The DOI matches its Crossref record; 40 of the 40 references it cites were found in a registry or an index.
Interactive Feedback between ENSO and the Indian Ocean
Abstract
A feedback process of the Indian Ocean SST on ENSO is investigated by using observed data and atmospheric GCM. It is suggested that warming in the Indian Ocean produces an easterly wind stress anomaly over Indonesia and the western edge of the Pacific during the mature phase of El Niño. The anomalous easterly wind in the western Pacific during El Niño helps a rapid termination of El Niño and a fast transition to La Niña by generating upwelling Kelvin waves. Thus, warming in the Indian Ocean, which is a part of the El Niño signal, operates as a negative feedback mechanism to ENSO. This Indian Ocean feedback appears to operate mostly for relatively strong El Niños and results in a La Niña one year after the mature phase of the El Niño. This 1-yr period of phase transition implies a possible role of Indian Ocean–ENSO coupling in the biennial tendency of the ENSO. Atmospheric GCM experiments show that Indian Ocean SST forcing is mostly responsible for the easterly wind anomalies in the western Pacific.
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Cites
The NCEP/NCAR 40-Year Reanalysis Project
Kalnay, E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., Gandin, L., Iredell, M., Saha, S., White, G., Woollen, J., et al. (1996) · Bulletin of the American Meteorological Society · doi:10.1175/1520-0477(1996)077<0437:tnyrp>2.0.co;2 · Cited by 28,360
A dipole mode in the tropical Indian Ocean
Saji, N. H., Goswami, B. N., Vinayachandran, P. N., & Yamagata, T. (1999) · Nature · doi:10.1038/43854 · Cited by 5,510
ATMOSPHERIC TELECONNECTIONS FROM THE EQUATORIAL PACIFIC1
BJERKNES, J. (1969) · Monthly Weather Review · doi:10.1175/1520-0493(1969)097<0163:atftep>2.3.co;2 · Cited by 3,551
Pacific–East Asian Teleconnection: How Does ENSO Affect East Asian Climate?
Wang, B., Wu, R., & Fu, X. (2000) · Journal of Climate · doi:10.1175/1520-0442(2000)013<1517:peathd>2.0.co;2 · Cited by 2,916
Coupled ocean–atmosphere dynamics in the Indian Ocean during 1997–98
Webster, P. J., Moore, A. M., Loschnigg, J. P., & Leben, R. R. (1999) · Nature · doi:10.1038/43848 · Cited by 2,144
An Equatorial Ocean Recharge Paradigm for ENSO. Part I: Conceptual Model
Jin, F.-F. (1997) · Journal of the Atmospheric Sciences · doi:10.1175/1520-0469(1997)054<0811:aeorpf>2.0.co;2 · Cited by 1,589
Remote Sea Surface Temperature Variations during ENSO: Evidence for a Tropical Atmospheric Bridge
Klein, S. A., Soden, B. J., & Lau, N.-C. (1999) · Journal of Climate · doi:10.1175/1520-0442(1999)012<0917:rsstvd>2.0.co;2 · Cited by 1,524
Svoboda, M., LeComte, D., Hayes, M., Heim, R., Gleason, K., Angel, J., Rippey, B., Tinker, R., Palecki, M., Stooksbury, D., et al. (2002) · Bulletin of the American Meteorological Society · doi:10.1175/1520-0477-83.8.1181 · Cited by 1,256
Relaxed Arakawa-Schubert. A Parameterization of Moist Convection for General Circulation Models
Moorthi, S., & Suarez, M. J. (1992) · Monthly Weather Review · doi:10.1175/1520-0493(1992)120<0978:rasapo>2.0.co;2 · Cited by 1,041
Battisti, D. S., & Hirst, A. C. (1989) · Journal of the Atmospheric Sciences · doi:10.1175/1520-0469(1989)046<1687:iviata>2.0.co;2 · Cited by 897
Cited by
Climate impacts of the El Niño–Southern Oscillation on South America
Cai, W., McPhaden, M. J., Grimm, A. M., Rodrigues, R. R., Taschetto, A. S., Garreaud, R. D., Dewitte, B., Poveda, G., Ham, Y.-G., Santoso, A., et al. (2020) · Nature Reviews Earth & Environment · doi:10.1038/s43017-020-0040-3 · Cited by 782
Changing El Niño–Southern Oscillation in a warming climate
Cai, W., Santoso, A., Collins, M., Dewitte, B., Karamperidou, C., Kug, J.-S., Lengaigne, M., McPhaden, M. J., Stuecker, M. F., Taschetto, A. S., et al. (2021) · Nature Reviews Earth & Environment · doi:10.1038/s43017-021-00199-z · Cited by 702
Self-citationOn the Atlantic–Pacific Niños connection: a multidecadal modulated mode.
Martín-Rey, M., Rodríguez-Fonseca, B., Polo, I., & Kucharski, F. (2014) · Climate Dynamics · doi:10.1007/s00382-014-2305-3 · Cited by 112
Omondi, P., Ogallo, L. A., Anyah, R., Muthama, J. M., & Ininda, J. (2013) · International Journal of Climatology · doi:10.1002/joc.3578 · Cited by 60
Metadata
- Authors
- Kug, J.-S., & Kang, I.-S.
- Venue
- Journal of Climate
- Publisher
- American Meteorological Society
- Published
- 2006-05-01
- Volume
- 19
- Issue
- 9
- Pages
- 1784-1801
- ISSN
- 0894-8755 (ISSN-L)
- 1520-0442
- OpenAlex
- W2003237794
- Cited by
- 342
- References
- 40
- FWCI
- 10.95
- Type
- journal article
- Language
- en
- Open access
- closed
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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