Contextualizing the 1997 warm event observed at Patriot Hills in the interior of West Antarctica
Between 5 and 8 December 1997, the surface air temperature increased up to 3°C in the interior of West Antarctica, at Patriot Hills (PH), located at about 80°08’S, 81°16ʹ W, at an elevation of 855 m a.s.l. This was about 15°C warmer than the mean air temperature (−12°C) for this location at this tim...
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Format: | Article in Journal/Newspaper |
Language: | English |
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Norwegian Polar Institute
2018
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Online Access: | https://polarresearch.net/index.php/polar/article/view/3404 |
_version_ | 1835018716288385024 |
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author | Carrasco, Jorge F. |
author_facet | Carrasco, Jorge F. |
author_sort | Carrasco, Jorge F. |
collection | Unknown |
description | Between 5 and 8 December 1997, the surface air temperature increased up to 3°C in the interior of West Antarctica, at Patriot Hills (PH), located at about 80°08’S, 81°16ʹ W, at an elevation of 855 m a.s.l. This was about 15°C warmer than the mean air temperature (−12°C) for this location at this time of the year. The ice surface field along the hills used as a runway for large aircraft melted, forming small ponds at the foot of the slope. This warm event was associated with a passing mid-tropospheric ridge that reached the interior of West Antarctica, whose anticyclonic circulation advected warm air towards the PH area. The foehn effect of the descending airflow on the northern slope of PH did not significantly contribute to the warming. The El Niño–Southern Oscillation (ENSO) was reaching its mature phase during the last quarter of 1997 and the warming/melting episode may be related to large-scale circulation associated with ENSO occurrence. However, warm events in the interior of West Antarctica may occur during any phase of ENSO. In contrast, the negative phase of the Antarctic Oscillation seems to support the development of the mid-tropospheric ridges that can advect warm maritime air towards the interior of West Antarctica. The 3°C registered at PH may be one of the highest near-surface air temperatures measured below 2500 m a.s.l. in the far interior coastal area of West Antarctica. This suggests a new subregion for determining air temperature records in Antarctica may need to be considered. |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Antarctica Polar Research West Antarctica |
genre_facet | Antarc* Antarctic Antarctica Polar Research West Antarctica |
geographic | Antarctic The Antarctic West Antarctica Patriot Hills |
geographic_facet | Antarctic The Antarctic West Antarctica Patriot Hills |
id | ftjpolarres:oai:journals.openacademia.net:article/3404 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-81.333,-81.333,-80.333,-80.333) |
op_collection_id | ftjpolarres |
op_relation | https://polarresearch.net/index.php/polar/article/view/3404/9064 https://polarresearch.net/index.php/polar/article/view/3404/9065 https://polarresearch.net/index.php/polar/article/view/3404 |
op_source | Polar Research; Vol 37 (2018) 1751-8369 |
publishDate | 2018 |
publisher | Norwegian Polar Institute |
record_format | openpolar |
spelling | ftjpolarres:oai:journals.openacademia.net:article/3404 2025-06-15T14:09:51+00:00 Contextualizing the 1997 warm event observed at Patriot Hills in the interior of West Antarctica Carrasco, Jorge F. 2018-12-11 application/pdf application/xml https://polarresearch.net/index.php/polar/article/view/3404 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/3404/9064 https://polarresearch.net/index.php/polar/article/view/3404/9065 https://polarresearch.net/index.php/polar/article/view/3404 Polar Research; Vol 37 (2018) 1751-8369 Air temperature El Niño–Southern Oscillation Antarctic Oscillation ERA-Interim reanalysis blocking ridge foehn effect warm advection info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2018 ftjpolarres 2025-05-20T03:03:13Z Between 5 and 8 December 1997, the surface air temperature increased up to 3°C in the interior of West Antarctica, at Patriot Hills (PH), located at about 80°08’S, 81°16ʹ W, at an elevation of 855 m a.s.l. This was about 15°C warmer than the mean air temperature (−12°C) for this location at this time of the year. The ice surface field along the hills used as a runway for large aircraft melted, forming small ponds at the foot of the slope. This warm event was associated with a passing mid-tropospheric ridge that reached the interior of West Antarctica, whose anticyclonic circulation advected warm air towards the PH area. The foehn effect of the descending airflow on the northern slope of PH did not significantly contribute to the warming. The El Niño–Southern Oscillation (ENSO) was reaching its mature phase during the last quarter of 1997 and the warming/melting episode may be related to large-scale circulation associated with ENSO occurrence. However, warm events in the interior of West Antarctica may occur during any phase of ENSO. In contrast, the negative phase of the Antarctic Oscillation seems to support the development of the mid-tropospheric ridges that can advect warm maritime air towards the interior of West Antarctica. The 3°C registered at PH may be one of the highest near-surface air temperatures measured below 2500 m a.s.l. in the far interior coastal area of West Antarctica. This suggests a new subregion for determining air temperature records in Antarctica may need to be considered. Article in Journal/Newspaper Antarc* Antarctic Antarctica Polar Research West Antarctica Unknown Antarctic The Antarctic West Antarctica Patriot Hills ENVELOPE(-81.333,-81.333,-80.333,-80.333) |
spellingShingle | Air temperature El Niño–Southern Oscillation Antarctic Oscillation ERA-Interim reanalysis blocking ridge foehn effect warm advection Carrasco, Jorge F. Contextualizing the 1997 warm event observed at Patriot Hills in the interior of West Antarctica |
title | Contextualizing the 1997 warm event observed at Patriot Hills in the interior of West Antarctica |
title_full | Contextualizing the 1997 warm event observed at Patriot Hills in the interior of West Antarctica |
title_fullStr | Contextualizing the 1997 warm event observed at Patriot Hills in the interior of West Antarctica |
title_full_unstemmed | Contextualizing the 1997 warm event observed at Patriot Hills in the interior of West Antarctica |
title_short | Contextualizing the 1997 warm event observed at Patriot Hills in the interior of West Antarctica |
title_sort | contextualizing the 1997 warm event observed at patriot hills in the interior of west antarctica |
topic | Air temperature El Niño–Southern Oscillation Antarctic Oscillation ERA-Interim reanalysis blocking ridge foehn effect warm advection |
topic_facet | Air temperature El Niño–Southern Oscillation Antarctic Oscillation ERA-Interim reanalysis blocking ridge foehn effect warm advection |
url | https://polarresearch.net/index.php/polar/article/view/3404 |