Posts Tagged ‘climate’

Trees to the (partial) rescue!

June 23rd, 2011 by Sarah Pryputniewicz

The Earth is getting warmer.  In warmer climes, decomposition occurs more quickly.  This releases more carbon dioxide into the atmosphere, leading to further warming.  But it needn’t get completely out of control–trees (and other plants) can come to the rescue!

A recent study in a central Massachusetts forest has shown that increased temperatures do indeed lead to increased decomposition.  But they also led to increased tree growth, partially offsetting the carbon dioxide release from decomposition.  Why?  The researchers found that nitrogen was also being liberated by the decomposition.

Because tree growth is limited by the availability of nitrogen, an increased supply of nitrogen results in increased growth.  The trees’ growth spurts result in some of the carbon dioxide being stored in the wood rather than being released into the atmosphere.  Unfortunately, the trees don’t take in ALL of the released carbon dioxide… trees to the (partial) rescue!

http://www.sciencedaily.com/releases/2011/05/110525120050.htm

The frozen tundra could heat the Earth

February 22nd, 2011 by Sarah Pryputniewicz

A new study from the University of Colorado suggests that 66% of Earth’s permafrost could disappear by the year 2200.  And this could be really bad for Earth’s temperature.

If the temperature increases, the permafrost melts.  Simple enough, right?  But it’s slightly more complicated.  Trapped in the permafrost is lots and lots of carbon–in the form of plant material trapped in the frozen soil.

When it’s frozen, bacteria and fungi don’t break it down quickly.  But when it’s thawed out, the plant material quickly decays.  As soil bacteria and fungi break down the organic matter, they release tons of carbon dioxide into the atmosphere. This leads to higher temperatures and more thawing permafrost.

“The amount we expect to be released by permafrost is equivalent to half of the amount of carbon released since the dawn of the Industrial Age,” said Kevin Schaefer, lead author on the study.

Greater reductions in fossil fuel emissions to account for carbon released by the permafrost will be a daunting global challenge, Schaefer said. “The problem is getting more and more difficult all the time,” he said. “It is hard enough to reduce the emissions in any case, but now we have to reduce emissions even more. We think it is important to get that message out now.”

http://www.sciencedaily.com/releases/2011/02/110216132100.htm

Explore the relationship between temperature and greenhouse gases in our activity, “What will Earth’s climate be in the future?

Going up?

February 17th, 2011 by Sarah Pryputniewicz
A new study from the University of Washington suggests that Earth’s temperature will keep increasing, even if all greenhouse gas emissions were stopped right now.
Why?  Because greenhouse gases will last longer in the atmosphere than particulate matter (aerosols) that reflect the sun’s light.  So, the solar radiation coming in will increase and the heat energy will be reflected by the greenhouse gases.  (Explore the relationship between temperature, greenhouse gases, and albedo in our activity, “What will Earth’s climate be in the future?“)
How much would the temperature rise if we were able to cut all greenhouse gas emissions right now?  In the best case scenario, global temperature will actually decline.  In the worst case scenario, the global temperature would rise by 3.5°F.
Why the big disparity?  Scientists don’t really know the overall effect of the aerosols, particles as disparate as soot from burning fossil fuels and sea salt.  But this doesn’t mean that their predictions are worthless:
“… uncertainties do not lessen the importance of the findings, he said. The scientists are confident, from the results of equations they used, that some warming would have to occur even if all emissions stopped now. But there are more uncertainties, and thus a lower confidence level, associated with larger temperature increases.”
Ending all greenhouse gas emissions immediately is not a realistic option.  So Earth’s temperature will likely increase further.  How much?  Scientists are still tweaking the models to determine that.
http://www.sciencedaily.com/releases/2011/02/110215150845.htm

Slow down glacial flow with warmer summers?

