http://www.carboncapturereport.org/about.html
Tuesday, November 16, 2010
Carbon Capture Report
http://www.carboncapturereport.org/about.html
Sunday, November 14, 2010
Revisiting Limits To Growth: Could The Club Of Rome Been Correct
http://www.greatchange.org/ov-simmons,club_of_rome_revisted.pdf
Friday, October 29, 2010
Jeff Rubin ASPO-USA 2010 Peak Oil Conference
Jeff Rubin ASPO-USA 2010 Peak Oil Conference from ASPO-USA on Vimeo.
Jeff Rubin (born August 24, 1954) is a Canadian economist and author. He is a former chief economist at CIBC World Markets.
Rubin graduated from McGill University with a Masters in Economics after completing his Economics B.A. at University of Toronto. He began his career as an economist at the Ontario Government Treasury Department where he was responsible for projecting future interest rates. He moved on to the brokerage firm Wood Gundy which was taken over by CIBC and became first CIBC Wood Gundy and then CIBC World Markets. He has accurately predicted fluctuations in interest rates and the value of the Canadian dollar. In the early 1990s he came to prominence projecting a major decline in the Ontario real estate market. He was one of the first economists to accurately predict soaring oil prices back in 2000 and is now a popular commentator on oil depletion and its economic repercussions. Jeff writes a blog published every Wednesday for The Globe and Mail newspaper. He is an avid fisherman known for exotic trips to northern Canada (B.C. and Yukon) who frequently uses fishing analogies and references to his own fishing experiences, in his writings.[1]
Rubin had worked at CIBC World Markets and its predecessors since 1988, and served as chief economist from 1992 to 2009, when he resigned.[2]
He authored the best selling 2009 book Why Your World Is About to Get a Whole Lot Smaller: Oil and the End of Globalization.[3][4]
Friday, August 13, 2010
The physics of climate modeling
Climate is a large-scale phenomenon that emerges from complicated interactions among small-scale physical systems. Yet despite the phenomenon's complexity, climate models have demonstrated some impressive successes.
| 1991 eruption of Mount Pinatubo |
The task climate modelers have set for themselves is to take their knowledge of the local interactions of air masses, water, energy, and momentum and from that knowledge explain the climate system's large-scale features, variability, and response to external pressures, or "forcings." That is a formidable task, and though far from complete, the results so far have been surprisingly successful. Thus, climatologists have some confidence that theirs isn't a foolhardy endeavor.
Climate modeling derives from efforts first formulated in the 1920s to numerically predict the weather. However, it wasn't until the 1960s that electronic computers were able to meet the extensive numerical demands of even a minimal description of weather systems. Since then, ever more components have been added to climate models—land, oceans, sea ice, and more recently, interactive atmospheric aerosols, atmospheric chemistry, and representations of the carbon cycle. Indeed, a significant part of the interdisciplinary work needed to understand climate change is being driven by climate model development. Today's models are flexible tools that can answer a wide range of questions, but at a price: They can be almost as difficult to analyze and understand as the real world.
Basic physics, emergent behavior
The physics in climate models can be divided into three categories. The first includes fundamental principles such as the conservation of energy, momentum, and mass, and processes, such as those of orbital mechanics, that can be calculated from fundamental principles. The second includes physics that is well known in theory, but that in practice must be approximated due to discretization of continuous equations. Examples include the transfer of radiation through the atmosphere and the Navier–Stokes equations of fluid motion. The third category contains empirically known physics such as formulas for evaporation as a function of wind speed and humidity.
For the latter two categories, modelers often develop parameterizations that attempt to capture the fundamental phenomenology of a small-scale process. For instance, the average cloudiness over a 100-km2 grid box is not cleanly related to the average humidity over the box. Nonetheless, as the average humidity increases, average cloudiness will also increase. That monotonic relationship could be the basis for a parameterization, though current schemes are significantly more complex than my example.
