Booklist: Limits to Growth, Overpopulation, Collapse, War, Extinction

 More booklists

Limits to Growth

  • Donella Meadows. 2004. The Limits to Growth: The 30 year update      
  • V Smil. Enriching the Earth: Fritz Haber, Carl Bosch, and the Transformation of World Food Production.
  • K Gever. Beyond Oil: The threat to food & fuel in the coming decades           
  • D. & M. Fisher. 2001. The Nitrogen Bomb.  Discover magazine      
  • William Catton.  Overshoot        
  • M Wackernagel. Our Ecological Footprint: Reducing Human Impact on the Earth
  • L Garrett. The Coming Plague: Newly Emerging Diseases in a World Out of Balance.
  • G Slade. Made to Break: Technology and Obsolescence in America 
  • Hopfenberg. Human population numbers as a function of food supply

Overpopulation                    

Escape to Mars & Outer Space

Collapse

Collapse, Russia                   

Collapse, North Korea      

Collapse, Venezuela

Collapse, Cuba

Collapse, Roman Empire

Collapse, Civil War, Refugees

D Mikhail. The Beekeeper. Rescuing the Stolen Women of Iraq 

Nuclear War

War

  • SA LeBlanc. Constant Battles: The Myth of the Peaceful, Noble Savage.
  • N Ohler. Blitzed: Drugs in the Third Reich
  • R O’Harrow. The Quartermaster: Montgomery C. Meigs, Lincoln’s General, Master Builder of the Union Army
  • J Weatherford. Genghis Kahn and the Making of the Modern World
  • J Weatherford. Secret History of the Mongol Queens
  • L Kleveman, The New Great Game:  Blood and Oil in Central Asia.
  • M Klare. Resource Wars: The New Landscape of Global Conflict.
  • M MacMillan. War How Conflict Shaped Us   
  • C Johnson. The Sorrows Of Empire: Militarism, Secrecy, and the End of the Republic.  
  • J Matloff. No friends but the mountains: Dispatches from the world’s violent highlands
  • P Coffee. American arsenal. A century of waging war.
  • D Vine. Base Nation: How U.S. Military bases abroad harm America and the World
  • A Rashid.  Taliban. Militant Islam, Oil and Fundamentalism in Central Asia.
  • P Turchin. 2 books: Secular Cycles. War and Peace and War. 
  • D Berreby. Us and Them. Understanding Your Tribal Mind. 
  • A Gat. War in Human Civilization. 
  • L Keeley. War before Civilization: The Myth of the Peaceful Savage.
  • J Waller.  Becoming Evil. How ordinary people commit genocide and mass killing. 
  • P Gourevitch. We Wish to Inform You That Tomorrow We Will be Killed With Our Families: Stories from Rwanda. 
  • D Goldhagen. Hitler’s Willing Executioners: Ordinary Germans & the Holocaust. 1997
  • Wrangham & Peterson. Demonic Males: Apes and the Origins of Human Violence. 1997
  • M Ghiglieri. The Dark Side of Man: Tracing the Origins of Male Violence
  • R Rhodes. Why They Kill: The Discoveries of a Maverick Criminologist.  
  • G MacDonogh. After the Reich. The Brutal History of the Allied Occupation.
  • C. Andrew. Secret world: A history of intelligence.  980 pages
  • M. Matthews. Head strong: how psychology is revolutionizing war
  • A Goldsworthy. Complete Roman Army 

CYBERWAR

What it’s like to be a soldier

  • Guy Sajer. The Forgotten Soldier  
  • K Marlantes. What it is like to go to war.
  • David Finkel. The Good Soldiers      
  • Peter Goldman. Charlie Company: What Vietnam Did to Us 
  • MD Matthews. Head Strong: How Psychology is Revolutionizing War  

Extinction

Alice Friedemann  www.energyskeptic.com  Author of Life After Fossil Fuels: A Reality Check on Alternative Energy; When Trucks Stop Running: Energy and the Future of Transportation”, Barriers to Making Algal Biofuels, & “Crunch! Whole Grain Artisan Chips and Crackers”.  Women in ecology  Podcasts: WGBH, Planet: Critical, Crazy Town, Collapse Chronicles, Derrick Jensen, Practical Prepping, Kunstler 253 &278, Peak Prosperity,  Index of best energyskeptic posts         

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Over and under-cooked oil — tar sands, “fracked” tight oil & gas

This article discusses why it’s so hard and expensive to extract difficult oils like fracked shale oil, Venezuelan and Canadian oil sands.

  • These are at the bottom of the resource pyramid, so there may be a lot of it, but it’s poor quality and expensive to extract.
  • The tar sands in Canada and Venezuela were once super-giant fields of light oil. But over millions of years it’s been “overcooked” — bacteria swallowed most of the hydrogen atoms, degrading and converting the light oil into a nasty tar requiring expensive upgrading 
  • Shale gas and tight oil are in rocks where hydrocarbons may have been overcooked or haven’t made it into porous reservoirs yet.  Robert Skinner says that getting them out “…amounts to giving the rocks an enema” with high pressure water, sand, and chemicals.
  • Kerogen shale is undercooked. Millions of years from now it will turn into oil, but trying to accelerate this process takes too much energy
  • Accelerating or reversing geology to get these difficult oils takes enormous amounts of cash, and energy, which in the end leads to huge amounts of GHG emissions.

2017: The Alberta Energy Regulator (AER) report on tar sands, oil, and gas production states

“2016 was another challenging year for hydrocarbon producers in Alberta. Faced with continued low global crude oil prices and weak natural gas prices, Alberta producers sought additional cost savings and curtailed capital budgets and activity. Capital expenditures fell for a second year. Conventional oil and gas wells placed on production dropped by 37.2% in 2016 relative to 2015, and crude oil production and natural gas production declined as a result. Additionally, wildfires in the area of Fort McMurray disrupted oil sands production in May, with impacts lasting into summer.

Total capital expenditures in the conventional oil and gas and oil sands sectors declined by an estimated 35% between 2015 and 2016 to Cdn$26 billion.1 This was due in part to projects being delayed because of the low oil price environment, as well as to reduced costs for materials and labour. Total capital expenditures are forecast to remain relatively flat in 2017, with capital expenditures forecast to increase in the conventional oil and gas sector but decline in the oil sands sector.”

Alice Friedemann   www.energyskeptic.com  author of “When Trucks Stop Running: Energy and the Future of Transportation”, 2015, Springer and “Crunch! Whole Grain Artisan Chips and Crackers”. Podcasts: Practical Prepping, KunstlerCast 253, KunstlerCast278, Peak Prosperity , XX2 report ]

Nikiforuk, A. 22 May 2013. Difficult Truths about ‘Difficult Oil’. As we work down the hydrocarbon pyramid, energy gets messier and much more costly. TheTyee.ca  

As the global economy switches to heavier, messier and costlier hydrocarbons, Robert Skinner is getting a bit worried about the future of his three grandchildren.  It’s all about the story of “difficult oil,” a term the highly respected energy expert and geologist first coined nearly a decade ago.

