Tropical Atlantic biases and their relation to surface wind stress and terrestrial precipitation

By Ingo Richter, Shang-Ping Xie, Andrew T. Wittenberg, Yukio Masumoto. Climate Dynamics, 2012

144 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/27f08bd2c87058d2e516293e62a63e35c72bceda

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Seiji Kato
2. R. Small
3. B. Medeiros
4. John M. Dennis
5. Ping Chang
6. Paquita Zuidema
7. C. Bitz
8. R. Tomas

In Global and Planetary Change

1. Seiji Kato
2. J. Thomas Farrar
3. R. Small
4. B. Medeiros
5. John M. Dennis
6. Frank O. Bryan
7. Ping Chang
8. Ingo Richter

In Oceanography

1. J. Thomas Farrar
2. R. Small
3. Frank O. Bryan
4. Ingo Richter
5. C. Bitz
6. R. Tomas
7. B. Kirtman

Citations in the corpus

• 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 (2016, methodology): “These initial wind errors are generally coupled with areas of deep convection (Richter et al. 2012), suggesting that atmospheric circulation errors coupled with model physics, especially tropical convection, originate the short-term systematic biases.”
• Impact of ocean model resolution on CCSM climate simulations (2012, background): “Here we highlight two uncoupled atmosphere-only and Several studies demonstrate that the EEA SST bias is connected to a springtime westerly equatorial trade wind bias (DeWitt 2005) that erroneously deepens the thermocline, inhibiting the summer cold tongue development (Chang et al. 2007; Richter and”