Re: Another blow to global warming doomsayers



On Sat, 15 Apr 2006 04:44:38 GMT, jsavard@xxxxxxxxxxxxxxxxxxxxxxxxxx
(John Savard) wrote:

On 14 Apr 2006 20:20:41 -0700, "Rich" <rander3127@xxxxxxxxx> wrote, in
part:

In research they published last year in the journal Geophysical
Research Letters, a team led by Beate Liepert at the Lamont-Doherty
Earth Observatory reported that they found a measurable decline between
1950 and 1990 in the amount of sun reaching the Earth's surface. The
team concluded that solar radiation is being reduced by growing
quantities of man-made particles in the atmosphere-in particular
those produced by burning fossil fuels.

Until recently, however, climate models hadn't factored in the massive
amounts of methane, a greenhouse gas more effective than carbon dioxide,
being released into the atmosphere by peat bogs in Russia. Peat bogs
that are thawing. Thawing because temperatures *really are* going up,
worldwide.

Not all particulate matter released by burning fossil fuels helps to
increase Earth's albedo. Soot, for example, is black. So the sunlight it
blocks from reaching the Earth's surface still warms the atmosphere.
Doubtless, being competent scientists, the authors of that paper have
considered this. Also, as the research was published _last year_,
presumably the scientific community is aware of their research, and has
taken it under consideration. If, therefore, scientists are still
warning us about global warming, presumably there is still a problem.

We can deal with the problem without going back to the stone age. There
happens to be such a thing as nuclear power.

Don't use that word around the enviro-wackos. Even though evidence
(such as France being 77% nuclear and having cleaner air than most
modern countries) points them away from paranoid theories about it.
In Canada, I'm looking forward to $500/m energy bills now they are
closing all the coal plants, buying expensive natural gas ones and
importing energy from places like New York State at 10x the price
we would be paying.
.



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