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.
| Main Authors: | , , , |
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| Format: | Still Image |
| Language: | unknown |
| Published: |
2021
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| Subjects: | |
| Online Access: | https://doi.org/10.1371/journal.pone.0253768.g004 |
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ftsmithonian:oai:figshare.com:article/16597316 |
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| record_format |
openpolar |
| spelling |
ftsmithonian:oai:figshare.com:article/16597316 2023-05-15T17:10:34+02:00 Fig 4 - 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.g004 unknown https://figshare.com/articles/figure/Fig_4_-/16597316 doi:10.1371/journal.pone.0253768.g004 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.g004 2021-12-20T02:32:39Z 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. 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) Fig 4 - |
| 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 |
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. |
| 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 |
Fig 4 - |
| title_short |
Fig 4 - |
| title_full |
Fig 4 - |
| title_fullStr |
Fig 4 - |
| title_full_unstemmed |
Fig 4 - |
| title_sort |
fig 4 - |
| publishDate |
2021 |
| url |
https://doi.org/10.1371/journal.pone.0253768.g004 |
| 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/Fig_4_-/16597316 doi:10.1371/journal.pone.0253768.g004 |
| op_rights |
CC BY 4.0 |
| op_rightsnorm |
CC-BY |
| op_doi |
https://doi.org/10.1371/journal.pone.0253768.g004 |
| _version_ |
1766067213856407552 |