Tumbling dice

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Statement of Pakistan’s Foreign Minister, Mahmood Qureshi to the UN general assembly:

Climate change, with all its severity and unpredictability, has become a reality for 170 million Pakistanis. The present situation in Pakistan reconfirms our extreme vulnerability to the adverse impacts of climate change. It also complicates the reconstruction and rehabilitation scenario in Pakistan. Nature has made a graphic endorsement to strengthen the case for a fair and equitable outcome from the ongoing UNFCCC negotiations.

For more on the Pakistan flood disaster, see the Guardian, BBC and The Cost of Energy amongst many others, and for those wishing to donate, 350.org has a useful page of options. My own choice for disaster relief is Oxfam.

Worth noting too that Indonesia is experiencing “super extreme” weather at the moment, and that floods have also hit the China/North Korea border region.

[Hat-tip to Only In It For The Gold for the cartoon. Do you feel lucky? Well, do you punk?]

[Rolling Stones, Knebworth ’76]

When warming burns…

Severe risks to human health will accompany the disturbed global climate which comes with global warming. We have only to consider the consequences of the heat waves, the flooding, the African droughts, of recent times to be alerted to that. Our experiences of climate change in New Zealand are unlikely to reach such extreme levels, but we would be wise to think and prepare ahead for the kind of human health hazards we may expect to encounter. Chapter 8 in Climate Change Adaptation in New Zealand (pdf download) is an attempt to sketch out measures we might prepare to take. Four of the five writers are from the Department of Public Health at the University of Otago and one from Victoria University.

The paper rehearses some of the widespread major impacts which will affect human health globally. Higher maximum temperature will lead to increased heat-related deaths and illnesses and contribute to an extended range of some pest and disease vectors. Droughts and forest fires will increase in severity and frequency. More intense rainfall will lead to slope instability, flooding and contaminated water supplies. More intense large-scale cyclones increase the risk of infectious disease epidemics (e.g. via damaging water supplies and sewerage systems) and the erosion of low-lying and coastal land through storm surges. Indirect effects include economic instability, loss of livelihoods and forced migrations.

We have early indications of what the changes are likely to be, and it’s important to be ready with a range of policies to address them rather than wait and react as they occur. Prevention is better than cure. New Zealand may not experience the extremes which will be felt in some parts of the world, but there is much that would wisely be given attention.

One eventuality for which we need to be prepared, and which the article highlights, is the possibility of New Zealand becoming a lifeboat to those living in more vulnerable Pacific countries who are displaced by the impacts of climate change. Particularly is this to be expected if a high carbon scenario prevails, as increasingly seems on the cards. Families forced to leave their island homes are likely to form a pattern of chain migration to New Zealand. Unless, under such circumstances, we recognise the need to build extended-family houses or generally increase the supply of low-income family housing to accommodate these immigrants, we are likely to see an increase in overcrowding in state houses and other low-income housing. This could mean a dramatic increase in the risk of a number of infectious diseases.

Infectious diseases are likely to become more prominent with climate change. Warmer temperatures and increased rainfall variability can increase food-borne and water-borne diseases. Vector organisms such as mosquitoes, ticks and sandflies are strongly affected by temperature levels and fluctuations. Hopefully the risk of dengue in New Zealand may remain below the temperature threshold for local transmission, but there is likely to be a potential for outbreaks of Ross River virus infection.

Flooding is another aspect of climate change to which the paper gives some attention. Adaptive responses, such as health and housing protection and provision during and after extreme events, should not increase health inequalities.  The spectre of New Orleans is invoked to illustrate this. The possible need for relocation of towns and even parts of cities looms in some areas of the world. In New Zealand the sustainability of Kaeo, flooded several times in recent years, has been questioned. But given low income levels and less disposable income for private insurance in such towns, government assistance is likely to be needed to facilitate relocation.

Other possible health impacts in New Zealand are touched on, including the effects of heat stress on outdoor workers, the exacerbation of asthma symptoms from increased amounts of allergen-producing pollens, the possibility of water charging by local authorities depriving lower income households of access sufficient to ensure general cleanliness.

Isolation and poor access to services puts people at increased risk. Severe mental health problems are identified as a likely risk in rural communities suffering the effects of extreme weather events. Such vulnerability extends also to low-income populations living in socio-economically disadvantaged, residentially segregated areas where there is less public transport and fewer people who own or have access to cars. The paper makes a good deal of the need for adaptation policies to be equitable and fair and inclusive.

Individual adaptive action can be hampered by lack of understanding, but may be attractive when there are co-benefits. An example is walking, cycling and taking public transport which can be presented as less a sacrifice of time and convenience and more an opportunity to socialise, keep fit, and do one’s bit towards a smaller carbon footprint.

