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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
Estructura fina termohalina en un frente oceanográfico de perfiles de reflexión sísmica
W Steven Holbrook1, Pedro Páramo, Scott Pearse
1Department of Geology and Geophysics, University of Wyoming, Laramie, WY 82071, USA. steveh@uwyo.edu
Resumen
La reflexión sísmica marina revela una detallada estructura termohalina oceánica. Esta tecnología traza mapas de distintas masas de agua e intrusiones termohalinas, mejorando la comprensión oceanográfica.
Área de la Ciencia:
- Oceanografía La oceanografía es la oceanografía.
- La geofísica es la geofísica.
- La acústica es la acústica.
Sus antecedentes:
- Los frentes oceánicos, como el entre las corrientes Labrador y el Atlántico Norte, son zonas complejas de interacción de masas de agua.
- Comprender la estructura a escala fina de estos frentes es crucial para el modelado oceanográfico y los estudios climáticos.
Objetivo del estudio:
- Para demostrar la utilidad de la reflexión sísmica marina para obtener imágenes de la estructura termohalina oceánica.
- Mapear distintas masas de agua y sus características internas en los frentes oceanográficos.
Principales métodos:
- Utilizó reflejos acústicos de baja frecuencia de perfiles de reflexión sísmica marina.
- La velocidad de sonido analizada contrasta en las interfaces donde cambia la temperatura.
- Interpretado reflejos de inmersión hacia el este asociados con intrusiones termohalinas.
Principales resultados:
- Se crearon con éxito imágenes acústicas de la estructura termohalina oceánica.
- Demostró que distintas masas de agua y sus estructuras internas pueden ser mapeadas.
- Intrusiones termohalinas identificadas dentro de los 1000 metros superiores del océano en el frente estudiado.
Conclusiones:
- La reflexión sísmica marina proporciona una alta resolución espacial para los fenómenos oceánicos.
- Esta técnica es efectiva para obtener imágenes de intrusiones termohalinas, ondas internas y remolinos.
- La reflexión sísmica ofrece una herramienta valiosa para estudios oceanográficos detallados.
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