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Generation of hyper climate modes
Author(s) -
Dommenget D.,
Latif M.
Publication year - 2008
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2007gl031087
Subject(s) - teleconnection , climatology , sea surface temperature , environmental science , mode (computer interface) , climate model , tropical climate , atmospheric sciences , tropics , climate change , geology , el niño southern oscillation , geography , oceanography , ecology , archaeology , computer science , biology , operating system
It is shown that some important aspects of the space‐time structure of multidecadal sea surface temperature (SST) variability can be explained by local air‐sea interactions. A concept for “Global Hyper Climate Modes” is formulated: surface heat flux variability associated with regional atmospheric variability patterns is integrated by the large heat capacity of the extra‐tropical oceans, leading to a continuous increase of SST variance towards longer timescales. Atmospheric teleconnections spread the extra‐tropical signal to the tropical regions. Once SST anomalies have developed in the Tropics, global atmospheric teleconnections spread the signal around the world creating a global hyper climate mode. A simple model suggests that hyper climate modes can vary on timescales longer than 1,000 years. Ocean dynamics may amplify theses modes and influence the regional expression of the variability, but are not at the heart of the mechanism which produces the hyper modes.