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Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean

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Figure

Figure 1. Study area. The coastal subset defined as the lidar scan is represented in red
Figure 2. Geomorphological map of retrogressive thaw slumps (RTSs) illustrating the complexity of RTS evolution along the Yukon Coast.(d) RTSs identified in 1952 (a) and in 1972 (b) overlap the 2011 RTSs (c)
Figure 3.! Map illustrating the different datasets used to model pre-slump topographies
Figure 4. Cross section of a retrogressive thaw slump (RTS) (a) illustrating the calculated volumes of sediments eroded through slumpingbetween 1972 and 2011
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