Doctors orders: NZ “must rapidly halve its greenhouse emissions”

fatlenny.jpgIn a hard-hitting article in today’s New Zealand Medical Journal, a group of senior health professionals call for NZ to halve its greenhouse gas emissions by 2020. The spokesperson for the recently formed Climate and Health Group, Dr Alex Macmillan says:

Climate change has been described as the biggest global health threat of the 21st century, and the substantial health benefits of action should be fully included in decision-making, as should the harms of inaction.

According to the paper, the health benefits of action to reduce emissions include:

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Fab four: ways to meet the climate challenge

Climatechallenge Yet another pre-Copenhagen report has been released, this time  jointly from the influential Center for American Progress, the progressive think tank headed by John Podesta, President Clinton’s former chief of staff,  and the United Nations Foundation, the body founded with Ted Turner’s $1 billion gift in 1998 to support UN causes and activities.

Meeting the Climate Challenge (PDF) is brief and as punchy as such reports can be. It identifies and focuses on four core elements which it believes can deliver the most immediate effective response to climate change. Importantly, they are attractive in their own right and can be undertaken without delay. The first three, energy efficiency, renewable energy, forest conservation and sustainable land use, between them can achieve up to 75 percent of needed emissions reductions in 2020. And far from being costly the measures would deliver a net savings of $14 billion!  The report’s source is a Project Catalyst analysis. Renewable energy costs are estimated at $34 billion per year, forest conservation and land use at $51 billion; but energy efficiency measures save a staggering $98 billion per year. Net saving is the result.

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A beginner’s guide to the importance of Arctic sea ice

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In this beginner’s guide Tom Wagner, NASA’s cryosphere programme manager, outlines why studying Arctic sea ice is important, illustrating his talk with some great graphics. Meanwhile, the NSIDC has announced the final figures for September’s sea ice minimum:

The average ice extent over the month of September, a reference comparison for climate studies, was 5.36 million square kilometers (2.07 million square miles). This was 1.06 million square kilometers (409,000 square miles) greater than the record low for the month in 2007, and 690,000 square kilometers (266,000 square miles) greater than the second-lowest extent in 2008. However, ice extent was still 1.68 million square kilometers (649,000 square miles) below the 1979 to 2000 September average.

NSIDC scientist Walt Meier thinks there may be some hope of “stabilising” the ice after recent heavy losses:

We’ve preserved a fair amount of first-year ice and second-year ice after this summer compared to the past couple of years. If this ice remains in the Arctic through the winter, it will thicken, which gives some hope of stabilizing the ice cover over the next few years. However, the ice is still much younger and thinner than it was in the 1980s, leaving it vulnerable to melt during the summer.

But will there be a longer term recovery back towards the sort of ice cover seen before 2000? The NSIDC team doesn’t think so.

NSIDC lead scientist Ted Scambos said, “A lot of people are going to look at that graph of ice extent and think that we’ve turned the corner on climate change. But the underlying conditions are still very worrisome.”

After a couple of cool summers, one wonders what impact another warm year might do to the ice. As ever, I shall be watching next year with great interest…

Nine ways to stuff up a planet

How is humanity stuffing up the planet — shall we count the ways? There are nine, according to new work by a multidisciplinary team lead by Johan Rockström of the Stockholm Resilience Centre — full paper and supporting materials (with videos of authors explaining key points) here. The diagram above (from Nature’s coverage) shows the nine “planetary boundaries” within which humanity would be wise to operate. The good news is that on five of the measures we’re still in the safety zone. The bad news is that we’re well over safe limits for climate change, biodiversity loss, and interference with the nitrogen cycle, and we don’t know the limits for the final two factors. Here’s the full table:

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What’s the worst that could happen?

What's the Worst That Could Happen?: Cutting Through the Hubbub Over Global Warming

Greg Craven has been a YouTube phenomenon. Seven million people have viewed his short climate change video posted in 2007, The Most Terrifying Video You’ll Ever See. It was followed up with a number of others. Now he’s produced a lively and engaging book What’s The Worst That Could Happen?  A Rational Response to the Climate Change Debate which may not reach quite as many people, but certainly deserves a wide readership.

