Abstract
The possible linear and nonlinear impact of the Maden-Julian Oscillation (MJO) on ENSO are studied. It is found that the former requires estimation of the low frequency tail of the MJO. The observed surface zonal wind stress is decomposed as the sum of different contributions with special emphasis on the intraseasonal MJO and its low frequency tail. The impact of such estimates in a hierarchy of ENSO coupled models is also presented.
| Original language | English (US) |
|---|---|
| Title of host publication | 26th Conference on Hurricanes and Tropical Meteorology |
| Pages | 252-253 |
| Number of pages | 2 |
| State | Published - 2004 |
| Externally published | Yes |
| Event | 26th Conference on Hurricanes and Tropical Meteorolgy - Miami, FL., United States Duration: May 3 2004 → May 7 2004 |
Other
| Other | 26th Conference on Hurricanes and Tropical Meteorolgy |
|---|---|
| Country | United States |
| City | Miami, FL. |
| Period | 5/3/04 → 5/7/04 |
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ASJC Scopus subject areas
- Engineering(all)
Cite this
Linear and nonlinear influence of the MJO on ENSO. / Zavala-Garay, Javier; Zhang, Chidong; Moore, A. M.; Sahami, K.
26th Conference on Hurricanes and Tropical Meteorology. 2004. p. 252-253.Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Linear and nonlinear influence of the MJO on ENSO
AU - Zavala-Garay, Javier
AU - Zhang, Chidong
AU - Moore, A. M.
AU - Sahami, K.
PY - 2004
Y1 - 2004
N2 - The possible linear and nonlinear impact of the Maden-Julian Oscillation (MJO) on ENSO are studied. It is found that the former requires estimation of the low frequency tail of the MJO. The observed surface zonal wind stress is decomposed as the sum of different contributions with special emphasis on the intraseasonal MJO and its low frequency tail. The impact of such estimates in a hierarchy of ENSO coupled models is also presented.
AB - The possible linear and nonlinear impact of the Maden-Julian Oscillation (MJO) on ENSO are studied. It is found that the former requires estimation of the low frequency tail of the MJO. The observed surface zonal wind stress is decomposed as the sum of different contributions with special emphasis on the intraseasonal MJO and its low frequency tail. The impact of such estimates in a hierarchy of ENSO coupled models is also presented.
UR - http://www.scopus.com/inward/record.url?scp=3042782040&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=3042782040&partnerID=8YFLogxK
M3 - Conference contribution
SP - 252
EP - 253
BT - 26th Conference on Hurricanes and Tropical Meteorology
ER -