Spatial variability in winter mass balance on Storglaciären modelled with a terrain-based approach

Although most processes governing the surface mass balance on mountain glaciers are well understood, the causes and extent of spatial variability in accumulation remain poorly constrained. In the present study, we couple an energy balance–snow and firn mass-balance model to terrain-based modelling r...

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Published in:Journal of Glaciology
Main Authors: Yoram Terleth, Ward J. J. van Pelt, Rickard Pettersson
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.96
https://doaj.org/article/862e53c62a3a4dff99797c129d71ffb0
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spelling ftdoajarticles:oai:doaj.org/article:862e53c62a3a4dff99797c129d71ffb0 2023-08-20T04:07:38+02:00 Spatial variability in winter mass balance on Storglaciären modelled with a terrain-based approach Yoram Terleth Ward J. J. van Pelt Rickard Pettersson 2023-08-01T00:00:00Z https://doi.org/10.1017/jog.2022.96 https://doaj.org/article/862e53c62a3a4dff99797c129d71ffb0 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S002214302200096X/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.96 0022-1430 1727-5652 https://doaj.org/article/862e53c62a3a4dff99797c129d71ffb0 Journal of Glaciology, Vol 69, Pp 749-761 (2023) Accumulation glacier mass balance glacier modelling mountain glaciers wind-blown snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.96 2023-07-30T00:36:44Z Although most processes governing the surface mass balance on mountain glaciers are well understood, the causes and extent of spatial variability in accumulation remain poorly constrained. In the present study, we couple an energy balance–snow and firn mass-balance model to terrain-based modelling routines estimating mass redistribution by snowdrift, preferential deposition and avalanching. We find this newly coupled model improves the spatial accuracy of winter balance simulations on Storglaciären, Sweden, while retaining versatility and a low computational cost. Accumulation on Storglaciären is primarily driven by direct precipitation, which is locally increased due to small-scale orographic effects. Wind-driven snow transport leads to substantial deposition in the accumulation zone and slight erosion in the ablation zone. Avalanching is the smallest contributor to winter balance, but cannot be neglected. The role of mass transporting processes in maintaining the current mass equilibrium on Storglaciären highlights the necessity to understand the links between climatic predictors and accumulation in order to accurately assess climate sensitivity. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Storglaciären ENVELOPE(18.560,18.560,67.904,67.904) Journal of Glaciology 1 13
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Accumulation
glacier mass balance
glacier modelling
mountain glaciers
wind-blown snow
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Accumulation
glacier mass balance
glacier modelling
mountain glaciers
wind-blown snow
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Yoram Terleth
Ward J. J. van Pelt
Rickard Pettersson
Spatial variability in winter mass balance on Storglaciären modelled with a terrain-based approach
topic_facet Accumulation
glacier mass balance
glacier modelling
mountain glaciers
wind-blown snow
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Although most processes governing the surface mass balance on mountain glaciers are well understood, the causes and extent of spatial variability in accumulation remain poorly constrained. In the present study, we couple an energy balance–snow and firn mass-balance model to terrain-based modelling routines estimating mass redistribution by snowdrift, preferential deposition and avalanching. We find this newly coupled model improves the spatial accuracy of winter balance simulations on Storglaciären, Sweden, while retaining versatility and a low computational cost. Accumulation on Storglaciären is primarily driven by direct precipitation, which is locally increased due to small-scale orographic effects. Wind-driven snow transport leads to substantial deposition in the accumulation zone and slight erosion in the ablation zone. Avalanching is the smallest contributor to winter balance, but cannot be neglected. The role of mass transporting processes in maintaining the current mass equilibrium on Storglaciären highlights the necessity to understand the links between climatic predictors and accumulation in order to accurately assess climate sensitivity.
format Article in Journal/Newspaper
author Yoram Terleth
Ward J. J. van Pelt
Rickard Pettersson
author_facet Yoram Terleth
Ward J. J. van Pelt
Rickard Pettersson
author_sort Yoram Terleth
title Spatial variability in winter mass balance on Storglaciären modelled with a terrain-based approach
title_short Spatial variability in winter mass balance on Storglaciären modelled with a terrain-based approach
title_full Spatial variability in winter mass balance on Storglaciären modelled with a terrain-based approach
title_fullStr Spatial variability in winter mass balance on Storglaciären modelled with a terrain-based approach
title_full_unstemmed Spatial variability in winter mass balance on Storglaciären modelled with a terrain-based approach
title_sort spatial variability in winter mass balance on storglaciären modelled with a terrain-based approach
publisher Cambridge University Press
publishDate 2023
url https://doi.org/10.1017/jog.2022.96
https://doaj.org/article/862e53c62a3a4dff99797c129d71ffb0
long_lat ENVELOPE(18.560,18.560,67.904,67.904)
geographic Storglaciären
geographic_facet Storglaciären
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 749-761 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S002214302200096X/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.96
0022-1430
1727-5652
https://doaj.org/article/862e53c62a3a4dff99797c129d71ffb0
op_doi https://doi.org/10.1017/jog.2022.96
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 13
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