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Le forçage orbital

Le forçage orbital est un changement du climat de la Terre causé par des changements dans l’inclinaison de l’axe de rotation de la planète et aussi par la forme de l’orbite de la Terre. Ces changements influencent la quantité d’énergie solaire reçue par la Terre. On croit que le forçage orbital est responsable de cycle des périodes de glace et des périodes interglaciaires.

Trois composantes principales influencent l’emplacement et la quantité de rayonnement solaire qui atteignent la surface de la Terre: l’excentricité, l’obliquité et la précession.

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