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Updated: Apr 24, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Published on: August 5, 2016

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Condición límite de las líneas de conexión a tierra antes del colapso, plataforma de hielo Larsen-B, Antártida

M Rebesco1, E Domack2, F Zgur1

  • 1Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42/C-34010, Sgonico (TS) Italy.

Science (New York, N.Y.)
|September 13, 2014
PubMed
Resumen

El colapso de la plataforma de hielo Larsen-B en 2002 probablemente fue impulsado por el calentamiento de la superficie, no por la inestabilidad de la zona de conexión a tierra. Esto sugiere que los procesos superficiales controlan la desintegración de la plataforma de hielo, lo que afecta a la regulación del flujo de hielo.

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