dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Added value of regional climate modeling over areas characterized by complex terrain
VerfasserIn Csaba Zsolt Torma, Filippo Giorgi, Erika Coppola
Konferenz EGU General Assembly 2015
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 17 (2015)
Datensatznummer 250101550
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2015-709.pdf
 
Zusammenfassung
We present an analysis of the added value (AV) of downscaling via regional climate model (RCM) nesting with respect to the driving global climate models (GCMs) over regions characterized by complex terrain. Specifically, we analyse precipitation from ensembles of driving GCM and nested RCM (two resolutions, 0.44° and 0.11°) simulations for the late 20th (1976-2005) and late 21st century (2070-2099) over an area encompassing the European Alps. The GCM simulations are provided by the Coupled Model Intercomparison Project Phase 5 (CMIP5) and the RCM experiments used for this study are from two regional initiatives within Coordinated Regional Downscaling Experiment (CORDEX), namely: EURO-CORDEX (whole European domain) and MED-CORDEX (centered over the Mediterranean region). The 21st century projections are for the high-end representative concentration pathway RCP8.5. Different metrics of AV are investigated, measuring aspects of precipitation where substantial AV can be expected in mountainous terrains: spatial pattern of mean precipitation, daily precipitation intensity distribution and daily precipitation extremes (R95). The metrics are calculated by comparing model precipitation output with data from a high quality, fine scale (5 km) gridded observational dataset. Our analysis shows substantial AV of RCM downscaling for all metrics selected, and in fact results are improved compared to the driving GCMs not only at fine scales but also when the RCM fields are upscaled at the scale of the GCM resolution. We also find consistent improvements in the high resolution (0.11°) vs. the medium resolution (0.44°) RCM simulations. In terms of precipitation change projections, we find that the RCM downscaling substantially modulates the GCM-derived change signal, particularly in terms of fine scale spatial pattern associated with the complex topography of the region. Our results thus clearly demonstrate the AV of RCM nesting and point to the important role that high resolution nested RCMs can play in the study of climate change over areas characterized by complex topographical features.