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Updated: Jul 1, 2025

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
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¿El derretimiento del Ártico está provocando olas de calor en Europa?
Resumen
El aumento del agua de deshielo está creando una "mancha fría" en el Atlántico Norte, alterando significativamente los patrones climáticos globales. Este fenómeno afecta a la circulación atmosférica y a las precipitaciones, con posibles consecuencias de largo alcance.
Área de la Ciencia:
- La oceanografía
- La climatología
- Meteorología
Sus antecedentes:
- La Corriente del Atlántico Norte, un componente crucial de la Circulación Meridional del Atlántico (AMOC), se está debilitando.
- El aumento de la afluencia de agua de deshielo de los glaciares y las capas de hielo, especialmente en Groenlandia, está contribuyendo al refrescamiento y enfriamiento de la superficie.
- Este efecto de enfriamiento está formando una región distinta de aguas superficiales más frías, denominada "mancha fría".
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