Doomer Porn
Global population, limits to growth, peak oil and climate change activists have been coming up with such similar contraction scenarios that they are beginning to echo each other.
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As the stragglers who came to the Peak Oil Revival Camp meetings after having got religion with climate change, we confess to having never quite received that part of the Peak Oil gospel with an open mind.
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If you lose your economic underpinnings, you could fall back on the economic development chart to where you were in 1930, or 1830, or even 1330, but you are still around as a species, assuming you don’t totally lose your cool and just nuke everything in sight on your way down.
In contrast, if you lose your climate underpinnings, it’s game over, man. You not only take down the higher vertebrates, homo included, but everything alive on this third rock from the sun, potentially even the microbes in deep caves and ocean depths. Earth, meet Venus.
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First, let us back up a month to May 19, and the publication by the Massachusetts Institute of Technology’s study involving 400 supercomputer runs of the best climate change measurements currently available. Conclusion: the effects of climate change are twice as severe as estimated just six years ago and the median probability of surface warming by
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A second report, by the Global Humanitarian Forum, found that 300,000 deaths per year are already attributable to climate change-related weather, food shortages, and disease. That could be called our baseline, or background count — of the 20th-century-long experience of less than a 1 degree C change.
All of these findings set the stage for the report released this past week by the Advisory Committee on Global Change Research, Global Climate Change Impacts in the United States (Cambridge
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The “Impacts” report takes the projections for the coming decades to about as fine a grain as can be had, given the behavior of interrelated and reciprocating climate systems undergoing rapid destabilization. Here are some findings that really
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- Warming over this century is projected to be considerably greater than over the last century. The global average temperature since 1900 has risen by about 1.5ºF. By 2100, it is projected to rise another 2 to 11.5ºF. The U.S. average temperature has risen by a comparable amount and is very likely to rise more than the global average over this century, with some variation from place to place.
- Climate-related changes have already been observed globally and in the United States. These include increases in air and water temperatures, reduced frost days, increased frequency and intensity of heavy downpours, a rise in sea level, and reduced snow cover, glaciers, permafrost, and sea ice. A longer ice-free period on lakes and rivers, lengthening of the growing season, and increased water vapor in the atmosphere have also been observed. Over the past 30 years, temperatures have risen faster in winter than in any other season, with average winter temperatures in the Midwest and northern Great Plains increasing more than 7ºF. Some of the changes have been faster than previous assessments had suggested.
Likely future changes for the United States and surrounding coastal waters include more intense hurricanes with related increases in wind, rain, and storm surges (but not necessarily an increase in the number of these storms that make landfall), as well as drier conditions in the Southwest and Caribbean. These changes will affect human health, water supply, agriculture, coastal areas, and many other aspects of society and the natural environment.
- Impacts are expected to become increasingly severe for more people and places as the amount of warming increases. Rapid rates of warming would lead to particularly large impacts on natural ecosystems and the benefits they provide to humanity. Some of the impacts of climate change will be irreversible, such as species extinctions and coastal land lost to rising seas.
- Unanticipated impacts of increasing carbon dioxide and climate change have already occurred and more are possible in the future. For example, it has recently been observed that the increase in atmospheric carbon dioxide concentration is causing an increase in ocean acidity. This reduces the ability of corals and other sea life to build shells and skeletons out of calcium carbonate.
Additional impacts in the future might stem from unforeseen changes in the climate system, such as major alterations in oceans, ice, or storms; and unexpected consequences of ecological changes, such as massive dislocations of species or pest outbreaks.
- - Unexpected social or economic changes, including major shifts in wealth, technology, or societal priorities would also affect our ability to respond to climate change. Both anticipated and unanticipated impacts become more challenging with increased warming.
- In an increasingly interdependent world, U.S. vulnerability to climate change is linked to the fates of other nations. For example, conflicts or mass migrations of people resulting from food scarcity and other resource limits, health impacts, or environmental stresses in other parts of the world could threaten U.S. national security.
The European heat wave of 2003 [with >30,000 heat-fatalities] is an example of the type of extreme heat event that is likely to become much more common. If greenhouse gas emissions continue to increase, by the 2040s more than half of European summers will be hotter than the summer of 2003, and by the end of this century, a summer as hot as that of 2003 will be considered unusually cool.
- There are also concerns regarding the potential for abrupt release of methane from thawing of frozen soils, from the sea floor, and from wetlands.
- Recent findings indicate that it is very likely that the strength of the North Atlantic circulation will decrease over the course of this century in response to increasing greenhouse gases. This is expected because warming increases the melting of glaciers and ice sheets and the resulting runoff of freshwater to the sea. This additional water is virtually salt-free, which makes it less dense than seawater. Increased precipitation also contributes fresh, less-dense water to the ocean. As a result, less surface water is dense enough to sink, thereby reducing the conveyor belt’s transport of heat. The best estimate is that the strength of this circulation will decrease 25 to 30 percent in this century, leading to a reduction in heat transfer to the North Atlantic. It is considered very unlikely that this circulation would collapse entirely during the next 100 years or so, though it cannot be ruled out.
While very unlikely, the potential consequences of such an abrupt event would be severe. Impacts would likely include sea-level rise around the North Atlantic of up to 2.5 feet (in addition to the rise expected from thermal expansion and melting glaciers and ice sheets), changes in atmospheric circulation conditions that influence hurricane activity, a southward shift of tropical rainfall belts with resulting agricultural impacts, and disruptions to marine ecosystems.
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Just don’t forget that what we need to do to extricate ourselves is also going to make our lives vastly better, and still better for our children, although, for them, it will be quite a bit warmer for a while.
Comments
My mother died unexpectedly Friday morning. the day you wrote this. Its been 48 hours but it feels like its been a week already. I'm glad she won't be worried by all this.
howard
Houner