Journal
JOURNAL OF CLIMATE
Volume 29, Issue 7, Pages 2359-2373Publisher
AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-15-0499.1
Keywords
Climate models; Geographic location/entity; Climate prediction; Climate variability; Circulation/ Dynamics; Atmosphere-ocean interaction; Sea ice; Baroclinic flows; Variability; Physical Meteorology and Climatology; Models and modeling
Categories
Funding
- Fonds de Recherche en Science du Climat (FRSCO) from the Ouranos Consortium
- Natural Sciences and Engineering Research Council (NSERC) Discovery grants program
- Canadian Sea Ice and Snow Evolution (CanSISE) Network
- Canadian Network for Regional Climate and Weather Prediction - NSERC Climate Change and Atmospheric Research program
- Fonds de Recherche Nature et Technologies (FRQNT)
- National Science Foundation
- Office of Science of the U.S. Department of Energy
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An important aspect of understanding the impacts of climate change on society is determining how the distribution of weather regimes will change. Arctic amplification results in greater warming over the Arctic compared to the midlatitudes, and this study examines how patterns of Arctic air masses will be affected. The authors employ the Community Earth System Model Large Ensemble (CESM-LE) RCP 8.5, consisting of 30 ensemble members run through the twenty-first century. Self-organizing maps are used to define archetypes of 850-hPa equivalent potential temperature [GRAPHICS] anomalies with respect to a changing climate and assess changes in their frequency of occurrence. In the model, a pattern with negative [GRAPHICS] anomalies over the central Arctic becomes less frequent in the future. There is also an increase in the frequency of patterns associated with an amplified ridge (trough) with positive (negative) [GRAPHICS] anomalies over western (eastern) North America. It is hypothesized that the increase in frequency of such patterns is the result of enhanced forcing of baroclinic waves owing to reduced sea ice over the western Arctic. There is also a decline in patterns that have anomalously high [GRAPHICS] over the North Atlantic, a pattern that is associated with intense ridging in the 500-hPa flow over the North Atlantic and colder [GRAPHICS] over Europe. The authors relate the decrease of these patterns to an enhancement of the North Atlantic jet induced by a warming deficit in the North Atlantic Ocean.
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