Given the nature of parameterizations among other features, a climate model depends on several expert judgment calls. Thus, each model will have its own unique details. However, much of the large-scale behavior projected by climate models is robust in that it does not depend significantly on the specifics of parameterization and spatial representation.
The most interesting behavior of the climate system is emergent. That is, the large-scale phenomena are not obvious functions of the small-scale physics but result from the complexity of the system. For instance, no formula describes the Intertropical Convergence Zone of tropical rainfall, which arises through a combination of the seasonal cycle of solar radiation, the properties of moist convection, Earth's rotation, and so on. Emergent qualities make climate modeling fundamentally different from numerically solving tricky equations.
Climate modeling is also fundamentally different from weather forecasting. Weather concerns an initial value problem: Given today's situation, what will tomorrow bring? Weather is chaotic; imperceptible differences in the initial state of the atmosphere lead to radically different conditions in a week or so. Climate is instead a boundary value problem—a statistical description of the mean state and variability of a system, not an individual path through phase space. Current climate models yield stable and nonchaotic climates, which implies that questions regarding the sensitivity of climate to, say, an increase in greenhouse gases are well posed and can be justifiably asked of the models. Conceivably, though, as more components—complicated biological systems and fully dynamic ice-sheets, for example—are incorporated, the range of possible feedbacks will increase, and chaotic climates might ensue.
Testing climate models
Model assessment occurs on two distinct levels—the small scale at which one evaluates the specifics of a parameterization and the large scale at which predicted emergent features can be tested. The primary test bed is the climate of the present era, particularly since 1979, when significant satellite data started to become readily available.
The 1991 eruption of Mount Pinatubo provided a good laboratory for model testing (see the figure). Not only was the subsequent global cooling of about 0.5 °C accurately forecast soon after the eruption, but the radiative, water-vapor, and dynamical feedbacks included in the models were quantitatively verified.
More than a dozen facilities worldwide develop climate models, whose ability to simulate the current climate has improved measurably over the past 20 years. Interestingly, the average across all models almost invariably outperforms any single model, which shows that the errors in the simulations are surprisingly unbiased. Significant biases common to most models do exist, however—for instance, in patterns of tropical precipitation.
Climate modelers are particularly interested in testing the variability of their models. Some variability is intrinsic, but modelers also study variability caused by changes in external forcings, such as in Earth's orbit or in solar activity. Those studies are complicated by incomplete observations, the nature of satellite data, uncertainties in the forcings, and other issues.
The most comprehensive comparison of models ever conducted is now under way using simulations that were performed in 2004 and 2005 for the Intergovernmental Panel on Climate Change. Those simulations for the 20th century and beyond are being examined by hundreds of independent teams who will assess the robustness of the results and help illuminate persistent problems.
Many challenging climate questions remain unanswered. Examples include how climate conditions influence El Niño; how responses can be predicted at the regional scale; and how simulations of rare, extreme events such as hurricanes and heat waves can be validated. Such issues may require better encapsulations of, for example, the turbulent behavior of the near-surface atmosphere, the effects of ocean eddies, or the microphysics of clouds and aerosols. The implementation of more sophisticated parameterizations and the ongoing increases in resolution as computer resources increase suggest that models will continue to improve. However, many results, such as the warming effect of increasing greenhouse gases that was first demonstrated in much simpler models decades ago, have proved extremely robust.
Climate models are unmatched in their ability to quantify otherwise qualitative hypotheses and generate new ideas that can be tested against observations. The models are far from perfect, but they have successfully captured fundamental aspects of air, ocean, and sea-ice circulations and their variability. They are therefore useful tools for estimating the consequences of humankind's ongoing and audacious planetary experiment.
Gavin Schmidt is a research scientist at the NASA Goddard Institute for Space Studies (http://www.giss.nasa.gov) in New York.
