Fig 4 -

A) Water pressure, B) channel depth, and C) velocity along a subglacial channel for a discharge ranging from 2000 to 40000 m 3 /s. Distances are measured increasing upstream of the glacier’s snout. Different color lines represent different discharges.

Bibliographic Details
Main Authors: Sergio Fagherazzi (6658952), Luca Baticci (11414144), Christine M. Brandon (11414147), Maria Cristina Rulli (6574757)
Format: Still Image
Language:unknown
Published: 2021
Subjects:
Biochemistry
Neuroscience
Ecology
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
numerical model based
mcmurdo dry valleys
wright upper glacier
saltating bed load
model results show
pressurized flow reaches
sediment particles cannot
sediment grain sizes
sediment load
recent results
subglacial flow
flow accelerates
sediment loads
xlink ">
wide range
transport rate
transport capacity
therefore conclude
subglacial channels
section constrictions
reducing abrasion
potential cross
possible signature
monotonic relationship
intermediate distance
glacier snout
glacial scour
geomorphic features
develop herein
complex interplay
classical theory
channel confluences
channel bottom
bottom profiles
McMurdo Dry Valleys
Wright Upper Glacier
Online Access:https://doi.org/10.1371/journal.pone.0253768.g004
Description
Summary:A) Water pressure, B) channel depth, and C) velocity along a subglacial channel for a discharge ranging from 2000 to 40000 m 3 /s. Distances are measured increasing upstream of the glacier’s snout. Different color lines represent different discharges.

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