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Stable Sediment Plumes Despite Tidewater Glacier Retreat in a South Greenland Fjord
1 Introduction The rapid retreat of Greenland tidewater glaciers since the 1980s, occurring at rates of tens to hundreds of meters per year (Ryan et al., 2024), has driven a six-fold increase in Greenland Ice Sheet mass loss (Greene et al., 2024; Moon et al., 2020; Mouginot et al., 2019).
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