On the hiatus in the acceleration of tropical upwelling since the beginning of the 21st century
Chemistry–climate models predict an acceleration of the upwelling branch of the Brewer–Dobson circulation as a consequence of increasing global surface temperatures, resulting from elevated levels of atmospheric greenhouse gases. The observed decrease of ozone in the tropical lower stratosphere duri...
Gorde:
| Egile Nagusiak: | , , , , , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Copernicus Publications
2014-12-01
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| Saila: | Atmospheric Chemistry and Physics |
| Sarrera elektronikoa: | http://www.atmos-chem-phys.net/14/12803/2014/acp-14-12803-2014.pdf |
| Etiketak: |
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