Category Archives: The Science

Latest research from the field and the lab

Positive Feedbacks in a Warming Arctic

A thermokarst study site near Toolik Field Station (Photo: Gretchen Weber)

The Arctic is warming, almost twice as fast as the global average, according to a recent study.  Much of the accelerated warming here is due to positive feedbacks, including one related to the loss of summer sea ice in recent decades.  White surfaces, like snow and ice, reflect most of the sun’s energy and have a high albedo, while the unfrozen ocean absorbs it.  This creates a feedback loop: the warmer the temperatures, the less sea ice.  The less sea ice, the more heat absorbed, the higher the temperatures.  (As Molly Samuel reported recently, scientists are studying albedo as it relates to California’s snowpack and water supply.)

Another concern in a warming Arctic is thawing permafrost.  Earlier this week, I was out with my polar fellow colleagues measuring the depth of the permafrost here around Toolik Lake with a metal probe and a plastic ruler.  In some places we measured it to be just centimeters below a thin surface layer of plant-supporting soil called the “active layer.”

According to Breck Bowden, a scientist from the University of Vermont who studies permafrost here at Toolik, the latest modeling shows that approximately half of the permafrost in the Arctic will thaw in the next 50 years.  That’s significant not just for the Arctic ecosystems, but potentially for the entire planet.  Scientists estimate that there’s one to two times as much carbon frozen in the Arctic soils as there is currently circulating in the atmosphere, said Bowden.   The problem is that as the permafrost thaws, that carbon (mostly in the form of frozen organic matter), some of which has been frozen for thousands of years, will be processed by microbes in the soil and ultimately released into the atmosphere as greenhouse gases: CO2 and methane.

“So why should someone who is living in Alabama, or Nigeria, or the Phillippines worry about what’s going on the Arctic?” said Bowden. “Well, they should worry a lot if there’s going to be a massive amount of CO2 that gets into the atmosphere and your sea level rises or your crops fail because of changes that are related to CO2 changes globally. What happens here in the Arctic is going to affect everything on the globe.”

One indicator that the permafrost in the Arctic is already thawing is the increase in thermokarsts, which are places where the permafrost has thawed and the ground has collapsed, causing a disturbance in the landscape, and often releasing large amounts of sediment into nearby streams. Several scientists, including Bowden, study thermokarsts around Toolik Lake, and they’ve observed that the number of them is increasing.

A group of us were in the field with Bowden yesterday as he paid a visit to one of his research sites about 20 minutes up the Dalton Highway from Toolik Field Station, and a 30-minute hike across the uneven ground that defines the tundra landscape.

Picking our way through the tundra (Photo: Gretchen Weber)

“The Arctic explorers uniformly and universally cursed walking on the tundra, and you can see why,” Bowden explained as we hiked.  “You step on it, you break your ankle. You step between it, you break your ankle.  It’s very lumpy.”

The thermokarst we hiked to was not particularly catastrophic-looking to my untrained eye.  It’s a gully that’s about 300 meters long, 20 meters wide, and about five meters deep.  The collapse happened in 2003, and in the subsequent years it has widened, and vegetation has grown back along its sides, giving them a gentle, convex shape.  Someone like me might have hiked down one side of this thermokarst and up the other without giving it much thought.

Bowden was careful to point out that thermokarsts are a natural phenomenon.  (They also have been known to occur when roads and houses are built in the Arctic without proper insulation.)  But he also believes that the increase in thermokarsts observed in remote areas around Toolik is not natural.

“Thermokarsts have been going on as long as there’s been an arctic landscape, and there have been more of them when it’s warmer and fewer of them when it’s colder,” he said.  “But I do firmly believe that there are more of them now than there were 20 years ago, as a consequence of warming we can document in a variety of places.  The question is, why is the warming occurring?”

