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Asymmetric dynamical ocean responses in warming icehouse and cooling greenhouse climates

Warm periods in Earth’s history tend to cool more slowly than cool periods warm. Here we explore initial differences in how the global ocean takes up and gives up heat and carbon in forced rapid warming and cooling climate scenarios. We force an intermediate-complexity earth system model using two a...

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Detalles Bibliográficos
Autores principales: Karin F Kvale, Katherine E Turner, David P Keller, Katrin J Meissner
Formato: Artigo
Lenguaje:Inglês
Publicado: IOP Publishing 2018-01-01
Colección:Environmental Research Letters
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Acceso en línea:https://doi.org/10.1088/1748-9326/aaedc3
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