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La compensación de los gradientes horizontales de temperatura y salinidad en la capa mixta de los océanos
Science (New York, N.Y.)
|January 23, 1999
Resumen
Los oceanógrafos estudian la capa mixta del océano, encontrando que los gradientes de temperatura y salinidad equilibran los efectos de densidad. Esto apoya las teorías de la mezcla horizontal impulsada por gradientes de densidad en el océano.
Área de la Ciencia:
- La oceanografía física es la oceanografía física.
- Dinámica de fluidos La dinámica de fluidos.
Sus antecedentes:
- La relación temperatura-salinidad es crucial para comprender los patrones de circulación oceánica.
- Las capas mixtas oceánicas juegan un papel importante en la distribución del calor y la sal.
Objetivo del estudio:
- Para investigar la relación entre la temperatura y los gradientes de salinidad en la capa mixta del océano.
- Para determinar cómo estos gradientes influyen en la densidad y la mezcla horizontal.
Principales métodos:
- Utilizó mediciones de alta resolución dentro de la capa mixta del océano.
- Se analizaron datos de temperatura y salinidad a través de escalas horizontales de 20 metros a 10 kilómetros.
Principales resultados:
- Se observó que los gradientes de temperatura y salinidad tienden a compensar el efecto de cada uno en la densidad.
- Se demostró que esta compensación se produce en escalas horizontales relevantes para los procesos de mezcla de océanos.
Conclusiones:
- Los hallazgos apoyan la hipótesis de que la mezcla horizontal en la capa mixta depende de los gradientes de densidad.
- Este mecanismo de compensación es clave para mantener la estructura de capas mixtas e influir en la circulación oceánica.
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