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

Description
Summary:	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).