Fig 7 -
A) Maximum erosion rate along the channel as a function of sediment supply per unit width and water discharge. D s = 10 cm. B) Maximum erosion rate along the channel as a function of sediment grain size and water discharge. q s = 40 kg/m/s.
| 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.g007 |
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ftsmithonian:oai:figshare.com:article/16597331 |
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| record_format |
openpolar |
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ftsmithonian:oai:figshare.com:article/16597331 2023-05-15T17:10:34+02:00 Fig 7 - 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.g007 unknown https://figshare.com/articles/figure/Fig_7_-/16597331 doi:10.1371/journal.pone.0253768.g007 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.g007 2021-12-20T02:32:39Z A) Maximum erosion rate along the channel as a function of sediment supply per unit width and water discharge. D s = 10 cm. B) Maximum erosion rate along the channel as a function of sediment grain size and water discharge. q s = 40 kg/m/s. 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 7 - |
| 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) Maximum erosion rate along the channel as a function of sediment supply per unit width and water discharge. D s = 10 cm. B) Maximum erosion rate along the channel as a function of sediment grain size and water discharge. q s = 40 kg/m/s. |
| 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 7 - |
| title_short |
Fig 7 - |
| title_full |
Fig 7 - |
| title_fullStr |
Fig 7 - |
| title_full_unstemmed |
Fig 7 - |
| title_sort |
fig 7 - |
| publishDate |
2021 |
| url |
https://doi.org/10.1371/journal.pone.0253768.g007 |
| 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_7_-/16597331 doi:10.1371/journal.pone.0253768.g007 |
| op_rights |
CC BY 4.0 |
| op_rightsnorm |
CC-BY |
| op_doi |
https://doi.org/10.1371/journal.pone.0253768.g007 |
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1766067214194049024 |