January 28th, 2011 by Sarah Pryputniewicz
It seems counter-intuitive, but it seems that warmer summers actually slow the flow of Greenland’s ice sheets.
A new study, published yesterday in Nature, explains how increased melting in warmer years causes the internal drainage system of the ice sheet to change, slowing the glacier’s flow towards the ocean.
Normally, the melt-water finds its way to the bottom of the ice sheet, acting as a lubricant that helps the glacier to flow towards the ocean.  With less melt-water below the glacier, its flow is impeded, so it doesn’t recede as quickly.
So, are hot summers the cure to glacial melting?  Obviously not.
Warmer temperatures do cause more melting.  Although the glaciers aren’t moving towards the ocean faster, they are melting from the surface downwards.  The big difference is in the plumbing–whether the melt-water is trapped under the glacier, lubricating its path to the sea, or whether the melt-water is drained away through a different plumbing system.  The ice will still melt.
This surprising data just shows that more research is needed to fully understand how glaciers are affected by changing temperatures.  Dr. Edward Hanna, one of the co-authors, underscored the importance of using models in studying the relationship between glacial melt and climate change:
“This work also underlines the usefulness of modern gridded climate datasets and melt-model simulations for exploring seasonal and year-to-year variations in Greenland ice sheet dynamics and their relationship with the global climate system.”
Explore the relationship between temperature and ice-melting in our activity, “What will Earth’s climate be in the future?
http://www.sciencedaily.com/releases/2011/01/110126131538.htm

It’s going to be a warm one in the south…

January 24th, 2011 by Sarah Pryputniewicz

Warm millennium, that is.  And Southern Hemisphere, that is.

New research suggests that Earth will continue to warm into the year 3000, even if human-caused carbon dioxide emissions stop right now.  According to their models, scientists predict that the Northern Hemisphere will fare much better, with the warming trend reversing within the millennium.  This is likely due to the much larger landmass in the Northern Hemisphere.

The Southern Hemisphere has much more ocean surface, which has thus far slowed the warming trend, as the ocean acts as a huge carbon dioxide and heat sink.

Shawn Marshall, Canada Research Chair in Climate Change and University of Calgary geography professor, explains this phenomenon:

“The global ocean and parts of the Southern Hemisphere have much more inertia, such that change occurs more slowly. The inertia in intermediate and deep ocean currents driving into the Southern Atlantic means those oceans are only now beginning to warm as a result of CO2 emissions from the last century. The simulation showed that warming will continue rather than stop or reverse on the 1000-year time scale.”

Does this mean certain doom for the planet?  No.  Throughout its history, Earth has had warmer periods than the one that is predicted by these models.  The Earth will be just fine.  The big question, for us humans, is how humans will fare.

Explore the role of oceans in Earth’s climate with our activity, “What will Earth’s climate be in the future?

http://www.sciencedaily.com/releases/2011/01/110109184025.htm

Burning the rainforest to cool the globe

December 22nd, 2010 by Sarah Pryputniewicz
Burning plant material in the Amazon rain forest can be good for the planet?
Yes–provided it’s done in the right way.  A scientist at Cornell University has discovered that the ancient practice of burning biomass underground, starved of oxygen.  The process produces “terra preta” (also known as “black gold” and biochar)–a carbon-rich soil that helps to fertilize the ground, making it possible to grow food crops in the nutrient-poor rainforest soil.
Johannes Lehmann holds biochar, left, and the biomass from which it was created
University Photography: Johannes Lehmann holds biochar, left, and the biomass from which it was created
In addition, burning the biomass underground produces “syngas,” an energy source that can be used to power homes and equipment.  Those are great benefits for the locals, but this process benefits everyone on the planet since it helps to store carbon in the soils.  Biochar can be 80% or more pure carbon!
The ancient people may not have known about global warming, but they did know how to sustain the local ecosystems.  This just adds more meaning to the old slogan, “Think Globally, Act Locally!”
Learn more about how carbon dioxide enhances global warming in our “What will Earth’s climate be in the future?” investigation.
Read more about biochar at: http://calsnews.cornell.edu/2010-fall/features/biochar.html

Science and Politics: What to do?

December 21st, 2010 by Sarah Pryputniewicz

From xkcd: http://www.xkcd.com/164/

Science is about facts and evidence.  There is a lot of evidence that carbon dioxide is a greenhouse gas.  You can explore with our models how carbon dioxide impacts the global temperature.

Politics is about what to do about those facts.  But politics too often turns into a blame game, in which people take sides without really listening to the evidence.

Do we ban the burning of fossil fuels because it increases carbon dioxide emissions?  Do we look  for ways to capture all carbon dioxide emissions from human activities?  Do we impose a “carbon tax” on all goods?  What would be the economic impacts of these policies?  Is the electronics-centric lifestyle to which we’ve become accustomed even compatible with low carbon dioxide emissions?

In the end, it all comes down to a cost-benefit analysis of the risks and rewards for each course of action.  What risks do we undertake by doing nothing?  What risks do we undertake by completely changing the ways by which people travel around the world?  What benefits do we gain from each action?

But to do a cost-benefit analysis, we have to understand the facts; we have to understand our “known knowns”–what we know we know–and our “known unknowns”–what we know we don’t know.  We have to remember that there are always “unknown unknowns”–those things that we don’t even know that we don’t know.

That’s why it’s up to each of us, as individuals, to learn about the science–about the facts and the real evidence and what’s still not fully understood–and then choose our actions based on our own understandings of the facts and preponderance of the evidence, not on someone else’s views.  We have to think for ourselves and act accordingly.

But we also have to remember that our actions impact those around us.  We’re all on this planet together.

Tracking the Permafrost Line

December 20th, 2010 by Sarah Pryputniewicz

From xkcd: http://www.xkcd.com/402/

The permafrost line is shifting.  It may be slow by tornado-chasing standards, but it’s shifting.

A study earlier this year from Université Laval in Quebec City, Canada showed that the permafrost line has moved northward by 130 kilometers in the last 50 years.  While climate change is the most probable explanation for the melting permafrost, there is not enough long-term data for scientists to confirm this.

And so the research goes on to study and better understand our ever-changing world.

Learn more about climate change in our “What will Earth’s climate be in the future?” investigation.

Carbon dioxide as a structural component?

December 20th, 2010 by Sarah Pryputniewicz
Yes–if you’re a coral.  Biologist Brent Constantz has formed a company to sequester carbon dioxide just as corals in the ocean do.  The strategy is simple–combine carbon dioxide, water, and calcium.  The carbon dioxide comes from the smokestacks of electrical power plants, and the water and calcium come from seawater.
The material produced is used to make cement that can be used to build buildings, just as corals build their limestone structures.  The first plant is capable of sequestering 550 tons of carbon dioxide per day.  With more plants scheduled to be built, this could make a significant impact on the level of carbon dioxide in the atmosphere.
Big buildings may one day be a sign of a carbon-capturing (rather than carbon-emitting) society…
Learn more about how carbon dioxide and global warming in our “What will Earth’s climate be in the future?” investigation.
Read the full article from Popular Science at: http://www.popsci.com/bown/2010/innovator/cement-thin-air

Climate and Pollution

December 6th, 2010 by Sarah Pryputniewicz

Pollution has its benefits.

With fewer particulates being released by smokestacks and cars, there are fewer aerosols in the atmosphere.  Fewer aerosols means that more solar radiation hits the ground.  With more sunlight hitting the Earth, the Earth warms up–faster than many scientists had initially predicted.

Calculations by Jan Magnus, Bertrand Melenberg, and Chris Muris, econometricians at Tilburg University in the Netherlands, suggest that carbon dioxide emissions will have to be reduced by an additional 50 million tons to compensate for the additional solar radiation reaching the surface.  That’s just to keep the temperature rise to 2 degrees Centigrade!

The Clean Air Act of 1970 gave us clear blue skies and pure white snows, but they weren’t counting on enhanced carbon dioxide emissions to accelerate the warming process.

Read the summary at http://www.sciencedaily.com /releases/2010/03/100309083700.htm.

Learn how albedo affects global temperature with our models in the “What will Earth’s climate be in the future?” investigation.