Fig 8 -

Evolution of a subglacial channel in time: A) erosion rate; B) bottom elevation. At the beginning of the simulations the channel has constant width (100m) and constant bottom elevation. Q = 20000 m 3 /s D s = 10cm q s = 40 kg/m/s.

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.g008

Description
Summary:	Evolution of a subglacial channel in time: A) erosion rate; B) bottom elevation. At the beginning of the simulations the channel has constant width (100m) and constant bottom elevation. Q = 20000 m 3 /s D s = 10cm q s = 40 kg/m/s.