Two Independent Triggers for the Indian Ocean Dipole/Zonal Mode in a Coupled GCM
By A. Fischer, P. Terray, Eric Guilyardi, Silvio Gualdi, Pascale Delecluse. 2005
200 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/2b42ffae5143c955a107b6e49f49b6e4049f251a
How researchers see this paper
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In Atmospheric Science
In Global and Planetary Change
- D. Dommenget
- Swadhin K. Behera
- M. Mcphaden
- Shang-Ping Xie
- H. Hendon
- Jin-Yi Yu
- Toshio Yamagata
- Jing‐Jia Luo
In Oceanography
- D. Dommenget
- Swadhin K. Behera
- M. Mcphaden
- Shang-Ping Xie
- H. Hendon
- Toshio Yamagata
- Jing‐Jia Luo
- M. Stuecker
Citations in the corpus
- Representation and prediction of the Indian Ocean dipole in the POAMA seasonal forecast model (2009, methodology): “Following Fischer et al. (2005) and Luo et al. (2007), we present in Figure 1(a–c) ensemble mean climatologies, as a function of lead time, for SST, U10, and D20 along the Equator in the Indian Ocean (2 ◦S–2◦N).”
- Pantropical climate interactions (2019, background): “1B), but the IOD can occur independently of (30), and have an impact on (4), ENSO.”
- Climate Fluctuations of Tropical Coupled Systems—The Role of Ocean Dynamics (2006, result): “The independent development of IOD is reported by most other CGCM studies (Yu et al. 2002; Gualdi et al. 2003; Lau and Nath 2004; Cai et al. 2005; Fischer et al. 2005) but for two exceptions (Baquero-Bernal et al.”