Bias corrected high resolution temperature and precipitation projection for Europe in daily temporal resolution from the SMHI RCA regional climate model driven by boundary conditions from the BCM global circulation model according to SRES A1B scenario, 1961-2099 (ENSEMBLES).

Daily values of mean, minimum, maximum temperature and total precipitation from the SMHI RCA-BCM transient climate change simulation for the period 1961-2099 have been corrected for biases according to Dosio and Paruolo, 2011: Bias correction of the ENSEMBLES high-resolution climate change projections for use by impact models: Evaluation on the present climate, J. Geophys. Res., 116, D16106, DOI: 10.1029/2011JD015934. These data have been produced from a transient climate change simulation for the period 1951-2099 driven by the coupled global model BCM of the Norwegian Bjerknes Centre according to the SRES A1B marker scenario. 121 different meteorological fields are stored in the database from this simulation; of these, 7 are saved 4 times daily, 4 are saved twice daily, and the rest is saved once daily. This simulation has been produced as part of Research Theme 3 (RT3) of the EU FP6 project ENSEMBLES (http://ensemblesrt3.dmi.dk/). Information on the simulations can be found at http://ensemblesrt3.dmi.dk/, in the special issue 44 of Climate Research (2010), or in the ENSEMBLES final report available at http://http://ensembles-eu.metoffice.com/docs/Ensembles_final_report_Nov09.pdf. Lineage: Simulation data from a regional numerical climate model with lateral and sea-surface conditions determined from the output of the BCN coupled global model. The simulation was produced at the Swedish Meteorological and Hydrological Institute (http://www.smhi.se/en) with the regional climate model RCA3.0. (UUID: 2797d34d-5e33-11e1-9105-0017085a97ab). Daily values of mean, minimum, maximum temperature and total precipitation from this simulation have been corrected for biases according to Dosio and Paruolo, 2011: Bias correction of the ENSEMBLES high-resolution climate change projections for use by impact models: Evaluation on the present climate, J. Geophys. Res., 116, D16106, DOI: 10.1029/2011JD015934