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...
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Copernicus Publications
2021
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Online Access: | https://doi.org/10.5194/tc-15-695-2021 https://doaj.org/article/6560505082334d6a9d869d17b49e1e4f |
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ftdoajarticles:oai:doaj.org/article:6560505082334d6a9d869d17b49e1e4f 2023-05-15T13:35:01+02:00 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 The Antarctic Svalbard Antarctic Peninsula Greenland The Cryosphere 15 2 695 714 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
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 |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
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 |
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 |
title |
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_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_sort |
exploratory modelling study of perennial firn aquifers in the antarctic peninsula for the period 1979–2016 |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doi.org/10.5194/tc-15-695-2021 https://doaj.org/article/6560505082334d6a9d869d17b49e1e4f |
geographic |
Antarctic The Antarctic Svalbard Antarctic Peninsula Greenland |
geographic_facet |
Antarctic The Antarctic Svalbard Antarctic Peninsula Greenland |
genre |
Antarc* Antarctic Antarctic Peninsula Greenland Svalbard The Cryosphere |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Greenland Svalbard The Cryosphere |
op_source |
The Cryosphere, Vol 15, Pp 695-714 (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_doi |
https://doi.org/10.5194/tc-15-695-2021 |
container_title |
The Cryosphere |
container_volume |
15 |
container_issue |
2 |
container_start_page |
695 |
op_container_end_page |
714 |
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1766060219589197824 |