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Updated: Jan 20, 2026

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
Restricciones en el nivel medio global del mar durante el calor del Plioceno
Oana A Dumitru1, Jacqueline Austermann2, Victor J Polyak3
1Karst Research Group, School of Geosciences, University of South Florida, Tampa, FL, USA.
Las épocas más cálidas pasadas revelan un aumento significativo del nivel del mar. Este estudio cuantifica los cambios globales del nivel medio del mar (GMSL) del Plioceno, mostrando que las capas de hielo son sensibles al calentamiento.
Área de la Ciencia:
- Paleoclimatología
- Ciencia del nivel del mar
- Dinámica de las capas de hielo
Sus antecedentes:
- La reconstrucción del nivel del mar es crucial para comprender las respuestas de las capas de hielo al calentamiento prolongado.
- Las estimaciones existentes del nivel medio global del mar del Plioceno (GMSL) tienen una incertidumbre considerable, lo que limita las evaluaciones de la estabilidad de las capas de hielo.
- La época del Plioceno, particularmente los períodos más cálidos como el Período Cálido Piacenciano medio y el Óptimo Climático del Plioceno, sirven como un análogo valioso para los escenarios climáticos futuros.
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