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Holoceno Variabilidad de la temperatura de la superficie del Océano Sur al oeste de la Península Antártica
A E Shevenell1, A E Ingalls, E W Domack
1School of Oceanography, University of Washington, Seattle, Washington 98195, USA. a.shevenell@ucl.ac.uk
Nature
|February 11, 2011
Resumen
Las temperaturas oceánicas de la Península Antártica se enfriaron durante más de 12.000 años, vinculadas a la insolación y los vientos occidentales del Océano Antártico. Esto impacta el ciclo global del carbono y la extensión del hielo marino.
Área de la Ciencia:
- Paleoclimatología Paleoclimatología
- Oceanografía La oceanografía es la oceanografía.
- Ciencias del clima Ciencias del clima Ciencias del clima
Sus antecedentes:
- La criosfera antártica es sensible al calentamiento atmosférico y oceánico.
- La variabilidad climática del Holoceno en la Península Antártica es poco conocida.
- Comprender el clima pasado es crucial para evaluar los cambios actuales.
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