HEИндивидуална стипендия2022–2023

POSTCOLD · Understanding the influence of sediment dynamics on postglacial landscape evolution

„Хоризонт Европа“ — Действия „Мария Склодовска-Кюри“

Период: 2022-06-15 → 2023-12-14
Финансиране от ЕС: 130 386 €
Участници: 1
Схема: HORIZON-TMA-MSCA-PF-EF

Линиите свързват координатора с партньорите.

Накратко на български

Динамиката на седиментите определя дали реките в планинските райони след ледниковите периоди ще издълбаят речните си легла по-бързо или по-бавно. Това помага за по-доброто управление на екосистемите и оценка на природните рискове при промяна на климата.

Този кратък обзор е генериран от изкуствен интелект

Кратко обяснение, генерирано от езиков модел по текста на CORDIS. Оригиналът е по-долу.

Резултати накратко

Understanding the influence of sediment dynamics on postglacial landscape evolution

Repeated glacial-interglacial cycles during the last 2.6 million years have significantly impacted the topography of many mountain ranges around the world. Yet, the response of landscape evolution to repeated climate oscillations has not been well quantified. In recently deglaciated landscapes, the transition from glacial to fluvial/hillslope processes have induced progressive topographic adjustments, and the large amounts of sediments inherited from glacial periods and generated through landsliding of oversteepened glaciated topography may act as a fundamental control on the incision of postglacial rivers. These sediments can enhance fluvial incision rate by providing more tools for erosion, or inhibit incision by armoring the river bed. Characterizing when and where sediment enhances or inhibits fluvial incision in postglacial landscapes is critical for understanding the response of mountain topography to deglaciation. The main scientific objectives of POSTCOLD were 1) to develop a landscape evolution model to account for the complex impact of sediment dynamics on fluvial incision in postglacial landscapes and 2) to investigate the response of fluvial incision to changes in sediment supply and assess the effects of sediment on postglacial landscape evolution. The results of POSTCOLD provide a quantitative understanding of postglacial fluvial incision histories, which is critical for ecosystem management and natural hazard assessment in recently deglaciated mid-latitude mountain ranges and perhaps in high-latitude mountain ranges where continued climate change may eventually lead to deglaciation.

Текст от CORDIS, на английски · Данни: CORDIS, © Европейски съюз

Цел на проекта

Repeated glacial-interglacial cycles during the Quaternary have significantly impacted the topography of many mountain ranges around the world. Yet, the response of landscape evolution to repeated climate oscillations has not been well quantified. In recently deglaciated landscapes, the transition from glacial to fluvial/hillslope processes have induced progressive topographic adjustments, and the large amounts of sediments inherited from glacial periods and generated through landsliding of oversteepened glaciated topography may act as a fundamental control on the incision of postglacial rivers. These sediments can enhance fluvial incision rate by providing more tools for erosion, or inhibit incision by armoring the river bed. Characterizing when and where sediment enhances or inhibits fluvial incision in postglacial landscapes is critical for understanding the changes in postglacial landscape evolution rates over time and quantifying the response times of mountain ranges to deglaciation. In this project, I propose to develop a landscape evolution model to account for the complex impact of sediment dynamics on fluvial incision in postglacial landscapes. I will utilize this model to investigate the response of fluvial incision to changes in sediment supply and assess the effects of sediment on postglacial landscape evolution. I will apply the model to quantify response times of the deglaciated European Alp, leveraging the rich observational datasets in this region. The proposed work will provide a quantitative understanding of postglacial fluvial incision histories, which is critical for ecosystem management and natural hazard assessment in recently deglaciated mid-latitude mountain ranges and perhaps in high-latitude mountain ranges where continued climate change may eventually lead to deglaciation.

Оригинален текст от CORDIS (на английски).

Участници

GFZ HELMHOLTZ-ZENTRUM FUR GEOFORSCHUNG · POTSDAMКоординаторГермания