Articles | Volume 13, issue 4
https://doi.org/10.5194/os-13-609-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-13-609-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
North Atlantic deep water formation and AMOC in CMIP5 models
Department of Marine Sciences, University of Gothenburg, Box 115, 405 30 Göteborg, Sweden
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- The impact of a parameterisation of submesoscale mixed layer eddies on mixed layer depths in the NEMO ocean model D. Calvert et al. 10.1016/j.ocemod.2020.101678
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- A perturbed parameter ensemble of HadGEM3-GC3.05 coupled model projections: part 2: global performance and future changes K. Yamazaki et al. 10.1007/s00382-020-05608-5
- Seasonality of the Meridional Overturning Circulation in the subpolar North Atlantic Y. Fu et al. 10.1038/s43247-023-00848-9
- The Atlantic inflow across the Greenland-Scotland ridge in global climate models (CMIP5) C. Heuzé et al. 10.1525/elementa.354
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- Projected sea surface temperatures over the 21st century: Changes in the mean, variability and extremes for large marine ecosystem regions of Northern Oceans M. Alexander et al. 10.1525/elementa.191
- Emergence of deep convection in the Arctic Ocean under a warming climate C. Lique et al. 10.1007/s00382-017-3849-9
- The Relationship Between U.S. East Coast Sea Level and the Atlantic Meridional Overturning Circulation: A Review C. Little et al. 10.1029/2019JC015152
- Biological Carbon Pump Sequestration Efficiency in the North Atlantic: A Leaky or a Long‐Term Sink? C. Baker et al. 10.1029/2021GB007286
Latest update: 15 Nov 2024
Short summary
Climate models are the best tool available to estimate the ocean’s response to climate change, notably sea level rise. To trust the models, we need to compare them to the real ocean in key areas. Here we do so in the North Atlantic, where deep waters form, and show that inaccurate location, extent and frequency of the formation impact the representation of the global ocean circulation and how much heat enters the Arctic. We also study the causes of the errors in order to improve future models.
Climate models are the best tool available to estimate the ocean’s response to climate change,...