GERALDINE (Google Earth Engine supRaglAciaL Debris INput dEtector): a new tool for identifying and monitoring supraglacial landslide inputs
Autor: | Stephen Brough, Stuart Dunning, Neil Ross, Jon Telling, William D. Smith |
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Jazyk: | angličtina |
Rok vydání: | 2020 |
Předmět: |
geography
geography.geographical_feature_category 010504 meteorology & atmospheric sciences lcsh:Dynamic and structural geology Glacier Landslide 010502 geochemistry & geophysics Snow Permafrost 01 natural sciences Debris Geophysics Paraglacial lcsh:QE500-639.5 Thematic Mapper Satellite imagery Physical geography Geology 0105 earth and related environmental sciences Earth-Surface Processes |
Zdroj: | Earth Surface Dynamics, Vol 8, Pp 1053-1065 (2020) EARTH SURFACE DYNAMICS |
ISSN: | 2196-6311 2196-632X |
Popis: | Landslides in glacial environments are high-magnitude, long-runout events, believed to be increasing in frequency as a paraglacial response to ice retreat and thinning and, arguably, due to warming temperatures and degrading permafrost above current glaciers. However, our ability to test these assumptions by quantifying the temporal sequencing of debris inputs over large spatial and temporal extents is limited in areas with glacier ice. Discrete landslide debris inputs, particularly in accumulation areas, are rapidly “lost”, being reworked by motion and icefalls and/or covered by snowfall. Although large landslides can be detected and located using their seismic signature, smaller (M≤5.0) landslides frequently go undetected because their seismic signature is less than the noise floor, particularly supraglacially deposited landslides, which feature a “quiet” runout over snow. Here, we present GERALDINE (Google Earth Engine supRaglAciaL Debris INput dEtector): a new free-to-use tool leveraging Landsat 4–8 satellite imagery and Google Earth Engine. GERALDINE outputs maps of new supraglacial debris additions within user-defined areas and time ranges, providing a user with a reference map, from which large debris inputs such as supraglacial landslides (>0.05 km2) can be rapidly identified. We validate the effectiveness of GERALDINE outputs using published supraglacial rock avalanche inventories, and then demonstrate its potential by identifying two previously unknown, large (>2 km2) landslide-derived supraglacial debris inputs onto glaciers in the Hayes Range, Alaska, one of which was not detected seismically. GERALDINE is a first step towards a complete global magnitude–frequency of landslide inputs onto glaciers over the 38 years of Landsat Thematic Mapper imagery. |
Databáze: | OpenAIRE |
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