Atlantic origin of asynchronous European interdecadal hydroclimate variability

Discharge time series of major large-catchment European rivers are known to display significant decadal and interdecadal fluctuations. However, the hydroclimate variability causing such fluctuations remains poorly understood, particularly due to a lack of a spatio-temporal integrated assessment. Her...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: Zanchettin D., Toniazzo T., Taricco C., Rubinetti, Sara, Rubino A., Tartaglione N.
Other Authors: Zanchettin, D., Toniazzo, T., Taricco, C., Rubino, A., Tartaglione, N.
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/10278/3717303
https://doi.org/10.1038/s41598-019-47428-6
Description
Summary:Discharge time series of major large-catchment European rivers are known to display significant decadal and interdecadal fluctuations. However, the hydroclimate variability causing such fluctuations remains poorly understood, particularly due to a lack of a spatio-temporal integrated assessment. Here, we demonstrate for the first time that European hydroclimate variability is dominated by a meridional delayed oscillation characterized by a lag of approximately 5 years in interdecadal discharge fluctuations of continental (northern) European rivers with respect to those of Euro-Mediterranean (southern) rivers. We demonstrate a connection of this coherent signal with the large-scale atmospheric circulation over the North Atlantic, and suggest a hitherto unexplored multiannual atmosphere-ocean mechanism in the subpolar North Atlantic at its root.