Abstract
Blocking as an extreme event in European weather is addressed. A daily blocking index isapplied to analyses of daily geopotential height at 500 hPa from 1949 to 1995. In order to allowfor a reconstruction of these blocking time series back to 1880, daily SLP analyses are used toextract similar indices, which are optimally correlated to those based on 500 hPa. Daily indicesare also determined for the geopotential height fields of 5 runs with the ECHAM3/T21 GCM, driven by monthly means of observed SST and sea ice boundaries for the years 1950–1994.These simulations differ only in their initial conditions, making it feasible to separate externalvariance (induced by SST and sea ice boundaries) from the atmospheric, model generated, internal variance. The index series reveal high variability both on time-scales of years to decadesand interannual. Time series of spatial means show poor correlations not only between observationsand simulations but also among the single runs of the model. Together with an analysis-of-variance (ANOVA) this leads to the conclusion, that Atlantic–European blocking is barelyinfluenced by SST and sea ice distribution. The blocking index time series from observationsis weak, yet significantly, negatively correlated to the NAO index time series favouring blockingsituations during weak NAO periods.
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