Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry

Precise measurements of snow structural parameters are crucial to understand snow stratigraphy and its formation by deposition and metamorphism. However, most snow measurements are limited in spatial and temporal resolution, and an important limiting factor is often the time needed to make measureme...

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Main Authors: Proksch, Martin, Schneebeli, Martin, Weißbach, Stefanie, Löwe, Henning
Format: Conference Object
Language:unknown
Published: 2013
Subjects:
Rho
Online Access:https://epic.awi.de/id/eprint/37203/
https://hdl.handle.net/10013/epic.44890
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spelling ftawi:oai:epic.awi.de:37203 2023-05-15T13:40:26+02:00 Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry Proksch, Martin Schneebeli, Martin Weißbach, Stefanie Löwe, Henning 2013-12-09 https://epic.awi.de/id/eprint/37203/ https://hdl.handle.net/10013/epic.44890 unknown Proksch, M. , Schneebeli, M. , Weißbach, S. and Löwe, H. (2013) Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry , AGU fall meeting, san francisco, 9 December 2013 - 13 December 2013 . hdl:10013/epic.44890 EPIC3AGU fall meeting, san francisco, 2013-12-09-2013-12-13 Conference notRev 2013 ftawi 2021-12-24T15:40:12Z Precise measurements of snow structural parameters are crucial to understand snow stratigraphy and its formation by deposition and metamorphism. However, most snow measurements are limited in spatial and temporal resolution, and an important limiting factor is often the time needed to make measurements. We demonstrate the potential of a high-resolution penetrometer by the stratigraphy of a 25 m long and 1.1 m deep transect through the snow and firn at Kohnen Station, Antarctica. We used a statistical model that extracts three major snow structural parameters, density (rho), correlation length (lex) and specific surface area (SSA). We could show using independent measurements from the site that the statistical model is indeed sufficient. The two-dimensional plots reveal the depositional and metamorphic events clearly. Based on these data, we are able to make a much more complete interpretation of the stratigraphic evolution at Kohnen Station. SnowMicroPen derived density of a 1.10 m deep and 25 m long snow and firn transect at Kohnen Station, Antarctica, measured in December 2012. Conference Object Antarc* Antarctic Antarctica Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Antarctic Kohnen ENVELOPE(0.000,0.000,-75.000,-75.000) Kohnen Station ENVELOPE(0.000,0.000,-75.000,-75.000) Rho ENVELOPE(-63.000,-63.000,-64.300,-64.300)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Precise measurements of snow structural parameters are crucial to understand snow stratigraphy and its formation by deposition and metamorphism. However, most snow measurements are limited in spatial and temporal resolution, and an important limiting factor is often the time needed to make measurements. We demonstrate the potential of a high-resolution penetrometer by the stratigraphy of a 25 m long and 1.1 m deep transect through the snow and firn at Kohnen Station, Antarctica. We used a statistical model that extracts three major snow structural parameters, density (rho), correlation length (lex) and specific surface area (SSA). We could show using independent measurements from the site that the statistical model is indeed sufficient. The two-dimensional plots reveal the depositional and metamorphic events clearly. Based on these data, we are able to make a much more complete interpretation of the stratigraphic evolution at Kohnen Station. SnowMicroPen derived density of a 1.10 m deep and 25 m long snow and firn transect at Kohnen Station, Antarctica, measured in December 2012.
format Conference Object
author Proksch, Martin
Schneebeli, Martin
Weißbach, Stefanie
Löwe, Henning
spellingShingle Proksch, Martin
Schneebeli, Martin
Weißbach, Stefanie
Löwe, Henning
Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry
author_facet Proksch, Martin
Schneebeli, Martin
Weißbach, Stefanie
Löwe, Henning
author_sort Proksch, Martin
title Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry
title_short Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry
title_full Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry
title_fullStr Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry
title_full_unstemmed Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry
title_sort reducing spatial uncertainty: stratigraphy of antarctic firn resolved by high-resolution penetrometry
publishDate 2013
url https://epic.awi.de/id/eprint/37203/
https://hdl.handle.net/10013/epic.44890
long_lat ENVELOPE(0.000,0.000,-75.000,-75.000)
ENVELOPE(0.000,0.000,-75.000,-75.000)
ENVELOPE(-63.000,-63.000,-64.300,-64.300)
geographic Antarctic
Kohnen
Kohnen Station
Rho
geographic_facet Antarctic
Kohnen
Kohnen Station
Rho
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source EPIC3AGU fall meeting, san francisco, 2013-12-09-2013-12-13
op_relation Proksch, M. , Schneebeli, M. , Weißbach, S. and Löwe, H. (2013) Reducing Spatial Uncertainty: Stratigraphy of Antarctic Firn Resolved by High-Resolution Penetrometry , AGU fall meeting, san francisco, 9 December 2013 - 13 December 2013 . hdl:10013/epic.44890
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