Abstract
The sign of the weighted temperature change over two periods (1950–64, 1942–72) for 15°–80°N was determined by the change in the polar region in spring and autumn, as it was in winter but not in summer. Each of the four seasons shows a different distribution of zonally averaged temperature changes.
| Original language | English |
|---|---|
| Pages (from-to) | 1591-1596 |
| Number of pages | 6 |
| Journal | Monthly Weather Review |
| Volume | 104 |
| Issue number | 12 |
| DOIs | |
| Publication status | Published - 1976 |