Sediment transport capacity response to variations in water discharge in pressurized subglacial channels
<p>Sediment transport capacity in both subaerial and subglacial channels depends on the shear stress exerted across the channel bottom, which varies with water velocity and channel width. In fully subaerial channels, water discharge variations are accommodated by flow depth and width changes a...
Saved in:
| Main Authors: | I. Delaney, A. J. Tedstone, M. A. Werder, D. Farinotti |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-08-01
|
| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/19/2779/2025/tc-19-2779-2025.pdf |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Controls on Sediment Transport From a Glacierized Catchment in the Swiss Alps Established Through Inverse Modeling of Geomorphic Processes
by: Ian Delaney, et al.
Published: (2024-04-01) -
Subglacial cavity collapses on Swiss glaciers: Spatiotemporal distribution and mass loss contribution
by: Leo Hösli, et al.
Published: (2025-01-01) -
Constraints on subglacial melt fluxes from observations of active subglacial lake recharge
by: George Malczyk, et al.
Published: (2023-12-01) -
Limited Impact of Subglacial Supercooling Freeze‐on for Greenland Ice Sheet Stratigraphy
by: Christine F. Dow, et al.
Published: (2018-02-01) -
Improved representation of laminar and turbulent sheet flow in subglacial drainage models
by: Tim Hill, et al.
Published: (2024-01-01)