The other Hot Topic

The Hot Topic: How to Tackle Global Warming and Still Keep the Lights on

A book of modest size but surprisingly wide scope, The Hot Topic: How to Tackle Global Warming and Still Keep the Lights on was co-authored last year by Sir David King, former chief scientific adviser to the UK government, and science writer and broadcaster Gabrielle Walker. It has now been published in a revised and updated paperback version. Straighforward clarity marks the writing, and combined with careful organisation of the material results in some readily understandable explanations of complex matters.  Both authors are trained scientists.

The book’s structure is simple. In three parts, it first explains the problem, then discusses the technological solutions and finally canvasses the political solutions.  The intention is to show that although global warming is probably the most serious problem that the human race has, collectively, ever faced, it is not unsolvable.

The problem.  The world is warming, more so and unequivocally in recent decades.  Carbon dioxide and its sister greenhouse gases are responsible, emitted by human activity. Already some of the effects of this heating are being felt in the natural world and in human suffering.  But there is more inescapably in the pipeline, currently delayed by the built-in lag of the ocean which takes a long time to warm up. Moreover there are climate wild cards which could dramatically escalate the scale of the problem, including the shut-down of parts of the oceans’ circulation, massive abrupt sea level rise following ice sheet slide into the ocean, melting permafrost triggering the release of massive amounts of carbon, or some as yet unsuspected danger hidden in the process. But our generation has the chance, the last chance, to avoid the worst of such scenarios.

The technological solutions. We may be able to keep the temperature rise to 2 degrees centigrade if we stay below 450 parts per million CO2 equivalent, lower than earlier estimates which were too optimistic. A rise of 2 degrees will be bad enough in its effects, but we should be spurred to action, not dismayed. The wedges strategy advanced by Socolow and Pacala is the best way to proceed. Efficiency savings are the low hanging fruit and can be achieved quickly.  In transport the right kind of biofuels can play a very useful part, public transport of various kinds can make a big difference to fuel use and hydrogen still remains a possibilty as a fuel.The usual technologies for clean power generation are discussed with some caution, including carbon capture and storage; the book remarks that enough sunlight falls on the earth to meet our energy needs 10,000 times over and in principle wind could generate five times the global electricity needs.  We have the technical wherewithal and ingenuity to achive the greenhouse reductions needed, and the time to start is now.

The political solutions are more difficult. Economics first. The economic debates over discount rates rather miss the point that the science says that action cannot be put off to some future date as some economists have argued – we have to act now.  In any case the costs are not beyond our ability to pay.  Fully global cap and trade schemes, if we learn from early mistakes, can work, though they will need additional regulatory action and government investment to keep us in the right direction. A “Green New Deal” could invigorate the global economy.

On to politics. Post-Kyoto agreement will need a global target, followed by the fiendishly difficult task of dividing the global reductions among the nations of the world. The book spends some time on how this might be done, surveying various possible approaches already on negotiating tables and concluding, perhaps surprisingly, that the choice of approach makes relatively little difference to the requirements for most countries. Carrot and stick financial mechanisms will be required to encourage nations to meet their targets and provide sanctions if they don’t.  The agreement finally will need a mechanism to transfer both technology and funds from the richest countries to the developing world.

There follows an interesting discussion of what will be needed from the five most rapidly developing nations – China, Brazil, South Africa, Mexico and India – and then from the major industrialised countries, noting in the case of the US the new hope that President Obama has brought to the possibility of effective action.

The book concludes with a reminder of actions we can take as individuals to contribute in small ways towards the result.  I appreciated the final paragraph urging us not to despair. “The climate problem is certainly a hard one, but it’s not intractable.” This statement is backed up by a map of the world showing six small squares distributed through the various land masses which would together provide enough energy to power the entire world’s requirements once we learned to capture sunlight efficiently.

The authors describe their aim as being “to tell you everything you wanted to know about global warming but were too depressed to ask.”  Readers who know that depressed feeling may be reassured by the book, though there is nothing facile about its optimism. Indeed there is an element of doggedness in the iteration that now is the time to act, not to despair. A doggedness, I hasten to add, that I am happy to share. The political solution is the sticking point.  I found the book particularly useful in its explanations of the issues in international negotiations and how they might be tackled successfully. The authors may not be politicians, but they draw on experience of the political world  and display a good understanding of how things work there. The interested reader will find complicated matters explained with admirable lucidity.

