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On the origin of equatorial Atlantic biases in coupled general circulation models.
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“One contribution to the insufficient cold tongue development in models is the equatorial westerly wind bias in March-May (Figure 9), which deepens the thermocline and inhibits cooling during the subsequent June-August upwelling season (Richter and Xie, 2008;Richter et al., 2012).”
From The tropical atlantic observing system (2019) · cites this paper as Richter and Xie, 2008
In the citing paper
“These biases have received much attention but seen little improvement (Davey et al., 2002;Richter and Xie, 2008;Richter et al., 2014b;Giarolla et al., 2015;Zuidema et al., 2016b).”
From The tropical atlantic observing system (2019) · cites this paper as Richter and Xie, 2008
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Self-citation
Metadata
- Authors
- Richter, I., & Xie, S.-P.
- Affiliations
- University of Hawaiʻi at Mānoa (US)
- Corresponding author
- Richter, Ingo
- Venue
- Climate Dynamics
- Published
- 2008-01-30
- Volume
- 31
- Issue
- 5
- Pages
- 587-598
- ISSN
- 0930-7575 (ISSN-L)
- 1432-0894
- OpenAlex
- W1992561914
- Cited by
- 294
- References
- 42
- Citations by year
- 2026: 3 · 2025: 10 · 2024: 13 · 2023: 19 · 2022: 21 · 2021: 19 · 2020: 27 · 2019: 16 · 2018: 22 · 2017: 23 · 2016: 12 · 2015: 17 · 2014: 14 · 2013: 23 · 2012: 20
- FWCI
- 10.22
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Climate Dynamics (publishedVersion)
- Funders
- National Oceanic and Atmospheric Administration
- Lawrence Livermore National Laboratory
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- coupled ocean-atmosphere general circulation model, Intertropical Convergence Zone, equatorial cold tongue, sea level pressure anomalies, thermocline depth, precipitation anomalies, tropical South America, tropical Africa, boreal spring
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