Graph analysis for subglacial hydrology and sediment flux to the ocean

A better knowledge of sediment flux to the ocean has many implications for understanding past and future cryosphere evolution including understanding potential impacts on ice shelf stability and ocean circulation, understanding the record of past cryosphere events from sediment records and understan...

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Main Author: Aitken, A.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018094
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018094 2023-06-18T03:38:13+02:00 Graph analysis for subglacial hydrology and sediment flux to the ocean Aitken, A. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018094 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1515 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018094 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1515 2023-06-04T23:39:42Z A better knowledge of sediment flux to the ocean has many implications for understanding past and future cryosphere evolution including understanding potential impacts on ice shelf stability and ocean circulation, understanding the record of past cryosphere events from sediment records and understanding impacts on nutrient supply and CO 2 drawdown. Physical model studies of subglacial sediment transport are relatively few, and due to computational expense, these often do not explore the broader model space for the glacial scenario of interest. The lack of a comprehensive quantitative knowledge of the subglacial sediment transport system limits our ability to understand sedimentary records of ice sheet change, and to express the potential impacts of future cryosphere change on the ocean. I present here a graph analysis approach to enable broad exploration of model space to understand hydrological change and for quantitative estimates of water and sediment fluxes through the system and to the ocean. The analysis is based on the outputs of physical models, including an ice sheet model output and a subglacial hydrology model output. The analysis defines catchment-scale graphs of the subglacial hydrology network, from which subgraphs are defined optimised to the problem at hand. Such representations greatly reduce the model size and allow efficient development of an ensemble result. These subgraphs may be defined from prior information, or ad-hoc during run-time based on stochastic, probabilistic or adaptive algorithms. I demonstrate the approach for a synthetic example and show examples from catchment-scale model studies in Greenland and Antarctica. Conference Object Antarc* Antarctica Greenland Ice Sheet Ice Shelf GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Greenland
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description A better knowledge of sediment flux to the ocean has many implications for understanding past and future cryosphere evolution including understanding potential impacts on ice shelf stability and ocean circulation, understanding the record of past cryosphere events from sediment records and understanding impacts on nutrient supply and CO 2 drawdown. Physical model studies of subglacial sediment transport are relatively few, and due to computational expense, these often do not explore the broader model space for the glacial scenario of interest. The lack of a comprehensive quantitative knowledge of the subglacial sediment transport system limits our ability to understand sedimentary records of ice sheet change, and to express the potential impacts of future cryosphere change on the ocean. I present here a graph analysis approach to enable broad exploration of model space to understand hydrological change and for quantitative estimates of water and sediment fluxes through the system and to the ocean. The analysis is based on the outputs of physical models, including an ice sheet model output and a subglacial hydrology model output. The analysis defines catchment-scale graphs of the subglacial hydrology network, from which subgraphs are defined optimised to the problem at hand. Such representations greatly reduce the model size and allow efficient development of an ensemble result. These subgraphs may be defined from prior information, or ad-hoc during run-time based on stochastic, probabilistic or adaptive algorithms. I demonstrate the approach for a synthetic example and show examples from catchment-scale model studies in Greenland and Antarctica.
format Conference Object
author Aitken, A.
spellingShingle Aitken, A.
Graph analysis for subglacial hydrology and sediment flux to the ocean
author_facet Aitken, A.
author_sort Aitken, A.
title Graph analysis for subglacial hydrology and sediment flux to the ocean
title_short Graph analysis for subglacial hydrology and sediment flux to the ocean
title_full Graph analysis for subglacial hydrology and sediment flux to the ocean
title_fullStr Graph analysis for subglacial hydrology and sediment flux to the ocean
title_full_unstemmed Graph analysis for subglacial hydrology and sediment flux to the ocean
title_sort graph analysis for subglacial hydrology and sediment flux to the ocean
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018094
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
Ice Sheet
Ice Shelf
genre_facet Antarc*
Antarctica
Greenland
Ice Sheet
Ice Shelf
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1515
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018094
op_doi https://doi.org/10.57757/IUGG23-1515
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