Now, Skinner, a 67-year energy veteran, has seen it all. He has not only worked extensively for industry and government (Energy Mines & Resources) but even for think tanks such as the prestigious Oxford Institute for Energy Studies. He also served as the policy director for the International Energy Agency in the early 90s as climate change and post-Soviet Europe seized the agency’s attention.

When not writing or thinking about difficult oil, Skinner now advises governments, universities and companies on strategy, whether for research, regulations or investment.

Skinner first saw the oil sands in 1966 as a student geologist. At the time it consisted of just one construction project for the first Suncor mine.

He has returned every decade since, first as a federal energy official, and then as an employee for the French oil giant, Total. In his last stint he served as senior vice president for Statoil Canada.

“I first saw the oil sands as a sideline, out-of-sight activity that governments were reluctant to approve — because it would compete with output from the string of discoveries after Leduc that governments were lobbying the U.S. to import. Today it is a burgeoning boomtown, world-scale industry that governments are again lobbying the U.S. to import.”

But his experiences working with bitumen over the last 45 years confirmed Skinner’s deepest suspicions: difficult oil is, well, difficult and really is a shift from business as usual. It is all about burning money to reverse or speed up geology. Moreover, technological breakthroughs to speed up or slow down geological forces are slow if not ponderous.

Skinner first dug up the important concept of “difficult oil” in 1998.

Difficult hydrocarbons, he explained, generally lie at the bottom of the resource pyramid. They might be massive in volume but high in cost, and often poor in quality.

Difficult oil has either been cooked too much, too little, or not at all. In some cases it has been degraded by bacteria. To accelerate or reverse geology generally requires ungainly amounts of energy along with clouds of GHG emissions.

The right degree of cooking over time, of course, produces light oil, notes Skinner, but much of the world’s conventional sources are now in steep decline.

That leaves over cooking or too much heat, which produces the so-called “wet gas fields,” now being pursued in the Eagle Ford field in western Texas.

How heavy oil got so heavy

The bitumen in Venezuela’s Orinoco basin and northern Alberta also requires massive geological tinkering, says Skinner.

Both heavy oil deposits actually began as super-giant fields of light oil. But over millions of years bacteria chewed up most of the hydrogen atoms degrading the resource into a thick heavy molasses-like tar. This goo can’t be turned into a commercial fuel stock without extensive upgrading to restore the ratio of hydrogen to carbon atoms.

To do so, hydrogen must be added to the bitumen or (more commonly) carbon must be subtracted, by “coking.” Coking creates mountains of petroleum coke, a coal-like substance.

Reversing geology, adds Skinner, “requires huge amounts of energy, labor, water, steel and capital. It’s all about the Second Law of Thermodynamics.”

Shale gas and tight oil, also belong to the difficult camp. They exist in source rocks where hydrocarbons may have been overcooked or not yet migrated up into porous reservoirs. As a consequence it requires some fiddling to wrestle them out of the shale. “To be graphic, it amounts to giving the rocks an enema,” says Skinner.

The cracking of these source rocks with high pressured volumes of water, sand and chemicals, a modern business frenzy, is all about accelerating geology “to speed up the migration” and release of these hydrocarbons.

But to Skinner reversing or accelerating geology ultimately adds up to one reality: spending big piles of cash.

“Difficult oil is by definition costly. And the costs are not coming down all that much.”

Bitumen remains the world’s most capital-intensive hydrocarbon. According to RSK Limited, an independent analysis firm, it takes $8 billion to develop a conventional oil field pumping one million barrels a day in the Middle East, while it takes $45 billion to produce the same result in the tar sands. (Venezuelan heavy oil is about $10 billion cheaper to produce than Canada’s bitumen.)

And that doesn’t include upgrading.

Moreover, the three biggest tight oil producers in the Bakken and Eagle Ford plays “have increased their long-term debt by over 300 per cent in the last three years. We’ve seen this over-leveraged train wreck before,” says Skinner.

The consultant also doesn’t think the capital intensity of difficult hydrocarbons gets enough attention among policy makers.

If interest rates increase and/or the price of oil sags, new production in the shale oil and oil sands becomes uneconomic, explains Skinner.

But as supply drops off, prices eventually increase again making for more volatility. The volatility of difficult oil in turn “compounds the inherent and ever-present instability caused by geopolitical factors.”

Reversing geology is not so easy

Another challenge plaguing difficult oil is the slowness and sheer difficulty of technological innovation. Reversing geology requires great complexity; progress is often incremental and disappointments are common.

“Every company, big and small, attempts to create a mystique around some ‘unique’ or ‘special’ black box or technique in particular or the firm’s technological prowess,” explains Skinner. “They do this to attract investors or to placate their environmental critics, or even to convince themselves that this business is for them.”

While new techniques and technologies, for example using solvents, are being tested, the oil sands is still running on technology several decades old. The steam plants, which boil water to make steam to melt deep underground bitumen, account for half of oil sands production. But the technologies that promised 20 years ago to produce more bitumen with less steam, still hasn’t delivered.

Instead of reducing the volume of steam needed to produce a barrel from 2.5 barrels to one barrel, most projects have increased their steam volumes (an average of 3.2 barrels now) along with energy and water costs due to the increasingly poor quality of deep reservoirs.

Nor is it just about the technology; “it’s the sheer difficulty of moving dozens of megaprojects through an overburdened regulatory process, construction and local infrastructure with an inadequate and ill-trained labor force.”

University of Calgary petroleum engineer Steve Larter has offered the same reality check: “Steam-Oil Ratios have tended to get worse with time as more difficult reservoirs are developed.” Moreover, “revolutionary technologies that lead to major downward shifts of the invested energy (e.g. steam) and emissions versus oil produced have not yet appeared.”

Skinner adds that most industry and government claims about getting cleaner are problematic at the moment: “Any company that claims its technology program will yield efficiency gains/emissions reductions beyond a modest, few percentage points within ten years — and they have yet to put steel in the ground to test their technologies — is simply naive or attempting to mislead someone. It can take more than three years just to get regulatory approval, two to build, one to three to ramp up, monitor and measure, and perhaps a couple more to analyze — and that is only for a pilot, not a full-scale commercial project: that can take another four to six years to produce initial results.”

 

Posted in Oil & Gas Fracked, Oil Shale, Tar Sands (Oil Sands) | Tagged , , , , , , | 2 Comments

Net metering and the death of US rooftop solar

April 22, 2016 by Roger Andrews at euanmearns.com

“Net metering” allows anyone with a solar installation to sell surplus solar power to the grid when the sun is shining and to purchase power back from the grid when it isn’t. Net metering has been described as the lifeblood of solar in America, and it’s probably true to state that without it there would be few, if any domestic rooftop solar installations anywhere in the country. However, the program is now coming under attack, with Hawaii and Nevada recently rolling back net metering benefits and with a number of other states also considering changes. What happens if enough states impose similar rollbacks, or maybe do away with net metering altogether? This post reviews this question and concludes that domestic solar in the US will slowly wither and die.

