Résumé
Future climate change will affect marine productivity, as well as other many components of Earth system. We have investigated the response of marine productivity to global warming with two different ocean biogeochemical schemes and two different atmosphere-ocean coupled general circulation models (GCM). Both coupled GCMs were used without flux correction to simulate climate response to increased greenhouse gases (+1% CO 2/yr for 80 years). At 2xCO 2, increased stratification leads to both reduced nutrient supply and increased light efficiency. Both effects drive a reduction in marine export production (-6%), although regionally changes can be both negative and positive (from -15% zonal average in the tropics to +10% in the Southern Ocean). Both coupled models and both biogeochemical schemes simulate a poleward shift of marine production due mainly to a longer growing season at high latitudes. At low latitudes, the effect of reduced upwelling prevails. The resulting reduction in marine productivity, and other marine resources, could become detectable in the near future, if appropriate long-term observing systems are implemented.
| langue originale | Anglais |
|---|---|
| Pages (de - à) | 81-99 |
| Nombre de pages | 19 |
| journal | Global Biogeochemical Cycles |
| Volume | 15 |
| Numéro de publication | 1 |
| Les DOIs | |
| état | Publié - 23 mai 2001 |
SDG des Nations Unies
Ce résultat contribue à ou aux Objectifs de développement durable suivants
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SDG 13 Action climatique
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SDG 14 Vie sous l’eau
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