Temporal downscaling of glaciological mass balance using seasonal observations

Glaciological mass-balance measurements have been the backbone of internationally coordinated glacier monitoring. The resulting annual observations have been used to understand glacier reactions to climate change, and to assess both regional and global glacier mass changes and related contributions...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Michael Zemp, Ethan Welty
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press
Subjects:
Online Access:https://doi.org/10.1017/jog.2023.66
https://doaj.org/article/9820a070230d4c9799c49b4c4e3083ac
id ftdoajarticles:oai:doaj.org/article:9820a070230d4c9799c49b4c4e3083ac
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:9820a070230d4c9799c49b4c4e3083ac 2023-11-12T04:19:55+01:00 Temporal downscaling of glaciological mass balance using seasonal observations Michael Zemp Ethan Welty https://doi.org/10.1017/jog.2023.66 https://doaj.org/article/9820a070230d4c9799c49b4c4e3083ac EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143023000667/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2023.66 0022-1430 1727-5652 https://doaj.org/article/9820a070230d4c9799c49b4c4e3083ac Journal of Glaciology, Pp 1-6 Glacier mass balance glacier modelling glacier monitoring temporal downscaling Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article ftdoajarticles https://doi.org/10.1017/jog.2023.66 2023-10-15T00:38:47Z Glaciological mass-balance measurements have been the backbone of internationally coordinated glacier monitoring. The resulting annual observations have been used to understand glacier reactions to climate change, and to assess both regional and global glacier mass changes and related contributions to runoff and sea-level rise. However, the comparability of annual observations is hampered by differences in survey periods and mass-balance amplitudes between glaciers, regions and hemispheres. This study presents a simple approach to temporally downscale glaciological mass balance using seasonal observations and sine functions. The proposed analytical model allows reconstruction of the seasonal course of glacier mass balance at weekly to monthly resolution from only annual or seasonal observations. Strengths and limitations of this analytical approach are discussed and compared with results from numerical mass-balance modelling. Potential applications include seasonal corrections of glaciological and geodetic observations and comparisons to monthly results from spaceborne gravimetry and altimetry. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 6
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Glacier mass balance
glacier modelling
glacier monitoring
temporal downscaling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Glacier mass balance
glacier modelling
glacier monitoring
temporal downscaling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Michael Zemp
Ethan Welty
Temporal downscaling of glaciological mass balance using seasonal observations
topic_facet Glacier mass balance
glacier modelling
glacier monitoring
temporal downscaling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Glaciological mass-balance measurements have been the backbone of internationally coordinated glacier monitoring. The resulting annual observations have been used to understand glacier reactions to climate change, and to assess both regional and global glacier mass changes and related contributions to runoff and sea-level rise. However, the comparability of annual observations is hampered by differences in survey periods and mass-balance amplitudes between glaciers, regions and hemispheres. This study presents a simple approach to temporally downscale glaciological mass balance using seasonal observations and sine functions. The proposed analytical model allows reconstruction of the seasonal course of glacier mass balance at weekly to monthly resolution from only annual or seasonal observations. Strengths and limitations of this analytical approach are discussed and compared with results from numerical mass-balance modelling. Potential applications include seasonal corrections of glaciological and geodetic observations and comparisons to monthly results from spaceborne gravimetry and altimetry.
format Article in Journal/Newspaper
author Michael Zemp
Ethan Welty
author_facet Michael Zemp
Ethan Welty
author_sort Michael Zemp
title Temporal downscaling of glaciological mass balance using seasonal observations
title_short Temporal downscaling of glaciological mass balance using seasonal observations
title_full Temporal downscaling of glaciological mass balance using seasonal observations
title_fullStr Temporal downscaling of glaciological mass balance using seasonal observations
title_full_unstemmed Temporal downscaling of glaciological mass balance using seasonal observations
title_sort temporal downscaling of glaciological mass balance using seasonal observations
publisher Cambridge University Press
url https://doi.org/10.1017/jog.2023.66
https://doaj.org/article/9820a070230d4c9799c49b4c4e3083ac
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Pp 1-6
op_relation https://www.cambridge.org/core/product/identifier/S0022143023000667/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2023.66
0022-1430
1727-5652
https://doaj.org/article/9820a070230d4c9799c49b4c4e3083ac
op_doi https://doi.org/10.1017/jog.2023.66
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 6
_version_ 1782336144152723456