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La estacionalidad de la acumulación de la Antártida.

Louise C Sime1, Eric W Wolff

  • 1British Antarctic Survey, Cambridge CB3 0ET, UK. lsim@bas.ac.uk

Nature
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PubMed
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Las señales de isótopos del núcleo de hielo antártico pueden no reflejar los impulsores climáticos del hemisferio norte. Los cambios estacionales en la acumulación de nieve en la Antártida, no solo la insolación, probablemente influyen en estas señales, desafiando las interpretaciones anteriores de la dinámica climática a escala orbital.

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  • Glaciología glaciología.
  • Sus antecedentes:

    • Los cambios climáticos a escala orbital a menudo se estudian utilizando registros de isótopos de núcleos de hielo antárticos.
    • Un estudio anterior sugirió que la insolación del hemisferio norte impulsa estas señales antárticas.
    • Esta interpretación se basó en la ponderación de la insolación antártica con una estimación de acumulación estacional estática.