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Le terme de forçage radiatif désigne une perturbation d'origine extérieure au système climatique qui impacte son bilan radiatif. Une telle perturbation peut être associée à des modifications du flux d'énergie solaire arrivant au sommet de l'atmosphère, à des variations de la concentration atmosphérique d'espèces radiativement actives ou encore à des variations d'autres agents pouvant affecter le bilan radiatif de la planète (ex: éruptions volcaniques). La perturbation conduit alors à une
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