Evaluation of precipitation and temperature simulation performance of the CMIP3 and CMIP5 historical experiments

• Main Authors: Κουτρουλης Αριστειδης(http://users.isc.tuc.gr/~akoutroulis), Koutroulis Aristeidis(http://users.isc.tuc.gr/~akoutroulis), Γρυλλακης Εμμανουηλ(http://users.isc.tuc.gr/~EGrillakis), Gryllakis Emmanouil(http://users.isc.tuc.gr/~EGrillakis), Τσανης Γιαννης(http://users.isc.tuc.gr/~gtsanis), Tsanis Giannis(http://users.isc.tuc.gr/~gtsanis), Παπαδημητριου Λαμπρινη(http://users.isc.tuc.gr/~lpapadimitriou), Papadimitriou Labrini(http://users.isc.tuc.gr/~lpapadimitriou)
• Format: Article in Journal/Newspaper
• Language: English
• Published: SpringerOpen 2018
• Subjects: CMIP3; CMIP5; Intercomparison; Precipitation; Skill score; Temperature; Antarc*; Antarctica
• Online Access: http://purl.tuc.gr/dl/dias/F972F781-3BE6-49DC-8C0A-E1C50762E14B; https://link.springer.com/article/10.1007%2Fs00382-015-2938-x 10.1007/s00382-015-2938-x

Summarization: The fifth phase of the Coupled Model Intercomparison Project (CMIP5) is the most recent coordinated experiment of global climate modeling. Compared to its predecessor CMIP3, the fifth phase of the homonymous experiment—CMIP5 involves a greater number of GCMs, run at higher resolutions with more complex components. Here we use daily GCM data from both projects to test their efficiency in representing precipitation and temperature parameters with the use of a state of the art high resolution gridded global dataset for land areas and for the period 1960–2005. Two simple metrics, a comprehensive histogram similarity metric based on the match of simulated and observed empirical pdfs and a metric for the representation of the annual cycle were employed as performance indicators. The metrics were used to assess the skill of each GCM at the entire spectrum of precipitation and temperature pdfs but also for the upper and lower tails of it. Results are presented globally and regionally for 26 land regions that represent different climatic regimes, covering the total earth’s land surface except for Antarctica. Compared to CMIP3, CMIP5 models perform better in simulating precipitation including relatively intense events and the fraction of wet days. For temperature the improvement is not as clear except for the upper and lower hot and cold events of the distribution. The agreement of model simulations is also considerably increased in CMIP5. Substantial improvement in intense precipitation is observed over North Europe, Central and Eastern North America and North East Europe. Nevertheless, in both ensembles some models clearly perform better than others from a histogram similarity point of view. The derived skill score metrics provide essential information for impact studies based on global or regional land area multi-model ensembles. Presented on: Climate Dynamics