July-August 2008

The Future Is Now

Scientists, industry experts, and investment fund managers look at how climate change may affect existing water resources.

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Photo: Dr. Ken Dewey, Applied Climate Sciences, University of Nebraska, Lincoln

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By Penelope B. Grenoble

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In February 2007, researchers at the Scripps Institution of Oceanography, University of California San Diego reported they had produced the first clear evidence of human-produced ocean warming. Working with colleagues at Lawrence Livermore National Laboratory’s (LLNL) Program for Climate Model Diagnosis and Intercomparison, research marine physicist Tim Barnett and climate scientist David Pierce established that warming produced by climate modeling corresponded to actual ocean measurements over the past 40 years with a confidence factor of over 95%. Efforts to explain warming through naturally occurring climate variations or external forces, such as solar or volcanic factors, didn’t come close to reproducing the observed human-induced effect.

Barnett called the findings not only “compelling evidence” of global warming, but also a clear demonstration of the ability to simulate its past and, likely, future evolution. “One of the models we used we also use for weather forecasting, and it turned out to be the best by far in reproducing what has happened in the last 40 years,” he says. “My position is we ought to believe it for the next 20 to 30 years at least. Even in that time frame, we were able to show we basically have a train wreck here in the West in terms of water and power production.”

As one aspect of the looming crisis, the Scripps researchers predict that, given the expected climate change, and with no future curtailment of water use, there is a 50–50 chance Lake Mead, one of the two large reservoirs on the Colorado River water system, will be dry by 2021, and a 50% chance that by 2017 water levels will be too low to generate power.

The National Center for Atmospheric Research describes climate change as any persistent change in the statistical distribution of climate variables, with global warming as the fundamental driver. Increases in carbon dioxide and other greenhouse gases have caused radioactive heating that traps solar energy in the atmosphere, a trend that’s expected to raise temperatures at the beginning of the next century as high as 6.6˚C (12˚F) above 1990 levels.

The Scripps and LLNL scientists are hardly alone in focusing on links between climate change and our water resources. Examining the results of 19 climate models, Richard Seager, senior research scientist at Columbia University’s Lamont-Doherty Earth Observatory, established that warmer temperatures are producing increased uplift of air masses in the earth’s tropics. The warm air cools as it rises, condensing and producing increased tropical precipitation. If that’s not enough, more bad news comes from the fact that the increased uplifted air warms as it descends over already drought-prone regions, such as southern California and the American Southwest. University of California Los Angeles professor Glen MacDonald carries the scenario further, suggesting that we could be in for decades of hot, dry weather, stretching from southern California north to the headwaters of the Sacramento and Colorado rivers (California’s water lifelines)—a combination of circumstances he describes as “the perfect drought.” MacDonald contends that global warming replicates natural conditions that occurred during the Middle Ages, particularly the 12th century, when a severe drought in southern California, combined with persistent low flows in both the Sacramento and Colorado rivers, produced a dry spell that lasted 60 years.

One of the practical challenges facing water managers attempting to deal with the effects of warming, is that current climate models are not precise enough to predict conditions at a regional level. “The thinking is that the equatorial regions will be wetter and the higher latitudes will likely be dryer,” says Jack Henderson, water supply program director at Tetra Tech. “But, the temperate latitudes are more difficult to predict.”

“The models agree substantially, but they have a more difficult time agreeing on precipitation,” remarks Sujoy Roy, a CA-based principal engineer for Tetra Tech. “In California, we definitely have a pretty good understanding of what might happen. If temperatures go up, for example, the snow pack will melt a few weeks earlier than normal. But, it’s trickier in the Northeast, where some models predict more precipitation and some less. The fact is that if you’re a water supply person, your main interest is precipitation, so you need to keep track of what’s going on in the modeling world, particularly in this regard, and understand how it’s evolving. With more and more interest from the water resources community, there will be pressure on scientists and model developers to produce better, and more defensible, arguments for ways water managers might move in the future.”

Henderson adds, “Tetra Tech has some of the most sophisticated models, but precipitation is one of the critical inputs to river system hydrological models. We’re working on coming up with better science-based tools to give us a better understanding of what kind of precipitation we should load in the models. While it’s already a consensus that we’ll see melting sooner in high mountain regions that rely on snow pack for their water supply, we’re also going to see lower river flows earlier in the summer and fall, which will make storage a key component in capturing runoff to use in the dryer parts of the year. In coastal areas, precipitation is expected to be more frequent and occur as exceptionally heavy storms. So again, the question is how do we capture the amount of fresh water we need through flood skimming or runoff capture for use during the dry periods, which are going to be longer and more significant.”

