Abstract
The largest increases in surface temperatures over the Northern Hemisphere in the decade prior to 1988 were in Alaska, while substantial decreases occurred in the North Pacific Ocean. In particular, from 1977 to 1988, there was a deeper and eastward-shifted Aleutian low-pressure system in the winter half year, which advected warmer and moister air into Alaska and colder air over the North Pacific. Associated changes in surface-wind stress and wind-stress curl altered the North Pacific Ocean currents, as revealed by the Sverdrup transport. The North Pacific changes appear to be linked through teleconnections to tropical atmosphere-ocean interactions and the frequency of El Nino versus La Nina events. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 988-993 |
| Number of pages | 6 |
| Journal | Bulletin of the American Meteorological Society |
| Volume | 71 |
| Issue number | 7 |
| DOIs | |
| State | Published - 1990 |
| Externally published | Yes |
Fingerprint
Dive into the research topics of 'Recent observed interdecadal climate changes in the Northern Hemisphere'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver