Strong El Niño events and nonlinear dynamical heating

By F. Jin, Soon-Il An, A. Timmermann, Jingxia Zhao. 2003

291 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/6080e74be7e191aabf8c8b994e925ccad1a3215e

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

In Global and Planetary Change

In Oceanography

Citations in the corpus

A simple approach to quantifying the noise–ENSO interaction. Part I: deducing the state-dependency of the windstress forcing using monthly mean data (2015, background): “Either additive noise in a system with deterministic nonlinear dynamics (Jin et al. 2003; Su et al. 2010) or state-dependent noise in a linear system can generate these asymmetries (Müller 1987; Sardeshmukh and Sura 2009; Levine and Jin 2010; Lopez and Kirtman 2014).”
Understanding Enso Physics—A Review (2013, background): “Wyrtki [1985] defined the warm water in the tropical Pacific between 15°S and 15°N.”
Climate Fluctuations of Tropical Coupled Systems—The Role of Ocean Dynamics (2006, background): “They further argued that the nonlinear heating induced changes in ENSO amplitude have a rectification effect on the climate mean state (Jin et al. 2003).”
ENSO suppression due to weakening of the North Atlantic thermohaline circulation (2005, background): “…the direct greenhouse warming effect, the equatorial thermocline sharpness (Timmermann et al. 1999a; Meehl et al. 2001), nonlinear dynamic heating (Jin et al. 2003; An and Jin 2004), changes in the strength of the annual cycle (Liu 2002a; Timmermann and Jin 2004), or offequatorial SST anomalies…”
Improved ensemble-mean forecasting of ENSO events by a zero-mean stochastic error model of an intermediate coupled model (2016, background): “Thus, during the ENSO cycles, the NDH due to the vertical advection is illustrated to be facilitated by certain temporal and spatial phase differences in the current fields and temperature gradient (Jin et al. 2003; An and Jin 2004).”