Craven is a high school science teacher in Oregon. He is open about the deep alarm he feels about climate change. But he’s not a climate scientist. He doesn’t set out to convince  readers of the reality of global warming. Instead he offers what he calls some thinking tools, not for working out whether climate change is true or not, but for working out whether we should be taking action or not. The decision grid “allows you to stop focusing on who’s right and instead ask, what’s the wisest thing to do, given the risks and consequences?“ Risk management, he calls it. The grid is a simple 2×2 affair, which compares and considers the consequences of action or inaction if global warming turns out to be either true or false. He’s aware that when he talks about a debate between “warmers” and “sceptics” he’s describing popular perception, not what goes on in climate science circles, but popular perception is what he is concerned to address.

The book was honed in the classroom. He found there’s no better way to refine a thought than to toss it out in front of a roomful of critical teenagers. The writing is crisp, quirky, often humorous, never ponderous. An active reader is presupposed, with pages set aside for participatory jottings. It’s hard to avoid engagement. Yet there’s an unmistakable drive and underlying seriousness to the vigorous text.

Craven offers useful observations about how science works, as a preliminary to embarking on the decision quest. Some examples: science is about pursuing the truth, but it never claims to actually get there. Its statements are usually very conservative. The presence of differing views doesn’t mean that something is controversial. Peer-reviewed papers are the basic currency of science. Science often runs counter to common sense, which would still have us thinking the sun goes round the earth.

The next preliminary step is to examine the ways our brains work (defectively). Confirmation bias is the main problem for us to be alert to, and he provides many suggestions as to how to manage that. Another feature important in the global warming debate is that the human brain’s alarm system has been conditioned over time to respond to threats that are immediate and visible.

Then it’s on to a tool he developed himself, the credibility spectrum. This is a ranking of sources by such factors as expertise, bias, track record, authority within the scientific community, reputation. Readers are invited to make up their own spectrum, but Craven shares his, which puts statements from professional societies at the top, along with statements from organizations that contradict their normal bias. Next down are government reports. In the middle come university research programmes, appropriately sourced petitions, think tanks and advocacy organisations. Down then to individual professionals, book writers, and finally individual lay people.  He chooses and identifies sources for each of those categories from both sides, warmers and sceptics.

There follows an excellent 30-page summary of what it is that the warmers are saying we should be concerned about and the doomsday they see ahead if we carry on as we are. The point of this chapter is simply to establish that their concern is not unreasonable and warrants at least the amount of attention needed to decide whether we should do anything about it or not. But the striking clarity of his account gives the chapter an importance well beyond that limited intention.

He then returns to his own credibility spectrum, warmers to the left, sceptics to the right, and explains why it could only lead him to the conclusion it did:

“When I look at the stunningly strident statements from all those calm professional sources at the top left, and I think, What are the chances they’re all out to lunch? and then I add my observations that the predictions have only been getting more dire and more immediate as time goes on, it scares the willies out of me. So I vote for slamming on the brakes. Hard. I can recover from any hot coffee that I spill on my lap.  But I can’t put myself and my car back together again if I drive confidently off a cliff, kids in the back.”

After that he sends his readers off with step by step instructions to build their own credibility spectrum and use the decision grid to produce their own conclusion.

For those readers who come to the same conclusion as he does, the appendix offers a strong recommendation. Craven stands with Hansen, because he has the best track record for predictions which mainstream science eventually catches up with. 350 ppm has to be the target for CO2 concentration in the atmosphere. This will require an effort similar to that which the US put into World War II when massive government action accomplished the seemingly impossible in an amazingly short passage of time. In perhaps the greatest economic mobilisation in the history of the world people invested an average of 25 percent of household income in War Bonds. And far from dooming the economy the collected effort of the citizenry brought the US out of the Great Depression and produced the world’s strongest economy.

Personal action to reduce our carbon footprint is fine, but it won’t get us to where we need to be. Only government action can do that. We need a collective determination, and the most significant contribution the individual can make is to spread the word, activate the interconnected web of communication that permeates our society.  Go viral. “Focus on burning the number 350 into the collective consciousness.” Over to the reader.

This is a most welcome book. It has proved astonishingly difficult for the findings of climate science to be communicated to the public. In part this is due to the success of the organised denialist campaign, in part to the cautious language of science itself, in part to the difficulty of comprehending how our apparently secure world can possibly be under the threat of such an enormous peril. Craven doesn’t try to fill the comprehension gap with information –- though what information he does provide along the way is mainstream and persuasive –- but invites his readers to give serious scientists the attention and respect their work demands. And he tries to do it not by telling, but by showing how they can get to the position where they find their own realisation that the science must be heeded.