The Indian Ocean SST dipole simulated in a coupled general circulation model

By S. Iizuka, Tomonori Matsuura, Toshio Yamagata. 2000

151 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/bed3fa820f9989de5e7f802d27c15642fe62269e

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. Renguang Wu
2. B. Kirtman
3. Swadhin K. Behera
4. S. Rao
5. Toshio Yamagata
6. Sébastien Masson
7. Jin-Yi Yu
8. Seon Tae Kim

In Global and Planetary Change

1. Toshio Yamagata
2. Renguang Wu
3. Swadhin K. Behera
4. B. Kirtman
5. S. Rao
6. Hameed N. Saji
7. K. Ashok
8. Jing‐Jia Luo

In Oceanography

1. Toshio Yamagata
2. Swadhin K. Behera
3. Renguang Wu
4. B. Kirtman
5. S. Rao
6. Hameed N. Saji
7. K. Ashok
8. Jing‐Jia Luo

Citations in the corpus

• Regimes of seasonal air–sea interaction and implications for performance of forced simulations (2007, methodology): “The roles of surface latent heat flux and shortwave radiation are consistent with previous analyses ( Iizuka et al. 2000; Murtugudde et al. 2000; Li et al. 2002; Wang et al. 2003; Hendon 2003; Annamalai et al. 2003; Shinoda et al. 2004; Lau and Nath 2004).”
• Climate Fluctuations of Tropical Coupled Systems—The Role of Ocean Dynamics (2006, unknown): “Iizuka et al. (2000) found a remarkable similarity between the observed IOD and”
• A CGCM Study on the Interaction between IOD and ENSO (2006, methodology): “While Iizuka et al. (2000) reported a weak relation between IOD and ENSO in their model study, Baquero-Bernal et al. (2002) could not find a coupled mode in the Indian Ocean in the absence of ENSO.”
• Comments on ''A Cautionary Note on the Interpretation of EOFs'' (2003, methodology): “…parameters (Saji et al. 1999; Webster et al. 1999; Behera et al. 1999; Rao et al. 2002a,b; Feng et al. 2001), on simulation studies using ocean general circulation models (Vinayachandran et al. 1999, 2002; Murtugudde et al. 2000), and coupled general circulation models (e.g., Iizuka et al. 2000).”
• Interannual subsurface variability in the tropical Indian Ocean with a special emphasis on the Indian Ocean Dipole (2002, background): “Most important finding from the recent studies on the TIO variability is existence of an ocean−atmosphere coupled mode as typified by the dipole structure in SST anomalies (Saji et al., 1999; Webster et al., 1999; Behera et al., 1999; Murtugudde et al., 2000; Iizuka et al., 2000).”
• A Look at the Relationship between the ENSO and the Indian Ocean Dipole (2003, result): “The present result is also supported by the recent studies using Ocean GCMs, Atmospheric GCMs, and coupled GCMs, all of which resolved the expected dynamics (Vinayachandran 2002; Iizuka et al. 2000; Ashok et al. 2001; Rao et al. 2002; Guan et al. 2002; Yu et al. 2002; Yu and Lau 2002), and the recen”