Regional land surface warming over South America induces a stronger tropical Pacific zonal SST gradient and more La Niña-like mean state via diabatic heating contrasts and stationary Rossby waves in coupled model experiments.
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Remote Influences of Land Surface Temperature and their Implications for Sea Surface Temperature Patterns
Regional land surface warming over South America induces a stronger tropical Pacific zonal SST gradient and more La Niña-like mean state via diabatic heating contrasts and stationary Rossby waves in coupled model experiments.