Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements

Calculation of the sensible and latent heat (turbulent) fluxes is required in order to close the surface energy budget of glaciers and model glacial melt. The aerodynamic roughness length, z0, is a key parameter in the bulk approach to calculating sensible heat flux; yet, z0 is commonly considered s...

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Main Authors: Chambers, JR, Smith, MW, Quincey, DJ, Carrivick, JL, Ross, AN, James, MR
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2020
Subjects:
Online Access:https://eprints.whiterose.ac.uk/155071/
https://eprints.whiterose.ac.uk/155071/8/2019JF005167.pdf
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spelling ftleedsuniv:oai:eprints.whiterose.ac.uk:155071 2023-05-15T15:09:19+02:00 Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements Chambers, JR Smith, MW Quincey, DJ Carrivick, JL Ross, AN James, MR 2020-02 text https://eprints.whiterose.ac.uk/155071/ https://eprints.whiterose.ac.uk/155071/8/2019JF005167.pdf en eng American Geophysical Union https://eprints.whiterose.ac.uk/155071/8/2019JF005167.pdf Chambers, JR, Smith, MW orcid.org/0000-0003-4361-9527 , Quincey, DJ orcid.org/0000-0002-7602-7926 et al. (3 more authors) (2020) Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements. Journal of Geophysical Research, 125 (2). e2019JF005167. ISSN 0148-0227 Article NonPeerReviewed 2020 ftleedsuniv 2023-01-30T22:25:32Z Calculation of the sensible and latent heat (turbulent) fluxes is required in order to close the surface energy budget of glaciers and model glacial melt. The aerodynamic roughness length, z0, is a key parameter in the bulk approach to calculating sensible heat flux; yet, z0 is commonly considered simply as a tuning parameter or generalized between surfaces and over time. Spatially and temporally distributed observations of z0 over ice are rare. Both direct (from wind towers and sonic anemometers) and indirect (from microtopographic surveys) measurements of z0 are subject to sensitivities and uncertainties that are often unstated or overlooked. In this study, we present a quantitative evaluation of aerodynamic profile‐based and microtopographic methods and their effect on z0 using data collected from Storglaciären and Sydöstra Kaskasatjäkkaglaciären, Tarfala Valley, Arctic Sweden. Aggressive data filters discard most of the wind tower data, but still produce realistic z0 values of 1.9 mm and 2 mm. Despite uncertainty introduced by scale and resolution dependence, microtopographic methods produced estimates of z0 comparable to wind tower values and those found on similar surfaces. We conclude that: 1) in the absence of direct turbulent flux measurements from sonic anemometers, the profile and microtopographic methods provide realistic z0 values, 2) both 2D and 3D microtopographic methods are dependent on scale, resolution, and the chosen detrending method, and 3) careful calibration of these parameters could enable glacier‐wide investigations of z0 from remotely sensed data, including those increasingly available from satellite platforms. Article in Journal/Newspaper Arctic Tarfala White Rose Research Online (Universities of Leeds, Sheffield & York) Arctic Tarfala ENVELOPE(18.608,18.608,67.914,67.914) Storglaciären ENVELOPE(18.560,18.560,67.904,67.904)
institution Open Polar
collection White Rose Research Online (Universities of Leeds, Sheffield & York)
op_collection_id ftleedsuniv
language English
description Calculation of the sensible and latent heat (turbulent) fluxes is required in order to close the surface energy budget of glaciers and model glacial melt. The aerodynamic roughness length, z0, is a key parameter in the bulk approach to calculating sensible heat flux; yet, z0 is commonly considered simply as a tuning parameter or generalized between surfaces and over time. Spatially and temporally distributed observations of z0 over ice are rare. Both direct (from wind towers and sonic anemometers) and indirect (from microtopographic surveys) measurements of z0 are subject to sensitivities and uncertainties that are often unstated or overlooked. In this study, we present a quantitative evaluation of aerodynamic profile‐based and microtopographic methods and their effect on z0 using data collected from Storglaciären and Sydöstra Kaskasatjäkkaglaciären, Tarfala Valley, Arctic Sweden. Aggressive data filters discard most of the wind tower data, but still produce realistic z0 values of 1.9 mm and 2 mm. Despite uncertainty introduced by scale and resolution dependence, microtopographic methods produced estimates of z0 comparable to wind tower values and those found on similar surfaces. We conclude that: 1) in the absence of direct turbulent flux measurements from sonic anemometers, the profile and microtopographic methods provide realistic z0 values, 2) both 2D and 3D microtopographic methods are dependent on scale, resolution, and the chosen detrending method, and 3) careful calibration of these parameters could enable glacier‐wide investigations of z0 from remotely sensed data, including those increasingly available from satellite platforms.
format Article in Journal/Newspaper
author Chambers, JR
Smith, MW
Quincey, DJ
Carrivick, JL
Ross, AN
James, MR
spellingShingle Chambers, JR
Smith, MW
Quincey, DJ
Carrivick, JL
Ross, AN
James, MR
Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements
author_facet Chambers, JR
Smith, MW
Quincey, DJ
Carrivick, JL
Ross, AN
James, MR
author_sort Chambers, JR
title Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements
title_short Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements
title_full Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements
title_fullStr Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements
title_full_unstemmed Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements
title_sort glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements
publisher American Geophysical Union
publishDate 2020
url https://eprints.whiterose.ac.uk/155071/
https://eprints.whiterose.ac.uk/155071/8/2019JF005167.pdf
long_lat ENVELOPE(18.608,18.608,67.914,67.914)
ENVELOPE(18.560,18.560,67.904,67.904)
geographic Arctic
Tarfala
Storglaciären
geographic_facet Arctic
Tarfala
Storglaciären
genre Arctic
Tarfala
genre_facet Arctic
Tarfala
op_relation https://eprints.whiterose.ac.uk/155071/8/2019JF005167.pdf
Chambers, JR, Smith, MW orcid.org/0000-0003-4361-9527 , Quincey, DJ orcid.org/0000-0002-7602-7926 et al. (3 more authors) (2020) Glacial aerodynamic roughness estimates: uncertainty, sensitivity and precision in field measurements. Journal of Geophysical Research, 125 (2). e2019JF005167. ISSN 0148-0227
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