The Nevada decision

On December 23, 2015, the Nevada State Legislature passed Senate Bill 374, following which the state Public Utilities Commission cut the rate payable to owners of domestic solar installations who sell surplus power to Nevada Energy. The rationale was that intermittent solar power sold to the NV Energy grid “differs from” the dispatchable power the grid sells back and that domestic solar owners were getting paid too much for the former and not paying enough for the latter:

The order separates the prices of energy and related services provided by NV Energy, and the intermittent renewable energy provided to NV Energy by net metering customers. This approach is fair because it recognizes that the energy and suite of energy services provided by NV Energy to net metering customers differs from the intermittent excess energy delivered to NV Energy’s system.

This decision will be welcomed by all who recognize that solar is incapable of providing more than a small fraction of total electricity supply because of prohibitive storage requirements and that it’s presently getting a free ride on the back of grid generation that substitutes for storage. Certainly my rooftop solar panels would be totally uneconomic if I couldn’t use grid power at night and had to use storage batteries instead.

The Nevada solar industry, however, was not amused. Three solar companies – SolarCity, Sunrun and Vivint – announced they would have to cease operations in the state and local installers have been forced to cut staff. Also not amused were Nevada’s 18,000 existing rooftop solar array owners, who thought they were “grandfathered” but found that they weren’t. Their response was to launch a class action lawsuit against NV Energy alleging the utility “conspired to unlawfully reduce incentives” and NV Energy caved in, announcing that it would file a proposal to keep existing customers on the old rates, recognizing the desire for a “stable and predictable cost environment.”

“A potentially worrisome precedent”

But still the outcome in Nevada sets a potentially worrisome precedent for the US solar industry, with roughly half of all U.S. states currently studying or changing their net metering policies. States are taking action now because domestic solar in the US has grown so fast that several of them are now approaching or have already reached their net-metering caps. (A net metering cap is a target set by state authorities and it’s usually related to some fraction of peak demand or to capacity. But each state uses different criteria and some of them are extremely complicated. Details for anyone who might want more information are available here and here).

Two states other than Nevada have already revisited the question of how much intermittent solar power is really worth and how much of it their state can really use. The first was Hawaii, where some of Hawaii Electric Company’s grids were getting swamped by rooftop solar to the point where solar generation exceeded total demand at daytime solar peak. An example is given in Figure 1, which shows “backfeed” conditions between 10.30am and 2pm on August 8, 2013:

Figure 1: Average transformer load showing “backfeed” conditions, Hawaii utilities

Because of growing problems of this type the Hawaii Public Utilities Commission shut the net metering program down for new participants in October last year. As was the case in Nevada this shutdown was also accompanied by weeping, wailing and lawsuits from the local solar industry and rooftop solar owners, but the situation was obviously unsustainable. And it arose with less than 1% overall annual solar penetration in the state, not the 10% commonly assumed. More about this later.

Another state on a collision course with net metering is California, the home of the “Duck Curve”: (The Hawaii curve is known as the “Nessie Curve”, although the resemblance is less obvious.)

Figure 2: The California “Duck Curve”

At expected rates of solar growth California will also have a potential overgeneration problem by 2020, and the ramp rates needed to cover the period between about 5pm and peak load at 9pm reach potentially alarming levels. California’s solution has been to mandate the installation of 1.3GW of storage capacity (again no “h” given) by 2020, but this is just a drop in the bucket by California standards.

Current Status of the US solar industry:

One of the remarkable things about the US solar industry is how insignificant it is. Figure 3 plots percent solar penetration in the 36 states for which solar data are available (estimated as total solar generation divided by total generation using 2015 data from the EIA detailed state generation data base). The average level of penetration in 2015 was only 0.6%, and many states generated effectively no solar at all:

Figure 3: Solar generation by state as a percentage of total generation.

Only California is anywhere close to 10% solar penetration. Solar penetration in Nevada is less than 5% and in Hawaii less than 1%. (I checked this number and found that according to Hawaii Electric Company it’s correct). The implication is that solar may begin to stress grids at levels of penetration much lower than 10%, particularly at the local level.

Discussion

What we are seeing here is a conflict between on the one hand the utilities and grid operators, who view solar as a threat to their bottom line and to grid stability, and on the other the green lobby plus the residential owners, installers and PV panel salesmen who are now benefiting from the proceeds of subsidized solar and the existence of net metering. The surprising thing, however, is that this conflict has broken out even though solar still contributes a negligible percentage of the US generation mix. Why should this be? I think partly because the hundreds of thousands of homeowners who have installed solar arrays are dependent on a continuation of net metering to recoup their investment, partly because 200,000 people are now employed in the US solar industry, partly because solar can in some cases destabilize grids even at low levels of penetration (viz. Hawaii) and partly because of the claims made by some scientific organizations as to the percentage of US electricity generation solar could ultimately fill, such as:

  • US National Renewable Energy Laboratory: 39% with rooftop solar PV alone
  • Stanford University: 38% by 2050
  • US Department of Energy: 27% by 2050
  • International Energy Agency: 36% by 2050 (with solar thermal)

Numbers like this, which assume an approximate sixty-fold expansion of US solar capacity over present levels, can only be described as wishful thinking. Yet in the minds of many they are realistic targets.

But what happens if net metering benefits are rolled back? I picked an example which should be fairly close to reality – a household in Southern Nevada that consumes 11,000 kWh/year, the US average, with a 5kW solar array on the roof. I constructed a crude daily demand curve to show a peak around the breakfast hour and a larger one in the evening when everyone is at home watching large-screen TV or playing computer games and all the lights have been left on. Figure 4A shows hourly consumption and solar generation for the household during an average day (which assumes 12 hours of sunshine and a capacity factor of 19%, which is about right for Southern Nevada.) When the sun isn’t shining the household gets all its power from the grid, but for about 7 hours it gets all its power from the 3kW solar array. And over this period the array generates a healthy surplus that gets fed back to the grid, sending the electricity meter into reverse and causing it to wind rapidly backwards:

Figure 4: Demand, solar generation and consumption for a “typical” Southern Nevada household with net metering in place

Figure 4B shows the cumulative impacts. At the end of the day the household has consumed 30.3kWh, but because of the surplus solar power sent to the grid it gets charged for only 6.7kWh of grid power, which at current Nevada retail rates of $0.11/kWh works out to the princely sum of 74 cents, or an annual bill of about $270. Compared to what the bill would have been without solar (about $1,200) this gives the owner something like a ten-year payback on his or her solar investment after federal and state tax credits, which is not too bad when one considers that the solar array adds value to the house and that the PV panels will, one assumes, continue to generate electricity after payback is reached.

Nevada’s net metering rollback will, however, ultimately reduce the payment homeowners receive for solar electricity sent to the grid by 75% . How much difference will this make? Instead of saving almost $1,000/year on electricity bills the homeowner will now save only about $250/year. Even allowing for federal and state tax credits this will make domestic solar totally uneconomic in Nevada. And if other states follow Nevada’s lead it will eventually become uneconomic in those states as well.