Erik Straser, general partner at Mohr Davidow Ventures, an early-stage venture capital firm in Menlo Park, CA, says that a change in climate brings about unpredictability, and that variability can be dangerous when it comes to water resource management. “The infrastructure we’ve developed for serving water was built on a set of presumptions about where the water is and when it comes,” he notes. “And if that changes, our ability to actually harvest water and move it to where we want it will be significantly impacted. We are already at this very interesting intersection between the needs of a modern society and the world’s finite water resources. Layer on climate change and you add both variability and risk.”

Piet Klop, Senior Fellow at the World Resources Institute (WRI), looks at this from a worldwide perspective. “It may actually be, that in some parts of the world, water is going to more a critical issue than energy, because energy is still easy to move around,” he acknowledges. “But there are parts of the world where we’ve settled millions of people without having adequate water resources, like the American Southwest or the northern plain of China. We’ve lived for a long time with the delusion that we could engineer our way out of water scarcity. In China they’re doing it, but at exorbitant cost. In most of the world, energy is more or less traded at market prices. Nothing could be farther from the truth when you talk about water, with the predictable result that it’s wasted. We’ve basically ignored the whole issue and done stupid things, like growing Las Vegas and Phoenix.”

Seager sees the response to climate predictions varying among water managers. “In New York City [NY], the problem is related to intense rainfall events coming in increasing frequency—brief, short downbursts that are flushing heavy organic loads into the upstate reservoirs. This increase has been predicted by the models, and now the water supply has been so affected by this increased organic intake, the water managers can’t shut their eyes to the fact that something is happening.”

Photo: Dr. Ken Dewey, Applied Climate Sciences, University of Nebraska, Lincoln

Lake Mead at Hoover Dam: According to researchers, the lake is 118 feet below maximum elevation.
To provide a better perspective on how climate change effects may actually play out, the Association of Metropolitan Water Agencies (AMWA), a nonprofit organization of the largest publicly owned drinking water systems in the US, commissioned a study evaluating its implications. Among the report’s key conclusions is that, although the leading edge impacts of climate change may already be apparent, the larger effects on water supplies will be more evident as the century unrolls and will continue for centuries to come. Secondarily, the report concludes that, despite their efforts, the present generation of utility managers will not be able to resolve the effects of climate change, but should, nonetheless, undertake planning and research to aid their successors.

Among its major effects, warming-induced climate change is expected to cause sea levels to rise, as warmer temperatures cause the oceans to expand and glaciers and ice sheets melt. As any number of experts have observed, warming will also accelerate the pace of the hydrological cycle. Warmer temperatures will cause water to evaporate more readily, causing the total amount of precipitation to increase on a global level. The predicted temperature increases also suggest that areas subject to drought may see more extensive drought and heat waves, while areas accustomed to snowfall will see warmer and shorter winters, which have already been implicated in reduction in the amount of water stored as ice in glaciers and seasonal snow packs. The thought is that an earlier spring melt will also have significant implications for downstream flows in late summer and early fall.

With increased rainfall frequency will come severe flooding and pollution of freshwater supplies from wastewater treatment, and storage and conveyance systems. The AMWA report notes that, for the most part, existing wastewater treatment plants and combined sewer overflow control programs have not considered climate change in their design. The result could be continually increasing influent challenges from sewage overflows, producing high concentrations of disease-causing Giardia, cryptosporidium, and coliforms.

Changes in basic climate variables such as temperature, rainfall, seasonal patterns, runoff characteristics, and recharge patterns of both ground and surface waters are also likely to produce significant baseline changes in the earth’s ecosystems, and, in turn, this could impact existing negotiated in-flow requirements aimed at providing sufficient cold water to sustain fish species or freshwater flows into estuaries, to maintain tolerable levels of salinity during summer months or periods of droughts.

So, what is there to do? AMWA’s report identifies a need for additional scientific research, both to better understand the impacts of climate change on existing fresh water resources and to help develop and assess the affordability of alternative sources of supply that include reuse, recycling, conservation, and desalination. In the applied arena, AMWA Executive Director Diane VanDe Hei has called for increased federal investment in water infrastructure to help offset the costs of developing new sources of supply and finance capital projects. Next Page >

What Do You Think?

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watergrrll

August 6th, 2008 8:33 PM PT

We all need to come to grips with the fact that there must be an increase in federal investment for water infrastructure.

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