Articles | Volume 12, issue 1
https://doi.org/10.5194/tc-12-325-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-12-325-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
26 Jan 2018
Research article |
| 26 Jan 2018
Surface formation, preservation, and history of low-porosity crusts at the WAIS Divide site, West Antarctica
John M. Fegyveresi
CORRESPONDING AUTHOR
Terrestrial and Cryospheric Sciences Branch, US Cold Regions Research and Engineering Laboratory (CRREL), Hanover, NH 03755, USA
Dept. of Geosciences, and Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802, USA
Richard B. Alley
Dept. of Geosciences, and Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802, USA
Atsuhiro Muto
Dept. of Earth and Environmental Science, College of Science and Technology, Temple University, Philadelphia, PA 19122, USA
Anaïs J. Orsi
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 91191, Gif-sur-Yvette, France
Matthew K. Spencer
School of Physical Sciences, Lake Superior State University, Sault Sainte Marie, MI 49783, USA
Viewed
Total article views: 2,942 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 29 Jun 2016)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 1,718 | 1,003 | 221 | 2,942 | 495 | 119 | 162 |
- HTML: 1,718
- PDF: 1,003
- XML: 221
- Total: 2,942
- Supplement: 495
- BibTeX: 119
- EndNote: 162
Total article views: 2,167 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 26 Jan 2018)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 1,270 | 744 | 153 | 2,167 | 256 | 96 | 96 |
- HTML: 1,270
- PDF: 744
- XML: 153
- Total: 2,167
- Supplement: 256
- BibTeX: 96
- EndNote: 96
Total article views: 775 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 29 Jun 2016)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 448 | 259 | 68 | 775 | 239 | 23 | 66 |
- HTML: 448
- PDF: 259
- XML: 68
- Total: 775
- Supplement: 239
- BibTeX: 23
- EndNote: 66
Cited
11 citations as recorded by crossref.
- Outlier accommodation with semiparametric density processes: A study of Antarctic snow density modelling D. Sheanshang et al. 10.1177/1471082X211043946
- Local Weather Conditions Create Structural Differences between Shallow Firn Columns at Summit, Greenland and WAIS Divide, Antarctica I. McDowell et al. 10.3390/atmos11121370
- Spatial Distribution of Crusts in Antarctic and Greenland Snowpacks and Implications for Snow and Firn Studies A. Weinhart et al. 10.3389/feart.2021.630070
- Melt in the Greenland EastGRIP ice core reveals Holocene warm events J. Westhoff et al. 10.5194/cp-18-1011-2022
- SE‐Dome II Ice Core Dating With Half‐Year Precision: Increasing Melting Events From 1799 to 2020 in Southeastern Greenland K. Kawakami et al. 10.1029/2023JD038874
- Very old firn air linked to strong density layering at Styx Glacier, coastal Victoria Land, East Antarctica Y. Jang et al. 10.5194/tc-13-2407-2019
- Identifying atmospheric processes favouring the formation of bubble-free layers in the Law Dome ice core, East Antarctica L. Zhang et al. 10.5194/tc-17-5155-2023
- Microstructural characterization of depth hoar and ice‐crust layers using a micro‐CT, and hypothesis of ice‐crust formation under a thunderstorm Y. Li et al. 10.1002/hyp.15060
- Microstructure of Snow and Its Link to Trace Elements and Isotopic Composition at Kohnen Station, Dronning Maud Land, Antarctica D. Moser et al. 10.3389/feart.2020.00023
- Physically Based Summer Temperature Reconstruction From Melt Layers in Ice Cores K. Fujita et al. 10.1029/2020EA001590
- Introduction to special section on the WAIS Divide Special Issue of Paleoceanography K. Taylor 10.1002/2016PA002995
10 citations as recorded by crossref.
- Outlier accommodation with semiparametric density processes: A study of Antarctic snow density modelling D. Sheanshang et al. 10.1177/1471082X211043946
- Local Weather Conditions Create Structural Differences between Shallow Firn Columns at Summit, Greenland and WAIS Divide, Antarctica I. McDowell et al. 10.3390/atmos11121370
- Spatial Distribution of Crusts in Antarctic and Greenland Snowpacks and Implications for Snow and Firn Studies A. Weinhart et al. 10.3389/feart.2021.630070
- Melt in the Greenland EastGRIP ice core reveals Holocene warm events J. Westhoff et al. 10.5194/cp-18-1011-2022
- SE‐Dome II Ice Core Dating With Half‐Year Precision: Increasing Melting Events From 1799 to 2020 in Southeastern Greenland K. Kawakami et al. 10.1029/2023JD038874
- Very old firn air linked to strong density layering at Styx Glacier, coastal Victoria Land, East Antarctica Y. Jang et al. 10.5194/tc-13-2407-2019
- Identifying atmospheric processes favouring the formation of bubble-free layers in the Law Dome ice core, East Antarctica L. Zhang et al. 10.5194/tc-17-5155-2023
- Microstructural characterization of depth hoar and ice‐crust layers using a micro‐CT, and hypothesis of ice‐crust formation under a thunderstorm Y. Li et al. 10.1002/hyp.15060
- Microstructure of Snow and Its Link to Trace Elements and Isotopic Composition at Kohnen Station, Dronning Maud Land, Antarctica D. Moser et al. 10.3389/feart.2020.00023
- Physically Based Summer Temperature Reconstruction From Melt Layers in Ice Cores K. Fujita et al. 10.1029/2020EA001590
1 citations as recorded by crossref.
Latest update: 25 Apr 2024
Short summary
Observations at the WAIS Divide site in West Antarctica show that near-surface snow is strongly altered by weather-related processes, such as strong winds and temperature fluctuations, producing features that are recognizable within the WDC06A ice core. Specifically, over 10 000 prominent crusts were observed in the upper 560 m of the core. We show that these crusts develop more often in summers, during relatively low-wind, low-humidity, clear-sky periods with intense daytime sunshine.
Observations at the WAIS Divide site in West Antarctica show that near-surface snow is strongly...