And the problem doesn’t stop there. US utilities, with some justification, are also angling for increased charges to cover the costs of integrating growing amounts of solar power with their grids. (Nevada’s “grid connection charge” is scheduled to triple over the next five years). The end of the net metering road will of course be reached when the grids can’t physically accept any more solar, or no one will be able to afford the grid connection charge, whereupon Figure 4A will look like this:

Figure 5: Demand, solar generation and consumption for a “typical” Southern Nevada household with no net metering in place. The household is capable of powering itself for only about 8 hours.

Yet some believe that net metering rollbacks will provide a new opportunity for US solar. This article (which describes net metering as solar’s “junk food”) proposes a “value-of-solar tariff” where “solar customers are paid for the value of the electricity they produce at the specific time and place they put it on the grid.” This seems fair, but it too would probably kill rooftop solar. The California duck curve shown in Figure 2 shows how. The solar power produced in the middle of the day exceeds grid requirements and would therefore have to be sold at a low price if not wasted altogether, and at the nine o’clock peak, when power is in greatest demand, the sun has set or in in the process of setting. Another article views net metering rollbacks as an opportunity for domestic solar producers to go off-grid entirely and fill demand from energy storage, either in a utility-owned or domestic storage facility. But “to make the storage option appealing to customers … it would need to be offered using a low capital expenditures (CAPEX) business model.” “Energy storage” and “low CAPEX” are, however, mutually-exclusive terms, so that won’t work either.

It therefore appears that the future of domestic US solar depends on how far the states that are currently considering or reconsidering their positions roll back net metering benefits. And they probably wouldn’t have to roll them back very far before rooftop solar becomes uneconomic – unless of course the government jumps in with yet more subsidies. But hope springs eternal, particularly in the breast of the US solar industry.

 

Posted in Other Experts, Photovoltaic Solar | Tagged , , , | 9 Comments

Limited Cognition

Gifford, R. May 2011. The Dragons of Inaction: Psychological barriers that limit climate change mitigation and adaptation.  PubMed.

Limited cognition.  Humans are far less rational than once believed. 

1: Ancient brain

Our physical brain hasn’t evolved much in 30,000 years. Back then, we were wandering around the savannah, concerned mainly with our immediate kith and kin, proximate dangers and quickly exploitable resources. Although we have learned to think (a bit!) about other people, distant threats and slowly exploitable resources, our ancient brain tends to fall back into the here and now, which is inconsistent with paying much heed to the gradual and often distant impacts of climate change. This makes us slow to act.

2: Ignorance.  Ignorance is a barrier to action in three ways: not knowing that climate change exists, not knowing what to do about it once you become aware of the problem, and being told wrong information. The first problem is shrinking, although factual knowledge still lags severely: my team recently tested the climate change knowledge of a representative sample of Canadians. We found that, on average, they could only correctly answer 1.5 out of 6 questions. Second comes a lack of knowledge about which actions to take, how to undertake those one is aware of, and the relative climate benefits of different actions. We are getting better at understanding the latter, and in broad terms we know what we should be doing. However, much remains to be learned, partly because the answers aren’t always universal – a best practice in London may not be a best practice in Vancouver, for example. Also, they aren’t always obvious – for instance, lamb raised in New Zealand and eaten in the UK has a smaller carbon footprint than lamb raised and eaten in the UK. And modern products are composed of many ingredients or component parts and have complex life cycles. Third, ignorance also stems from disciplined and deliberate attempts by groups with a vested interest in the production and use of greenhouse gases to cast doubt on climate science.

3: Environmental numbness. This dragon comes in two subspecies. First, every environment is made up of more elements than we can wholly grasp, so we attend to them selectively. Sometimes we attend to salient elements at the expense of less salient but more dangerous ones, which is how accidents happen. Climate change is like that for many: a dangerous phenomenon that isn’t salient because it isn’t causing any immediate personal difficulties. This makes action unlikely. The second form occurs at the other end of the stimulus spectrum. When people see the same advert many times, they get used to it and stop paying attention. Similarly, hearing about climate change too often, particularly if the message isn’t varied, can lead to message numbness and the attenuation of behaviours that would help ameliorate the problem.

4: Uncertainty. Experiments show that uncertainty – both real and perceived – reduces the frequency of pro-environmental behaviour. For example, when asked how many fish they would harvest from a hypothetical ocean, the more uncertain the number of fish left, the more people said they would take. People tend to interpret any sign of uncertainty as sufficient reason to act in self-interest. This happens in the real world too. In its 2007 report, the Intergovernmental Panel on Climate Change expressed its level of confidence in its predictions very carefully, using phrases such as “likely” or “very likely”. This led many to interpret the report as indicating a lower likelihood than the IPCC intended. Thus, we are left with a perplexing problem: how to present the likelihood of climate outcomes honestly without promoting underestimates of the problem, which of course help to justify inaction.

5: Discounting. One well-known psychological bias is our tendency to undervalue distant and future risks. This is also true of climate change. For example, my colleagues and I found that citizens in 15 of 18 countries believe that environmental conditions are worse in other countries. Although conditions often are objectively worse elsewhere, this tendency occurs even in similar places, such as English villages a few kilometres apart. People also tend to discount environmental risks that will occur in the future. Both types of discounting are a barrier to action against climate change. If conditions are presumed to be worse elsewhere and in the future, people will be less motivated to act.

6: Optimism bias. Optimism is generally a healthy, desirable outlook that can produce useful personal outcomes. However, it can be overdone, to the detriment of well-being. For example, people are overly optimistic about their chances of having a happy marriage or avoiding illness. They are also overly optimistic about environmental risks.

7: Perceived lack of behavioral control. Because climate change is a diffuse and global problem, many people do nothing because they think that their behaviour has little or no impact on the outcome. Closely related to this is fatalism – the sense that nothing can be done, not only by oneself, but even by collective human action.

8: Confirmation bias. We like to be told that we are correct. Therefore, people tend to read and watch media that tells them they are on the right track. Those who have doubts about climate science prefer to read newspapers and watch broadcasts that reinforce their convictions. That, in turn, is a serious barrier to engaging in climate-positive behaviour.

9: Time is money. Studies show that when people view the time they have available in monetary terms, they tend to skip acting in environmentally positive ways. Money is the epitome of self-interest, and so when one’s time becomes associated with it, the environment suffers.

10: Perceived inability. Many pro-climate actions require some extra knowledge, skill or ability. Some people are unable to act because of a physical disability, for example. However, many more are capable of, say, riding a bicycle or changing their diet, but claim to be unable to do so.

2. Ideologies. “When people have a comfortable lifestyle, their tendency to not rock the boat grows”

11: World views. World views are broad swathes of connected attitudes. Some of them include a special place for views on climate change. For example, support for free-enterprise capitalism is especially associated with disbelief in global warming. Capitalism has clearly produced comfortable lifestyles for millions, but some aspects of it, such as a belief in the freedom of the commons – that common resources should be exploitable by anyone – have also led to the devastation of fisheries, forests and landscapes around the world. Having a financial or emotional stake in capitalist organisations isn’t compatible with adopting climate-positive behaviours.

