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...

Full description

Bibliographic Details
Published in:Polar Research
Main Author: Jorge F. Carrasco
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2018
Subjects:
Air temperature
El Niño–Southern Oscillation
Antarctic Oscillation
ERA-Interim reanalysis
blocking ridge
foehn effect
warm advection
Environmental sciences
GE1-350
Oceanography
GC1-1581
Antarctic
Patriot Hills
The Antarctic
West Antarctica
Antarc*
Antarctica
Polar Research
Online Access:https://doi.org/10.1080/17518369.2018.1547041
https://doaj.org/article/506398b33c15414a827bb08d79140ba6
Description
Summary: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.

Similar Items