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Tropical Atlantic biases and their relation to surface wind stress and terrestrial precipitation.
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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 et al., 2012
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Metadata
- Authors
- Richter, I., Xie, S.-P., Wittenberg, A. T., & Masumoto, Y.
- Affiliations
- University of Hawaiʻi at Mānoa (US)
- NOAA Geophysical Fluid Dynamics Laboratory (US)
- Japan Agency for Marine-Earth Science and Technology (JP)
- Corresponding author
- Richter, Ingo
- Venue
- Climate Dynamics
- Published
- 2011-03-04
- Volume
- 38
- Issue
- 5-6
- Pages
- 985-1001
- ISSN
- 0930-7575 (ISSN-L)
- 1432-0894
- OpenAlex
- W2093765598
- Cited by
- 146
- References
- 37
- Citations by year
- 2026: 3 · 2025: 7 · 2024: 9 · 2023: 4 · 2022: 19 · 2021: 12 · 2020: 7 · 2019: 12 · 2018: 16 · 2017: 10 · 2016: 8 · 2015: 10 · 2014: 8 · 2013: 9 · 2012: 11
- FWCI
- 7.94
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Climate Dynamics (publishedVersion)
- Funders
- National Oceanic and Atmospheric Administration
- 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 › Meteorological Phenomena and Simulations
- Keywords
- tropical Atlantic, equatorial easterlies, cold tongue, Bjerknes feedback, wind stress, land surface processes, soil moisture, albedo, Kelvin waves, seasonal cycle, interannual variability
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