Challenges and Prospects for Reducing Coupled Climate Model SST Biases in the Eastern Tropical Atlantic and Pacific Oceans: The U.S. CLIVAR Eastern Tropical Oceans Synthesis Working Group

By Paquita Zuidema, Ping Chang, B. Medeiros, B. Kirtman, R. Mechoso, E. Schneider, T. Toniazzo, Ingo Richter, R. Small, K. Bellomo and 10 more. 2016

135 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/837a0e4f3936d8637f4e8f60cda96e0de36b3b34

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In Atmospheric Science

1. P. Nabat
2. Bertrand Decharme
3. A. Alias
4. Sophie Valcke
5. M. Bentsen
6. O. Geoffroy
7. D. Saint‐Martin
8. Michael Schulz

In Global and Planetary Change

1. O. Geoffroy
2. A. Voldoire
3. D. Oliviè
4. P. Nabat
5. Bertrand Decharme
6. A. Alias
7. Sophie Valcke
8. M. Bentsen

In Oceanography

1. M. Bentsen
2. Sophie Valcke
3. Gurvan Madec
4. A. Voldoire
5. C. Cassou
6. J. Tjiputra
7. M. Webb
8. T. Andrews

Citations in the corpus

• Evaluation of CMIP6 DECK Experiments With CNRM‐CM6‐1 (2019, background): “This type of SST warm bias is systematic to many climate models (Hourdin et al., 2015; Richter, 2015) and several origins have been pointed out in the literature (Zuidema et al., 2016, and references herein).”
• Overview of the Norwegian Earth System Model (NorESM2) and key climate response of CMIP6 DECK, historical, and scenario simulations (2020, background): “Model Dev., 13, 6165–6200, 2020 cause rooted in both local (including mesoscale) and remote (including equatorial) biases in both atmosphere- and ocean-model components (Toniazzo and Woolnough, 2014; Zuidema et al., 2016; Stammer et al., 2019).”