In the forced simulation with varying SST, the geographical distribution and the statistics of the cyclones are not altered compared to the coupled ECHAM-4/HOPE-G simulation. In the climatological and the ML-simulation, considerable deviations of the mean cyclone distribution are found, which occur mainly in the North Pacific, and can be traced back to missing ENSO variability. In the North Atlantic, the climatological experiment is superior to the ML-experiment. The variability of the cyclone paths, as determined by the cluster analysis, reveals the same types of propagation directions for all four representations of the lower boundary. The largest discrepancies for the cluster occupations are found for the climatological and the ML-simulation.
KeyWords Plus:Midlatitude cyclone tracks, GCM simulation, Cluster analysis
Addresses: Raible C.C., Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstr. 5, CH-3012 Bern, Switzerland. Blender R, Univ Hamburg, Inst Meteorol, Bundesstr 55, D-20146 Hamburg, Germany
Reprints (after having been accepted): Raible CC, Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland, raible@climate.unibe.ch