Errors in Short-Term Ablation Measurements on Melting Ice Surfaces

Rapid changes in time and space in the micro-relief of an ablating glacier surface and radiation-induced melt within the uppermost ice layer, termed the “weathering crust”, seriously affect the accuracy of the short-term ablation measurements. The various measuring techniques commonly used (stakes,...

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Published in:Journal of Glaciology
Main Authors: Müller, Fritz, Keeler, Charles M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1969
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000020785
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020785
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spelling crcambridgeupr:10.1017/s0022143000020785 2024-09-15T18:15:38+00:00 Errors in Short-Term Ablation Measurements on Melting Ice Surfaces Müller, Fritz Keeler, Charles M. 1969 http://dx.doi.org/10.1017/s0022143000020785 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020785 en eng Cambridge University Press (CUP) Journal of Glaciology volume 8, issue 52, page 91-105 ISSN 0022-1430 1727-5652 journal-article 1969 crcambridgeupr https://doi.org/10.1017/s0022143000020785 2024-07-24T04:01:31Z Rapid changes in time and space in the micro-relief of an ablating glacier surface and radiation-induced melt within the uppermost ice layer, termed the “weathering crust”, seriously affect the accuracy of the short-term ablation measurements. The various measuring techniques commonly used (stakes, ablatometers, ablatographs) and some new methods (measurement of discharge from a small supra-glacial drainage basin, and mass loss directly measured on core samples) are critically reviewed and assessed in the light of these phenomena. The implications for studies of heat and mass balance are discussed. It appears that the direct measurement of mass flux is the most accurate means of assessing short-terni ablation rates. The errors in short-term ablation measurements by any method are largely compensatory and consequently do not influence long-period mass-balance estimates. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 8 52 91 105
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Rapid changes in time and space in the micro-relief of an ablating glacier surface and radiation-induced melt within the uppermost ice layer, termed the “weathering crust”, seriously affect the accuracy of the short-term ablation measurements. The various measuring techniques commonly used (stakes, ablatometers, ablatographs) and some new methods (measurement of discharge from a small supra-glacial drainage basin, and mass loss directly measured on core samples) are critically reviewed and assessed in the light of these phenomena. The implications for studies of heat and mass balance are discussed. It appears that the direct measurement of mass flux is the most accurate means of assessing short-terni ablation rates. The errors in short-term ablation measurements by any method are largely compensatory and consequently do not influence long-period mass-balance estimates.
format Article in Journal/Newspaper
author Müller, Fritz
Keeler, Charles M.
spellingShingle Müller, Fritz
Keeler, Charles M.
Errors in Short-Term Ablation Measurements on Melting Ice Surfaces
author_facet Müller, Fritz
Keeler, Charles M.
author_sort Müller, Fritz
title Errors in Short-Term Ablation Measurements on Melting Ice Surfaces
title_short Errors in Short-Term Ablation Measurements on Melting Ice Surfaces
title_full Errors in Short-Term Ablation Measurements on Melting Ice Surfaces
title_fullStr Errors in Short-Term Ablation Measurements on Melting Ice Surfaces
title_full_unstemmed Errors in Short-Term Ablation Measurements on Melting Ice Surfaces
title_sort errors in short-term ablation measurements on melting ice surfaces
publisher Cambridge University Press (CUP)
publishDate 1969
url http://dx.doi.org/10.1017/s0022143000020785
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020785
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 8, issue 52, page 91-105
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000020785
container_title Journal of Glaciology
container_volume 8
container_issue 52
container_start_page 91
op_container_end_page 105
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