Abstract
The lower boundary of the alpine permafrost extent is thought to be especially sensitive to climate warming. Studies at a regional scale interpreted the occurrence of conspicuous debris flow activity at this margin as an indicator of a causal relationship. Yet, these studies do not adequately consider the baseline debris flow activity in alpine periglacial areas, i.e. high-altitude areas subjected to seasonal or perennial frost. Activity is likely to be innately high in these areas due to the combination of steep slopes, high regolith production rates owing to intense frost weathering, and the presence of permafrost. However, the role of periglacial influences on debris flow activity in high-alpine areas has so far not been systematically investigated. This study analyses debris flow activity in the alpine areas of the Southern Alps, New Zealand, during the last six decades. It focuses on determining debris flow preconditioning factors, i.e. the environmental conditions within source areas that facilitate debris flow development. By analysing a wide range of potential factors, including topography, lithology, and geomorphic legacy (e.g. the presence of Quaternary deposits), this study aims to determine whether debris flow systems subjected to periglacial influences, i.e. intense frost weathering and the presence of permafrost, are more active than systems outside the periglacial realm. This chapter introduces the background and rationale of this study, defines the study’s aims and objectives, and describes the thesis structure.
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Sattler, K. (2016). Introduction. In: Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand. Springer Theses. Springer, Cham. https://doi.org/10.1007/978-3-319-35074-5_1
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DOI: https://doi.org/10.1007/978-3-319-35074-5_1
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