Asymmetric dynamical ocean responses in warming icehouse and cooling greenhouse climates

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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Bibliographic Details
Main Authors: Karin F Kvale, Katherine E Turner, David P Keller, Katrin J Meissner
Format: Article
Language:English
Published: IOP Publishing 2018-01-01
Series:Environmental Research Letters
Subjects:
ocean dynamics
greenhouse
cooling climate
warming climate
icehouse
ocean circulation
Online Access:https://doi.org/10.1088/1748-9326/aaedc3

Internet

https://doi.org/10.1088/1748-9326/aaedc3

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