Temporal variability in snow accumulation and density at Summit Camp, Greenland ice sheet

A 3-year record of weekly snow water equivalent (SWE) accumulation at Summit Camp, central Greenland ice sheet, obtained by direct sampling, is presented. While the overall SWE accumulation of 24.2 cm w.e. a−1 matches long-term ice core estimates, variability increases at shorter timescales. Half of...

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Published in:Journal of Glaciology
Main Author: Ian M. Howat
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2022
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.21
https://doaj.org/article/c1db0ab7277246e1a8833e404721cc66
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spelling ftdoajarticles:oai:doaj.org/article:c1db0ab7277246e1a8833e404721cc66 2023-05-15T16:27:42+02:00 Temporal variability in snow accumulation and density at Summit Camp, Greenland ice sheet Ian M. Howat 2022-12-01T00:00:00Z https://doi.org/10.1017/jog.2022.21 https://doaj.org/article/c1db0ab7277246e1a8833e404721cc66 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000211/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.21 0022-1430 1727-5652 https://doaj.org/article/c1db0ab7277246e1a8833e404721cc66 Journal of Glaciology, Vol 68, Pp 1076-1084 (2022) Accumulation ice-sheet mass balance snow/ice surface processes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.1017/jog.2022.21 2023-03-12T01:30:54Z A 3-year record of weekly snow water equivalent (SWE) accumulation at Summit Camp, central Greenland ice sheet, obtained by direct sampling, is presented. While the overall SWE accumulation of 24.2 cm w.e. a−1 matches long-term ice core estimates, variability increases at shorter timescales. Half of the annual SWE accumulation occurs during a few large events, with the average accumulation rate decreasing 35% between the first and second halves of the record coinciding with exceptional anticyclonic conditions in the spring and summer of 2019. No seasonality in accumulation is detected. Rather, local accumulation rates appear to be significantly impacted by wind redistribution that obscures temporal patterns in snowfall. Surface snow density is consistent, on average, with previously measured values but does not correlate with near surface temperature or wind speed. Two surface mass balance reanalysis models significantly underestimate accumulation rates at Summit Camp. This is concerning because such models are often used to estimate ice-sheet mass loss. Article in Journal/Newspaper Greenland ice core Ice Sheet Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Greenland Summit Camp ENVELOPE(-38.453,-38.453,72.579,72.579) Journal of Glaciology 68 272 1076 1084
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Accumulation
ice-sheet mass balance
snow/ice surface processes
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Accumulation
ice-sheet mass balance
snow/ice surface processes
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Ian M. Howat
Temporal variability in snow accumulation and density at Summit Camp, Greenland ice sheet
topic_facet Accumulation
ice-sheet mass balance
snow/ice surface processes
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description A 3-year record of weekly snow water equivalent (SWE) accumulation at Summit Camp, central Greenland ice sheet, obtained by direct sampling, is presented. While the overall SWE accumulation of 24.2 cm w.e. a−1 matches long-term ice core estimates, variability increases at shorter timescales. Half of the annual SWE accumulation occurs during a few large events, with the average accumulation rate decreasing 35% between the first and second halves of the record coinciding with exceptional anticyclonic conditions in the spring and summer of 2019. No seasonality in accumulation is detected. Rather, local accumulation rates appear to be significantly impacted by wind redistribution that obscures temporal patterns in snowfall. Surface snow density is consistent, on average, with previously measured values but does not correlate with near surface temperature or wind speed. Two surface mass balance reanalysis models significantly underestimate accumulation rates at Summit Camp. This is concerning because such models are often used to estimate ice-sheet mass loss.
format Article in Journal/Newspaper
author Ian M. Howat
author_facet Ian M. Howat
author_sort Ian M. Howat
title Temporal variability in snow accumulation and density at Summit Camp, Greenland ice sheet
title_short Temporal variability in snow accumulation and density at Summit Camp, Greenland ice sheet
title_full Temporal variability in snow accumulation and density at Summit Camp, Greenland ice sheet
title_fullStr Temporal variability in snow accumulation and density at Summit Camp, Greenland ice sheet
title_full_unstemmed Temporal variability in snow accumulation and density at Summit Camp, Greenland ice sheet
title_sort temporal variability in snow accumulation and density at summit camp, greenland ice sheet
publisher Cambridge University Press
publishDate 2022
url https://doi.org/10.1017/jog.2022.21
https://doaj.org/article/c1db0ab7277246e1a8833e404721cc66
long_lat ENVELOPE(-38.453,-38.453,72.579,72.579)
geographic Greenland
Summit Camp
geographic_facet Greenland
Summit Camp
genre Greenland
ice core
Ice Sheet
Journal of Glaciology
genre_facet Greenland
ice core
Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology, Vol 68, Pp 1076-1084 (2022)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022000211/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.21
0022-1430
1727-5652
https://doaj.org/article/c1db0ab7277246e1a8833e404721cc66
op_doi https://doi.org/10.1017/jog.2022.21
container_title Journal of Glaciology
container_volume 68
container_issue 272
container_start_page 1076
op_container_end_page 1084
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