dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Representation of XX century midlatitude atmospheric variability in ERA-CLIM simulations
VerfasserIn Alessandro Dell'Aquila, Susanna Corti, Tim Palmer, Sandro Calmanti, Antje Weisheimer, Hans Hersbach, Carole Peubey, Adrian Simmons
Konferenz EGU General Assembly 2015
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 17 (2015)
Datensatznummer 250112302
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2015-12448.pdf
 
Zusammenfassung
We analyse the representation of midlatitude winter atmospheric variability as depicted in XX century-long simulations. We analyse the recent atmospheric integrations produced in the framework of ERA-CLIM project in terms of their capability in reproducing midlatitude planetary waves variability as well as baroclinic activity compared against several reanalysis products. The simulations of ERA-CLIM project (the ERA-20C reanalysis product together with ERA-20CM atmospheric model integrations) could be a quite appealing source of information to catch signals of long term changes. We apply process oriented metrics and ad hoc indexes to validate the ERA-CLIM simulations and, on the same time, to evaluate signals of multi-decadal variability for planetary and baroclinic waves. When observational fields are assimilated (even if only the surface ones, as in the case of ERA-20C reanalysis), the representation of atmospheric variability for the last decades of XX century is in a fair close agreement with other reanalysis products (i.e. NCEP , ERA-Interim reanalysis). However, in the first part of the century (up to 40s’ ) the planetary and baroclinic waves exhibit a quite low activity in the reanalysis. This behaviour cannot be found in the ERA-20CM atmospheric integrations that show, on the other hand, a huge variability, in term of representation of large scale atmospheric waves, between different ensemble members.