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| Título: | Timing of glacier retreat and spatio-temporal variations in the vertical deformation rate of the Horseshoe Island, Marguarite Bay, west Antarctic Peninsula |
| Autor: | Erturaç, Mehmet Korhan Şahiner, Eren Kandemir, R. Okur, Hilal Salman, İrem Hasözbek, Altuğ Öncel, M. S. Qin, J. Akçar, N. |
| Palabras clave: | Antarctic Peninsula;Glacial evolution;Holocene |
| Fecha de publicación: | abr-2025 |
| Editorial: | European Geosciences Union (EGU) |
| Citación: | EGU General Assembly 2025, 27 Apr–2 May, Vienna, Austria & Online |
| Resumen: | 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 |
| Descripción: | 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 |
| Versión del Editor: | https://doi.org/10.5194/egusphere-egu25-6751 |
| Tipo: | Presentation Other |
| Aparece en las colecciones: | Congresos, encuentros científicos y estancias de investigación Geocronología y Geología |
Ficheros en este ítem:
| Fichero | Descripción | Tamaño | Formato | |
|---|---|---|---|---|
| Timing of glacier retreat and spatio-temporal variations in the vertical deformation rate of the Horseshoe Island, Marguarite Bay, west Antarctic Peninsula_Erturaç, M. K._et al_2025.pdf | 1.05 MB | Adobe PDF |  Visualizar/Abrir |
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