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Cited by 20Climate variability and modelsOceanographic and Atmospheric ProcessesGeology and Paleoclimatology Research

An ocean perspective on CMIP6 climate model evaluations

Liu, Hailong, Song, Zhenya, Wang, Xidong, Misra, Vasu·2022·Deep Sea Research Part II: Topical Studies in Oceanography
DOI 10.1016/j.dsr2.2022.105120
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  • Both at an annual and seasonal scale, CMIP6 GCMs tend to overestimate coastal and oceanic SST with respect to OISST 1/4, although this overestimation is much more pronounced nearshore, especially in the BUS and CAUS.

    “Both at an annual and seasonal scale, CMIP6 GCMs tend to overestimate coastal and oceanic SST with respect to OISST 1 /4, although this overestimation is much more pronounced nearshore, especially in the BUS and CAUS, as pointed out by previous authors [56].”

    From Examining the ability of CMIP6 models to reproduce the upwelling SST imprint in the Eastern Boundary Upwelling Systems (2022) · cites this paper as [56]

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Authors
Liu, H., Song, Z., Wang, X., & Misra, V.
Affiliations
  • Shanghai Jiao Tong University (CN)
  • Ministry of Natural Resources (CN)
  • Hohai University (CN)
  • Florida State University (US)
Corresponding author
Song, Zhenya
ORCID
Venue
Deep Sea Research Part II: Topical Studies in Oceanography
Publisher
Elsevier BV
Published
2022-07
Volume
201
Pages
105120
ISSN
0967-0645 (ISSN-L)
DOI
10.1016/j.dsr2.2022.105120
OpenAlex
W4281771796
Cited by
20
References
0
Citations by year
2026: 1 · 2025: 9 · 2024: 7 · 2023: 2 · 2022: 1
Type
journal article
Language
en
Open access
closed
Licence
Locations
Deep Sea Research Part II Topical Studies in Oceanography (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
Keywords
CMIP6, climate model evaluation, sea surface temperature, sea surface salinity, marine heatwaves, central tropical Pacific, global sea level, Atlantic meridional overturning circulation

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