Nonlinear Feedbacks Associated with the Indian Ocean Dipole and Their Response to Global Warming in the GFDL-ESM2M Coupled Climate Model

A feature of the Indian Ocean dipole (IOD) is its positive skewness, with cold IOD east pole (IODE) sea surface temperature anomalies (SSTAs) exhibiting larger amplitudes than warm SSTAs. Using the coupled Geophysical Fluid Dynamics Laboratory Earth System Model with Modular Ocean Model version 4 (M...

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Veröffentlicht in:	Journal of climate 2014-06, Vol.27 (11), p.3904-3919
Hauptverfasser:	Ng, Benjamin, Cai, Wenju, Walsh, Kevin
Format:	Artikel
Sprache:	eng
Schlagworte:	Amplitudes Anomalies Asymmetry Brittleness Climate Climate change Climate models Climatology. Bioclimatology. Climate change Cold Damping Data assimilation Dipoles Dynamical systems Earth, ocean, space El Nino Evaporation Exact sciences and technology External geophysics Feedback Fluid dynamics Geophysical fluids Global warming Heating Hydrodynamics Indian Ocean Marine Meteorology Modelling Modular systems Nonlinear dynamics Nonlinear feedback Ocean models Oceans Radiation Radiation-cloud interactions Regression coefficients Sea surface Sea surface temperature Sea surface temperature anomalies Shoaling Short wave radiation Skewed distribution Skewness Standard deviation Surface temperature Temperature anomalies Thermocline Thermoclines Westerlies Wind Winds
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