Equatorial Origin of the Observed Tropical Pacific Quasi‐Decadal Variability From ENSO Nonlinearity

Author:

Liu Chao1ORCID,Zhang Wenjun1ORCID,Jin Fei‐Fei2ORCID,Stuecker Malte F.3ORCID,Geng Licheng2

Affiliation:

1. CIC‐FEMD/ILCEC Key Laboratory of Meteorological Disaster of Ministry of Education (KLME) Nanjing University of Information Science and Technology Nanjing China

2. Department of Atmospheric Sciences School of Ocean and Earth Science and Technology (SOEST) University of Hawai‘i at Mānoa Honolulu HI USA

3. Department of Oceanography & International Pacific Research Center (IPRC) School of Ocean and Earth Science and Technology (SOEST) University of Hawai‘i at Mānoa Honolulu HI USA

Funder

China Scholarship Council

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference83 articles.

1. Nonlinearity and Asymmetry of ENSO*

2. The Role of Zonal Advection Feedback in Phase Transition and Growth of ENSO in the Cane-Zebiak Model

3. Evaluation of the ECMWF ocean reanalysis system ORAS4

4. Behringer D. &Xue Y.(2004). Evaluation of the global ocean data assimilation system at NCEP: The Pacific Ocean. Paper presented at Eighth Symposium on Integrated Observing and Assimilation Systems for Atmosphere Ocean and Land Surface American Meteorological Society 84th Annual Meeting American Meteorological Society Seattle WA.

5. ATMOSPHERIC TELECONNECTIONS FROM THE EQUATORIAL PACIFIC1

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