Thursday 23 August 2007

Greenhouse gases and clouds

Many of you will have seen Al Gore's An Inconvenient Truth and Martin Durkin's The Great Global Warming Swindle, probably leaving you confused over whether man really does have anything to do with global warming or not.

The official answer: no-one's really sure.
The real answer: probably.
The first incorrect answer: definitely.
The second incorrect answer: definitely not.

Double the incorrectness if the 'definitely not' is followed by conspiracy theory rambling.

The main reason that man is suggested as a cause is due to his greenhouse gas emissions.
Humans and human industry emit thousands of millions of tonnes of various gases each year, considerably affecting the composition of the Earth's atmosphere.
As an example, carbon dioxide, the most commonly cited of these emissions, is up to a concentration of 385 parts per million (ppm)1, or 385 molecules of carbon dioxide in every million molecules of the Earth's atmosphere (or,alternatively, 0.0385% of the atmosphere).
Prior to the Industrial Revolution, when human industry began to grow in earnest, the levels
were around 280 ppm (and had remained below 290 ppm for at least 400,000 years prior to today)2.
Methane, another commonly cited emission, has grown by about 150% since 1750,
around the beginning of the early Industrial Revolution. It is, however, still present in much smaller quantities than carbon dioxide (approximately 1,750 parts per thousand million (ppb) in 1998)3.

Several gases that we emit are categorised as 'greenhouse gases', gases which retain heat radiation from the Sun in our atmosphere.
Naturally occurring greenhouse gases keep our planet significantly warmer than it would otherwise be, making it suitable for life such as our own.4

It has been shown that greenhouse gas concentrations remained relatively stable for several hundred millennia, although when we go back further we see that there were much higher concentrations in the atmosphere than today.
In particular there were extremely large amounts of carbon dioxide and, more importantly, methane, in the atmosphere around the time of the Permian extinction event, approximately 250 million years ago.5
There is strong evidence to suggest that the temperatures around the equator increased by five or more degrees Celsius at this time, meaning that temperatures at other latitudes would have increased by higher amounts.6

That these greenhouse gases, which include water vapour, carbon dioxide and methane, increase temperatures on the Earth is undoubted. However, what is disputed is the extent to which additional amounts other than the natural will affect the Earth's present climate.

This may seem a simple question - well, if they increase temperatures, then more will increase them still further, obviously - but it is actually quite complicated.
For one, not all factors affecting climate are known or are understood well enough to produce perfect mathematical models of climate.
Clouds are a particularly big unknown; logically, more are formed when there is a higher concentration of water vapour in the atmosphere, but how do clouds affect us?
At night they appear to retain heat by reflecting outgoing radiation back to the Earth, but at
day they do both this and they reflect incoming radiation from the Sun.7
Which one is dominant? How exactly does the amount of water vapour affect their formation? A controversial one, do cosmic rays affect their formation (the answer seems to be 'not really')?8
Even worse, computers are not powerful enough to answer this for us. The most powerful supercomputers designed for climate models cannot handle anything but cells on the Earth about a thousand times bigger than the average cloud, so any effect has to be guessed at by scientists and an approximation fed into the machine.9
Clouds are not the only great unknown. Also unknown are many things about the Earth's oceanic circulatory systems, which have a large effect on climate. Only the simplest of models for these can be produced, and any inaccuracies are likely to be quite large and will multiply in scale with each time-step as the models are run to predict future climate.

There are many other things which also affect the climate, including positive and negative feedback loops. These will be the main topic of the next post (note how in this post we have not arrived at a conclusion as to whether man is causing any warming. The science of climatology is relatively young as a science and there are too many uncertainties to arrive at any definite conclusion, only probabilities).

References:

1. http://www.esrl.noaa.gov/gmd/webdata/ccgg/trends/co2_mm_mlo.dat
2. http://cdiac.ornl.gov/ftp/trends/co2/vostok.icecore.co2
3. http://www.epa.gov/methane/scientific.html#atmospheric
4. http://www.physicalgeography.net/fundamentals/7h.html
5. http://www.astrobio.net/news/print.php?sid=582
6. http://en.wikipedia.org/wiki/Permian-Triassic_extinction_event#Methane_hydrate_gasification
7. http://www.giss.nasa.gov/research/briefs/rossow_01/
8. http://environment.newscientist.com/channel/earth/climate-change/dn11651
9. http://www.aip.org/history/climate/GCM.htm

5 comments:

Anonymous said...

god knows

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