Irreversible ocean thermal expansion under carbon dioxide removal

• Published in: Earth System Dynamics
• Main Authors: Ehlert, Dana, Zickfeld, Kirsten
• Format: Text
• Language: English
• Published: 2018
• Subjects: Southern Ocean; North Atlantic
• Online Access: https://doi.org/10.5194/esd-9-197-2018; https://esd.copernicus.org/articles/9/197/2018/

In the Paris Agreement in 2015 countries agreed on holding global mean surface air warming to <q>well below 2 °C above pre-industrial</q> levels, but the emission reduction pledges under that agreement are not ambitious enough to meet this target. Therefore, the question arises of whether restoring global warming to this target after exceeding it by artificially removing CO 2 from the atmosphere is possible. One important aspect is the reversibility of ocean heat uptake and associated sea level rise, which have very long (centennial to millennial) response timescales. In this study the response of sea level rise due to thermal expansion to a 1 % yearly increase of atmospheric CO 2 up to a quadrupling of the pre-industrial concentration followed by a 1 % yearly decline back to the pre-industrial CO 2 concentration is examined using the University of Victoria Earth System Climate Model (UVic ESCM). We find that global mean thermosteric sea level (GMTSL) continues to rise for several decades after atmospheric CO 2 starts to decline and does not return to pre-industrial levels for over 1000 years after atmospheric CO 2 is restored to the pre-industrial concentration. This finding is independent of the strength of vertical sub-grid-scale ocean mixing implemented in the model. Furthermore, GMTSL rises faster than it declines in response to a symmetric rise and decline in atmospheric CO 2 concentration partly because the deep ocean continues to warm for centuries after atmospheric CO 2 returns to the pre-industrial concentration. Both GMTSL rise and decline rates increase with increasing vertical ocean mixing. Exceptions from this behaviour arise if the overturning circulations in the North Atlantic and Southern Ocean intensify beyond pre-industrial levels in model versions with lower vertical mixing, which leads to rapid cooling of the deep ocean.