A Sauna…for Science

The sauna at Toolik Field Station

Last night I celebrated my first summer solstice in the Arctic by participating in one of the most beloved activities here at Toolik Field Station.  I took a sauna. Then I jumped in the lake, which still had ice on it one week ago, according to the Toolik Naturalist’s Journal.  The sauna at Toolik is spoken about in almost reverential tones, and with good reason.  It’s a small wooden cabin a few dozen yards from the main camp, perched at the water’s edge, and there’s a window that lets you soak up the stunning expanse of lake, tundra, and mountains, while you warm your bones after a plunge in the frigid waters.  “Sauna Nirvana” was how one of the scientists described the experience.

But people don’t just love the sauna for the view and the warmth.  They also love it because here at Toolik, it’s the main way to get clean.  The process entails warming up in the sauna, running outside and dumping lake water over yourself, soaping up with some biodegradeable cleanser, dumping more lake water over yourself, and then running back into the sauna so you don’t freeze to death.  Or, if you are hard-core, you can skip the water-dumping part and just jump in the lake.

Pitchers for bathing, on hooks outside the sauna (photo: Gretchen Weber)

The station didn’t have any showers at all until 2001 (researchers have been coming here since 1975), and even now, residents are limited to two two-minute showers per week.  Water conservation here is taken very seriously, not because there isn’t enough supply, but because all of the waste water from the showers, kitchen, and outhouses, has to be trucked 140 miles north to Prudhoe Bay for disposal at a cost of $1.24 per gallon.  Because this is such an active research site, scientists aren’t too keen on the idea of a leach field right next to the spots where they are sampling nitrogen and phosphorus.  So, in the name of science, we sauna.

Last summer, 85,680 gallons of waste water were trucked out of Toolik, which translates to 9.77 gallons of water per day, per person, according to Michael Abels, the Toolik Operations Supervisor.   Compare that with the 99 gallons per day that San Franciscans use, per capita, or the 287 gallons in Sacramento.  True, the conditions here are pretty extreme, but it’s an interesting experiment to see what it’s like to get along on 10 gallons of water each day. Of course, no one here is watering any lawns or trying to keep a swimming pool full.  And since we’re only allowed one load of laundry every two weeks, maybe everyone smells a little differently than they do in the rest of the US–but I think most people here would agree that living on 10 gallons of water a day isn’t half bad.

Field Notes from the Arctic: The Journey North

Sleeping quarters at Toolik Field Station, at midnight (photo: Gretchen Weber)

Naively, I thought Alaska’s “Haul Road” would be smooth.  For some reason, I’d pictured the 414-mile route that runs north, from near Fairbanks, to Deadhorse, near Prudhoe Bay, to be a picture of modern asphalt-laying engineering, and that, during our 350-mile drive to Toolik Field Station, I would be able to catch up on some of the sleep I’d been missing after two nights in a University of Fairbanks dorm room (think college students on summer break in a place where the sun barely sets).  After all, this is the road that tracks the Trans-Alaska Pipeline, connecting the largest oil field in North America (which happens to be operated by BP) to the rest of the continent.

As it turns out, I was heartbreakingly wrong.  Roughly a quarter of the road, which is officially called the Dalton Highway, is paved.  And the paved parts are actually the worst. Between the frost heaves caused by the alternate freezing and thawing of the ground, and those Ice Road Trucker tires chewing up the road, driving the Haul Road is more like an amusement park ride, at least from the back seat of a 15-person van.  Suffice it to say that I did not catch up on any sleep during the ride, which turned out to be a good thing, because the second half of this ride was through some of the most beautiful country I have ever seen.

View from just below Atigun Pass (4643 ft) in the Brooks Range (photo: Gretchen Weber)

About 70 miles north of Coldfoot, one of the three “towns” along the road, and 120 miles north of the Arctic Circle, we passed a sign marking the “Farthest North Spruce Tree.”  It actually wasn’t the farthest north spruce tree we saw, and also, it was dead, but right around there was where we crossed the treeline, leaving behind the white and black spruces stunted from extreme temperatures, and crossed into the tundra.

