| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1777015 | Journal of Atmospheric and Solar-Terrestrial Physics | 2011 | 21 Pages |
Abstract
⺠The SW1 peaks near the South Pole in December and near the North Pole in March. ⺠SW1 is stronger in the southern hemisphere. ⺠The two-year variations in the March northern SW1 zonal amplitude may be QBO related. ⺠Increases in the mid-latitude SW2 during SSW events were observed but not always consistent. ⺠SW2 increases may be related to an increase of ozone at mid and high latitudes during SSWs.
Related Topics
Physical Sciences and Engineering
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Geophysics
Authors
Q. Wu, D.A. Ortland, S.C. Solomon, W.R. Skinner, R.J. Niciejewski,