Multiple flow regimes in the Northern Hemisphere winter. Part II: sectorial regimes and preferred transitions

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Abstract

This paper presents an observational analysis of recurrent flow patterns in the Northern Hemisphere (NH) winter, based on a 37-year series of daily 700-mb height anomalies. Large-scale anomaly patterns that appear repeatedly and persist beyond synoptic time scales are identified by searching for local maxima of probability density in a phase subspace, which is spanned by the leading empirical orthogonal functions (EOFs). By using an angular probability density function (PDF), we focus on the shape, not magnitude, of the anomaly patterns. The PDF estimate is nonparametric; that is, our algorithm makes no a priori assumption on symmetry with respect to the climatological mean as in one-point correlation and rotated EOF analyses. The local density maxima are searched by iterative bump hunting. A synoptic characterization of onsets and breaks for the flow regimes obtained is given by compositing. In situ evolutions of anomaly patterns, slow westward shifts of high-latitude anomaly centers, and successive downstream increase of anomaly magnitudes are the typical signatures of such events. -from Authors

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Kimoto, M., & Ghil, M. (1993). Multiple flow regimes in the Northern Hemisphere winter. Part II: sectorial regimes and preferred transitions. Journal of the Atmospheric Sciences, 50(16), 2645–2673. https://doi.org/10.1175/1520-0469(1993)050<2645:MFRITN>2.0.CO;2

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