In recent weeks as I have read the North American Monthly Weather Review, it has often occurred to me that harsh winters in certain parts of the Northern Hemisphere correlate with mild winters in another part – although I have not noticed a consistent basis by which this occurs.
Analysing Monthly Weather Review issues from the 1970s when hysteria occurred over another ice age after three extreme winters in the eastern United States, I noticed how often higher-than-average temperatures in Alaska seemed to occur alongside extreme cold in the contiguous US (e.g. Januaries 1937, 1963, 1977, 1979). Owing to the cold temperatures and extremely low population densities of Alaska and the Canadian Arctic, little attention was paid to this by Americans faced with extreme cold and shortages of heating oil in January 1977.
Today, I did a table of January temperatures over the contiguous US (apart from the southern States westward to New Mexico) by NWS region and for three representative districts of Alaska, and then did both Spearman rank correlation and Pearson product-moment correlations for them.
To minimise the effect of man-made global warming, I limited my data to the period from 1925 (when Alaska climate data begin) to 1980.
These results constitute a critical contrast with precipitation changes: precipitation changes in a single region are much easier to compare with expected observed changes in circulation from warming of the troposphere – especially the poleward spread of the subtropical arid belts along the west coasts of Australia and South America, as noted by Dian Seidel in ‘Widening of the Tropical Belt in a Changing Climate’ back in 2007 (since when these trends have intensified) – and can also be correlated with inverse precipitation trends in other regions (e.g. eastern WA affected by increased flow of tropical air from monsoons and cyclones) to much more consistent effect.