Glaciers and Paleorecords Tell Us How Atmospheric Circulation Changes and Successive Cooling Periods Occurred in the Fennoscandia during the Holocene
Two major climatic phenomena that occurred during the Holocene are interpreted from the resonance in subharmonic modes of long-period Rossby waves winding around the North Atlantic gyre, the so-called gyral Rossby waves (GRWs). These are, on the one hand, the change in atmospheric circulation that o...
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| Natura: | Artigo |
| Lingua: | Inglês |
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MDPI AG
2021-07-01
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| Serie: | Journal of Marine Science and Engineering |
| Soggetti: | |
| Accesso online: | https://www.mdpi.com/2077-1312/9/8/832 |
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