Abstract
Abstract. This work aims to assess the performance of state-of-the-art global climate models in representing the upper-tropospheric Rossby wave pattern in the
Northern Hemisphere and over the European–Atlantic sector. A diagnostic based on finite-amplitude local wave activity is used as an objective metric to
quantify the amplitude of Rossby waves in terms of Rossby wave activity. This diagnostic framework is applied to a set of coupled historical climate
simulations at different horizontal resolutions, performed in the framework of the PRIMAVERA project and compared with observations (ERA5
reanalysis). At first, the spatio-temporal characteristics of Rossby wave activity in the Northern Hemisphere are examined in the multimodel mean of
the whole PRIMAVERA set. When examining the spatial distribution of transient wave activity, only a minimal improvement is found in the high-resolution
ensemble. On the other hand, when examining the temporal variability of wave activity, a higher resolution is beneficial in all models apart from
one. In addition, when examining the Rossby wave activity time series, no evident trends are found in the historical simulations (at both standard and
high resolutions) and in the observations. Finally, the spatial distribution of Rossby wave activity is investigated in more detail focusing on the
European–Atlantic sector, examining the wave activity pattern associated with weather regimes for each model. Results show a marked inter-model
variability in representing the correct spatial distribution of Rossby wave activity associated with each regime pattern, and an increased horizontal
resolution improves the models' performance only for some of the models and for some of the regimes. A positive impact of an increased horizontal
resolution is found only for the models in which both the atmospheric and oceanic resolution is changed, whereas in the models in which only the
atmospheric resolution is increased, a worsening model performance is detected.
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