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Bottom line is heating of the surface, Andrew. "Insolation" is the buzzword.
Over land, the amount of heat absorbed/reflected determines the amount and rate of rising air parcels...over water, the absorption rate is pretty constant. I'm not saying that there are no differences over water, only that the differences are small...the jet stream plays a part in moving pressure systems around on the face of the earth with little attention paid to the composition of the surface. Bob Gardner "Andrew Sarangan" wrote in message ... Looking at the worldwide surface analysis chart, it looks like land areas have far more pressure variations than oceans. However, I am not sure if this is a real effect or simply an artifact of the fact that there aren't many observation stations on the oceans. Any thoughts? Here is an example: http://www.opc.ncep.noaa.gov/UA.shtml |
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