Measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface

Parameterization of turbulent heat fluxes with bulk aerodynamic methods has been shown to perform relatively poorly in the presence of shallow katabatic winds. Identifying when and how the bulk methods under-perform is essential to reduce uncertainty in surface energy balance modelling of glacier me...

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Main Authors: Radic, V., Lord-May, C.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020520
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5020520 2023-07-23T04:19:24+02:00 Measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface Radic, V. Lord-May, C. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020520 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3135 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020520 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-3135 2023-07-02T23:40:09Z Parameterization of turbulent heat fluxes with bulk aerodynamic methods has been shown to perform relatively poorly in the presence of shallow katabatic winds. Identifying when and how the bulk methods under-perform is essential to reduce uncertainty in surface energy balance modelling of glacier melt. Here, we evaluate the most commonly used bulk method in simulating 30-min sensible heat fluxes over two summer months at the Kaskawulsh glacier in the Yukon, Canada. As our reference data, we use eddy-covariance (EC) measurements from one on-glacier site at three different heights (1 m, 2 m, and 3 m). To adequately process the EC-data, we propose two new methods: a statistical method that ensures the fluxes are derived from time windows with (near-)stationary turbulence, and a filtering method that ensures the fluxes are representative of surface conditions, in particular during shallow katabatic winds. We find that the agreement between EC-derived fluxes and those modelled with the bulk method substantially improves with the implementation of the two data-processing methods. The least data-processing is required for the measurements at 1 m above the surface, the height that also yields the best performance of the bulk method. Contrary to the previous findings, the bulk method does perform well during shallow katabatic flows if the measurements of temperature and wind speed are taken close to the surface (<= 1 m) and well below the wind speed maxima. We conclude that adequate data processing and filtering are critical in obtaining accurate sensible heat fluxes at glacier surfaces. Conference Object glacier* Yukon GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Canada Kaskawulsh Glacier ENVELOPE(-139.104,-139.104,60.749,60.749) Yukon
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Parameterization of turbulent heat fluxes with bulk aerodynamic methods has been shown to perform relatively poorly in the presence of shallow katabatic winds. Identifying when and how the bulk methods under-perform is essential to reduce uncertainty in surface energy balance modelling of glacier melt. Here, we evaluate the most commonly used bulk method in simulating 30-min sensible heat fluxes over two summer months at the Kaskawulsh glacier in the Yukon, Canada. As our reference data, we use eddy-covariance (EC) measurements from one on-glacier site at three different heights (1 m, 2 m, and 3 m). To adequately process the EC-data, we propose two new methods: a statistical method that ensures the fluxes are derived from time windows with (near-)stationary turbulence, and a filtering method that ensures the fluxes are representative of surface conditions, in particular during shallow katabatic winds. We find that the agreement between EC-derived fluxes and those modelled with the bulk method substantially improves with the implementation of the two data-processing methods. The least data-processing is required for the measurements at 1 m above the surface, the height that also yields the best performance of the bulk method. Contrary to the previous findings, the bulk method does perform well during shallow katabatic flows if the measurements of temperature and wind speed are taken close to the surface (<= 1 m) and well below the wind speed maxima. We conclude that adequate data processing and filtering are critical in obtaining accurate sensible heat fluxes at glacier surfaces.
format Conference Object
author Radic, V.
Lord-May, C.
spellingShingle Radic, V.
Lord-May, C.
Measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface
author_facet Radic, V.
Lord-May, C.
author_sort Radic, V.
title Measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface
title_short Measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface
title_full Measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface
title_fullStr Measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface
title_full_unstemmed Measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface
title_sort measurements and modelling of turbulent fluxes under different flow regimes at a glacier surface
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020520
long_lat ENVELOPE(-139.104,-139.104,60.749,60.749)
geographic Canada
Kaskawulsh Glacier
Yukon
geographic_facet Canada
Kaskawulsh Glacier
Yukon
genre glacier*
Yukon
genre_facet glacier*
Yukon
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3135
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020520
op_doi https://doi.org/10.57757/IUGG23-3135
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