Back in Fairbanks, over breakfast (reindeer sausage), a biologist named Andi Lloyd had talked about her research on the treeline in Alaska.  There’s a lot of evidence showing that climate in the Arctic is changing faster than any place on Earth.  Here, mean winter temperatures have climbed between six and eight degrees F since 1960, and in summer, between two and three, said Lloyd.  This change is affecting how the boreal forest is expanding, she said, and causing the treeline to move north. In some places, such as the Seward Peninsula, Lloyd says it has moved ten kilometers (six miles) in the last century. “The Arctic is changing faster than we can study it,” said Lloyd.

But the relationship between climate change and the forest is not as simple as warmer temperatures equal northern expansion.  Rising temperatures also mean a drier environment, said Lloyd, as precipitation in the region has not increased as much as temperatures, and more warmth means more evaporation.  Lloyd and others have found that trees in the boreal forest are increasingly drought-stressed, which means they are growing much slower than they did in the mid 1900s, and that they are more vulnerable to insect infestation.

“I had a naive idea that the temperature controlled everything, but then I had a dawning awareness that the boreal forest is a moisture-limited forest,” she said.

There are no trees here at Toolik Station, where I will be for the next two weeks talking to scientists about the changing Arctic. The camp is nestled on the shore of Toolik Lake, in the northern foothills of Alaska’s Brooks Range. During the time I am here, the population of the camp will be about 140 people.  We arrived at 10 p.m., after 13 hours of driving, and the sun was still high in the sky.  It was still up there casting shadows when I awoke at 2:30 a.m.  At breakfast time, however, camp is encased in fog, and the temperature is about 45 degrees–kind of feels like I never left San Francisco.

Climate Watch associate producer Gretchen Weber is spending two weeks at Toolik Station, as a Logan Polar Science Fellow.

The Dalton Highway (photo: Gretchen Weber)

When Planes Punch “Holes” in the Sky

This post also appears at Climate Central, a content partner of Climate Watch.

By Michael D. Lemonick

How did this happen? The crazy-looking cloud formation in the photo above isn’t a still from a sci-fi movie. It’s not “Photoshopped.” It’s quite real.

It’s also totally artificial, which requires a bit of an explanation.

Since at least as early as the 1940s, meteorologists have been noticing formations like this, and it wasn’t long before they figured out that aircraft were probably involved somehow–perhaps by creating a pressure wave as they passed through, or by heating the clouds and evaporating them.

By the 1980s, says Andrew Heymsfield, a scientist with the National Center for Atmospheric Research (NCAR) in Boulder, Colorado, the holes had become more common and the explanation clearer: as planes punch through cloud decks that have particular characteristics, the air is compressed, then expands and cools, just like the coolant in an air conditioner. The cooling forces water droplets to freeze into tiny ice particles; these in turn act as seeds around which raindrops or snowflakes can form. The clouds then “rain out” or “snow out,” leaving a hole in their wake.

That’s the theory, anyway, though the phenomenon also makes great fodder for tabloids. But now Heymsfield has the smoking gun (outlined in a press release from NCAR), so to speak. Back in 2007, he and some colleagues flew their research aircraft through a snow squall west of Denver. They checked later with ground radar and learned that the band of precipitation was oddly shaped–about 20 miles long–but only about 2½ miles wide. It had appeared and disappeared quite abruptly, leaving a couple of inches of snow in its wake. Then they checked the cameras on their plane and discovered a hole in the clouds. Sandwiched between solid cloud decks, it wasn’t visible from the ground.

You might not have seen it from a satellite either; such holes are often hidden entirely. But that’s not the case in this image (below) from space, centered over the Texas-Louisiana border. Nearly all of the spots, big or small, are holes punched by ascending or descending aircraft. Some of the lines are also caused by planes traveling through the clouds at a constant altitude. “You can probably see around 50 of these artifacts in the image,” Heymsfield said.

The holes don’t just close up right away, either. “We’ve tracked some of them (by satellite) for up to five hours,” said Heymsfield.

