An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016

In this study, we focus on the model detection in the Antarctic Peninsula (AP) of so-called perennial firn aquifers (PFAs) that are widespread in Greenland and Svalbard and are formed when surface meltwater percolates into the firn pack in summer, which is then buried by snowfall and does not refree...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: J. M. van Wessem, C. R. Steger, N. Wever, M. R. van den Broeke
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-15-695-2021
https://doaj.org/article/6560505082334d6a9d869d17b49e1e4f
_version_ 1821519583678300160
author J. M. van Wessem
C. R. Steger
N. Wever
M. R. van den Broeke
author_facet J. M. van Wessem
C. R. Steger
N. Wever
M. R. van den Broeke
author_sort J. M. van Wessem
collection Directory of Open Access Journals: DOAJ Articles
container_issue 2
container_start_page 695
container_title The Cryosphere
container_volume 15
description In this study, we focus on the model detection in the Antarctic Peninsula (AP) of so-called perennial firn aquifers (PFAs) that are widespread in Greenland and Svalbard and are formed when surface meltwater percolates into the firn pack in summer, which is then buried by snowfall and does not refreeze during the following winter. We use two snow models, the Institute for Marine and Atmospheric Research Utrecht Firn Densification Model (IMAU-FDM) and SNOWPACK, and force these (partly) with mass and energy fluxes from the Regional Atmospheric Climate MOdel (RACMO2.3p2) to construct a 1979–2016 climatology of AP firn density, temperature, and liquid water content. An evaluation using 75 snow temperature observations at 10 m depth and density profiles from 11 firn cores shows that output of both snow models is sufficiently realistic to warrant further analysis of firn characteristics. The models give comparable results: in 941 model grid points in either model, covering ∼28 000 km 2 , PFAs existed for at least 1 year in the simulated period, most notably in the western AP. At these locations, surface meltwater production typically exceeds 200 <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="unit"><mi mathvariant="normal">mm</mi><mspace width="0.125em" linebreak="nobreak"/><mi mathvariant="normal">w</mi><mo>.</mo><mi mathvariant="normal">e</mi><mo>.</mo><mspace linebreak="nobreak" width="0.125em"/><msup><mi mathvariant="normal">yr</mi><mrow><mo>-</mo><mn mathvariant="normal">1</mn></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="61pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="ff6da8763e65c65d71b7ee9dba2d73a5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-15-695-2021-ie00001.svg" width="61pt" height="15pt" ...
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctic Peninsula
Greenland
Svalbard
The Cryosphere
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Greenland
Svalbard
The Cryosphere
geographic Antarctic
Antarctic Peninsula
Greenland
Svalbard
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
Greenland
Svalbard
The Antarctic
id ftdoajarticles:oai:doaj.org/article:6560505082334d6a9d869d17b49e1e4f
institution Open Polar
language English
op_collection_id ftdoajarticles
op_container_end_page 714
op_doi https://doi.org/10.5194/tc-15-695-2021
op_relation https://tc.copernicus.org/articles/15/695/2021/tc-15-695-2021.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-15-695-2021
1994-0416
1994-0424
https://doaj.org/article/6560505082334d6a9d869d17b49e1e4f
op_source The Cryosphere, Vol 15, Pp 695-714 (2021)
publishDate 2021
publisher Copernicus Publications
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:6560505082334d6a9d869d17b49e1e4f 2025-01-16T19:01:13+00:00 An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016 J. M. van Wessem C. R. Steger N. Wever M. R. van den Broeke 2021-02-01T00:00:00Z https://doi.org/10.5194/tc-15-695-2021 https://doaj.org/article/6560505082334d6a9d869d17b49e1e4f EN eng Copernicus Publications https://tc.copernicus.org/articles/15/695/2021/tc-15-695-2021.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-15-695-2021 1994-0416 1994-0424 https://doaj.org/article/6560505082334d6a9d869d17b49e1e4f The Cryosphere, Vol 15, Pp 695-714 (2021) Environmental sciences GE1-350 Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.5194/tc-15-695-2021 2022-12-31T12:03:25Z In this study, we focus on the model detection in the Antarctic Peninsula (AP) of so-called perennial firn aquifers (PFAs) that are widespread in Greenland and Svalbard and are formed when surface meltwater percolates into the firn pack in summer, which is then buried by snowfall and does not refreeze during the following winter. We use two snow models, the Institute for Marine and Atmospheric Research Utrecht Firn Densification Model (IMAU-FDM) and SNOWPACK, and force these (partly) with mass and energy fluxes from the Regional Atmospheric Climate MOdel (RACMO2.3p2) to construct a 1979–2016 climatology of AP firn density, temperature, and liquid water content. An evaluation using 75 snow temperature observations at 10 m depth and density profiles from 11 firn cores shows that output of both snow models is sufficiently realistic to warrant further analysis of firn characteristics. The models give comparable results: in 941 model grid points in either model, covering ∼28 000 km 2 , PFAs existed for at least 1 year in the simulated period, most notably in the western AP. At these locations, surface meltwater production typically exceeds 200 <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="unit"><mi mathvariant="normal">mm</mi><mspace width="0.125em" linebreak="nobreak"/><mi mathvariant="normal">w</mi><mo>.</mo><mi mathvariant="normal">e</mi><mo>.</mo><mspace linebreak="nobreak" width="0.125em"/><msup><mi mathvariant="normal">yr</mi><mrow><mo>-</mo><mn mathvariant="normal">1</mn></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="61pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="ff6da8763e65c65d71b7ee9dba2d73a5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-15-695-2021-ie00001.svg" width="61pt" height="15pt" ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Greenland Svalbard The Cryosphere Directory of Open Access Journals: DOAJ Articles Antarctic Antarctic Peninsula Greenland Svalbard The Antarctic The Cryosphere 15 2 695 714
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
J. M. van Wessem
C. R. Steger
N. Wever
M. R. van den Broeke
An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016
title An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016
title_full An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016
title_fullStr An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016
title_full_unstemmed An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016
title_short An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016
title_sort exploratory modelling study of perennial firn aquifers in the antarctic peninsula for the period 1979–2016
topic Environmental sciences
GE1-350
Geology
QE1-996.5
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
url https://doi.org/10.5194/tc-15-695-2021
https://doaj.org/article/6560505082334d6a9d869d17b49e1e4f