Additional resources
Wednesday, August 11, 2010
Soojenemise loogika
- Humans are currently emitting around 30 billion tonnes of CO2 into the atmosphere (CDIAC). Of course, it could be coincidence that CO2 levels are rising so sharply at the same time so let’s look at more evidence that we’re responsible for the rise in CO2 levels.
- When we measure the type of carbon accumulating in the atmosphere, we observe more of the type of carbon that comes from fossil fuels (Manning 2006).
- This is corroborated by measurements of oxygen in the atmosphere. Oxygen levels are falling in line with the amount of carbon dioxide rising, just as you’d expect from fossil fuel burning which takes oxygen out of the air to create carbon dioxide (Manning 2006).
- Further independent evidence that humans are raising CO2 levels comes from measurements of carbon found in coral records going back several centuries. These find a recent sharp rise in the type of carbon that comes from fossil fuels (Pelejero 2005).
- So we know humans are raising CO2 levels. What’s the effect? Satellites measure less heat escaping out to space, at the particular wavelengths that CO2 absorbs heat, thus finding “direct experimental evidence for a significant increase in the Earth’s greenhouse effect”. (Harries 2001, Griggs 2004, Chen 2007).
- If less heat is escaping to space, where is it going? Back to the Earth’s surface. Surface measurements confirm this, observing more downward infrared radiation (Philipona 2004, Wang 2009). A closer look at the downward radiation finds more heat returning at CO2 wavelengths, leading to the conclusion that “this experimental data should effectively end the argument by skeptics that no experimental evidence exists for the connection between greenhouse gas increases in the atmosphere and global warming.” (Evans 2006).
- If an increased greenhouse effect is causing global warming, we should see certain patterns in the warming. For example, the planet should warm faster at night than during the day. This is indeed being observed (Braganza 2004, Alexander 2006).
- Another distinctive pattern of greenhouse warming is cooling in the upper atmosphere, otherwise known as the stratosphere. This is exactly what’s happening (Jones 2003).
- With the lower atmosphere (the troposphere) warming and the upper atmosphere (the stratophere) cooling, another consequence is the boundary between the troposphere and stratophere, otherwise known as the tropopause, should rise as a consequence of greenhouse warming. This has been observed (Santer 2003).
- An even higher layer of the atmosphere, the ionosphere, is expected to cool and contract in response to greenhouse warming. This has been observed by satellites (Laštovi?ka 2006).
Tuesday, August 10, 2010
Norwegian Company Designs Giant 10MW Wind Turbine
A majority of the wind farms in the United States use 2.5 megawatt
Europe has seen a lot of advantages to building larger wind turbines, such as avoiding environmental issues by using larger turbines in deeper waters. There is less of a risk of encountering environmental problems the further offshore the turbines are located. Europe seems to build larger turbines as the water grows deeper, as well.
Another advantage to building larger turbines is the cost. The cost per megawatt decreases as the the size of the wind
The 533 foot tall wind turbine was designed by Sway, a Norwegian turbine developer, and will have 476 foot long blades. Sway has been working on the design since 2004, but the company is not working on Europe's largest turbine alone. It is partnering with Norwegian state utility Enova and UK-based Clipper Marine to bring the 10 megawatt monster turbine to life.
The giant turbine certainly dwarfs the 2.5 megawatt and the newer 5 megawatt turbines being used now. In fact, it is so large that it requires a whole new offshore wind design.
The new design does not attach the wind turbine to the sea floor like smaller models. This 10 megawatt turbine, while giant in size, will be lightweight enough to "sway" around a fixed base and float in the ocean. It also has the ability to swivel on this base to produce energy when the direction of the wind changes.
"This is pioneering stuff," said Feargal Brennan, head of offshore, process and energy engineering at Cranfield University. "I believe 10MW turbines are right on the limit of our knowledge; they may even prove to be over the limit. We may find that they work for several years and then start to develop problems. Will 10MW turbines still be working after 10, 15, 20 years of operation?"
