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 ECHAM5/OMI global circulation model according to SRES A1B scenario, 1961-2099 (ENSEMBLES).
Description
Daily values of mean, minimum, maximum temperature and total precipitation from the SMHI RCA-ECHAM5 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 ECHAM5/OMI of the Max-Planck-Institut für Meteorologie 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 ECHAM5 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: fcc9011e-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