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Roussenov, Vassil, Williams, Ric ORCID: 0000-0002-3180-7558 and Katavouta, Anna (2021) Added and redistributed heat and carbon in climate model projections for the Southern Ocean.

Williams, Ric ORCID: 0000-0002-3180-7558, Ceppi, Paulo ORCID: 0000-0002-3754-3506 and Katavouta, Anna (2021) Controls of the TCRE in Earth system models.

Williams, Ric, Ceppi, Paulo and Katavouta, Anna ORCID: 0000-0002-1587-4996 (2020) Controls of the Transient Climate Response to Emissions: effects of physical feedbacks, heat uptake and saturation of radiative forcing. In: EGU General Assembly 2020, 2020-5-4 - 2020-5-8, Online.

Ma, Liping (2021) How Does the Atmospheric Jet Stream Affect the Atlantic Ocean? PhD thesis, University of Liverpool.

Pimm, Ciara, Williams, Ric ORCID: 0000-0002-3180-7558, Jones, Dan ORCID: 0000-0002-8701-4506 and Meijers, Andrew ORCID: 0000-0003-3876-7736 (2021) How does heat flux affect potential vorticity in the Southern Ocean?

Pimm, Ciara, Meijers, Andrew ORCID: 0000-0003-3876-7736, Jones, Dan ORCID: 0000-0002-8701-4506 and Williams, Ric ORCID: 0000-0002-3180-7558 (2022) Identifying the drivers of Subantarctic mode water thickness across the south Pacific.

Turner, Katherine (2022) Impacts of thermal and carbon processes on climate reconstructions and projections. PhD thesis, University of Liverpool.

Williams, Ric ORCID: 0000-0002-3180-7558 (2020) Is there warming in the pipeline? A multi-model analysis of the zero emission commitment from CO2. Biogeosciences.

Vakilifard, Negar, Turner, Katherine, Williams, Ric ORCID: 0000-0002-3180-7558, Holden, Philip ORCID: 0000-0002-2369-0062, Edwards, Neil and Beerling, David (2021) Large ensemble assessment of how the global surface warming response to cumulative carbon differs for negative and positive carbon emissions  .

Alvarado Bustos, Ruben Mixing in the continental slope: study case Gulf of Cadiz. Doctor of Philosophy thesis, University of Liverpool.

Goodwin, Philip, Williams, Ric ORCID: 0000-0002-3180-7558 and Ridgwell, Andy (2015) Sensitivity of climate to cumulative carbon emissions due to compensation of ocean heat and carbon uptake. Nature Geoscience, 8 (1). pp. 29-34.