Abstract
A climatology of cold air outbreaks (CAOs) over North America is presented on the basis of a 50 year simulation of the Whole Atmosphere Community Climate Model (WACCM). This climatology is compared to a similar CAO climatology based on 45 years (1957-2002) of European Centre for Medium-Range Weather Forecasts 40 Year Re-Analysis Project (ERA-40) data. A CAO is identified at a given grid point if the following criteria are met: (1) the surface temperature is lower than 1.5 standard deviations below the 31 day climatological running mean, (2) the standard deviation in temperature is greater than 2 K, and (3) conditions 1 and 2 are satisfied over a contiguous area of ∼5° longitude by 5° latitude. WACCM and ERA-40 comparisons are shown for CAO frequency, temperature anomaly from 31 day climatological mean, geographical location, minimum temperature, and areal extent. Overall, CAOs in WACCM occur ∼30% less frequently than in ERA-40 but cover ∼30% greater area and are 1-2 K lower. In midwinter, WACCM CAOs form at lower latitudes and penetrate to lower latitudes compared to CAOs in ERA-40. Copyright © 2011 by the American Geophysical Union.
Cite
CITATION STYLE
Wheeler, D. D., Harvey, V. L., Atkinson, D. E., Collins, R. L., & Mills, M. J. (2011). A climatology of cold air outbreaks over North America: WACCM and ERA-40 comparison and analysis. Journal of Geophysical Research Atmospheres, 116(12). https://doi.org/10.1029/2011JD015711
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.