ENSO Warm (El Niño) and Cold (La Niña) Event Life Cycles: Ocean Surface Anomaly Patterns, Their Symmetries, Asymmetries, and Implications.

By N. Larkin, D. E. Harrison. 2002

266 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/6d5f1b5be87618ccd7002ced8c5b00f7280af729

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. Robert Hallberg
2. S. Griffies
3. Andrew T. Wittenberg
4. I. Held
5. Alistair Adcroft
6. T. Bayr
7. F. Jin
8. Claudia Frauen

In Global and Planetary Change

1. S. Griffies
2. F. Jin
3. Robert Hallberg
4. T. Bayr
5. Alistair Adcroft
6. Claudia Frauen
7. Chunzai Wang
8. D. Dommenget

In Oceanography

1. Robert Hallberg
2. S. Griffies
3. Alistair Adcroft
4. T. Bayr
5. I. Held
6. Claudia Frauen
7. Chunzai Wang
8. F. Jin

Citations in the corpus

• Analysis of the non-linearity in the pattern and time evolution of El Niño southern oscillation (2013, background): “Further, it has been noted that the time evolutions of strong El Niño events are different from those of strong La Niña events (Larkin and Harrison 2002; Ohba and Ueda 2009; D. Dommenget (&) C. Frauen School of Mathematical Sciences, Monash University, Clayton, VIC, Australia e-mail:…”
• A Proposed Mechanism for the Asymmetric Duration of El Niño and La Niña (2011, background): “A proposed mechanism for the asymmetric duration of El Niño and La Niña”
• The GFDL Earth System Model Version 4.1 (GFDL‐ESM 4.1): Overall Coupled Model Description and Simulation Characteristics (2020, background): “1 shows a realistically broad spectral peak, arising from both the episodic character and the interdecadal modulation of ENSO (Atwood et al., 2017; Kessler, 2002; Larkin & Harrison, 2002; Wittenberg, 2009; Wittenberg et al., 2014).”
• Understanding Enso Physics—A Review (2013, background): “ENSO as a stable mode triggered by stochastic forcing (or noise) has been suggested by many authors [e.g., McWilliams and Gent, 1978; Lau, 1985; Penland and Sardeshmukh, 1995; Blanke et al., 1997; Kleeman and Moore, 1997; Eckert and Latif, 1997; Moore and Kleeman, 1999a, b; Thompson and Battisti, 20”
• Hemispheric-scale wind selection facilitates bar-tailed godwit circum-migration of the Pacific (2014, background): “…the genesis, intensity and tracks of storms that, over existing migration corridors, can create both favourable and unfavourable conditions (Chand & Walsh, 2011; Froude, 2009; Larkin & Harrison, 2002; Mantua & Hare, 2002; Mesquita et al., 2010; Overland et al., 1999; Whysall, Cooper, & Bigg, 1987).”
• Combination Mode Dynamics of the Anomalous Northwest Pacific Anticyclone (2015, result): “A circulation asymmetry between different ENSO phases has been noted in previous studies (Larkin and Harrison 2002; McGregor et al. 2013).”
• The Impact of Convection on ENSO: From a Delayed Oscillator to a Series of Events (2008, unknown): “tropical variability on inter-annual timescales (Larkin and Harrison 2002; Rasmusson and Carpenter 1982).”