Abstract
The time-longitude lag-correlation analysis of Fraedrich and Lutz is modified to include a second spatial dimension, thereby allowing coherent wave structure to be traced in time in the zonal-height or zonal-meridional planes. The analyses reveal vertical propagation of Rossby wavetrains from the troposphere into the stratosphere in midlatitudes; the correlation patterns suggest a downstream vertical splitting of the wave trains, with short horizontal scales confined to the troposphere. Zonal-meridional time-lag correlations of time-filtered data reveal the familiar teleconnection and stormtrack patterns seen in previous studies; similarities and differences between hemispheres are discussed. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 257-271 |
| Number of pages | 15 |
| Journal | Tellus, Series A: Dynamic Meteorology and Oceanography |
| Volume | 40 A |
| Issue number | 4 |
| DOIs | |
| State | Published - Aug 1988 |
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