Preprints
https://doi.org/10.5194/egusphere-2024-274
https://doi.org/10.5194/egusphere-2024-274
06 Mar 2024
 | 06 Mar 2024
Status: this preprint is open for discussion.

Modelling subglacial fluvial sediment transport with a graph-based model, GraphSSeT

Alan Robert Alexander Aitken, Ian Arburua Delaney, Guillaume Pirot, and Mauro Werder

Abstract. A quantitative understanding of how sediment discharge from subglacial fluvial systems varies in response to glacio-hydrological conditions is essential for understanding marine systems around Greenland and Antarctica and for interpreting sedimentary records of cryosphere evolution. Here we develop a graph based approach, GraphSSeT, to model subglacial fluvial sedimentary transport using subglacial hydrology model outputs as forcing. GraphSSeT includes glacial erosion of bedrock and a dynamic sediment model with exchange between the active transport system and a basal sediment layer. Sediment transport considers transport-limited and supply-limited regimes and includes stochastically-evolving grain size, network scale flow management and tracking of detrital provenance. GraphSSeT satisfies volume balance and sediment velocity and transport capacity constraints on flow. GraphSSeT is demonstrated for synthetic scenarios that probe the impact of variations in hydrological, geological and glaciological characteristics on sediment transport over multi-diurnal to seasonal timeframes. For steady-state hydrology scenarios on seasonal timescales we find a primary control from the scale and organisation of the channelised hydrological flow network. The development of grain size dependant selective transport is identified as the major secondary control. Non-steady-state hydrology is tested on multi-diurnal timescales, for which sediment discharge scales with peak water input leading to increased sediment discharge compared to steady state. With increasing application of subglacial hydrology models, GraphSSeT extends this capacity to define quantitatively the volume, grain size distribution and detrital characteristics of sediment discharge, and enables a stronger connection of models of the glacio-hydrological system with constraints from the sediment record and impacts on marine systems.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Alan Robert Alexander Aitken, Ian Arburua Delaney, Guillaume Pirot, and Mauro Werder

Status: open (until 30 May 2024)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-274', Anonymous Referee #1, 10 Apr 2024 reply
  • RC2: 'Comment on egusphere-2024-274', Anonymous Referee #2, 15 May 2024 reply
Alan Robert Alexander Aitken, Ian Arburua Delaney, Guillaume Pirot, and Mauro Werder
Alan Robert Alexander Aitken, Ian Arburua Delaney, Guillaume Pirot, and Mauro Werder

Viewed

Total article views: 333 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
241 69 23 333 31 18 10
  • HTML: 241
  • PDF: 69
  • XML: 23
  • Total: 333
  • Supplement: 31
  • BibTeX: 18
  • EndNote: 10
Views and downloads (calculated since 06 Mar 2024)
Cumulative views and downloads (calculated since 06 Mar 2024)

Viewed (geographical distribution)

Total article views: 346 (including HTML, PDF, and XML) Thereof 346 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 28 May 2024
Download
Short summary
Understanding how glaciers generate and transport sediment to the ocean is important for understanding ocean ecosystems and for developing knowledge of past cryosphere from marine sediments. This manuscript presents a new way to simulate sediment transport in rivers below ice sheets and glaciers and quantify volumes and characteristics of sediment that can be used to reveal the hidden record of the subglacial environment for both past and present glacial conditions.