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1000 Titel
  • Spatial distribution of vertical density and microstructure profiles in near-surface firn around Dome Fuji, Antarctica
1000 Autor/in
  1. Inoue, Ryo |
  2. Fujita, Shuji |
  3. Kawamura, Kenji |
  4. Oyabu, Ikumi |
  5. Nakazawa, Fumio |
  6. Motoyama, Hideaki |
  7. Aoki, Teruo |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-01-30
1000 Erschienen in
1000 Quellenangabe
  • 18(1):425-449
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-425-2024 |
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1000 Abstract/Summary
  • <jats:p>Abstract. To better understand the near-surface evolution of polar firn in low-accumulation areas (&lt;30 mm w.e. yr−1), we investigated the physical properties – density, microstructural anisotropy of ice matrix and pore space, and specific surface area (SSA) – of six firn cores collected within 60 km of Dome Fuji, East Antarctica. The physical properties were measured at intervals of ≤0.02 m over the top 10 m of the cores. The main findings are (i) a lack of significant density increase in the top ∼4 m, (ii) lower mean density near the dome summit (∼330 kg m−3) than in the surrounding slope area (∼355 kg m−3) in the top 1 m, (iii) developments of a vertically elongated microstructure and its contrast between layers within the top ∼3 m, (iv) more pronounced vertical elongation at sites and periods with lower accumulation rates than those with higher accumulation rates, (v) a rapid decrease in SSA in the top ∼3 m, and (vi) lower SSA at lower-accumulation sites, but this latter trend is less pronounced than that of microstructural anisotropy. These observations can be explained by a combination of the initial physical properties on the surface set by wind conditions and the metamorphism driven by water vapor transport through the firn column under a strong vertical temperature gradient (temperature gradient metamorphism, TGM). The magnitude of TGM depends on the duration of firn layers under the temperature gradient, determined by the accumulation rate; longer exposure causes a more vertically elongated microstructure and lower SSA. Overall, we highlight the significant spatial variability in the near-surface physical properties over the scale of ∼100 km around Dome Fuji. These findings will help us better understand the densification over the whole firn column and the gas-trapping process in deep firn and possible difference in them between existing deep ice cores and the upcoming “Oldest-Ice” cores collected tens of kilometers apart. </jats:p>
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  1. Japan Society for the Promotion of Science |
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    1000 Förderer Japan Society for the Promotion of Science |
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1000 Erstellt am 2024-05-23T17:53:24.127+0200
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1000 Zuletzt bearbeitet Mon May 27 10:30:27 CEST 2024
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