In this study, we evaluate capabilities of 9 CORDEX regional climate models (RCMs) with lateral boundary conditions provided by the ERA-Interim reanalysis to reproduce three-dimensional (3D) structures of heat waves in several European regions in the 1989–2008 period. Heat waves are defined based on positive temperature anomalies from the 95th percentile in near-surface, 850 hPa, and 500 hPa levels with temporal and spatial criteria imposed. Based on predominant locations of positive temperature anomalies, heat waves are classified into four types: i) near-surface, ii) lower-tropospheric, iii) higher-tropospheric, and iv) omnipresent. Characteristics of individual types (e.g. frequency, severity, typical length and occurrence within a summer season) are evaluated against the ERA5 reanalysis. We show contrasting patterns among individual RCMs, pointing to different roles of processes governing heat waves across these simulations.
No takes yet. Share an insight, caveat, or question.
Lhotka et al. (2024) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: