IPCC GCM coldwave statistics

We present here a sample of our results from an NSF sponsored research project investigating the statistics and mechanisms behind extreme Cold Air Outbreaks (CAOs).

Below are temperature statistics from two modern global climate models (GCMs). Included on each page are winter (DJF) mean temperatures and standard deviations as simulated by the models. These panels illustrate how the mean temperatures are coldest over the snow and ice covered regions of the Northern Hemisphere. In addition, the variability (as measured by the standard deviations) are also highest over those same snow and ice covered regions. These summaries are output from GCMs simulating conditions as close to possible to the past 20-years (1981-2000). They use observed greenhouse gass concentrations for the 1981-2000 period.

The second set of panels show the frequency of cold air outbreaks over the 1981-2000 as simulate by the climate models. The frequency is expressed as CAO days/year. In these plots, CAOs are defined as the number of winter days whose temperature is below the mean by at least two standard deviations for an extended period. The right panels show the number of cold air outbreaks projected to occur by the GCM for the years 2081-2100 in a moderate greenhouse gas increased climate scenario (the IPCC SRESA1B scenario).

Finally, in the bottom panels, we present the change in CAO frequency projected by the models for this greenhouse gas increased climate scenarios in both absolute differences (# days per year) in the left panel, and as a percentage change in frequency in the right panels. In both difference panels, blues and greens denote decreases in cold air outbreak frequencies and yellows and reds indicate increases in CAO frequencies for the 2081-2100 period.

Choose a model:
GFDL
MIROC: MEDIUM RESOLUTION

While the temperatures are expected to warm over the source regions of the coldwaves and the coverage of snow and ice are projected to correspondingly decrease, the GCMs do not necessarily project a corresponding decrease in the number of coldwaves in all regions. One likely explanaion is changes in the wintertime circulation patterns. The patterns of mean sea level pressure and therefore low-level atmospheric circulations simulated and projected by the climate models are presented below for three timeslices: 1981-2000, 2011-2030, 2041-2060, and 2081-2100. Differences from the "control state" (1981-2000) are also shown for the projected periods. In some cases, while the source region and surface boundary conditions are projected to change to be less favorable for cold air mass formation, circulation shifts can counterbalance these climate changes and bring more frequent transports of those cold air masses that do form. The means and differences presented below represent composites of projections made by 14 GCMs from the IPCC Fourth Assessment.

composite IPCC scenarios
SRESA1B composite sea level pressure
Please contact William Chapman with any questions and/or comments or if you would like to see similar statistics for other GCMs.


This material is based upon work supported by the National Science Foundation under Grant No. 0332081.
Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.