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consequences of climate change over the next twenty, forty, a<br />

hundred, thousands of years, what the significance of those<br />

are for different groups of societies, different individuals in<br />

society, are actually much more contested. So I think it is<br />

much harder to converge on a single consensus and accept<br />

what the consequences are for society, although again the<br />

IPCC does make some effort to move in that direction.<br />

PROFESSOR PIDGEON: Chris, I think you had some<br />

comments in your written evidence on climate sensitivity. I<br />

thought it was interesting that, regarding the climate system,<br />

you made a statement that the 2 to 3 degrees may be higher<br />

or there was a chance that it may be higher? Can that be<br />

related to the forthcoming IPCC report?<br />

DR WEST: Yes. I think the IPCC report will give a figure --<br />

it will be hidden away in tables -- for the sensitivity; a<br />

theoretical number that says what the global temperature does<br />

with doubling of carbon dioxide. A hundred years ago it was<br />

said to be between four and six. I think now people are<br />

coming to a figure somewhere between two and three,<br />

somewhere near there, but interesting results at the Exeter<br />

conference a year ago suggested it was possible that the<br />

sensitivity is much higher. I think that is a risk that is not<br />

zero. There is a significant risk that it is higher. I would put<br />

this in the category of uncertainties as opposed to facts which<br />

cover, if you like, the causes and the causal relationship<br />

between greenhouse gases, temperature rise, sea level rise,<br />

changed climate systems, that is a quantification of all of that<br />

of which the sensitivity of the climate system is one that, if<br />

you like, we are approaching better and better knowledge, but<br />

clearly we will not know what it is until it happens, if then. I<br />

think, more importantly, there are the other uncertainties in<br />

that sort of sensitivity of the human system to climate<br />

change, which we do not have either any experimental<br />

evidence for or any modelling evidence for. As Mike says,<br />

that is very much harder to project forward. Then I think<br />

there are uncertainties of yet another sort where we know --<br />

this is a Donald Rumsfeld known/unknown. There are bits in<br />

the climate system that can switch from one state to another.<br />

What we do not know is when or how likely it is. Of course<br />

there are the same sorts of state functional changes possible<br />

in human systems, and I do not think we have begun to think<br />

what those changes might mean.<br />

PROFESSOR PIDGEON: Can you just give us a couple of<br />

examples of both types; the climate ones?<br />

DR WEST: A known/unknown, if you like, the North<br />

Atlantic circulation partly driven by salinity drawdown off<br />

Greenland. We know that in the past that circulation has<br />

collapsed. We anticipate it is possible it collapses again. We<br />

do not know how it might collapse -- it has been very hard to<br />

recreate it in models -- but it is a possibility. Most models<br />

show the flow diminishing but not stopping. If it stopped<br />

that would be a very serious consequence. So we know<br />

something about what it would be like if it happened, but we<br />

cannot say anything about when or how likely it is to happen.<br />

On the unknown unknowns on the human side; if we look at<br />

a country like Bangladesh, which clearly is vulnerable to sea<br />

level rise, at some point it is possible that the population no<br />

longer put up with increased frequency of flooding and they<br />

want to move somewhere else. May be that number of<br />

people moving to higher ground has global geopolitical<br />

consequences. It is a very difficult thing to investigate.<br />

DR PARR: Could I just add a couple of comments about the<br />

role of uncertainty in policy? My observation on the way<br />

that the climate debate is often carried out is that the level of<br />

certainty that seems to be sought is of a completely different<br />

order of magnitude -- well, no, that is wrong -- but it is very<br />

different from the sort of certainty that is expected for other<br />

policy interventions. For example, what is the evidence base<br />

for assuming that all class sizes in a school should be below<br />

thirty? That is an established policy or has been an<br />

established policy for the Labour <strong>Party</strong>. What, one might<br />

mischievously ask, is the evidence for weapons of mass<br />

destruction being in particular countries? What is the<br />

evidence that certain forms of taxation stimulates certain<br />

forms of behaviour? On many of these issues there are<br />

actually uncertainties that seem to me to be way beyond the<br />

uncertainties in terms of climate science . I talk here about<br />

policies demanding mitigation rather than adaptation policies<br />

because I think that my two colleagues have suggested they<br />

are a different order of magnitude there. My point is that<br />

somehow there seems to be a search for complete certainty<br />

where it feels to me to be an inappropriate search for<br />

certainty given that, broadly, we know that there are some<br />

unpleasant things going to happen as a result of climate<br />

change, and certainly our belief is that it is one of the greatest<br />

threats to human society that there is.<br />

PROFESSOR PIDGEON: That led on to the next question<br />

we were interested in, which is do we need more science?<br />

Well, we do need more science; that is a rhetorical question.<br />

But, on the climate side, do we need more science or do we<br />

actually need to act now? Has the balance shifted radically in<br />

the last five years or so?<br />

DR PARR: My view would clearly be that we need to act<br />

now. I am certainly not saying we do not need more<br />

research, in some cases, of a very different kind. We need<br />

more research, but we clearly need action. Action is far more<br />

important this point. We have the evidence base that we need<br />

to say we need to do something.<br />

PROFESSOR PIDGEON: Do the others have a view on<br />

that?<br />

DR WEST: I would support that: we have enough evidence<br />

to act. Whether we have enough evidence to say how much<br />

we should act, that is harder to say, but at this point in time<br />

the action we have does not look like enough. It would be<br />

hard to go much further than that.<br />

PROFESSOR PIDGEON: Thank you. In a sense that leads<br />

on to the next question that we were interested in. Given that<br />

--<br />

PROFESSOR WHITBY: Mike, you did not comment on<br />

that. Do you agree?<br />

PROFESSOR HULME: Just on the uncertainty? On<br />

research versus action?<br />

PROFESSOR PIDGEON: Yes.<br />

PROFESSOR HULME: I think there is scientific evidence<br />

that humans are often confused in ways that are potentially<br />

damaging, or even, if they are not potentially damaging, at<br />

least in ways that potentially society needs to respond to in<br />

order to continue to sustain the sort of economic and social<br />

functions that we currently have. That evidence is clear that<br />

in some way, shape or form is necessary. I think that the<br />

problems come -- and this is obviously what we lead on to<br />

later on -- in actually deciding what are the appropriate types<br />

of responses. Are they ones that can only be addressed<br />

globally? Are they ones that actually can be implemented on<br />

much more local scales? I think, in reality, the climate is<br />

changing, humans are implicated, and that challenges a huge<br />

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