Quoting Bob Blakely <[EMAIL PROTECTED]>:

> I'm not necessarily right, Jostein, this is just my best take on global
> warming with a little (but by no means exhaustive) backup.

Bob,
I apologise for being harsh. I guess I should have considered your reply to Dag
more in light of the subject line. I guess it was the "who told you..."
questions.

Now, I'm not necessarily right either, but i'd love to share the thoughts I
have, and the information I gathered, while I was still in the ecology trade.

Since this _is_ off-topic, those of you not interested will do well to bail out
now. I have a feeling this is going to get long...

There are at least 3 gasses that contribute to the greenhouse effect.

The most important is, as you said, water vapour. The abundance of water
vapour in the atmosphere is basically dependent on the degree of evaporation,
which in turn depends on temperature. Clouds do a particularly good job 
retaining heat in the atmosphere, and still allows much of the solar radiation
down to the surface. One key question wrt the greenhouse effect of water vapour
is whether it regulates itself by purely meteorological mechanisms or if
other factors influence it as well. Airplane traffic has been pointed out, but
the effect is thought to be small. One controversial theory is that cloud
formation is influenced by cosmic radiation that rains into the atmosphere all
the time. Cosmic radiation is in turn dependent on the solar wind, which
varies with sunspot activity. Intriguingly, the lowest levels of sunspot 
activity ever recorded (around 1850) coincided with a period of harsh winters
and cold summers. This is controversial, but if this theory is right, our CO2
emissions has probably much less to say than we have been lead to believe.

The second most important gas is CO2. The numbers Bob mentioned is correct, 
afaik, and most of his arguments has been voiced before. 3% increase over 150
years seems like a small drop in the ocean, but the problem is; we don't really
know how much change is needed to tilt the balance. Also, it is suspected that
the current rate of change is faster than any before, seen in a geological
time frame. Another undertainty is that CO2 is water soluble, and the oceans
can absorb quite a lot of it. OTOH, solubility goes down as water temperature
increase... CO2 has also been claimed to be a limiting factor for growth in 
plants, but that's not really true. There's only a small group of plants,
called the C4-plants, that can effectively use higher levels of CO2. Maize is
one example.

The third most important gas is methane. There's very little of it in the
atmosphere, but molecule by molecule it gives 4 times more greenhouse effect
than do CO2. Important sources of methane is biological decomposition in
oxygen-free environments. The gut of cattle, elephants and other plant eaters
is indeed a good example, as Bob W. pointed out. A bit unfair on the Masai
people, though... Wetlands all over the world also generate a lot of methane.
Rice fields are important because the rice plants use the roots to ventilate
the soil of toxic substances like H2S, and let out soil-trapped methane as well.
There are also _huge_ deposits of methane locked by permafrost in the marshlands
of Siberia and Northern Canada, and locked by high pressure in the depths of the
large oceans.

In the "disaster-scenarios" envisioned by the climatologists, the key variable
is always CO2. The questions they try to answer is "what will happen to the
climate if CO2 change?" 

The current consensus is that the most likely scenario is an overall increase
in global temperature, but the total effect is much debated.

One worst-case scenario is that the greenhouse effect from CO2 will alter 
the sea currents enough to let loose the marine deposits of methane, which
will accelerate the process and in turn thaw enough permafrost to unleash
the methane locked up in the arctic bogs. Increased temperature from the
effect of CO2 and methane will increase evaporation from the seas, and
thus the amount of water vapour and cloud cover, further accelerating the 
process. If, otoh, the sea currents change so that the arctic regions receive 
less heat rather than more, the outcome may be colder polar regions, and the 
onset of a new ice age because precipitation come as snow.

As you see, if you have bothered to read me this far, the factors are
complicated and predictions are fraught with uncertainty. We can be sceptical to
the political correctness of crying wolf, but there is one good point in favour:
We would err on the safe side, as Mike said.

oh, well. A long rant... Thanks for reading.


Cheers,
Jostein




 


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