Gist wrote on Jan 9
th, 2012 at 7:35pm:
gizmo_2655 wrote on Jan 9
th, 2012 at 7:18pm:
Yes, and THAT is the point...a rise in artic/temperate/subtropical temperatures would decrease the difference between high and lower pressure systems (warmer arctic (etc) air is closer to subtropic and tropic temps) whereas cooler arctic and temperate temps would lead to a greater difference...
Think of an aqua duct....if it's closer to level...then the water flows slower....drop the low end and the water flows faster.....now substitute pressure cells for water..The BIGGER the incline, the more severe the storm....
You keep telling me that that is the point while never understanding the point yourself. If you want to use your aquaduct example - you claim that global warming is balancing up the aquaduct to make it more level.
Why would that happen?If you mention anything about glacial and interglacial periods then you have NOT understood what I am talking about. Please go back and read my posts again.
I DO see the point you are making Gist...
Quote:But I'm not sure how it applies to the current situation given you're comparing temperatures probably hundreds of thousands of years apart. We're not in a glacial period, we're in an interglacial period and there are no signs of that changing in the next couple of years.
Quote:A glacial period features large ice masses in the polar regions which would significantly increase reflectivity in the arctic zones. The equatorial zones don't have the ice masses so continue to absorb radiation (sunlight) more or less unchanged. In fact, thinking about it, they may actually get greater sunlight exposure due to less cloud cover (on average) thanks to so much water being trapped in ice at the poles.
And both these points are relevant...
Point one: I was talking about the difference BETWEEN glacial and interglacial temperatures in each zone...i.e in the equatorial zone, there is a far smaller variation between glacial (ice age) and interglacial (now) temperatures than exists in arctic and sub-arctic zones.....so (as an example) the temperatures in Alaska fluctuated much more between the ice age temps compared to the later (holcene) 'current' temps than did the equatorial temps...
Point two: YES, the albedo from the ice cover has a much higher reflecion index, so the temperatures over the ice sheets would be far lower, compared to the temperatures around the equator....( Norway was MUCH colder than New Guinea)..but NOW the temperatures (in the interglacial period) are closer between Norway and New Guinea.......
The basic idea is the closer the temperature..the LESS severe the storm cells....
In a nutshell...an icecube melts slower in cold water than it does in hot water....