Bottom elevation gradient before and after each junction for channels A-B and C-D in Fig 1.

• 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.g012

The numbers refer to lateral tributaries discharging in the main trunk. Negative is defined as upstream.