Merapi, volcanoes and cooling

Back in April, when Eyjafjallajökull in Iceland was erupting and causing much disruption to air travel in Europe and the North Atlantic, there was some concern that the volcano’s ash and aerosols could cause global cooling. As I said at the time, there was little chance of that happening because volcanoes need to be near the equator to cause global cooling events. However, we now we have an eruption in Indonesia that has the potential to cause a noticeable global cooling. Merapi is Indonesia’s most active volcano, and the eruptive sequence which began at the end of October has already killed at least 153 people and emitted a considerable amount of sulfate aerosols as this NASA Earth Observatory image shows:

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At the time of writing the eruption was showing signs of easing off, and the amounts of sulfur emitted to date haven’t been sufficient (or reached high enough altitudes) to cause a significant cooling. However, as Jeff Masters notes, Merapi’s volcanic history indicates that it is capable of very powerful eruptions which could mimic or exceed the Pinatubo eruption in 19941991 which caused a 0.5ºC cooling over the following 18 months. As ever, the best place to follow events is at vulcanologist Erik Klemetti’s Eruptions blog (note: new web address). Definitely one to watch.

NZ glaciers holding their own (just)

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New Zealand’s glaciers just about held their own over last summer, showing a very slight gain in mass on average according to NIWA’s annual end of summer snowline survey, released today. The Park Pass glacier (above) in the Mt Aspiring National Park between the Hollyford Valley and the head of Lake Wakatipu (map) is one of the 50 index glaciers in the NIWA survey. From the press release:

“A moderate El Niño developed in the tropical Pacific in spring last year. This brought more southwesterlies, with normal to below normal temperatures through last summer and into autumn this year. The overall effect was to hold snowlines in a near steady state this year,” says [NIWA scientist] Dr Hendrikx. The previous two years (2007–08 and 2008–09) had seen end-of-summer snowlines rise significantly as not enough snow fell to compensate for melting.

The impact of the El Niño shows as a (very) small uptick at the end of the ice mass graph, but the overall trend remains strongly downwards.

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The full report (with lots of pictures from the aerial survey) can be downloaded from the NIWA web site. The Park Pass photo above was taken on March 6th this year on the fourth leg of NIWA’s alpine flight, and shows some spectacular icebergs in the proglacial lake. The extent of the glacier’s retreat can be seen in the Google Earth imagery at Mauri Pelto’s From A Glacier’s Perspective blog post on the nearby Donne Glacier. With a strong La Niña now influencing weather patterns in NZ, it’ll be interesting to see how the glaciers fare. I wonder if I can blag a seat on the 2011 flight? ;-)

La modélisation du climat

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A little bit of French language practise for the weekend — an excellent visualisation of how climate models work, produced by the Institut Pierre Simon Laplace, the leading French modelling group. Even if you can’t follow the commentary, the images are pretty much self-explanatory and very nicely done. There are more animations at the DSM Youtube channel.

Hat tip to Steve Easterbrook, who has a version with English subtitles, but we don’t need those, do we? 😉

Preparing for Climate Change

Preparing for Climate Change (Boston Review Books)

The global climate is changing. The impacts on human society are likely to be very serious. We would be foolish indeed not to plan ahead for coping strategies. Michael Mastrandrea and the late Stephen Schneider have produced a small book setting out what we can best do to be ready for what is in store.  Preparing for Climate Change is one of the Boston Review Books, a series of “accessible, short books that take ideas seriously”.

It’s a thoughtful, well-organised piece of writing which leads the reader by steps through what is needed to prepare for what climate change will  bring. The first step is to understand that global warming is for real. It’s under way and it is largely due to anthropogenic forces. However predicting its future course is difficult because of two things we don’t know — how much more greenhouse gases humans will emit and exactly how the natural climate system will respond to those emissions. The temperature rises we face will depend on the level of emissions, and the range of projections for the year 2100 that the IPCC has estimated on the basis of six different scenarios is very wide, from as low as 1.1 degrees to as much as 6.4 degrees. The latter could be catastrophic. The former looks increasingly likely to be well surpassed. But even a comparatively low level of temperature rise would bring damaging changes for some communities and ecosystems. Indeed the 0.75 degree increase of the past century is already showing some worrying impacts.

The authors then outline the key vulnerabilities that need to be taken into consideration. They include glacier loss, melting ice sheets, sea level rise, higher infectious disease transmission, increases in the severity of extreme events, large drops in farming productivity especially in hotter areas, the loss of cultural diversity as people have to leave their historical communities, and an escalating rate of species extinction. Many of these can already be witnessed in their early stages, and the book provides examples from various parts of the globe. Additionally, however, there is the possibility of “surprises”, fast non-linear climate responses which may occur when environmental thresholds are crossed. Some can be imagined, such as a collapse of the North Atlantic ocean currents or the deglaciation of Greenland or the West Antarctic ice sheets. But because of the enormous complexities of the climate system there is also the possibility of unforeseeable surprises.

In the face of inherent uncertainty we have to proceed by risk assessment and risk management as we make our policy decisions.  Risk assessment is primarily a scientific enterprise. Risk management – deciding which risks to tolerate and which to try to avoid – is a political matter where values enter into play.  However the relationship between the two is complicated by the uncertainties of the scientific predictions. These uncertainties will be reduced as research proceeds under normal scientific practice, but answers of some kind are needed well before this time. There are policy decisions to be taken before there is a clear consensus on all the important scientific conclusions. The authors discuss type I and type II errors at this point. A type I error will be committed if we act to mitigate climate change and discover that our worries prove exaggerated and anthropogenic greenhouse-gas emissions cause little dangerous change. A type II error will be committed if we delay action until greater certainty is established and in the process allow serious damage to occur. We have a choice as to which type of error it is better to avoid.

