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Wind-driven effects on ocean variability

Claudia Pasquero, Eli Tziperman

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Abstract

A simple model was constructed to study the effects of a wind-driven ocean gyre on the thermohaline overturning circulation. It was found that the presence of a surface gyre allows for stable (self-sustained) oscillations about a mean state characterized by high-latitude deep-water formation regions. The gyre transport had a negative feedback that eliminates the advective instability, allowing for self-sustained thermohaline variability.

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What this paper is about

A simple model was constructed to study the effects of a wind-driven ocean gyre on the thermohaline overturning circulation. It was found that the presence of a surface gyre allows for stable (self-sustained) oscillations about a mean state characterized by high-latitude deep-water formation regions. The gyre transport had a negative feedback that eliminates the advective instability, allowing for self-sustained thermohaline variability.

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Available abstract

A simple model was constructed to study the effects of a wind-driven ocean gyre on the thermohaline overturning circulation. It was found that the presence of a surface gyre allows for stable (self-sustained) oscillations about a mean state characterized by high-latitude deep-water formation regions. The gyre transport had a negative feedback that eliminates the advective instability, allowing for self-sustained thermohaline variability.

Key concepts: Environmental science, Meteorology, Climatology, Oceanography, Geology, Atmospheric sciences, Geography

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