other side of the hills, lawn or no lawn.

The acre foot is a basic unit of life in California. Yes, weather people and water management officials count inches of rain and snow in the winter. But those units are incidental in a place that needs to capture and store an immense amount of water to irrigate roughly 15,000 square miles of crops and to supply 36 million people. The acre foot is the fundamental currency of reservoir storage and water delivery.

Up and down California, the federal government, the state government, electric utilities, county and city water companies, and irrigation districts have built reservoirs. They’re big bathtubs that together hold something like 42 million acre feet; that would be enough to submerge the entire state of Wisconsin under a foot of water. They reservoirs are expected to fill up in the winter and spring with runoff from the rains and melting snow running down from the Sierra Nevada. Then the water is pumped out during the dry season to help the fields and orchards thrive and to keep the showers and garden hoses flowing. Some water is even set aside for the fish that swim in dwindling numbers through the maze of waterways between reservoir, farm, and town.

A wet winter here–what people like to think of as normal, with nature’s tap switched on when we get into the middle of autumn–keeps our big bathtubs full and the water running where it’s needed. But there are other kinds of winters, too. Very wet ones, where the system simply can’t hold all the water coming down the rivers. And dry and very dry ones, where the water level in the reservoirs falls and keeps falling if two dry years come back to back.

We’re in what appears to be our third dry–or drier than “normal”–year in a row. Three of the biggest federal reservoirs in Northern California– Shasta, Oroville, and Folsom–all fell to critically low levels in December and January. Together, the three reservoirs can hold about 9 million acre feet; that’s about enough to supply a year’s worth of household water for New York, Pennsylvania, New Jersey, Massachusetts, Connecticut, Rhode Island, New Hampshire, Vermont, and Maine. That’s every U.S. resident east of the Great Lakes and north of the Mason-Dixon Line.

Remember,: that’s the capacity of just three reservoirs. There are dozens of others. During the last five weeks, copious rains have fallen and the water has started to rise in some of those big bathtubs. More about that later.