If this phenomenon were just an example of gee-whiz science, the paper Heymsfield and four co-authors published about it in the Bulletin of the American Meteorological Society would be fascinating enough. But it turns out that it has military implications as well. Heymsfield has consulted with Boeing on how to fly jets so as not to leave their calling cards in the sky. “Military aircraft,” he notes, “really don’t want to be visible. (On the day the satellite image was taken) we saw a fantastic trail from a B-52.”

The study also underscores how one of our most natural instincts is simply wrong; that the Earth is so enormous, it seems impossible that human activity could alter the planet in any significant way. Unfortunately, there’s no lack of evidence showing how wrong our instincts can be. Oil spewing into the Gulf, another set of record warm temperatures, and endangered species wherever we look are just a few examples. Holes punched in clouds can now be added to the list of human modifications of the environment around us, even if the results do look like science fiction.

NCAR researcher Andrew Heymsfield discusses his aircraft-induced cloud modification study. (Video: NCAR)

“Merchants of Doubt” Traces Roots of Denial

A new book asserts that the very same group of Cold War ideologues who banded together to spread doubt about the link between tobacco and cancer also spearheaded the first efforts to discredit climate scientists as they began warning about the effects of anthropogenic global warming.

In “Merchants of Doubt,”  science historians Naomi Oreskes of UC San Diego and Erik Conway of the NASA Jet Propulsion Laboratory at CalTech, argue that the seeds of the current groundswell of climate change “denial,” and an assault on science in general, were planted decades ago.

The authors say it started with a handful of respected scientists, who, motivated by free-market political ideology and funded by the tobacco industry, worked to cast doubt on well-established scientific knowledge.

Conway discussed the book last Friday with Greg Dalton of Climate One at the Commonwealth Club of San Francisco.

“One of the strategies the tobacco companies decided to pursue in the early 1990’s is the undermining of science, broadly,” said Conway. “They began to use their PR apparatus not just to undermine the science of tobacco and cancer and health effects, but…to attack all regulatory sciences in general.”

That strategy was one of the motivations for the book, said Conway.  “We wondered, ‘What effect will this have on science when it’s being under continuous corporate assault, especially in a society that is very dependent on science and engineering?”

According to Conway, one of the scientists central to the tobacco industry’s efforts was Fred Seitz, a physicist and former president of the U.S. National Academy of Sciences.   Others were the prominent physicists Fred Singer, Robert Jastrow, and William Nierenberg, who was once the director of the Scripps Institution of Oceanography in San Diego.  All were associated with a conservative think tank, the George C. Marshall Institute.  In the 1990’s, said Conway, “the Marshall Institute decided to make its main issue the effort to cast doubt on global warming.”

Conway said that the scientists were motivated by their experiences during the Cold War and the political beliefs they developed during that time.

“Really, this is about opposition to government regulation,” he said. “We don’t think the scientists were in this for the money. They were working for the tobacco industry, to defend Star Wars (the Reagan administration’s space defense plan), to prevent acid rain and global warming regulation.” Conway says these “merchants of doubt” were pursuing “a political ideology to defend market fundamentalism and their political beliefs, not because they were in the pay for big money.”

The authors argue that the legacy of this Cold War ideology lives on in today’s climate change “denial” discourse.  The seeds planted then continue to sprout, they contend, despite the fact that today’s “merchants” are far less influential within the scientific community.

“There is a second generation, but one that is not nearly as respected,” said Conway. “The think tank network  now exists and has been institutionalized and is self-perpetuating. They simply hire their own people who have some credentials, rarely actually climate scientists, who continue to do that kind of thing.  But they don’t have nearly the kind of stature that Nierenberg did or that Fred Seitz had.”

A 2008 study also makes a link between conservative think tanks an climate skepticism.  The report, published in the journal Environmental Politics, found that of 141 English-language, “environmentally sceptical” books published between 1972 and 2005, 92% have links to conservative think tanks, 90% of which, the report found, “espouse environmental scepticism.”

