How to Recognize a True Mode of Atmospheric Circulation Variability. Issue 3 (11th March 2021)

• Record Type: Journal Article
• Authors: Huth, Radan; Beranová, Romana
• Is Part Of: Earth and space science. Volume 8:Issue 3(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-03-11
• Subjects: Arctic oscillation -- Barents oscillation -- modes of low‐frequency variability -- North Atlantic Oscillation -- principal component analysis -- teleconnections; Space sciences -- Periodicals; Geophysics -- Periodicals; 500.5
• DOI: 10.1029/2020EA001275
• Languages: English
• ISSNs: 2333-5084

Abstract

Abstract: It has been demonstrated several times that when principal component analysis (PCA) is used for detection of modes of atmospheric circulation variability (teleconnections), principal components must be rotated. Despite it, unrotated PCA is still often used. Here we demonstrate on the examples of North Atlantic Oscillation (NAO), Arctic Oscillation (AO), Barents Oscillation (BO), and the summer East Atlantic (SEA) pattern that unrotated PCA results in patterns that are artifacts of the analysis method rather than true modes of variability. This claim is based on the comparison of the spatial patterns of the modes with spatial autocorrelations, on the sensitivity of the patterns to spatial and temporal subsampling, and, for the SEA pattern, on correlations with tropical sea surface temperature. Unlike NAO, which is defined by rotated PCA, the other modes, that is, AO, BO, and SEA pattern, defined by unrotated PCA, do not correspond well to underlying autocorrelation structures and are more sensitive to choices of spatial domain and time interval over which they are defined. We reiterate that a great care must be taken when interpreting outputs of PCA when applied to the detection of modes of circulation variability: a comparison with spatial autocorrelations and check for their spatial and temporal stability are necessary to distinguish true modes from statistical artifacts, which we call "ghost patterns." Key Points: North Atlantic Oscillation, Arctic Oscillation, Barents Oscillation, and the summer East Atlantic pattern are examined as for their correspondence with underlying correlation structures and spatial and temporal subsampling Arctic Oscillation, Barents Oscillation, and the summer East Atlantic pattern are not true modes of atmospheric circulation variability We reiterate that rotated principal component analysis must be used to detect modes of circulation variability; the use of unrotated principal component analysis is more likely to result in statistical artifacts