Observing and modeling the influence of layering on bubble trapping in polar firn

International audience Interpretation of ice core trace gas records depends on an accurate understanding of the processes that smooth the atmospheric signal in the firn. Much work has been done to understand the processes affecting air transport in the open pores of the firn, but a paucity of data f...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Mitchell, Logan, Buizert, Christo, Brook, Edward, A, Breton, Daniel, Fegyveresi, John, Baggenstos, Daniel, Orsi, Anais, Severinghaus, Jeffrey, Alley, Richard, Albert, Mary, Rhodes, Rachael, A, Mcconnell, Joseph, A, Sigl, Michael, Maselli, Olivia, A, Gregory, Stephanie, Ahn, Jinho
Other Authors: College of Earth, Ocean and Atmospheric Sciences Corvallis (CEOAS), Oregon State University (OSU), Scripps Institution of Oceanography (SIO - UC San Diego), University of California San Diego (UC San Diego), University of California (UC)-University of California (UC), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Desert Research Institute (DRI), Laboratory of Radio- and Environmental Chemistry Villigen, Paul Scherrer Institute (PSI)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2015
Subjects:
Online Access:https://hal.science/hal-01806235
https://hal.science/hal-01806235/document
https://hal.science/hal-01806235/file/2014JD022766.pdf
https://doi.org/10.1002/2014JD022766
id ftinsu:oai:HAL:hal-01806235v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Mitchell, Logan
Buizert, Christo
Brook, Edward, A
Breton, Daniel
Fegyveresi, John
Baggenstos, Daniel
Orsi, Anais
Severinghaus, Jeffrey
Alley, Richard
Albert, Mary
Rhodes, Rachael, A
Mcconnell, Joseph, A
Sigl, Michael
Maselli, Olivia, A
Gregory, Stephanie
Ahn, Jinho
Observing and modeling the influence of layering on bubble trapping in polar firn
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience Interpretation of ice core trace gas records depends on an accurate understanding of the processes that smooth the atmospheric signal in the firn. Much work has been done to understand the processes affecting air transport in the open pores of the firn, but a paucity of data from air trapped in bubbles in the firn-ice transition region has limited the ability to constrain the effect of bubble closure processes. Here we present high-resolution measurements of firn density, methane concentrations, nitrogen isotopes, and total air content that show layering in the firn-ice transition region at the West Antarctic Ice Sheet (WAIS) Divide ice core site. Using the notion that bubble trapping is a stochastic process, we derive a new parameterization for closed porosity that incorporates the effects of layering in a steady state firn modeling approach. We include the process of bubble trapping into an open-porosity firn air transport model and obtain a good fit to the firn core data. We find that layering broadens the depth range over which bubbles are trapped, widens the modeled gas age distribution of air in closed bubbles, reduces the mean gas age of air in closed bubbles, and introduces stratigraphic irregularities in the gas age scale that have a peak-to-peak variability of~10 years at WAIS Divide. For a more complete understanding of gas occlusion and its impact on ice core records, we suggest that this experiment be repeated at sites climatically different from WAIS Divide, for example, on the East Antarctic plateau.
author2 College of Earth, Ocean and Atmospheric Sciences Corvallis (CEOAS)
Oregon State University (OSU)
Scripps Institution of Oceanography (SIO - UC San Diego)
University of California San Diego (UC San Diego)
University of California (UC)-University of California (UC)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Desert Research Institute (DRI)
Laboratory of Radio- and Environmental Chemistry Villigen
Paul Scherrer Institute (PSI)
format Article in Journal/Newspaper
author Mitchell, Logan
Buizert, Christo
Brook, Edward, A
Breton, Daniel
Fegyveresi, John
Baggenstos, Daniel
Orsi, Anais
Severinghaus, Jeffrey
Alley, Richard
Albert, Mary
Rhodes, Rachael, A
Mcconnell, Joseph, A
Sigl, Michael
Maselli, Olivia, A
Gregory, Stephanie
Ahn, Jinho
author_facet Mitchell, Logan
Buizert, Christo
Brook, Edward, A
Breton, Daniel
Fegyveresi, John
Baggenstos, Daniel
Orsi, Anais
Severinghaus, Jeffrey
Alley, Richard
Albert, Mary
Rhodes, Rachael, A
Mcconnell, Joseph, A
Sigl, Michael
Maselli, Olivia, A
Gregory, Stephanie
Ahn, Jinho
author_sort Mitchell, Logan
title Observing and modeling the influence of layering on bubble trapping in polar firn
title_short Observing and modeling the influence of layering on bubble trapping in polar firn