NASA Launches Arctic Sea Ice Expedition

Coast Guard Cutter Healy (Photo by Petty Officer Patrick Kelley, US Coast Guard)

Next week, a NASA team of more than 40 scientists will take to the seas for a five-week expedition in the Arctic to study how changing conditions there are affecting ocean chemistry and ecosystems.  The voyage, NASA’s first dedicated oceanographic research mission, is named ICESCAPE, which stands for “Impacts of Climate on Ecosystems and Chemistry of the Arctic Pacific Environment.”  It will take place aboard the US Coast Guard Cutter Healy.

“We’re  trying to address what is the long term impact of climate variability and change, both natural and anthropogenic, on the biogeochemistry and ecology of the Arctic,” said Paula Bontempi, program manager for NASA’s ocean biology and biogeochemistry research program.

The expedition will give scientists a chance to make field observations about the ocean, sea ice, and the atmosphere in regions where researchers often must rely on remote sensing technology for their data.  One main focus of the research will be to observe how changes, such as a substantial decrease in sea ice, may be affecting the ocean’s ability to absorb CO2 from the atmosphere and the consequent effects on ecosystems.

“The Arctic is in the midst of some substantial changes,” said ICESCAPE Chief Scientist Kevin Arrigo of Stanford.  “In the last 10 years, the ice-free season in the Arctic Ocean has increased by about 45 days.  And this has a big impact on organisms in the Arctic that are keyed to these events.”

Arrigo says that the sea ice retreats about 28 days sooner than it did just a decade ago, and advances about 17 days later. He says this change has shifted the timing of food production.  Phytoplankton, the base of the food chain in the Arctic Ocean, are now growing a month earlier than they did in the 1990s, says Arrigo, which could spell a problem for organisms such as the California gray whales, which time their migrations around peak food production.

“Over the years satellite imagery has shown a significant decline in the Arctic ice cover,” said Don Perovich, a research geophysicist at the Cold Regions Research and Engineering Laboratory in Hanover, NH, who is part of the ICESCAPE expedition. “But there’s really more to it than just the ice.  It’s important to remember that sea ice isn’t just some isolated component. It’s part of larger system.”

Sea ice, he said, serves as a barrier between the atmosphere and the ocean, limiting the exchange of heat, moisture and gases; acts as a reflector of sunlight; and is a habitat for a rich marine ecosystem.

“It’s an ecosystem where sea ice and biology are intricately intertwined,” said Perovich. “You can think of the ice and the biology as executing this intricate dance, but it’s a dance where one of the partners has started changing its steps. And that partner is the sea ice cover.”

The 2010 ICESCAPE expedition starts in Dutch Harbor in the Aleutian Islands, will continue across the southern Chukchi Sea and into the Beaufort Sea along Alaska’s northern shelf.  A second expedition is planned for 2011.   NASA estimates the cost of the ICESCAPE project to be $10 million over four years.

The expedition blog has already launched, and will be updated daily once the expedition is underway, according to NASA spokesman Steve Cole.

I’ll be launching my own “Arctic expedition” next week.  Starting June 18th, I’ll be spending two weeks with climate scientists at the Toolik Field Station in northern Alaska, as part of the Logan Science Journalism Program, run by the Marine Biological Laboratory in Woods Hole, MA.   Check back here for periodic dispatches about the science, the landscape, and the impacts of constant daylight on one journalist’s mental state.

Study Eyes Climate Impacts on Ocean Ecosystems

Farallone Islands (Photo: Jan Roletto, NOAA)

The north-central California coast is likely to experience rising seas, more extreme weather events and coastal erosion, increased ocean acidity, and shifting marine habitats as a result of climate change, according to a new report released today from the National Oceanic and Atmospheric Administration.

The report, “Climate Change Impacts: Gulf of the Farallones and Cordell Bank National Marine Sanctuaries,” was developed in collaboration with 16 agencies and organizations and was released today at the California Academy of Sciences in San Francisco.