12: Suprahuman powers. Some people take little or no action because they believe that a religious or secular deity will not forsake them, or will do what it wishes anyway. When researchers at the University of Melbourne in Australia interviewed people living on Tuvalu’s main island, Funafuti, which is threatened by rising sea levels, they found that about half weren’t worried, maintaining that God wouldn’t break the biblical promise never to flood Earth again. More commonly, secular people believe Mother Nature will take a course that we mere mortals cannot influence. Climate inaction follows naturally from these beliefs.

13: Technosalvation. Technical innovation has a long and admirable history of improving our standard of living. Clearly, it can be a partner in mitigating climate change: witness the recent drop in the price of solar panels. However, some go further and believe that technology can solve all the problems associated with climate change. Such overconfidence can serve as another barrier to climate-mitigating behaviour.

14: System justification. This is the tendency to defend and justify the status quo. When people have a comfortable lifestyle, the tendency to not rock the boat grows and – more importantly – so does the desire not to let anyone alter the way things are. Climate change will require major adjustments; system justifiers normally won’t adopt them, and will argue against them. On a positive note, if mitigation can be portrayed as part of the system, this can change.

3. Social comparison. Humans are social animals; comparing our own situation to that of others is a deeply ingrained tendency.  

15: Social comparison. People routinely compare their actions with those of others. When we compare ourselves to someone we admire, we gravitate toward their choices; if that someone happens to harbor anti-climate-science views, we are likely to decide that the climate isn’t such a problem.

16: Social norms and networks. Norms are what we see as the proper courses of action. They can be a potent positive force for climate action, but they can also be regressive. Social networks create and informally enforce norms. If the network’s sentiment is toward doubt, a dragon of inaction naturally reigns. But it works both ways. In one US neighborhood, for example, dwelling proximity in the network helped explain why 16% of householders installed photovoltaic panels, far higher than the national average of 1%.

17: Perceived inequity. Perceived inequity is often heard as a reason for inaction: “Why should I change if they won’t change?” Usually other nations or well-known figures are cited as not cooperating, which serves as a convenient justification for one’s own inaction. This is backed up by experiments that show when any inequality, real or perceived, exists, cooperation tends to decline.

4. Sunk Costs

18: Financial investments.  Once we have invested in something, disinvesting in it for climate reasons becomes difficult. The cardinal example here is car ownership. If I have bought a car and am now paying for its insurance and upkeep, why should I sell this cosy portable living room or leave it on the driveway? Similarly, if someone has a financial stake or a job in a fossil fuel industry, believing that burning these fuels damages the environment can lead to cognitive dissonance. It’s often easier to reduce this dissonance by changing your belief (“burning these fuels isn’t causing a problem”) than by changing your behaviour (disposing of the stake).

19: Habit. In 1890, pioneering psychologist William James called habit the “enormous flywheel of society” – that is, a powerful force for keeping things regular and ordered. In the context of climate change, habit can lead to the routine, mindless performance of damaging actions. Of course, climate-positive habits are a potential boon. Habit isn’t a glamorous dragon, but it is one of the most important because many repeated actions are highly resistant to permanent change – think of diet and transportation. Some people use the term “behavioural momentum” instead, because it aptly expresses this resistance to change. The use of cars, for example, has a great deal of behavioural momentum, and therefore is very difficult to change.

20: Conflicting goals, values and aspirations. Everyone has multiple goals in life, and these aren’t all compatible with climate change mitigation. The near-universal aspiration to “get ahead” often means engaging in actions that compete with the goal of reducing climate change, such as buying a larger house, taking exotic holidays or owning a new car. That climate-related goals frequently take a back seat to others is revealed when people are asked to rank climate change against other problems or concerns: they usually assign it a low importance. Polls carried out by the Pew Research Center think tank reveal that 80 per cent of US respondents say climate change is an “important issue”, yet it comes 20th out of 20 when ranked against other issues. Many people favour addressing the economic cost of climate change, as long as it doesn’t come out of their own pockets.

21: Place attachment.  Individuals are more likely to care for places they feel an attachment to. Weak attachment can therefore act as a barrier to climate-positive behavior. However, so can strong place attachment, for example in Nimbyish opposition to nearby wind farms.

5. Discredence. When people think ill of others, they are unlikely to believe what they say or take direction from them. These negative views can take a range of forms.

22: Mistrust. Trust is essential for healthy relationships. When it is absent between citizens and scientists or government officials, resistance in one form or another follows. There is ample evidence that many people mistrust messages that come from scientists or government officials. When trust sours, the probability of positive behaviour change diminishes.

23: Perceived programme inadequacy. Policy-makers have implemented many programs designed to encourage sustainable or climate-friendly behavior. Most of these are voluntary, such as a rebate for buying loft insulation or energy-efficient appliances. Thus, people choose whether to accept the offer, and often they decide it isn’t good enough for their participation.

24: Denial. Uncertainty, mistrust and sunk costs can easily lead to active denial of the problem. This may include denial that climate change is occurring at all or that it is caused by us – something believed by substantial minorities in most countries. Those holding this view tend to be outspoken. One newspaper reader’s comments on an article about research by environmental psychologists is typical of the emotional intensity felt by some deniers: “It figures that a bunch of psychologists need to mess with people’s heads to get them to fall in line with this ‘eco-friendly’ nonsense.”

25: Reactance. Mistrust and denial lead to what psychologists call reactance, the tendency to struggle against whatever appears to threaten one’s freedom. Of course, some circumstances should promote reactance, but climate change isn’t one of them. Reactance is especially problematic when it comes to climate because it may promote actions that go beyond inaction into destructive territory.

6. Perceived risk. Changing one’s behavior is risky.  

26: Functional risk. Will it work? If one purchases, for example, an electric car, it may, as a new technology, have operational problems. The same could be said for many green technologies.

27: Physical risk. Some adaptations may have, or at least be perceived to have, some danger associated with them. Bicycles, for example, produce virtually no greenhouse gases after they are manufactured, but they result in quite a few visits to emergency rooms.

28: Financial risk. Many green solutions require capital outlays or premiums. How long is the payback? If the product becomes a fixed part of a residence, such as solar panels, will I recoup the installation costs or accrue enough energy savings before moving on? Is the premium for that electric car worth it?

29: Social risk. Other people notice many of our choices. This leaves us open to judgement, which could damage our reputation or ego. Will riding a bicycle make me look odd? What about becoming a vegan? Or keeping my old mobile phone?

30: Psychological risk. This risk is perhaps less likely for most people, but can occur. If we are teased, criticized or even bullied for engaging in climate-positive actions, we risk damage to our self-esteem and self-confidence.

31: Temporal risk. Another risk is the potential that the time I spend planning and adopting a climate-friendly course of action might fail to produce the desired results. Many people spend considerable time trying to decide whether to install solar panels, buy an electric car, become a vegetarian or cycle to a destination. Fear that the choice might not result in the desired benefits can lead to inaction: the time spent planning a change may be wasted.

