Atlantic meridional overturning circulation stable over the last 150 years
The Atlantic Meridional Overturning Circulation (AMOC) describes the northward flow of warm, salty water in the upper layers, and the southward flow of colder water in the deep Atlantic layers. AMOC strength estimates at 41°N latitude based on satellite sea surface height (SSH), and ARGO ocean tempe...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Sciendo
2019-09-01
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| Series: | Quaestiones Geographicae |
| Subjects: | |
| Online Access: | https://doi.org/10.2478/quageo-2019-0026 |