High-resolution density profiles of two firn cores from Union Glacier, Ellsworth Mountains, West Antarctica

Fuente: PANGAEA
Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: Hoffmann-Abdi, Kirstin, Fernandoy, Francisco, Meyer, Hanno, Thomas, Elizabeth R, Aliaga, Marcelo, Tetzner, Dieter, Freitag, Johannes, Opel, Thomas, Arigony-Neto, Jorge, Göbel, Christian Florian, Jaña, Ricardo, Rodríguez Oroz, Delia, Tuckwell, Rebecca, Lynch, Emily, McConnell, Joseph R, Schneider, Christoph
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2024
Schlagworte:
Online-Zugang:
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
_version_ 1867171377791893504
author Hoffmann-Abdi, Kirstin
Fernandoy, Francisco
Meyer, Hanno
Thomas, Elizabeth R
Aliaga, Marcelo
Tetzner, Dieter
Freitag, Johannes
Opel, Thomas
Arigony-Neto, Jorge
Göbel, Christian Florian
Jaña, Ricardo
Rodríguez Oroz, Delia
Tuckwell, Rebecca
Lynch, Emily
McConnell, Joseph R
Schneider, Christoph
author_facet Hoffmann-Abdi, Kirstin
Fernandoy, Francisco
Meyer, Hanno
Thomas, Elizabeth R
Aliaga, Marcelo
Tetzner, Dieter
Freitag, Johannes
Opel, Thomas
Arigony-Neto, Jorge
Göbel, Christian Florian
Jaña, Ricardo
Rodríguez Oroz, Delia
Tuckwell, Rebecca
Lynch, Emily
McConnell, Joseph R
Schneider, Christoph
collection Datos científicos de ciencias marinas y ambientales
contents Firn cores BAL-1 and PASO-1 were both retrieved in November 2015 from the Union Glacier region, located in the Ellsworth Mountains at the northern edge of the West Antarctic Ice Sheet. BAL-1 was drilled in a U-shaped glacial valley (Balish Glacier) at an altitude of approximately 1520 m above sea level (a.s.l.) to a depth of 17.28 m. PASO-1 was drilled on a plateau west of the Gifford Peaks at an altitude of about 1920 m a.s.l. to a depth of 15.04 m. Both firn cores were obtained using a portable solar-powered and electrically operated ice-core drill (Backpack Drill; icedrill.ch AG). Density measurements of the two firn cores were performed at the ice-core processing facilities of the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI) in Bremerhaven, Germany, in spring and autumn 2016. X-ray microfocus computer tomography (ICE-CT; Freitag et al., 2013, doi:10.3189/2013JoG13J028) was used for the measurements, providing depth-density profiles with a resolution of better than 1 mm. The density data were used to analyse the firn core stratigraphy (e.g., determination of the snow-firn transition depth, identification of wind crusts), to calculate diffusion lengths as well as to derive accumulation rates for the firn-core drill sites.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_963192
institution PANGAEA
language en
publishDate 2024
publisher PANGAEA
record_format pangaea
spellingShingle High-resolution density profiles of two firn cores from Union Glacier, Ellsworth Mountains, West Antarctica
Hoffmann-Abdi, Kirstin
Fernandoy, Francisco
Meyer, Hanno
Thomas, Elizabeth R
Aliaga, Marcelo
Tetzner, Dieter
Freitag, Johannes
Opel, Thomas
Arigony-Neto, Jorge
Göbel, Christian Florian
Jaña, Ricardo
Rodríguez Oroz, Delia
Tuckwell, Rebecca
Lynch, Emily
McConnell, Joseph R
Schneider, Christoph
Antarctica; density; firn core; snow density; Snowpack; West Antarctica
Firn cores BAL-1 and PASO-1 were both retrieved in November 2015 from the Union Glacier region, located in the Ellsworth Mountains at the northern edge of the West Antarctic Ice Sheet. BAL-1 was drilled in a U-shaped glacial valley (Balish Glacier) at an altitude of approximately 1520 m above sea level (a.s.l.) to a depth of 17.28 m. PASO-1 was drilled on a plateau west of the Gifford Peaks at an altitude of about 1920 m a.s.l. to a depth of 15.04 m. Both firn cores were obtained using a portable solar-powered and electrically operated ice-core drill (Backpack Drill; icedrill.ch AG). Density measurements of the two firn cores were performed at the ice-core processing facilities of the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI) in Bremerhaven, Germany, in spring and autumn 2016. X-ray microfocus computer tomography (ICE-CT; Freitag et al., 2013, doi:10.3189/2013JoG13J028) was used for the measurements, providing depth-density profiles with a resolution of better than 1 mm. The density data were used to analyse the firn core stratigraphy (e.g., determination of the snow-firn transition depth, identification of wind crusts), to calculate diffusion lengths as well as to derive accumulation rates for the firn-core drill sites.
title High-resolution density profiles of two firn cores from Union Glacier, Ellsworth Mountains, West Antarctica
topic Antarctica; density; firn core; snow density; Snowpack; West Antarctica
url https://doi.org/10.1594/PANGAEA.963192