Rapid summer warming in Greenland since the early 1990s is much greater than global warming over the same period. This Arctic amplification may well have consequences for the behaviour of the northern hemisphere polar jet stream: a giant river of airflow in the atmosphere which is driven by thermal contrast between tropical and polar air masses.
Website address: http://www.sheffield.ac.uk/geography/staff/hanna_edward/index
This Frostbyte was made by Edward Hanna for the Writing workshop "Linkage between Arctic Climate Change and Mid-latitude Weather Extremes". 2-7 September 2014 Seattle, WA, USA
No comments:
Post a Comment