SI
SI
discoversearch

We've detected that you're using an ad content blocking browser plug-in or feature. Ads provide a critical source of revenue to the continued operation of Silicon Investor.  We ask that you disable ad blocking while on Silicon Investor in the best interests of our community.  If you are not using an ad blocker but are still receiving this message, make sure your browser's tracking protection is set to the 'standard' level.
Politics : The Environmentalist Thread -- Ignore unavailable to you. Want to Upgrade?


To: Alastair McIntosh who wrote (26809)12/11/2009 4:38:46 PM
From: Win Smith  Respond to of 36917
 
I don't think the "forcing" means that the earth is absorbing that much more energy; my general understanding is that there's very little net energy absorbed and that radiation in = radiation out, energy wise, just at different frequencies and relative intensities. A wikipedia blurb, less clear than usual:

The radiative forcing of the surface-troposphere system due to the perturbation in or the introduction of an agent (say, a change in greenhouse gas concentrations) is the change in net (down minus up) irradiance (solar plus long-wave; in Wm-2) at the tropopause AFTER allowing for stratospheric temperatures to readjust to radiative equilibrium, but with surface and tropospheric temperatures and state held fixed at the unperturbed values. [2]
In a subsequent report[3], the IPCC defines it as:

"Radiative forcing is a measure of the influence a factor has in altering the balance of incoming and outgoing energy in the Earth-atmosphere system and is an index of the importance of the factor as a potential climate change mechanism. In this report radiative forcing values are for changes relative to preindustrial conditions defined at 1750 and are expressed in watts per square metre (W/m2).":36
en.wikipedia.org

I think the "surface and tropospheric temperature and state held fixed" is the issue here; what actually happens under forcing is that they heat up and radiate more energy out to restore the balance. I think it's pretty clear at this point that there a lot of complications in measuring the radiation balance precisely, and things are a lot more complicated than "forcing raises temperature", though.

If the DSCOVR satellite would provide a good measurement of the net radiation absorbed or lost by the earth I can't imagine why it wouldn't be launched. The expense seems to be trivial as it would pretty well settle the question of global warming.

There's a story there, somewhat polemically told in nytimes.com .