Combined solar and QBO effects on the modes of low-frequency atmospheric variability in the Northern Hemisphere

Details Combined solar and QBO effects on the modes of low-frequency atmospheric variability in the Northern Hemisphere Combined solar and QBO effects on the modes of low-frequency atmospheric variability in the Northern Hemisphere

Sep 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009jastp..71.1471h&link_type=abstract

Journal of Atmospheric and Solar-Terrestrial Physics, Volume 71, Issue 13, p. 1471-1483.

Physics

Solar Activity, Quasi-Biennial Oscillation, Tropospheric Circulation, Modes Of Variability

Scientific paper

We examine joint effects of the solar activity and phase of the quasi-biennial oscillation (QBO) on modes of low-frequency variability of tropospheric circulation in the Northern Hemisphere in winter. The winter months (December-March) are stratified by the solar activity into two (below/above median) classes, and each of these classes is subdivided by the QBO phase (west or east). The variability modes are determined by rotated principal component analysis of 500 hPa heights separately in each class of solar activity and QBO phase. Detected are all the modes known to exist in the Northern Hemisphere. The solar activity and QBO jointly affect the shapes, spatial extent, and intensity of the modes; the QBO effects are, however, generally weaker than those of solar activity. For both solar maxima and minima, there is a tendency to the east/west phase of QBO to be accompanied by a lower/higher activity of zonally oriented modes and increased meridionality/zonality of circulation. This means that typical characteristics of circulation under solar minima, including a more meridional appearance of the modes and less activity of zonal modes, are strengthened during QBO-E; on the other hand, circulation characteristics typical of solar maxima, such as enhanced zonality of the modes and more active zonal modes, are more pronounced during QBO-W. Furthermore, the zonal modes in the Euro-Atlantic and Asian sectors (North Atlantic Oscillation, East Atlantic pattern, and North Asian pattern) shift southwards in QBO-E, the shift being stronger in solar maxima.

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