Bare ice fields developed in the inland part of the Antarctic ice sheet
Observations of a bare ice field were carried out at Seal Rock in the Sor Rondane area, East Antarctica. A large sublimation rate, 200 to 280mm/a, was observed on the bare ice field. Air temperature on the bare ice was about 1℃ higher than that on the snow surface. The large sublimation rate was exp...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
National Institute of Polar Research
1997
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| Subjects: | |
| Online Access: | https://doi.org/10.15094/00008987 https://doaj.org/article/c47686687c84442d88f4430e3bb6eb45 |
| _version_ | 1821735264785006592 |
|---|---|
| author | Shuhei Takahashi |
| author_facet | Shuhei Takahashi |
| author_sort | Shuhei Takahashi |
| collection | Unknown |
| description | Observations of a bare ice field were carried out at Seal Rock in the Sor Rondane area, East Antarctica. A large sublimation rate, 200 to 280mm/a, was observed on the bare ice field. Air temperature on the bare ice was about 1℃ higher than that on the snow surface. The large sublimation rate was explained from the low albedo of bare ice; its value was roughly estimated from heat budget considerations. The bare ice fields were classified into 4 types according to origin. |
| format | Article in Journal/Newspaper |
| genre | Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
| genre_facet | Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
| geographic | Antarctic The Antarctic East Antarctica Sor-Rondane Seal Rock |
| geographic_facet | Antarctic The Antarctic East Antarctica Sor-Rondane Seal Rock |
| id | fttriple:oai:gotriple.eu:oai:doaj.org/article:c47686687c84442d88f4430e3bb6eb45 |
| institution | Open Polar |
| language | English |
| long_lat | ENVELOPE(25.000,25.000,-72.000,-72.000) ENVELOPE(-54.298,-54.298,49.550,49.550) |
| op_collection_id | fttriple |
| op_doi | https://doi.org/10.15094/00008987 |
| op_relation | doi:10.15094/00008987 0085-7289 2432-079X https://doaj.org/article/c47686687c84442d88f4430e3bb6eb45 |
| op_rights | undefined |
| op_source | Antarctic Record, Vol 41, Iss 1, Pp 433-445 (1997) |
| publishDate | 1997 |
| publisher | National Institute of Polar Research |
| record_format | openpolar |
| spelling | fttriple:oai:gotriple.eu:oai:doaj.org/article:c47686687c84442d88f4430e3bb6eb45 2025-01-16T19:18:21+00:00 Bare ice fields developed in the inland part of the Antarctic ice sheet Shuhei Takahashi 1997-03-01 https://doi.org/10.15094/00008987 https://doaj.org/article/c47686687c84442d88f4430e3bb6eb45 en other eng National Institute of Polar Research doi:10.15094/00008987 0085-7289 2432-079X https://doaj.org/article/c47686687c84442d88f4430e3bb6eb45 undefined Antarctic Record, Vol 41, Iss 1, Pp 433-445 (1997) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1997 fttriple https://doi.org/10.15094/00008987 2023-01-22T17:51:31Z Observations of a bare ice field were carried out at Seal Rock in the Sor Rondane area, East Antarctica. A large sublimation rate, 200 to 280mm/a, was observed on the bare ice field. Air temperature on the bare ice was about 1℃ higher than that on the snow surface. The large sublimation rate was explained from the low albedo of bare ice; its value was roughly estimated from heat budget considerations. The bare ice fields were classified into 4 types according to origin. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Unknown Antarctic The Antarctic East Antarctica Sor-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) Seal Rock ENVELOPE(-54.298,-54.298,49.550,49.550) |
| spellingShingle | geo envir Shuhei Takahashi Bare ice fields developed in the inland part of the Antarctic ice sheet |
| title | Bare ice fields developed in the inland part of the Antarctic ice sheet |
| title_full | Bare ice fields developed in the inland part of the Antarctic ice sheet |
| title_fullStr | Bare ice fields developed in the inland part of the Antarctic ice sheet |
| title_full_unstemmed | Bare ice fields developed in the inland part of the Antarctic ice sheet |
| title_short | Bare ice fields developed in the inland part of the Antarctic ice sheet |
| title_sort | bare ice fields developed in the inland part of the antarctic ice sheet |
| topic | geo envir |
| topic_facet | geo envir |
| url | https://doi.org/10.15094/00008987 https://doaj.org/article/c47686687c84442d88f4430e3bb6eb45 |