a sed transport process unique to marine-terminating glaciers are meltwater plumes that are discharged at the grounding line — they buoyantly rise to create a sea-surface plume and sediment rains out I need to educate myself more about this — what are some 'go to' papers about this process? ⚒️🧊🌊

for example, are there any studies from modern settings with direct observations/measurements of these buoyant plumes with sediment in suspension? how vigorous can the discharge at the grounding line be?