“This report provides insight into how climate change will play out in our region, how the ocean environment in the Gulf of the Farallones and over Cordell Bank will change and how the organisms that live there will be impacted by it,” said the report’s lead author, oceanographer John Largier of the Bodega Marine Laboratory and UC Davis.

Largier was careful to explain that the report does not make predictions about the future, nor is it a complete assessment of current conditions.

“It’s a group of scientists getting together and making their best judgment of how things are changing, how things will change, and what are we most concerned about,” said Largier.

Topping the list of concerns, he said, are rising sea levels of approximately 1.5 meters by 2100, warming oceans, an increase in the variability of precipitation (drier dry years and wetter wet ones), and ocean acidification, which he called, “the other CO2 problem,” and stressed as both a global and regional concern.

“There are a lot of things we know that are happening.  The real question we have to figure out now is how much this could all this change the ecosystem,” said Largier.  “The system is so complex, it’s not totally clear how it’s going to evolve.  Some populations might do a lot better with climate change, and others are going to be hammered. ”

NOAA
Image: NOAA

The report makes some recommendations for the sanctuaries, including a greater focus on public education, implementing policies that allow for flexibility and adaptation to change, and mitigating other factors that impact the ecosystem such as pollution, invasive species, fishing, and infrastructure development.

“We are just now getting to the state where we say what does climate change mean for us, for my community?” said Largier.  “It’s warming, sure, but what does it mean for ‘here’?  How is it going to play out? And what are the things that are going to happen that really matter at a regional and local level?  This is a huge scientific challenge that we are struggling with, but it’s an essential management and policy challenge.”

Bill Douros, the West Coast Regional Director of NOAA’s Marine Sanctuary program expressed the same sentiment in his opening remarks at the Cal Academy today.

“As we all know, the ocean is going to warm, it’s going to get more acidic, sea levels are going to rise, and those concepts are important, but what’s really important to someone who might be managing those marine protected areas is “How much?” and “By when are the sea levels going to rise and temp going to increase?”  And that’s what this report today provides to us.”

Key Issues highlighted in the report:
⇒ Observed increase in sea level (100-year record at mouth of San Francisco Bay)

⇒ Expected increase in coastal erosion associated with changes in sea level and storm waves

⇒ Observed decrease in spring runoff of freshwater through San Francisco Bay (decreased Sierra snowpack)

⇒ Observed increase in precipitation variability (drier dry years, wetter wet years)

⇒ Observed increase in surface ocean temperature off the continental shelf
(50 year record)

⇒ Observed increase in winds driving coastal upwelling of nutrient-rich waters and
associated observed decrease in surface ocean temperature over the continental
shelf (30 year record)

⇒ Observed increase in extreme weather events (winds, waves, storms)

⇒ Expected decrease in seawater pH, due to uptake of CO2 by the ocean

⇒ Observed northward shift of key species (including Humboldt squid, volcano
barnacle, gray whales, bottlenose dolphins)

⇒ Possible shift in dominant phytoplankton (from diatom to dinoflagellate blooms)

⇒ Potential for effects of climate change to be compounded by parallel
environmental changes associated with local human activities

Fire Data: Dry Winters Mean More Charred Acres

Tim Walton
Photo: Tim Walton

Last year around this time, I asked some state fire officials what to expect in terms of the fire season and got a definite “It depends.” On the one hand, scant precipitation over the winter had left behind a dry landscape. On the other hand, spring rains had given a boost to rebounding vegetation, providing more fuel for later in the season. I was reminded of the old joke about politicians searching for a “one-handed economist” and found myself wishing for a one-handed forester.

Whether a good spring dousing is more likely to inhibit wildfires or feed them is a common source of confusion, which San Jose Mercury News writer Paul Rogers has sought to extinguish. By dipping into four decades of fire data, Rogers and his researchers at the Merc conclude that dry winters generally make for more intense fire seasons in California.