What actions does sensible risk management indicate? We know that reducing emissions will reduce the level of temperature increase that would otherwise occur, but we also know that further climate change will happen no matter how quickly we are able to reduce emissions. We must therefore both try to limit future emissions and at the same time adapt to what we cannot escape.  Mitigation and adaptation must be complementary and concurrent.

The authors recognise some adaptation as autonomous; it is reactive in response to the impacts of climate change. However they consider it vital to also plan adaptation. Planned adaptation may be reactive, but the book lays stress on planning which is anticipatory, as for example in the protection of coastal infrastructure.  Anticipatory adaptation is an investment, but one which may not be able to be afforded by poorer developing countries. The book notes that the Copenhagen Accord recognised this and included a commitment to provide resources for adaptation investment in such countries.

But adaptation measures can only go so far, and mitigation must be seriously pursued in tandem. Although the book focuses a good deal of its attention on how we can plan for adaptation it is clear that there must be a mix with mitigation measures adequate to keep adaptation manageable.  The third more drastic response to climate change of geoengineering is briefly considered, and described as desperate: understandable, but not what the situation demands as a first response.

Whatever mix of mitigation and adaptation we adopt the authors are firm that equity issues must be part of planning. The needs of vulnerable and marginalised groups must be a prominent consideration when forming climate policy.

The question of vulnerability is faced in their final chapter. They see vulnerability assessment as an essential tool to inform the development of climate change policies.  Exposure to stress, sensitivity to the exposure, and adaptive capacity are the three components which need to be considered. Mitigation reduces vulnerability by reducing exposure. Adaptation reduces vulnerability by turning adaptive potential into adaptive capacity. New Orleans before Katrina had quite high adaptive potential, but it was not realised and adaptive capacity was therefore low. Vulnerability assessment is a complex task and they argue for a close relationship between those on the ground in specific regions (bottom-up) and the climate-impact assessments of scientists (top-down). Again, questions of justice are high in their priorities.  We must be sure that marginalised countries and groups are not ignored as we tackle the potentially dangerous, irreversible climate events ahead.

For those familiar with the subject the ground the book covers is probably not new.  But the writers are authoritative and their treatment is well organised and logically ordered. It is also informed by a strong sense of humanity. Their book is an excellent short statement for the general reader and a useful summary analysis for those who appreciate a reminder of how the various elements fit together. Don’t be misled by the moderate tone or the acknowledgement of the uncertainty which must attend predictions of future change. The authors know they are writing of an urgent and pressing need to prepare in advance if we are to avoid the worst consequences of climate change.

[Help Hot Topic to meet its running costs by buying via Fishpond (NZ), Amazon.com, or Book Depository (UK, with free shipping worldwide).]


 

Under African skies

Guardian journalist Madeleine Bunting has been in Mali, learning how it is affected by climate change. In an article published on Sunday she wrote of her visit to the remote town of Anakila where an enormous encroaching sand dune threatens.

“For years now, the elders explain, they have been worried by climate change. Disrupted rain patterns, shifts in winds have no parallel in collective memory; they notice how it is prompting changes in the behaviour of animals and birds. But all of these anxieties are dwarfed by the sand dune now looming above their town – the result of those drier, fierce winds and erratic, intense rainfall.”

 

She describes the action of the dune and the measures the people are taking to try to contain it. But it’s difficult to see it as other than a losing battle.

“The ecological niche in which they have built their lives has always been full of uncertainties – and often hardship – but now the niche on which they have built cultures of great sophistication and resilience is shrinking beneath them as desert threatens.”

Bunting comments that it is in remote places like this that climate change will hit first and hardest, in cultures built on a deep understanding of their environment.

“Anakila’s residents are the canaries down the mine, their experience a foretaste of an Earth hostile to human inhabitation. But their experience of threat, potential devastation and loss of livelihood is discounted and ignored. No dunes are threatening Manchester.”

She goes on to discuss the requirement of environmental justice that rich countries should assist affected populations in poor countries to adapt to the changes that are upon them, noting however the dismal likelihood that funds for climate adaptation will simply be poached from development aid budgets.

The deniers were out in force in the comments that followed the article, and are still going strong as I write this. No surprises in what they have to say. They have no difficulty brushing aside the notion that something exceptional is occurring. These are perennial problems not related to human-caused climate change which isn’t happening anyway. The population increase in Mali is the reason for the problem. The aid organisations are making a big song and dance out of natural events in order to get more of our money. African governments are corrupt. And so on…and on.

These kinds of arguments will continue to be advanced until doomsday by those who have committed themselves to the view that human-caused climate change isn’t happening. But the experience of the people in the town of Anakila is consonant with the expected impacts of climate change in their region. Sure it may have been worsened by deforestation and sure a rapidly growing population is not the best armoury against a diminishing environment. But the global warming which is basically driving the changes is not within the power of the local population to affect. It is within the power of the major industrialised and industrialising nations. Need those nations wait until they see grave impacts within their own populations, which they undoubtedly will before too much longer? Articles such as Bunting’s are early casualty reports of the damage inflicted on humanity at large by the emissions we continue to pour into the atmosphere.  We owe assistance to those already suffering the effects. And if we have any sense we will also take a warning from what is happening to them.

The Guardian has an accompanying photo gallery of the Anakila dune here, and some blogs of Bunting’s visits to other parts of the country here and here and here. She does a fine job of taking the reader right to where she is. Serious and responsible journalism at its best.

[Paul Simon & Miriam Makeba]