Academic Journal

Discrepancies in the Climatology and Trends of Cloud Cover in Global and Regional Climate Models for the Mediterranean Region

التفاصيل البيبلوغرافية
العنوان: Discrepancies in the Climatology and Trends of Cloud Cover in Global and Regional Climate Models for the Mediterranean Region
المؤلفون: Enríquez Alonso, Aarón, Calbó Angrill, Josep, Sánchez Lorenzo, Arturo, Tan, Elcin
المساهمون: Ministerio de Economía y Competitividad (Espanya)
المصدر: © Journal of Geophysical Research: Atmospheres, 2017, vol. 122, núm. 21, p. 664-677 ; Articles publicats (D-F) ; Enríquez Alonso, Aarón Calbó Angrill, Josep Sánchez Lorenzo, Arturo Tan, Elcin 2017 Discrepancies in the Climatology and Trends of Cloud Cover in Global and Regional Climate Models for the Mediterranean Region Journal of Geophysical Research: Atmospheres 122 21 664 677
بيانات النشر: American Geophysical Union (AGU)
سنة النشر: 2017
المجموعة: Universitat de Girona: DUGiDocs (UdG Digital Repository)
مصطلحات موضوعية: Climatologia, Climatology, Climatologia -- Simulació, Mètodes de, Climatology -- Simulation methods
الوصف: The present study aims at comparing total cloud cover (TCC) as simulated by regional climate models (RCM) from CORDEX project with the same variable as simulated by the driving global climate models (GCM), which are part of the fifth phase of the Climate Model Intercomparison Project ensemble. The comparison is performed for the Mediterranean region, and for the 1971-2005 period, when results from the 'historical' scenario can also be compared with two data sets of ground-based cloud observations. We work with 14 modeling results (resolution, 0.11° × 0.11°), which are a combination of five GCMs and five RCMs. In general, RCMs improve only very slightly the climatic estimation of TCC when compared with observations. Indeed, not all RCMs behave the same, and some indicators (monthly evolution of the relative bias) show an enhancement, while other indices (overall mean bias and annual range difference) improve only very slightly with respect to GCMs. Changes in the estimate of TCC in summer might be the most relevant value added by RCMs, as these should describe in a more proper way several mesoscale processes, which play a more relevant role in summer. Noticeably, RCMs are unable to capture the observed decadal trend in TCC. Thus, TCC simulated by RCMs is almost stable, in contradiction with observations and GCMs, which both show statistically significant decreasing trends in the Mediterranean area. This result is somewhat unsatisfactory, as if RCMs cannot reproduce past trends in TCC, their skill in projecting TCC into the future may be questioned ; This research was supported by the Spanish Ministry of Science and Innovation (currently Ministry of Economy and Competitiveness) Project CGL2014-55976-R
نوع الوثيقة: article in journal/newspaper
وصف الملف: 13 p.; application/pdf
اللغة: English
Relation: info:eu-repo/semantics/altIdentifier/issn/2169-897X; info:eu-repo/semantics/altIdentifier/eissn/2169-8996; info:eu-repo/grantAgreement/MINECO//CGL2014-55976-R/ES/EXPLORANDO LA FRONTERA ENTRE NUBE Y AEROSOL MEDIANTE OBSERVACIONES DESDE SUPERFICIE Y MODELIZACION DE LA TRANSFERENCIA RADIATIVA/; http://hdl.handle.net/10256/14756
الاتاحة: http://hdl.handle.net/10256/14756
Rights: Tots els drets reservats ; info:eu-repo/semantics/openAccess
رقم الانضمام: edsbas.4AD71BB4
قاعدة البيانات: BASE