Direct measurement of optical properties of glacier ice using a photon-counting diffuse LiDAR

Abstract The production of meltwater from glacier ice, which is exposed at the margins of land ice during the summer, is responsible for a large proportion of glacier mass loss. The rate of meltwater production from glacier ice is especially sensitive to its physical structure and chemical compositi...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Allgaier, Markus, Cooper, Matthew G., Carlson, Anders E., Cooley, Sarah W., Ryan, Jonathan C., Smith, Brian J.
Other Authors: University of Oregon
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2022
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2022.34
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302200034X
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spelling crcambridgeupr:10.1017/jog.2022.34 2024-03-03T08:46:08+00:00 Direct measurement of optical properties of glacier ice using a photon-counting diffuse LiDAR Allgaier, Markus Cooper, Matthew G. Carlson, Anders E. Cooley, Sarah W. Ryan, Jonathan C. Smith, Brian J. University of Oregon 2022 http://dx.doi.org/10.1017/jog.2022.34 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302200034X en eng Cambridge University Press (CUP) https://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 68, issue 272, page 1210-1220 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2022 crcambridgeupr https://doi.org/10.1017/jog.2022.34 2024-02-08T08:28:33Z Abstract The production of meltwater from glacier ice, which is exposed at the margins of land ice during the summer, is responsible for a large proportion of glacier mass loss. The rate of meltwater production from glacier ice is especially sensitive to its physical structure and chemical composition which combine to determine the albedo of glacier ice. However, the optical properties of near-surface glacier ice are not well known since most prior work has focused on laboratory-grown ice or deep cores. Here, we demonstrate a measurement technique based on diffuse propagation of nanosecond-duration laser pulses in near-surface glacier ice that enables the independent measurement of the scattering and absorption coefficients, allowing for a complete description of the processes governing radiative transfer. We employ a photon-counting detector to overcome the high losses associated with diffuse optics. The instrument is highly portable and rugged, making it optimally suited for deployment in remote regions. A set of measurements taken on Crook and Collier Glaciers, Oregon, serves as a demonstration of the technique. These measurements provide insight into both physical structure and composition of near-surface glacier ice and open new avenues for the analysis of light-absorbing impurities and remote sensing of the cryosphere. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Collier ENVELOPE(-61.864,-61.864,-70.221,-70.221) Journal of Glaciology 1 11
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Allgaier, Markus
Cooper, Matthew G.
Carlson, Anders E.
Cooley, Sarah W.
Ryan, Jonathan C.
Smith, Brian J.
Direct measurement of optical properties of glacier ice using a photon-counting diffuse LiDAR
topic_facet Earth-Surface Processes
description Abstract The production of meltwater from glacier ice, which is exposed at the margins of land ice during the summer, is responsible for a large proportion of glacier mass loss. The rate of meltwater production from glacier ice is especially sensitive to its physical structure and chemical composition which combine to determine the albedo of glacier ice. However, the optical properties of near-surface glacier ice are not well known since most prior work has focused on laboratory-grown ice or deep cores. Here, we demonstrate a measurement technique based on diffuse propagation of nanosecond-duration laser pulses in near-surface glacier ice that enables the independent measurement of the scattering and absorption coefficients, allowing for a complete description of the processes governing radiative transfer. We employ a photon-counting detector to overcome the high losses associated with diffuse optics. The instrument is highly portable and rugged, making it optimally suited for deployment in remote regions. A set of measurements taken on Crook and Collier Glaciers, Oregon, serves as a demonstration of the technique. These measurements provide insight into both physical structure and composition of near-surface glacier ice and open new avenues for the analysis of light-absorbing impurities and remote sensing of the cryosphere.
author2 University of Oregon
format Article in Journal/Newspaper
author Allgaier, Markus
Cooper, Matthew G.
Carlson, Anders E.
Cooley, Sarah W.
Ryan, Jonathan C.
Smith, Brian J.
author_facet Allgaier, Markus
Cooper, Matthew G.
Carlson, Anders E.
Cooley, Sarah W.
Ryan, Jonathan C.
Smith, Brian J.
author_sort Allgaier, Markus
title Direct measurement of optical properties of glacier ice using a photon-counting diffuse LiDAR
title_short Direct measurement of optical properties of glacier ice using a photon-counting diffuse LiDAR
title_full Direct measurement of optical properties of glacier ice using a photon-counting diffuse LiDAR
title_fullStr Direct measurement of optical properties of glacier ice using a photon-counting diffuse LiDAR
title_full_unstemmed Direct measurement of optical properties of glacier ice using a photon-counting diffuse LiDAR
title_sort direct measurement of optical properties of glacier ice using a photon-counting diffuse lidar
publisher Cambridge University Press (CUP)
publishDate 2022
url http://dx.doi.org/10.1017/jog.2022.34
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302200034X
long_lat ENVELOPE(-61.864,-61.864,-70.221,-70.221)
geographic Collier
geographic_facet Collier
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 68, issue 272, page 1210-1220
ISSN 0022-1430 1727-5652
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2022.34
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 11
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