7. Limited behavior. Most of us engage in at least minimal action to help limit the emission of greenhouse gases. However, most of us could do more.  

32: Tokenism. Some climate-related behaviors are easier to adopt than others, but have little or no impact on greenhouse gas emissions. One example is taking your own shopping bags to the supermarket. However, their ease of adoption means these tend to be chosen over higher-cost but more effective actions, such as commuting by bike or public transport, or switching to a vegetarian or vegan diet. Nevertheless, they might be considered a gateway to better things.

33: The rebound effect. Often, after some positive change is made, the gains are diminished or erased by subsequent actions. For example, people who buy a fuel-efficient car may drive further than when they owned a less efficient one. Like reactance, this dragon may go beyond cancelling out the benefits and produce overall negative consequences.

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Missing monsoon crashes Indus Valley Civilization

19 March 2014 Withering monsoon may have doomed past Asian society. NewScientist.

The Indian summer monsoon abruptly weakened 4200 years ago. The ensuing drought may have led to the collapse of the Indus Valley Civilization, which flourished around the Indus river, in what is now Pakistan and north-west India. It was at its height from 2600 BC to 1900 BC, but after that its cities were mysteriously abandoned.

Shifts in the monsoon have also been linked to the fall of China’s Tang dynasty, and of the Mayan civilization in South America, both around AD 900.

Yama Dixit and her colleagues at the University of Cambridge dug up snail shells from Kotla Dahar, a lake near one of the cities. The shells record changes in the lake’s water level in their composition. The team found that the lake was deep from 4500 to 3800 BC. Although it shallowed a little up to 2200 BC, after this time there was a sharp drop in the water level, suggesting the summer monsoon abruptly weakened for 200 years, meaning less rainfall. The Indus valley people relied on the monsoon for crops, says Dixit. “It is inevitable that they were affected.” The dates of the drought don’t match perfectly with the collapse, but Dixit says both are uncertain. The idea is credible because the results agree with data elsewhere, says Supriyo Chakraborty of the Indian Institute of Tropical Meteorology in Pune.

The journal article:

Dixit, Y., et al. February 24, 2014. Abrupt weakening of the summer monsoon in northwest India ~4100 years ago. Geology.

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Climate change impacts on energy, water, and land use in the U.S.

Hibbard, K., et al. 2014: Ch. 10: Energy, Water, and Land Use. Climate Change Impacts in the United States: The Third National Climate Assessment, U.S. Global Change Research Program, 257-281.

http://nca2014.globalchange.gov/report/sectors/energy-water-and-land

[ Excerpts from this 25 page document, charts/tables: best to see original if you have time, this is a placeholder to make you aware it exists and whether you want to read the full article]

The links between and among energy, water, and land sectors mean that they are susceptible to cascading effects from one sector to the next.

An example is found in the drought and heat waves experienced across much of the U.S. during the summers of 2011 and 2012. In 2011, drought spread across the south-central U.S., causing a series of energy, water, and land impacts that demonstrate the connections among these sectors. Texans, for example, experienced the hottest and driest summer on record. Summer average temperatures were 5.2°F higher than normal, and precipitation was lower than previous records set in 1956. The associated heat wave, with temperatures above 100°F for 40 consecutive days, together with drought, strained the region’s energy and water resources.3,4,5 These extreme climate events resulted in cascading effects across energy, water, and land systems.

Extreme climate events result in cascading effects across energy, water, and land systems.

High temperatures caused increased demand for electricity for air conditioning, which corresponded to increased water withdrawal and consumption for electricity generation.

Heat, increased evaporation, drier soils, and lack of rain led to higher irrigation demands, which added stress on water resources required for energy production. At the same time, low-flowing and warmer rivers threatened to suspend power plant production in several locations, reducing the options for dealing with the concurrent increase in electricity demand.

The impacts on land resources and land use were dramatic. Drought reduced crop yields and affected livestock, costing Texas farmers and ranchers more than $5 billion, a 28% loss compared to average revenues of the previous four years.6 With increased feed costs, ranchers were forced to sell livestock at lower profit. Drought increased tree mortality,7 providing more fuel for record wildfires that burned 3.8 million acres (an area about the size of Connecticut) and destroyed 2,763 homes.8

The Texas example shows how energy, land, water, and weather interacted in one region. Extreme weather events may affect other regions differently, because of the relative vulnerability of energy, water, and land resources, linkages, and infrastructure. For example, sustained droughts in the Northwest will affect how water managers release water from reservoirs, which in turn will affect water deliveries for ecosystem services, irrigation, recreation, and hydropower. Further complicating matters, hydropower is increasingly being used to balance variable wind generation in the Northwest, and seasonal hydroelectric restrictions have already created challenges to fulfilling this role.

With electricity demands at all-time highs, water shortages threatened more than 3,000 megawatts of generating capacity – enough power to supply more than one million homes. 9

Competition for water also intensified. More than 16% of electricity production relied on cooling water from sources that shrank to historically low levels,9 and demands for water used to generate electricity competed with simultaneous demands for agriculture and other human activities.

Energy, land, water, and weather interactions are not limited to drought. For instance, 2011 also saw record flooding in the Mississippi basin. Floodwaters surrounded the Fort Calhoun nuclear power plant in Nebraska, shut down substations, and caused a wide range of energy, land, and water impacts (Ch. 3: Water).

GAS FRACKING: A typical shale gas well requires from two to four million gallons of water to drill and fracture (equivalent to the annual water use of 20 to 40 people in the U.S, or three to six Olympic-size swimming pools). The gas extraction industry has begun reusing water in order to lower this demand. However, with current technology, recycling water can require energy-intensive treatment, and becomes more difficult as salts and other contaminants build up in the water with each reuse.30 In regions where climate change leads to drier conditions, hydraulic fracturing could be vulnerable to climate change related reductions in water supply. The competition for water is expected to increase in the future. State and local water managers will need to assess how gas extraction competes with other priorities for water use, including electricity generation, irrigation, municipal supply, industry use, and livestock production, particularly in water-limited regions that are projected to, or become, significantly drier.

Utility-scale photovoltaic systems can require three to ten acres per megawatt (MW) of generating capacity32 and consume as much as five gallons of water per megawatt hour (MWh) of electricity production.

Utility-scale concentrating solar systems can require up to 15 acres per MW33 and consume 1,040 gallons of water per MWh34 using wet cooling (and 97% less water with dry cooling). The U.S. Department of Energy study concluded that 14% of the U.S. demand for electricity could be met with solar power by 2030.34 To generate that amount of solar power would require rooftop installations plus about 0.9 million to 2.7 million acres, equivalent to about 1% to 4% of the land area of Arizona, for utility-scale solar power systems and concentrating solar power (CSP). 34 Recognizing water limitations, most large-scale solar power systems now in planning or development are designed with dry cooling that relies on molten salt or other materials for heat transfer. However, while dry cooling systems reduce the need for water, they have lower plant thermal efficiencies, and therefore reduced production on hot days.35 Overall, as with other generation technologies, plant designs will have to carefully balance cost, operating issues, and water availability.

