Relating to atmospheric or oceanic conditions where pressure surfaces align with density surfaces, creating a stable fluid state.
From Greek 'baros' (pressure) + 'tropos' (turning/direction). The term was developed in meteorology and oceanography in the 20th century to describe pressure-density relationships.
Meteorologists use 'barotropic' to describe simple, predictable weather patterns where pressure and density line up nicely, making forecasting easier—whereas 'baroclinic' conditions are chaotic and dangerous, spawning storms and unpredictability.
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