Fig 2 -

a) Typical cross section in the Labyrinth, Antarctica, derived from the LiDAR survey (black line) and the trapezoidal cross section adopted in the model (dotted red lines). The location of the cross section is indicated in red in Fig 1 b) glacier thickness profile reconstructed by Hall and Denton (2...

Full description

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 Valley
Labyrinth
Wright Upper Glacier
Antarc*
Antarctica
Online Access:https://doi.org/10.1371/journal.pone.0253768.g002
Description
Summary:a) Typical cross section in the Labyrinth, Antarctica, derived from the LiDAR survey (black line) and the trapezoidal cross section adopted in the model (dotted red lines). The location of the cross section is indicated in red in Fig 1 b) glacier thickness profile reconstructed by Hall and Denton (2005) in the eastern Wright Valley, Antarctica.

Similar Items