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Ozone impacts on climate change

Filed under: — gavin @ 27 July 2007

In a nice example of how complicated climate feedbacks and interactions can be, Sitch and colleagues report in Nature advance publication on a newly modelled effect of ground level (or tropospheric) ozone on carbon uptake on land (BBC). The ozone they are talking about is the ‘bad’ ozone (compared to ‘good’ stratospheric ozone) and is both a public health hazard and a greenhouse gas. Tropospheric ozone isn’t directly emitted by human activity, but is formed in the atmosphere as a result of photolytic reactions related to CH4, CO, NOx and VOCs (Volatile Organic Compounds like isoprene, benzene etc.) – the so-called ozone precursors.

It’s well known that increased ozone levels – particularly downwind of cities – can be harmful to plants, and in this new study with a carbon-climate model, they quantify how by how much increasing ozone levels make it more difficult for carbon to be sequestered by the land biosphere. This leads to larger CO2 levels in the atmosphere than before. Hence the ozone has, as well as its direct effect as a greenhouse gas, an indirect effect on CO2, which in this model at least appears to be almost as large.

Actually it’s even more complicated. Methane emissions are one of the principal causes of the rise of ozone, and the greenhouse effect of ozone can be thought of as an indirect effect of CH4 (and CO and VOCs). But while NOx is an ozone precursor, it actually has an indirect effect that reduces CH4, so that the net impact of NOx has been thought to be negative (i.e. the reduction in CH4 outweighs the increase of ozone in radiative forcing – see this paper for more details). This new result might prompt a re-adjustment of that balance – i.e. if the ozone produced by NOx has a stronger effect than previously thought (through this new indirect mechanism), than it might outweigh the reduction in CH4, and lead to NOx emissions themselves being a (slightly) positive forcing.

In a bizarre way this is actually good news. There are plenty of reasons to reduce NOx emissions already because of it’s impact on air pollution and smog, but this new result might mean that reductions wouldn’t make climate change any worse. It also, once again, highlights the role of CH4 (the second biggest GHG forcing), and points out a further reason (if that was required) why further methane reductions could be particularly welcome in moderating future changes in climate and air quality.

Green and Armstrong’s scientific forecast

Filed under: — gavin @ 20 July 2007

There is a new critique of IPCC climate projections doing the rounds of the blogosphere from two ‘scientific forecasters’, Kesten Green and Scott Armstrong, who claim that since the IPCC projections are not ‘scientific forecasts’ they must perforce be wrong and that a naive model of no change in future is likely to be more accurate that any IPCC conclusion. This ignores the fact that IPCC projections have already proved themselves better than such a naive model, but their critique is novel enough to be worth a mention.
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Friday roundup

Filed under: — group @ 13 July 2007

An eclectic round-up of the week’s climate science happenings (and an effort to keep specific threads clear of clutter).

It’s the sun! (not)

As regular readers here will know, the big problem for blaming the sun for the recent global warming is that there hasn’t been a trend in any index of solar activity since about 1960, and that includes direct measurements of solar output by satellites since 1979. Well, another paper, has come out saying exactly the same thing. This is notable because the lead author Mike Lockwood has worked extensively on solar physics and effects on climate and certainly can’t be credibly accused of wanting to minimise the role of solar forcing for nefarious pro-CO2 reasons!

Stefan was quoted in Nature as saying this is the ‘last nail in the coffin’ for solar enthusiasts, but a better rejoinder is a statement from Ray P: “That’s a coffin with so many nails in it already that the hard part is finding a place to hammer in a new one.”

TGGWS Redux

The still-excruciating ‘Great Global Warming Swindle’ got another outing in Australia this week. The heavily edited ‘new’ version dumped some of the obviously fake stuff that was used the first time around, and edited out the misleading segment with Carl Wunsch. There is some amusing feedback in the post-show discussion panel and interview (via DeSmogBlog).

RC Wiki

As an aside, this is as good a time as any to point people to a new resource we are putting together: RC Wiki, which is an index to the various debunkings of the contrarian articles, TV programs, and internet pseudo-science that is out there. The idea is to have a one-stop shop so that anyone who comes across a piece and wants to know what the real story just has to start there. For instance, the page on TGGWS has a listing of many of the substantive criticisms from the time of the first showing.

Editing the wiki is by invitation only, but let us know if you want to help out, or if you have any suggestions or comments.

The sweet spot for climate predictability

Between the difficulty of long-term weather forecasts and the impossibility of accurate predictions for economic conditions a century hence, there is a sweet spot for climate forecasts. This spot, maybe between 20 and 50 years out, is where the emissions scenarios don’t matter too much (given the inertia of the system) and where the trends start to be discernible over the noise of year to year weather. Cox and Stephenson have a good discussion of the point in this week’s Science and a great conceptual graphic of the issues.

One could quibble with the details (we’d put the sweet spot a little earlier) but the underlying idea is sound, and in judging climate forecasts, it will be projections in that range that should be judged (i.e. the early Hansen projections).

Making sense of Greenland’s ice

Filed under: — gavin @ 9 July 2007

A widely publicised paper in Science last week discussed the recovery ancient DNA from the base of the Dye-3 ice core (in southern Greenland). This was an impressive technical feat and the DNA recovered may well be the oldest pure DNA ever, dating back maybe half a million years. However much of the press coverage of this paper dwelt not on the positive aspects of the study but on its supposed implications for the stability of the Greenland ice sheet and future sea level rise, something that was not greatly discussed in the paper at all. So why was this?
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No man is an (Urban Heat) Island

Filed under: — gavin @ 2 July 2007

Observant readers will have noticed a renewed assault upon the meteorological station data that underpin some conclusions about recent warming trends. Curiously enough, it comes just as the IPCC AR4 report declared that the recent warming trends are “unequivocal”, and when even Richard Lindzen has accepted that globe has in fact warmed over the last century.

The new focus of attention is the placement of the temperature sensors and other potential ‘micro-site’ effects that might influence the readings. There is a possibility that these effects may change over time, putting in artifacts or jumps in the record. This is slightly different from the more often discussed ‘Urban Heat Island’ effect which is a function of the wider area (and so could be present even in a perfectly set up urban station). UHI effects will generally lead to long term trends in an affected station (relative to a rural counterpart), whereas micro-site changes could lead to jumps in the record (of any sign) – some of which can be very difficult to detect in the data after the fact.

There is nothing wrong with increasing the meta-data for observing stations (unless it leads to harassment of volunteers). However, in the new found enthusiasm for digital photography, many of the participants in this effort seem to have leaped to some very dubious conclusions that appear to be rooted in fundamental misunderstandings of the state of the science. Let’s examine some of those apparent assumptions:
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