Micheletti, N. and Lambiel, C. and Lane, S.N. (2015)
Investigating decadal scale geomorphic dynamics in an Alpine mountain setting
- Cite key
- Journal of Geophysical Research - Earth Surface
- We know little about the effect of recent climate variability upon landscapes at the time scale of decades because of (1) the complex, non-linear and path-dependent nature of the response of a landscape to climate forcing, and (2) the difficulty of quantifying spatially-distributed impacts at the timescale of decades to centuries, despite this being the timescale over which significant hypotheses have been raised over human impacts upon climate change and hence geomorphic systems. A unique resource to investigate the linkages between climatic variability and geomorphic response is provided by the extensive coverage of aerial imagery commonly available since the 1950s. Here, we use archival digital photogrammetry to produce high precision digital elevation models (DEMs) over large spatial scales, and so to reconstruct the quantitative history of surface downwasting and sediment flux in a high mountain Alpine system, over the timescales of decades. Propagation of error methods are used to identify locations of significant landscape response and to compute volumes of significant surface change. Orthorectified aerial images are used in an image correlation framework to detect horizontal and vertical displacements of components of the landscape. Results are coupled to extant climate data and modelled snow cover to show how the landscape responds to climate forcing and to geomorphological maps to understand how this response varies between landscape elements. The results show distinct landscape response to both warming and cooling periods and a tendency for the acceleration of surface displacement under warming conditions. Precipitation and snow cover are critical in controlling glacier dynamics and rock glacier displacement velocities. However, whilst some landforms might lead to locally high sediment flux, landscape heritage can disconnect zones of high change rates from the valley bottom. Hence, the landscape response to climate forcing is not necessarily reflected in valley system processes or sediment deposits.
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