At the community level the paper points to the critical role of local government. The progressive modification of urban form will be an important part of adaptation. Intensifying housing, for example, can reduce the vulnerability of dispersed communities and at the same time help build social capital that links together different social and ethnic groups, while reducing car dependence and energy use. Health and environmental benefits can flow from this.

New Zealand cities have little high density housing and a good many large sprawling suburbs. Some attention is beginning to be given to climate change adaptation issues. The paper focuses on dealing with storm-water run-off and urban heat island effects. Trees, parks and roof-top gardens and reduction of roads and parking lots are among the measures to reduce heat effects. Passive cooling of buildings through good design and the painting white of some surfaces also works to this end. Measures to slow storm water run-off, such as rooftop collection, replacement of hard surfaces by porous paving and well-vegetated low-lying areas can reduce risks. Steps to prevent the incursion of storm water into sewerage systems are important.

Enhanced social networks in cities and other local communities will be needed to provide closer monitoring of, and assistance to, vulnerable people and populations. Living behind locked doors with little neighbourhood contact is not a good preparation for the stresses climate change will bring.

Some needed changes require central government involvement. The paper mentions such matters as retrofitting houses to make them more energy efficient, raising standards in the Building Code, providing social housing. But it also notes that the government record to date shows little sign of advance, and that lack of government progress on mitigation makes adaptation more difficult.

Local government in New Zealand is already expected to take climate change into consideration in its planning, and is provided with useful information by the Ministry for the Environment for doing so. The kind of thinking about health impacts expressed in this paper fits well into the overall intention to “avoid or limit adverse consequences and enable future generations to provide for their needs, safety and well-being.”  Some of it overlaps with measures already recommended to councils. All of it is worth taking up in the discussions and reports that mark local government.  Central government seems trickier ground, more subject to the vagaries of ministers and politics, but one hopes that the good sense represented in papers such as this makes its way there too.

Fire and rain

The last few weeks have seen some extraordinary weather events around the world: relentless extreme heat in Russia, biblical flooding in Pakistan and devastating landslides in China. Tens of millions of people have had their lives disrupted and thousands have died, and — beyond reasonable doubt — global warming is playing a part in creating these extremes. But how much of a part? Michael Tobis asked this question in a recent post:

Are the current events in Russia “because of” “global warming”? To put the question in slightly more formal terms, are we now looking at something that is no longer a “loading the dice” situation but is a “this would, practically certainly, not have happened without human interference” situation?

The answer, at least in the case of the current extremes, would appear to be yes.

Continue reading “Fire and rain”

When the rain comes…

The extreme weather flavour of the moment is without doubt heavy rain and flooding. As I write, severe flooding has caused 132 deaths in southern China and 19 in Burma. The Var region in southern France is recovering from spectacular flash flooding that killed 25 people (watch the BBC video), Tennessee’s recovering from a 1000 year flood in May, and NZ hasn’t escaped. The Metservice blog reports that the flooding in Whakatane a few weeks ago was caused by rainfall of 89.8mm in one hour (with more heavy rain either side of that hour). As the blog notes, that’s tropical rain happening well outside the tropics. But what struck me at the time was a comment from a Whakatane resident included in the TV3 News coverage of that flooding. I can’t remember his precise words, but it was something along the lines of “should be a wake-up call for anyone who doesn’t think global warming’s an issue, because this is what global warming delivers…” Perceptive, I thought, because one of the more robust predictions of climate science is sometimes described as an intensification of the hydrological cycle.

Continue reading “When the rain comes…”

Wetter and drier: we did it

The new Nature paper that prompted yesterday’s post on rainfall intensity is covered in detail by the BBC and New Scientist. Rainfall patterns around the globe are shown to be changing in response to increasing greenhouse gases, in line with model predictions. From New Scientist:

Tropical regions north of the equator, including such areas as the Sahel in Africa which borders the Sahara desert, have already begun to get even drier and will continue to do so, the data show. Regions in the far north, including Canada, Northern Europe and Russia, will get wetter, as will the southern tropics.

The magazine also quotes the paper’s lead author, Francis Zwiers of the Canadian Centre for Climate Modelling and Analysis in Toronto, on changes in rainfall intensity:

Zwiers says an important message from the combined models is that they consistently show that, for all regions, there will be a significant increase in extremes of precipitation – both floods and droughts. Thus, even desert areas that will undergo serious drying could simultaneously suffer greater risks of flash flooding. “More or less uniformly across all the models, these extreme events will become more intense just about everywhere,” he says.

Time to reassess flood risks in NZ, perhaps.