marcusmarcusrc (
marcusmarcusrc) wrote2010-05-20 05:51 pm
![[personal profile]](https://www.dreamwidth.org/img/silk/identity/user.png)
Summary of Climate Change Policy Philosophy
The CBO director has posted a nice summary of the tenets of a good climate change policy:
http://cboblog.cbo.gov/?p=902
I appreciate the nod towards non-market solutions as well as price-based solutions (a common example of why more than just a price signal may be required is the "principal-agent" problem, where, for example, a landlord has no incentive to put in insulation because the tenant pays for the heat - or alternatively, in apartments like mine where utilities are included, I have no market incentive not to use excessive heat and or air conditioning because my landlord pays for it).
http://cboblog.cbo.gov/?p=902
I appreciate the nod towards non-market solutions as well as price-based solutions (a common example of why more than just a price signal may be required is the "principal-agent" problem, where, for example, a landlord has no incentive to put in insulation because the tenant pays for the heat - or alternatively, in apartments like mine where utilities are included, I have no market incentive not to use excessive heat and or air conditioning because my landlord pays for it).
no subject
(Anonymous) 2010-06-18 02:15 pm (UTC)(link)Can you give me a ballpark best guess (as these things go - as precise as a global average could ever be) for ocean salinity, acidity, and temperature in 10-15 years?
can you point me to educated best guesses for this sort of thing?
(friend of rifmeister, posting anon from work, will login this evening)
no subject
no subject
Ocean surface acidity will increase (my guess would be about 0.04 pH points per decade, given that we've increase about 0.1 pH points in the past century and ocean uptake of carbon is much higher now than it was in the past), but I don't actually know all that much about acidification.
Salinity, I _really_ know very little about. In the Arctic, salinity will decrease due to melting sea ice and increased river flow from melting glaciers. In areas without land or sea ice contributing fresh water, increased evaporation might make things slightly saltier?
no subject