Quote:
Originally Posted by freebeard
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Ice-cores from around the globe have demonstrated that low-latitude,inland,interior land areas,especially at high elevations are the most sensitive to global warming,and are where deglaciation and interstadial events began over the last 420,000 years.
The warming always precedes the ice-sheet and glacier retreats and iceberg calving events,and melting.
The ice loss is a consequence of the warming,not the other way around.
The 'operative' language of the paper would be the limited scope of 'Southern.'
There may be local,regional heat distribution effects,however,globally,we'll continue to warm.It's impossible for it not to be.