Depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in Fig 1 (channel A-B and channel C-D).

The numbers refer to lateral tributaries discharging in the main trunk (see Fig 1 ). The red lines are a second order polynomial interpolation of the bottom elevation (parabola).

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.g010
id ftsmithonian:oai:figshare.com:article/16597349
record_format openpolar
spelling ftsmithonian:oai:figshare.com:article/16597349 2023-05-15T17:10:34+02:00 Depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in Fig 1 (channel A-B and channel C-D). Sergio Fagherazzi (6658952) Luca Baticci (11414144) Christine M. Brandon (11414147) Maria Cristina Rulli (6574757) 2021-09-09T17:30:39Z https://doi.org/10.1371/journal.pone.0253768.g010 unknown https://figshare.com/articles/figure/Depth_bottom_elevation_and_bottom_gradient_of_the_two_subglacial_channels_indicated_in_Fig_1_channel_A-B_and_channel_C-D_/16597349 doi:10.1371/journal.pone.0253768.g010 CC BY 4.0 CC-BY 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 Image Figure 2021 ftsmithonian https://doi.org/10.1371/journal.pone.0253768.g010 2021-12-20T02:32:38Z The numbers refer to lateral tributaries discharging in the main trunk (see Fig 1 ). The red lines are a second order polynomial interpolation of the bottom elevation (parabola). Still Image McMurdo Dry Valleys Unknown McMurdo Dry Valleys Wright Upper Glacier ENVELOPE(160.583,160.583,-77.533,-77.533)
institution Open Polar
collection Unknown
op_collection_id ftsmithonian
language unknown
topic 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
spellingShingle 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
Sergio Fagherazzi (6658952)
Luca Baticci (11414144)
Christine M. Brandon (11414147)
Maria Cristina Rulli (6574757)
Depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in Fig 1 (channel A-B and channel C-D).
topic_facet 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
description The numbers refer to lateral tributaries discharging in the main trunk (see Fig 1 ). The red lines are a second order polynomial interpolation of the bottom elevation (parabola).
format Still Image
author Sergio Fagherazzi (6658952)
Luca Baticci (11414144)
Christine M. Brandon (11414147)
Maria Cristina Rulli (6574757)
author_facet Sergio Fagherazzi (6658952)
Luca Baticci (11414144)
Christine M. Brandon (11414147)
Maria Cristina Rulli (6574757)
author_sort Sergio Fagherazzi (6658952)
title Depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in Fig 1 (channel A-B and channel C-D).
title_short Depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in Fig 1 (channel A-B and channel C-D).
title_full Depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in Fig 1 (channel A-B and channel C-D).
title_fullStr Depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in Fig 1 (channel A-B and channel C-D).
title_full_unstemmed Depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in Fig 1 (channel A-B and channel C-D).
title_sort depth, bottom elevation, and bottom gradient of the two subglacial channels indicated in fig 1 (channel a-b and channel c-d).
publishDate 2021
url https://doi.org/10.1371/journal.pone.0253768.g010
long_lat ENVELOPE(160.583,160.583,-77.533,-77.533)
geographic McMurdo Dry Valleys
Wright Upper Glacier
geographic_facet McMurdo Dry Valleys
Wright Upper Glacier
genre McMurdo Dry Valleys
genre_facet McMurdo Dry Valleys
op_relation https://figshare.com/articles/figure/Depth_bottom_elevation_and_bottom_gradient_of_the_two_subglacial_channels_indicated_in_Fig_1_channel_A-B_and_channel_C-D_/16597349
doi:10.1371/journal.pone.0253768.g010
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1371/journal.pone.0253768.g010
_version_ 1766067214024179712

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