Ocean temperature impact on ice shelf extent in the eastern Antarctic Peninsula
ETOURNEAU, Johan
Environnements et Paléoenvironnements OCéaniques [EPOC]
Instituto Andaluz de Ciencias de la Tierra [IACT]
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Environnements et Paléoenvironnements OCéaniques [EPOC]
Instituto Andaluz de Ciencias de la Tierra [IACT]
ETOURNEAU, Johan
Environnements et Paléoenvironnements OCéaniques [EPOC]
Instituto Andaluz de Ciencias de la Tierra [IACT]
Environnements et Paléoenvironnements OCéaniques [EPOC]
Instituto Andaluz de Ciencias de la Tierra [IACT]
WILLMOTT, Verónica
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine [AWI]
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine [AWI]
DAMSTÉ, Jaap S. Sinninghe
Universiteit Utrecht / Utrecht University [Utrecht]
Royal Netherlands Institute for Sea Research [NIOZ]
Universiteit Utrecht / Utrecht University [Utrecht]
Royal Netherlands Institute for Sea Research [NIOZ]
KIM, Jung-Hyun
Royal Netherlands Institute for Sea Research [NIOZ]
Korea Polar Research Institute [KOPRI]
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Royal Netherlands Institute for Sea Research [NIOZ]
Korea Polar Research Institute [KOPRI]
Idioma
EN
Article de revue
Este ítem está publicado en
Nature Communications. 2019, vol. 10, n° 1, p. 304
Resumen en inglés
The recent thinning and retreat of Antarctic ice shelves has been attributed to both atmosphere and ocean warming. However, the lack of continuous, multi-year direct observations as well as limitations of climate and ice ...Leer más >
The recent thinning and retreat of Antarctic ice shelves has been attributed to both atmosphere and ocean warming. However, the lack of continuous, multi-year direct observations as well as limitations of climate and ice shelf models prevent a precise assessment on how the ocean forcing affects the fluctuations of a grounded and floating ice cap. Here we show that a +0.3–1.5 °C increase in subsurface ocean temperature (50–400 m) in the northeastern Antarctic Peninsula has driven to major collapse and recession of the regional ice shelf during both the instrumental period and the last 9000 years. Our projections following the representative concentration pathway 8.5 emission scenario from the Fifth Assessment Report of the Intergovernmental Panel on Climate Change reveal a +0.3 °C subsurface ocean temperature warming within the coming decades that will undoubtedly accelerate ice shelf melting, including the southernmost sector of the eastern Antarctic Peninsula.< Leer menos
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