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- W1977177875 abstract "[1] A kinematic mechanism for the positive feedback between the North Atlantic Oscillation (NAO) and synoptic eddies are depicted based on observational data analyses. Using three-point rescaled covariance statistics of band-pass-filtered (2–8 days) synoptic eddy fields, we examined observed eddy structure changes associated with winter-mean NAO anomalous flow. It is demonstrated that the NAO flow anomalies systematically deform the structures of recurring synoptic eddies to generate seasonal-mean eddy-vorticity flux anomalies predominately directed to the left-hand side of the NAO flow anomalies. These anomalous eddy-vorticity fluxes converge into the cyclonic center and diverge from the anticyclonic center of the anomalous NAO flow, and thus enhance the NAO flow." @default.
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- W1977177875 date "2009-06-13" @default.
- W1977177875 modified "2023-10-12" @default.
- W1977177875 title "A kinematic mechanism for positive feedback between synoptic eddies and NAO" @default.
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- W1977177875 doi "https://doi.org/10.1029/2009gl037294" @default.
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