Biomass-based energy is currently the largest renewable energy source in the U.S., and biofuels from crops, grass, and trees are the fastest growing renewable domestic bioenergy sector.13 In 2011, approximately 40 million acres of cropland in the U.S. were used for ethanol production, roughly 16% of the land planted for the eight major field crops.37 Consumptive water use over the life cycle of corn-grain ethanol varies widely, from 15 gallons of water per gallon of gasoline equivalent for rain-fed corn-based ethanol in Ohio, to 1,500 gallons of water per gallon of gasoline equivalent for irrigated corn- based ethanol in New Mexico. In comparison, producing and refining petroleum-based fuels uses 1.9 to 6.6 gallons of water per gallon of gasoline.38,41

Carbon Capture and Sequestration (CCS) substantially increases the cost of building and operating a power plant, both through up-front costs and additional energy use during operation (referred to as “parasitic loads” or an energy penalty). 46 Substantial amounts of water are also used to separate CO2 from emissions and to generate the required parasitic energy. With current technologies, CCS can increase water consumption 30% to 100%. 48 Gasification technologies, where coal or biomass are converted to gases and CO2 is separated before combustion, reduce the energy penalty and water requirements, but currently at higher capital costs.49

CCS facilities for electric power plants are currently operating at pilot scale. Although the potential opportunities are large, many uncertainties remain, including cost, demonstration at scale, environmental impacts, and what constitutes a safe, long-term geologic repository for sequestering carbon dioxide.51

A few of the many interesting figures to look at in the original:

Figure 10.4. U.S. regions differ in the manner and intensity with which they use, or have available, energy, water, and land. Water bars represent total water withdrawals in billions of gallons per day (except Alaska and Hawai’i, which are in millions of gallons per day); energy bars represent energy production for the region in 2012; and land represents land cover by type (green bars) or number of people (black and green bars). Only water withdrawals, not consumption, are shown (see Ch. 3: Water). Agricultural water withdrawals include irrigation, livestock, and aquaculture uses.

Figure 10.5 The top panel shows water withdrawals for various electricity production methods. Some methods, like most conventional nuclear power plants that use “once-through” cooling systems, require large water withdrawals but return most of that water to the source (usually rivers and streams). For nuclear plants, utilizing cooling ponds can dramatically reduce water withdrawal from streams and rivers, but increases the total amount of water consumed. Beyond large withdrawals, once-through cooling systems also affect the environment by trapping aquatic life in intake structures and by increasing the temperature of streams.18 Alternatively, once-through systems tend to operate at slightly better efficiencies than plants using other cooling systems. The bottom panel shows water consumption for various electricity production methods. Coal-powered plants using recirculating water systems have relatively low requirements for water withdrawals, but consume much more of that water, as it is turned into steam.

Figure 10.6. The figure shows illustrative projections for 2030 of the total land-use intensity associated with various electricity production methods. Estimates consider both the footprint of the power plant as well as land affected by energy extraction. There is a relatively large range in impacts across technologies.

Figure 10.9. In many parts of the country, competing demands for water create stress in local and regional watersheds. Map shows a “water supply stress index”

Figure 10.10. Agriculture is in yellow, forests are shades of green, shrublands are gray, and urban areas are in red. The river is used for hydropower generation,

 

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Clouds may not curb global warming as much as hoped for

The following article, Clouds Play Lesser Role in Curbing Warming, Study Finds, is from climatecentral.org

Analysis of the first seven years of data from a NASA cloud-monitoring mission suggests clouds are doing less to slow the warming of the planet than previously thought, and that temperatures may rise faster than expected as greenhouse gas pollution worsens — perhaps 25 percent faster.

Clouds can play an important role in slowing global warming by reflecting energy back into space. As temperatures rise, clouds contain more liquid water and fewer ice crystals, making them brighter, meaning they reflect more sunlight.

The new research, however, suggests climate models have overestimated how much ice is in clouds, meaning less is available to be converted to liquid as temperatures rise.

“When carbon dioxide concentrations and temperatures rise, then mixed-phase clouds will increase their liquid water content,” said Ivy Tan, a PhD candidate at Yale University who led the research, which investigated common clouds that contain both ice and water. “Many models are overestimating how much ice is in the mixed-phase clouds.”

The repercussions of the findings, which were published Thursday in Science, could make it harder to hold warming to limits set during recent United Nations climate negotiations

The coldest clouds are full of ice; the warmest are full of water. Modeling experiments by Tan and two other scientists focused on inbetweeners — mixed-phase clouds, such as undulating stratiform and fluffy stratocumulus clouds, which are abundant over the vast Southern Ocean and around the Northern Hemisphere north of New York.

For their study, the researchers used the NASA data to guide the modification of a popular earth model. They added more liquid and less ice to the clouds in their model simulations, striving to create more realistic conditions.

Because there was less ice, cloud brightness increased more slowly than it did in the unmodified model, since fewer ice crystals were replaced with reflective liquid as temperatures warmed.

One of climate science’s great quests is to project how much earth warms when carbon dioxide  concentrations double — something known as climate sensitivity. When carbon dioxide levels were doubled in the modified model, temperatures rose by at least a quarter more than they did when the unmodified model was used — to at least 5°C (9°F).

What the findings might actually mean for earth will depend heavily on how much carbon dioxide, methane and other greenhouse gases yet gets billowed into the atmosphere, and how quickly. But the discovery suggests impacts from climate change will be worse, and that they will get worse more quickly than earth models had previously indicated.

Isaac Held, a National Oceanic and Atmospheric Administration climate scientist, said he agreed with the researchers about the “the importance of getting the ice-liquid ratio in mixed-phase clouds right,” but he doesn’t agree that global climate models generally underestimate climate sensitivity.

Based on past observations, Held, who was not involved with the study, said the climate sensitivity of 5°C or more shown by the new research may be implausible.

“Admittedly, it is a rather high estimate, which may reflect the fact that the model used is already on the sensitive side,” said Mark Zelinka, a cloud modeling expert at Lawrence Livermore National Laboratory who worked with Tan on the research. But, based on Zelinka’s interpretation of historical data, he said it “seems premature” to dismiss it as implausible.

Tan, meanwhile, said it would be a mistake to focus too closely on the exact number. The sensitivity result from the modeling experiments should be taken “with a grain of salt,” she said.

That’s because the study was based on a single model. A main point in conducting the experiments was to show that climate models contain a bias that could be corrected. The group hopes other scientists will conduct similar experiments using different models to help hone in on a more reliable measure of climate sensitivity.

Michael Mann, a meteorology professor at Penn State who was not involved with the study, said it’s “speculative” but “plausible” that global climate models have been underestimating climate sensitivity by assuming too much cloud glaciation.

“This is one of several recent studies that provide sobering evidence that earth’s climate sensitivity may lie in the upper end of the current uncertainty range,” Mann said in an email. “That means that avoiding dangerous 2°C warming might be an even greater challenge.”

