Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/3449
Title: Timing of glacier retreat and spatio-temporal variations in the vertical deformation rate of the Horseshoe Island, Marguarite Bay, west Antarctic Peninsula
Authors: Erturaç, Mehmet Korhan
Şahiner, Eren
Kandemir, R.
Okur, Hilal
Salman, İrem
Hasözbek, Altuğ
Öncel, M. S.
Qin, J.
Akçar, N.
Keywords: Antarctic Peninsula;Glacial evolution;Holocene
Issue Date: Apr-2025
Publisher: European Geosciences Union (EGU)
Citation: EGU General Assembly 2025, 27 Apr–2 May, Vienna, Austria & Online
Abstract: The Antarctic Peninsula is uplifting rapidly due to the isostatic response to ice sheet unloading since the Holocene. Understanding the timing and rate of this process is crucial for addressing several key research questions: (1) exploring the elastic interactions between the mantle and lithosphere to improve Glacial Isostatic Adjustment (GIA) models, (2) assessing the contribution of the Antarctic ice sheet to Holocene global sea level rise, and (3) investigating the modern response of Antarctic ice sheets to climate change, helping to identify high-impact research areas for polar science
Description: Poster presentado en: EGU General Assembly 2025, 27 Apr–2 May, Vienna, Austria & Online
URI: https://cir.cenieh.es/handle/20.500.12136/3449
DOI: 10.5194/egusphere-egu25-6751
Editor version: https://doi.org/10.5194/egusphere-egu25-6751
Type: Presentation
Other
Appears in Collections:Congresos, encuentros científicos y estancias de investigación
Geocronología y Geología



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