A Theory for the Indian Ocean Dipole–Zonal Mode*

By Tim Li, Bin Wang, Chih-Pei Chang, Yongsheng Zhang. 2003

421 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/d673a241fef57c4240317befbc9158406990fff4

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Citations in the corpus

Development of a four‐dimensional variational coupled data assimilation system for enhanced analysis and prediction of seasonal to interannual climate variations (2008, background): “This type of air-sea feedback is considered to be an important factor in explaining the seasonal phase lock of IODMs [ Li et al., 2003; Wang et al., 2003; Gualdi et al., 2003].”
Climate Fluctuations of Tropical Coupled Systems—The Role of Ocean Dynamics (2006, background): “After reviewing the recent rapid progress in the understanding of coupled dynamics in the region, this study focuses on the active role of ocean dynamics in a seasonally locked east–west internal mode of variability, known as the Indian Ocean dipole (IOD).”
Two Independent Triggers for the Indian Ocean Dipole/Zonal Mode in a Coupled GCM (2005, background): “…Pacific, the signature of the peak of the El Niño events present in REF and absent in noENSO. b. IOZM atmosphere–ocean feedbacks active in the model Li et al. (2003) suggest that there are two positive feedbacks involved in the IOZM, one being the Bjerknes-type wind–thermocline–SST feedback…”
A CGCM Study on the Interaction between IOD and ENSO (2006, background): “One important mechanism that favors IOD formation is the development of an anomalous high over the eastern Indian Ocean (e.g., Saji et al. 1999; Behera et al. 1999; Gualdi et al. 2003; Li et al. 2003; Annamalai et al. 2003).”
Role of the ENSO–Indian Ocean coupling on ENSO variability in a coupled GCM (2006, background): “An, I.-S. Kang, J.-J. Luo,”