Rogers writes that “the worst fire seasons come after dry winters, not wetter ones like the one we’ve just had.” That would seem to bear out a conversation I had in 2007 with Crawford Tuttle, Chief Deputy Director at CalFire, fire protection arm of the state’s department of forestry. Walking through the burn zone of a Sierra wildfire that broke out in May of that year, Tuttle said that early-season fire was “a great demonstration of how (the) fire regime–fire severity is expanding in California.” Tuttle told me that when moisture levels in the air, vegetation and soil are lower, earlier in the season, it’s likely that the fire season will be intense.

The preceding winter had been dry by historical standards, with just over half the normal amount of precipitation and indeed, wildfires went on to char almost a million acres in the state that year.

Rising Temps Taking a Toll on Lizards

The mesquite lizard is a member of the Sceloporus genus. Sinervo’s study included 48 species of Sceloporus.

A new study published this week in the journal Science finds that local lizard populations around the world are going extinct, likely due to climate change.  According to the research, conducted by a team of scientists including Barry Sinervo, a herpetologist at UC Santa Cruz, four percent of the world’s lizard populations have disappeared in the last 35 years, and another 20% of all lizard species could go extinct by 2080 if global temperatures continue to rise.

Using field observation and experiments, and computer modeling, Sinervo and his team determined that increased daytime temperatures in some areas have shortened the amount of time each day during which lizards can forage for food. The data–and that of collaborating scientists on five continents–indicates that higher temperatures and reduced feeding time correlates with the pattern of local extinctions among lizard species across the globe (the Science website has a slideshow explaining how the research was conducted).

Sinervo described his research today on the NPR program Science Friday as part of a panel discussing modern extinctions.  He was joined by UC Berkeley integrative biology professor Tony Barnosky and San Francisco State Biology professor Vance Vredenberg.  Christopher Joyce reported on the study’s findings yesterday on NPR’s All Things Considered.

Polls Underestimate Climate Change Concerns, Study Finds

A historic water marker left high and dry at Lake Powell in April 2010. (Photo: Gretchen Weber)

If you’ve been paying attention at all over the last year, you’ve no doubt heard that Americans don’t care very much about climate change.  Pew polls, Yale polls, Gallup polls–all have found in the past year that climate change and the environment rank pretty much dead last when it comes to issues people care about in the United States.  But new research out of Stanford suggests that the truth might actually be a bit more complicated, and that Americans might be a lot more concerned about climate change than these polls indicate.

As it turns out, it’s all in the asking.

Jon Krosnick, a Senior Fellow at Stanford’s Woods Institute for the Environment, recently found that the standard “Most Important Problem” question, which has been a staple of polls and surveys for generations, might not capture the true nature of public sentiment toward environmental issues.

Krosnick has been studying the public’s perception of climate change since the 1990s. He said that during that time his findings have continually indicated that “huge majorities” agreed that the planet is heating up and that the government should take action, but that global warming was repeatedly left off the list when people were asked what was the country’s most important problem.

It was a Stanford undergraduate, Samuel Larson, who suggested that perhaps how the question was being asked was influencing the answers, said Krosnick.  Maybe, Larson postulated, if the question were opened up to consider the world, rather than just the United States, and if it asked about the future, rather than today, people’s answers might reflect something different.

In fact, their answers changed dramatically, researchers found.  In the May 2010 study, the team analyzed the results of two polls from the fall of 2009 that addressed the issue in two distinct ways.   When asked, “What do you think is the most important issue facing the world today?” about half (49%) of respondents in the first poll answered “the economy” or “unemployment,” while only one percent mentioned global warming or the environment.  In the second poll, the responses were 54% economy and two percent environment.

But when the question was re-framed as “What do you think is the most serious problem facing the world in the future if nothing is done to stop it?” the results swung dramatically.  In the first poll, 25% said the environment or global warming, and 10% said the economy.  In the second poll the results were 21% and 16%, respectively.

For specific data on Californians and their views on environmental issues and climate policy, see last summer’s PPIC report: Californians and the Environment.