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Titel Seasonal to interannual variability in density around the Canary Islands and their influence on the Atlantic Meridional Overturning Circulation at 26N
VerfasserIn Aurelie Duchez, Eleanor Frajka-Williams, Natalia Castro, Joel Hirschi, Andrew Coward
Konferenz EGU General Assembly 2014
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 16 (2014)
Datensatznummer 250091343
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2014-5631.pdf
 
Zusammenfassung
The meridional interior flow obtained from the RAPID array is determined by horizontal density fluctuations at the eastern and western boundary of 26N. The physical causes of these density variations are responsible for fluctuations in the Atlantic Meridional Overturning Circulation (AMOC) and through it, the meridional heat transport of the Atlantic. In this modelling study, a high resolution ocean model is used to investigate the source and origin of the AMOC variability associated with the density fluctuations at the eastern boundary. The AMOC in the model is in good agreement with the RAPID observations and appears to adequately represent the smaller scale features of variability around the Canary Islands. In this study, we identify a robust relationship between the density structure south of the Canary Islands, the local wind stress curl and the AMOC using an empirical orthogonal functions analysis, wavelet transform and wavelet coherence. We find that the deep density fluctuations at the eastern boundary of 26N arise from the pumping effect of the spatial pattern of wind stress curl south of the islands. These deep density fluctuations drive the AMOC both on seasonal and interannual timescales, through their influence on the basinwide tilt of the thermocline. At seasonal timescales, the density fluctuations south of the islands are driven by the WSC and directly influence the AMOC. At interannual timescales, a significant coherence is found between the density fluctuation and the southward UMO transport although the origin of these density fluctuations is not explained by the direct pumping caused by the WSC.