title_full Observing and modeling the influence of layering on bubble trapping in polar firn
title_fullStr Observing and modeling the influence of layering on bubble trapping in polar firn
title_full_unstemmed Observing and modeling the influence of layering on bubble trapping in polar firn
title_sort observing and modeling the influence of layering on bubble trapping in polar firn
publisher HAL CCSD
publishDate 2015
url https://hal.science/hal-01806235
https://hal.science/hal-01806235/document
https://hal.science/hal-01806235/file/2014JD022766.pdf
https://doi.org/10.1002/2014JD022766
genre Antarc*
Antarctic
ice core
Ice Sheet
genre_facet Antarc*
Antarctic
ice core
Ice Sheet
op_source ISSN: 2169-897X
EISSN: 2169-8996
Journal of Geophysical Research: Atmospheres
https://hal.science/hal-01806235
Journal of Geophysical Research: Atmospheres, 2015, 120 (6), pp.2558 - 2574. ⟨10.1002/2014JD022766⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/2014JD022766
hal-01806235
https://hal.science/hal-01806235
https://hal.science/hal-01806235/document
https://hal.science/hal-01806235/file/2014JD022766.pdf
doi:10.1002/2014JD022766
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1002/2014JD022766
container_title Journal of Geophysical Research: Atmospheres
container_volume 120
container_issue 6
container_start_page 2558
op_container_end_page 2574
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spelling ftinsu:oai:HAL:hal-01806235v1 2024-04-28T08:00:36+00:00 Observing and modeling the influence of layering on bubble trapping in polar firn Mitchell, Logan Buizert, Christo Brook, Edward, A Breton, Daniel Fegyveresi, John Baggenstos, Daniel Orsi, Anais Severinghaus, Jeffrey Alley, Richard Albert, Mary Rhodes, Rachael, A Mcconnell, Joseph, A Sigl, Michael Maselli, Olivia, A Gregory, Stephanie Ahn, Jinho College of Earth, Ocean and Atmospheric Sciences Corvallis (CEOAS) Oregon State University (OSU) Scripps Institution of Oceanography (SIO - UC San Diego) University of California San Diego (UC San Diego) University of California (UC)-University of California (UC) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Desert Research Institute (DRI) Laboratory of Radio- and Environmental Chemistry Villigen Paul Scherrer Institute (PSI) 2015-03-27 https://hal.science/hal-01806235 https://hal.science/hal-01806235/document https://hal.science/hal-01806235/file/2014JD022766.pdf https://doi.org/10.1002/2014JD022766 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2014JD022766 hal-01806235 https://hal.science/hal-01806235 https://hal.science/hal-01806235/document https://hal.science/hal-01806235/file/2014JD022766.pdf doi:10.1002/2014JD022766 info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://hal.science/hal-01806235 Journal of Geophysical Research: Atmospheres, 2015, 120 (6), pp.2558 - 2574. ⟨10.1002/2014JD022766⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2015 ftinsu https://doi.org/10.1002/2014JD022766 2024-04-05T00:40:08Z International audience Interpretation of ice core trace gas records depends on an accurate understanding of the processes that smooth the atmospheric signal in the firn. Much work has been done to understand the processes affecting air transport in the open pores of the firn, but a paucity of data from air trapped in bubbles in the firn-ice transition region has limited the ability to constrain the effect of bubble closure processes. Here we present high-resolution measurements of firn density, methane concentrations, nitrogen isotopes, and total air content that show layering in the firn-ice transition region at the West Antarctic Ice Sheet (WAIS) Divide ice core site. Using the notion that bubble trapping is a stochastic process, we derive a new parameterization for closed porosity that incorporates the effects of layering in a steady state firn modeling approach. We include the process of bubble trapping into an open-porosity firn air transport model and obtain a good fit to the firn core data. We find that layering broadens the depth range over which bubbles are trapped, widens the modeled gas age distribution of air in closed bubbles, reduces the mean gas age of air in closed bubbles, and introduces stratigraphic irregularities in the gas age scale that have a peak-to-peak variability of~10 years at WAIS Divide. For a more complete understanding of gas occlusion and its impact on ice core records, we suggest that this experiment be repeated at sites climatically different from WAIS Divide, for example, on the East Antarctic plateau. Article in Journal/Newspaper Antarc* Antarctic ice core Ice Sheet Institut national des sciences de l'Univers: HAL-INSU Journal of Geophysical Research: Atmospheres 120 6 2558 2574