Abstract
The “Warm-Arctic/Cold-continents” (WACC) winter weather pattern is investigated using the European Centre for Medium-Range Weather Forecasts 20th Century reanalysis data (ERA20C) spanning 1901–2010. Both the 1920–1940 and 1990–2010 periods are characterized by Arctic amplification (AA) and mid-latitude continental cooling, although the Arctic warming signal for 1990–2010 is twice as strong as that for 1920–1940. Significant weakening in the mid-latitude polewards temperature gradient and zonal wind, wavier upper-level flow character, and strong regional blocking frequency/intensity changes are also detected during both AA periods. These results based on statistical analyses highlight the possible role of AA in affecting mid-latitude weather patterns, but further work is needed to quantify the influence of AA on particular mid-latitude dynamical features.
Original language | English (US) |
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Pages (from-to) | 5245-5254 |
Number of pages | 10 |
Journal | International Journal of Climatology |
Volume | 38 |
Issue number | 14 |
DOIs | |
State | Published - Nov 30 2018 |
All Science Journal Classification (ASJC) codes
- Atmospheric Science
Keywords
- Arctic amplification
- blocking frequency/intensity
- cold-continents
- jet stream
- mid-latitude weather
- warm-Arctic