Earth-prints repository, logo   Istituto Nazionale di Geofisica e Vulcanologia

Istituto Nazionale di Geofisica e Vulcanologia
 
|earth-prints home page | roma library | bologna library | catania library | milano library | napoli library | palermo library

Earth-prints >
Editorial Initiatives >
eJournals >
Annals of Geophysics >

Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/978

Share this record with your favourite social network:     Del.icio.us     Citeulike     Connotea
Facebook     Stumble it!     reddit    
Title: Influence of the North Atlantic on simulated atmospheric variability
Authors: Conil, S.*
Li, Z. X.*
Keywords: atmospheric general circulation model
internal/external variability
climate predictability
teleconnections
Issue Date: 2003
Publisher: INGV
Series/Report no.: 46 (1)
Abstract: An atmospheric general circulation model is used to investigate the influence of the North Atlantic Ocean on atmospheric variability. The study covers the period from 1950 to 1994. The observed sea surface temperature and sea ice extension are used to force the atmospheric model. Several configurations of the oceanic boundary conditions were made to isolate the role of the North Atlantic and to study its non-linear interaction with forcings from other oceanic basins. The multi-realization character of the experiments distinguishes between the internal random part and the external forced part of the total variability. The potential predictability can thus be evaluated. The response of the atmosphere is also studied with a modal approach in terms of hemispheric teleconnection patterns. The North Atlantic Ocean has a direct influence on both the Northern Hemisphere annular mode and the Pacific-North-America pattern, leading to a weak predictability. However the direct response is largely modulated by forcings from other oceanic basins. The non-linearity of the system compensates the predictable component of the annular mode induced by the North Atlantic forcing. Furthermore it reduces the forced component of the Pacific-North-America pattern, increasing its chaoticity.
URI: http://hdl.handle.net/2122/978
Appears in Collections:Annals of Geophysics
03.01.01. Analytical and numerical modeling
02.04.01. Atmosphere/sea ice/ocean interaction

Files in This Item:

File SizeFormat
57_70Conil.pdf1.75MbAdobe PDFView/Open

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

 

Valid XHTML 1.0! ICT Support, development & maintenance are provided by theAePIC team @CILEA.Powered onDSpace Software. Feedback