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Sergio Fagherazzi
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Climatic oscillations influence the flooding of Venice
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Bedrock erosion in subglacial channels.
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Constants.
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Bottom elevation gradient before and after each junction for channels A-B and C-...
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Change in channel width and depth after a junction for channels A-B and C-D in F...
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Fig 8 -
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Depth, bottom elevation, and bottom gradient of the two subglacial channels indi...
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Illustration of a subglacial bedrock channel.
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Distribution of erosion rates in a subglacial channel before and after a conflue...
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Left: Satellite image of the Dry Valleys region derived from the Landsat Image M...
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Related Subjects
Biochemistry
Biological Sciences not elsewhere classified
Ecology
Environmental Sciences not elsewhere classified
Neuroscience
bottom profiles
channel bottom
channel confluences
classical theory
complex interplay
develop herein
flow accelerates
geomorphic features
glacial scour
glacier snout
intermediate distance
mcmurdo dry valleys
model results show
monotonic relationship
numerical model based
possible signature
potential cross
pressurized flow reaches
recent results
reducing abrasion
saltating bed load
section constrictions
sediment grain sizes
sediment load
sediment loads
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