Ocean heat uptake and its consequences for the magnitude of sea level rise and climate change

By Till Kuhlbrodt, J. Gregory. 2012

221 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/78073a85e3d3f73aec84302628481cd5a9238365

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. John Marshall
2. S. Griffies
3. J. Gregory
4. M. Buckley
5. M. Webb
6. K. Armour
7. Bjorn Stevens
8. Robert Hallberg

In Oceanography

1. John Marshall
2. S. Griffies
3. Robert Hallberg
4. M. Buckley
5. Gokhan Danabasoglu
6. B. Fox‐Kemper
7. Raffaele Ferrari
8. K. Armour

Citations in the corpus

• OMIP contribution to CMIP6: experimental and diagnostic protocol for the physical component of the Ocean Model Intercomparison Project (2016, background): “These terms will help to understand mechanisms for the large spread in ocean heat uptake efficiency found in CMIP5 simulations (Kuhlbrodt and Gregory, 2012), which in turn impact on the spread in projected sea level rise (Slangen et al., 2012; Church et al., 2013b; Hallberg et al., 2013; Slangen et…”
• Origins of the Solar Radiation Biases over the Southern Ocean in CFMIP2 Models (2014, background): “As one of the few areas where the deep ocean is connected to the surface, it also plays a key role in CO2 and heat uptake (Caldeira and Duffy 2000; Kuhlbrodt and Gregory 2012).”
• Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “Moreover, analyses suggest that differences in ocean heat uptake may explain a significant portion of the large intermodel spread in simulated warming [Raper et al., 2002; Boé et al., 2009; Hansen et al., 2011; Kuhlbrodt and Gregory, 2012; Geoffroy et al., 2013a, 2013b].”
• Resolving and Parameterising the Ocean Mesoscale in Earth System Models (2020, background): “horizontal resolution when moving from the eddyparameterising to the eddy-present regime [115], to the near surface vertical resolution [116], and, in eddy-parameterising models, to the magnitude of the thickness diffusion parameter [117].”
• Impact of the Atlantic meridional overturning circulation on ocean heat storage and transient climate change (2014, background): “Moreover, analyses suggest that differences in ocean heat uptake may play an important role for the large inter-model spread in simulated warming [Raper et al., 2002; Boé et al., 2009; Hansen et al., 2011; Kuhlbrodt and Gregory , 2012; Geoffroy et al., 2013a, b].”