So much to say (so little time)

NZETS.jpgGareth has suggested I might like to post on Hot Topic my submissions to the ETS Review committee.  I am doing so because the closing date for submissions has been extended by two weeks – it is now 27 February – and I would like to urge readers who haven’t done so to consider making a submission. You will see from what follows that I operate from a slighter base than Gareth, and that may encourage others in a like position. For this post I have chosen four of the terms of reference to which I responded, to keep it within reasonable length.  You can make a submission without responding to every term of reference. And you can be quite brief.  There will be some heavy artillery brought to bear on the committee – indeed it seems that the extension is to accommodate them – but think of what sniper fire can accomplish. The terms of reference are here. Extraordinarily, submissions are required to be posted (two copies) to Committee Secretariat, Emissions Trading Scheme Review, Parliament Buildings, Wellington.  There is helpful material on making a submission here. If you have queries you can ring the Secretariat at 04 817 9560 – they’re servants of the public remember.  (If you get a recorded message I suggest going to reception and asking for the assistant, who I found helpful.)  

Here are my submissions on four of the terms of reference:

Continue reading “So much to say (so little time)”

Five feet high and rising!

Sea.jpg Yesterday, while dissembling, I had what I might loosely describe as a “bugger” moment. Yale’s Enviroment360 web site (which I plugged on its introduction last June) currently features an interview with Robert Bindschadler, a NASA ice expert who is working on the Pine Island and Thwaites glaciers in West Antarctica. The “bugger” moment?

e360: And in the theoretical case that Pine Island and Thwaites glaciers completely dump into the ocean – obviously it’s not going to happen in the near-future – what kind of sea level rise would they contribute to?

Bindschadler: That portion of West Antarctica, that third that flows northward primarily through those two glaciers, has the potential to raise sea level 1½ meters. That’s sort of an upper bound, a worst case. But the time scale is what really matters. Some say that we won’t see these ice shelves disappear in our lifetime – I’m not so sure. I think we might well.

e360: Are you kidding?

Bindschadler: No, no at all.

Bindschadler looks to be about my age. He reports that the ice shelf is melting from the underneath at a rate of about 50 metres per year at the grounding line. And then, a little later, just to make me spill my tea on the keyboard:

e360: I know that the IPCC was saying maybe 1 ½ feet or a half-meter of sea level rise in the 21st century. Is it your opinion that we could be looking at significantly larger sea level rise?

Bindschadler: Yeah, I think there’s sort of an unspoken consensus in my community that if you want to look at the very largest number in the IPCC report, they said 58 centimeters, so almost two feet by the end of the century. That’s way low, and it’s going to be well over a meter. We may see a meter by the middle of the century.

e360: Oh my gosh.

Bindschadler: And if this behavior that we’re seeing in Pine Island, and even Greenland continues – and we don’t see any reason why it wouldn’t continue – well, over a meter by the end of the century, I think is almost certain.

How notably prim the interviewer is. I think I might have managed something a little more Anglo Saxon. A “meter by the middle of the century” is a very long way above most people’s worst case (though not, perhaps, Hansen’s), but it makes our vulnerability to sea level rise much more of a near-term danger than a comfortable reading of AR4 might suggest. It’s a fascinating article — goes into more detail about the WA ice sheet and PIG (yes, that’s what they call it) than anything else I’ve seen in the last few years. Recommended, but not if you have beachfront property.

Meanwhile, a workshop being held at VUW in Wellington is looking at Andrill results, and finding that the WA ice sheet shows signs of repeated meltbacks over the last five million years [Stuff]:

Professor Tim Naish, director of Victoria University’s Antarctic Research Centre […] is co-science leader of the $30 million Andrill project on the ice, with Professor Ross Powell from Northern Illinois University in the United States.

“Antarctica’s ice sheets have grown and collapsed at least 40 times over the past five million years,” Prof Naish said.

“The story we are telling is around the history and behaviour of the ice sheet … as an analogue for the future,” he said.

Not good news, it seems. Expect a rush of papers covering Andrill work over the next few months.

[Johnny Cash]

Someone took the words away

NZETS.jpgDone and dusted. My submission to the Emissions Trading Scheme Review has been safely committed to the tender mercies of NZ Post. It’s a bit long to be posted in full — it’s over 3,500 words (there’s a PDF of the full document here), but I will run through the main recommendations I make. Because the terms of reference were very widely drawn they gave me scope for a submission that tries to put the ETS into a wider climate policy context, and so I’ve taken the opportunity to make some fairly wide ranging suggestions.

[Update: No Right Turn notes that the deadline for submissions has been extended to Feb 27th. Good. But I wish I’d known earlier…]

Continue reading “Someone took the words away”

Smoke on the water

SmokeNZ.jpg

On Monday there was a haze over the Canterbury plains. It looked like someone was burning scrub to the west. Today’s MODIS Image Of The Day shows the source. The image captured on Feb 8th shows that smoke travelled from the Victorian fires (red dots top left — click image to see larger version) across the Tasman and over the South Island. Last weekend was also notably warm on the east coast, as air already warmed by Australia’s heatwave reached NZ and experienced additional heating due to the fohn effect when crossing the Southern Alps. The smoke followed along…

PS: For those not familiar with the local geography, the distance from Melbourne to Christchurch is roughly the same as London to Moscow, or Houston to New York.[Hat tip: MH]

[Deep Purple]