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At the Hungarian Meteorological Service, twoexperiments were accomplished with the REMO5.0 regional climate model: (1) asimulation of a past period from 1961 to 2000, driven by the ECMWF ERA40re-analysis data, and (2) a transient run from 1951 to 2100 driven by theECHAM5/MPI-OM global coupled atmosphere-ocean model using SRES A1B forcing.The integration domain covers continental Europe with 25 km horizontalresolution in both experiments. Present article is dedicated to theinvestigation of the simulation results for the past period. The results for1961–1990 were compared on the one hand with observations, and on the otherhand, with each other and the corresponding global fields in order to assessthe impact of the different lateral boundary conditions on the resultsfocusing on the area of our interest, i.e., Hungary. The evaluationindicated that the re-analysis driven experiment provides warm and in summerdry past climate over the Carpathian Basin, whereas lower temperature andhigher precipitation values are obtained when the lateral boundaryinformation is derived from a global climate model. Based on the validation,it is concluded that the temperature characteristics in thesimulation-driven case outperformed the experiment forced by quasi-perfect(i.e., re-analysis) data, however, similar apparent conclusion cannot bedrawn for precipitation. This paper is undertaking to give deeper insightinto the details and possible reasons for these outcomes

Diagnostic study of the influence of lateral boundary conditions for the REMO RCM simulations over the Carpathian Basin