In an attempt to answer that question,
While Sway, Clipper Marine and Enova are on their way with this development, they're not the only ones. According to other reports, British company Wind Power Limited has recently exposed the details its new 10 megawatt offshore wind generator, called Aerogenerator X. This unit is expected to reach completion by 2013 or 2014, and will generate enough electricity for 5,000 - 10,000 homes.
http://www.dailytech.com/Norwegian+Company+Designs+Giant+10MW+Wind+Turbine/article19275.htm
Monday, August 9, 2010
Küsiltus
This survey is part of an investigation of general public opinion concerning a variety of social issues.
You will probably find that you agree with some of the statements, and disagree with others, to varying
extents. Please indicate your reaction to each statement on the line to the left of each item according
to the following scale:
Write down a -4 if you very strongly disagree with the statement.
Write down a -3 if you strongly disagree with the statement.
Write down a -2 if you moderately disagree with the statement.
Write down a -1 if you slightly disagree with the statement.
Write down a +1 if you slightly agree with the statement.
Write down a +2 if you moderately agree with the statement.
Write down a +3 if you strongly agree with the statement.
Write down a +4 if you very strongly agree with the statement.
If you feel exactly and precisely neutral about an item, write down a “0."
Important: You
may find that you sometimes have different reactions to different parts of a statement. For example,
you might very strongly disagree (“-4") with one idea in a statement, but slightly agree (“+1") with
another idea in the same item. When this happens, please combine your reactions, and write down how
you feel on balance (a “-3" in this case).
___ 1. The established authorities generally turn out to be right about things, while the radicals
and protestors are usually just “loud mouths” showing off their ignorance.
___ 2. Women should have to promise to obey their husbands when they get married.
___ 3. Our country desperately needs a mighty leader who will do what has to be done to destroy
the radical new ways and sinfulness that are ruining us.
___ 4. Gays and lesbians are just as healthy and moral as anybody else.
___ 5. It is always better to trust the judgment of the proper authorities in government and
religion than to listen to the noisy rabble-rousers in our society who are trying to create
doubt in people’s minds
___ 6. Atheists and others who have rebelled against the established religions are no doubt every
bit as good and virtuous as those who attend church regularly.
___ 7. The only way our country can get through the crisis ahead is to get back to our traditional
values, put some tough leaders in power, and silence the troublemakers spreading bad ideas.
___ 8. There is absolutely nothing wrong with nudist camps.
___ 9. Our country needs free thinkers who have the courage to defy traditional ways, even if this
upsets many people.
___ 10. Our country will be destroyed someday if we do not smash the perversions eating away at
our moral fiber and traditional beliefs.
___ 11. Everyone should have their own lifestyle, religious beliefs, and sexual preferences, even if
it makes them different from everyone else.
___ 12. The “old-fashioned ways” and the “old-fashioned values” still show the best way to live.
___ 13. You have to admire those who challenged the law and the majority’s view by protesting
for women’s abortion rights, for animal rights, or to abolish school prayer.
___ 14. What our country really needs is a strong, determined leader who will crush evil, and take
us back to our true path.
___ 15. Some of the best people in our country are those who are challenging our government,
criticizing religion, and ignoring the “normal way things are supposed to be done.”
___ 16. God’s laws about abortion, pornography and marriage must be strictly followed before it is
too late, and those who break them must be strongly punished.
___ 17. There are many radical, immoral people in our country today, who are trying to ruin it for
their own godless purposes, whom the authorities should put out of action.
___ 18. A “woman’s place” should be wherever she wants to be. The days when women are
submissive to their husbands and social conventions belong strictly in the past.
___ 19. Our country will be great if we honor the ways of our forefathers, do what the authorities
tell us to do, and get rid of the “rotten apples” who are ruining everything.
___ 20. There is no “ONE right way” to live life; everybody has to create their own way.
___ 21. Homosexuals and feminists should be praised for being brave enough to defy “traditional
family values.
___ 22. This country would work a lot better if certain groups of troublemakers would just shut up
and accept their group’s traditional place in society.