The new findings underscore the urgency of taking steps to slash rates of greenhouse gas pollution, Mann said.

Carbon dioxide levels have risen more than 40 percent to 400 parts per million since before the Industrial Revolution, and they continue to rise at a hastening pace.

The increase in carbon dioxide levels recorded so far has played the most important role in pushing average global temperatures up by 1°C (1.8°F) during the last 200 years. That has worsened heat waves, floods and droughts, leading to record-breaking temperatures in 2014 and then again in 2015.

A U.N. pact negotiated in Paris in December set a goal for limiting warming to well below 2°C. Plans by the world’s biggest polluters to protect the climate, including China, the U.S. and Europe, however, so far fall well short of the measures needed to achieve that goal.

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Promoting soil health in agriculture at U.S. House hearing 2014

Consequences of degraded soils

Consequences of degraded soils

Preface.  At last, many years after I first published “Peak soil: Why biofuels destroy ecosystems and civilizations” in 2007, Congress had a hearing to educate House members on why preserving topsoil is so essential for food production for future generations.  But I see no legislation in 2022 to prepare the younger generations for a transition to smaller organic farms. Quite the opposite, we’re on the way to feudalism in the U.S.

Continue reading

Posted in Biomass, Peak Topsoil, Pesticides, Soil, U.S. Congress Infrastructure, Water Pollution | Tagged , , , , , , | Comments Off on Promoting soil health in agriculture at U.S. House hearing 2014

Twice as many El Niños in 21st century

Expect more drought, flooding, and other crazy weather

In Nature Climate Change, doi.org/q4c, researchers predict that  El Niños will become twice as common, about once a decade in the future versus every 20 years the past century.

Another recent study showed that even normal El Niños will bring more severe drought and rain (Nature, doi.org/n9n).

Extreme El Niños can kill tens of thousands of people by causing a tenfold increase in rain in South America, flooding in the Americas, and drought in Australia, Africa, and elsewhere.

Until now scientists weren’t sure if climate change would affect El Niño because  it wasn’t known if temperatures in the Pacific would vary more in the future, but since the eastern Pacific is warming faster than the western Pacific this will eat up the east and shift rainfall.

Other scientists have found that El Ninos have grown more intense between 1979-2009 than 1590-1880  (Climate of the Past, doi.org/q28).

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Global warming spreads disease in the arctic

[ A summary of the spread of disease in the Arctic  in the August 2014 issue of Scientific American follows ]

Pathogens moving northward:

  • Aleutian Islands, Alaska. A distemper virus that infects seals in the North Atlantic ocean now attacks sea otters in the North Pacific
  • Saint Lawrence Island, Bering Sea. Avian cholera 200 kilometers off the alaskan mainland has killed hundreds of northern fulmars, murres, and crested auklets–seabirds unafflicted before.
  • Sahtu, Northwest Territories. Ticks, never observed here efore, have been discovered on moose hides.
  • Victoria Island, Arctic Archipelago. Lungworm has spread several hundred kilometers north across the musk oxen population
  • Hay Island, Nova Scotia. Ringed seals have passed a parasite to gray seals that killed 400 pups in 2012.
  • Sweden. Mosquitoes have spread the tularemia bacterium to people across the country. This can cause severe fever, inflammation and death.  Sweden also has more hantavirus infections because of warming.
  • Arkhangelsk Oblast, Russia. Tick-borne encephalitis cases in humans rose 50-fold from the decade 1980-1989 to the decade 2000-2009.

A warming climate helps parasites mature fast. Cold summers that used to keep parasites in check do so less often. A tipping point has happened, warmth lasts longer. Parasites like the lungworm now mature in one summer instead of two. This has caused musk ox populations to decline dramatically.

In Russia forests are advancing into tundra at a rate of about 1 km per year, and ticks along with them, affecting 4 million people.

Summary: For eons arctic cold kept a cap on disease, which wildlife has gotten used to. It’s thought that one reason birds migrate north is to avoid disease to devote their energy to raising young. Viruses, fungi and parasites are not just invading the north, but also tropical and temperate ecosystems as the climate heats up.

 

[ This is the transcript from NPR’s July 20th, As Polar Icebox Shrinks, Infectious Pathogens Move North. ]

Science writer Chris Solomon tells NPR’s Arun Rath that global warming has caused an influx of new diseases in animals that could eventually spread to humans.

ARUN RATH, HOST: Infectious diseases may be spreading more quickly, thanks to global warming. Viruses that were kept in check by the polar ice box are being released. And as some animals move north to keep cool, they’re bringing all sorts of parasites with them, from microbes to ticks. Christopher Solomon has written about this in the August issue of “Scientific American.”  Christopher, you wrote about sea otters off the coast of Alaska’s Aleutian Islands that are now infected with a virus from halfway around the world. What happened?

SOLOMON: There is something called phocine distemper virus, and it’s a relative of canine distemper. Phocine distemper has killed 50,000 seals over the last 25 years in the North Atlantic. And as scientists were trying to figure out why sea otters splashing in the Aleutian Islands were not doing so well, they found evidence of phocine distemper in them, and it became a detective story. And they said, well, what’s it doing in the North Pacific? And their theory is that it has made its way through the fabled Northwest passage via a seal or its feces and met animals on the other side due to the dramatic level of sea ice reduction.

RATH: So in addition to opening up lanes for shipping, warming has opened up a highway for viruses?

SOLOMON: Yes. In essence, disease is finding new lanes of travel. Existing disease up there is becoming invigorated. And new disease is hitchhiking on all sorts of wildlife, whether it’s fish or wild boars or ticks that are moving north in search of new habitat that’s cooler.

RATH: Wow. And in terms of land animals, I know with your article there is a photo of a big herd of very serious looking musk oxen. And they’ve been affected as well?

SOLOMON: Yes, this is another interesting case. Musk oxen – people may be able to visualize from a Disney or Pixar movie – they’re those smelly, kind of shaggy, horned relics of the Ice Age. And they’ve had a relationship with this parasitical lung worm for eons. It gave them a bit of a smoker’s cough. But the lung worm was always kept in check because it never was able to thrive in the brutal Arctic environment too well. And now, with essentially longer, warmer summers, the lung worm can complete its life cycle in one summer instead of two. And it has proliferated and has expanded it’s range up to where 30% of the world population of musk oxen live. And this is not good for the declining number of musk oxen in the far north.

RATH: Now, diseases can sometimes jump from animals to humans. How much is there for people to worry about, beyond animal populations?

SOLOMON: Well, that’s the interesting point in all of this. Since 1940, 60% of the new infectious diseases we’ve discovered in humans have come from animals. We’ve knocked down the borders between the natural world and the man-made world. Or, in these cases, the borders are simply melting away.

As one parasitologist Michael Grigg at the National Institutes of Health told me – he said, if the animals get sick, we can get sick. So we really need to pay attention to what’s happening out there. I’m not saying that the Arctic is collapsing under the weight of contagion right now. But things are happening that the scientists are really only starting to grasp in the north. And we need to pay attention to these flares that are going up.

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