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- W2013455912 abstract "Abstract A series of experiments are performed to examine the response of an ocean general circulation model to different surface temperature anomalies. The model used is the Bryan‐Cox primitive equation model, with a horizontal resolution of 2° × 2° in longitude/latitude and an idealized North Atlantic basin geometry. Ten levels are used in the vertical. The model is forced at the surface by temperature anomalies with magnitudes characteristic of simulated global warmings. The time‐scales of the forcing consist of an abrupt switch‐on, as well as a gradual switch‐on forcing over 100 years. The sensitivity to lateral and isopycnal mixing, and the asymmetry of the responses to warm and cold temperature anomalies are also examined. There is an asymmetric behaviour in the transient response for the warm and cold anomaly cases, with the cold case responding more energetically. However, the new equilibrium circulations are approximately symmetric. The warm anomaly case forces a weakened ther‐mohaline circulation in the short term and a strengthened thermohaline circulation in the long term. The opposite behaviour is observed for the cold anomaly case. The abrupt and gradual time‐scales of the forcing produce identical equilibrium circulations but different transient responses. The isopycnal mixing parametrization yields a more rapid and energetic response compared to lateral mixing." @default.
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- W2013455912 date "1992-12-01" @default.
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- W2013455912 title "The response of an ocean general circulation model to long time‐scale surface temperature anomalies" @default.
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- W2013455912 doi "https://doi.org/10.1080/07055900.1992.9649459" @default.
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