Regional climate variability driven by foehn winds in the McMurdo Dry Valleys, Antarctica
Warm, dry and gusty foehn winds are frequently experienced in the McMurdo Dry Valleys (MDVs), Antarctica; however, their significance in the region's climate is unknown. Foehn events in the MDVs are caused by topographic modification of southwesterly airflow which is related to the occurrence o...
Published in: | International Journal of Climatology |
---|---|
Other Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2012
|
Subjects: | |
Online Access: | https://doi.org/10.1002/joc.3481 |
id |
ftncar:oai:drupal-site.org:articles_21497 |
---|---|
record_format |
openpolar |
spelling |
ftncar:oai:drupal-site.org:articles_21497 2023-07-30T03:58:16+02:00 Regional climate variability driven by foehn winds in the McMurdo Dry Valleys, Antarctica Speirs, Johanna C. (author) McGowan, Hamish A. (author) Steinhoff, Daniel F. (author) Bromwich, David H. (author) 2012-04-30 https://doi.org/10.1002/joc.3481 en eng International Journal of Climatology--Int. J. Climatol.--08998418 articles:21497 ark:/85065/d7wd438p doi:10.1002/joc.3481 Copyright 2012 Royal Meteorological Society. article Text 2012 ftncar https://doi.org/10.1002/joc.3481 2023-07-17T18:16:04Z Warm, dry and gusty foehn winds are frequently experienced in the McMurdo Dry Valleys (MDVs), Antarctica; however, their significance in the region's climate is unknown. Foehn events in the MDVs are caused by topographic modification of southwesterly airflow which is related to the occurrence of synoptic-scale cyclones in the Amundsen/Ross Sea region. The intra- and interannual frequency and intensity of foehn events therefore varies in response to the position and frequency of cyclones in this region that are believed to be strongly influenced by the El Nino Southern Oscillation (ENSO) and the Southern Annular Mode (SAM). Here, we present a 20-year climatology of foehn winds from observational records in the MDVs. The SAM is found to significantly influence foehn wind frequency during the Antarctic summer and autumn months, whereas ENSO only holds significant correlations with winter air temperatures in the MDVs. The positive relationship between the SAM and the foehn wind regime in summer is particularly significant as foehn winds frequently cause summer temperatures to rise above 0 degrees C leading to extensive melt and thaw in MDVs. Foehn winds are a major climatological feature of the MDVs with their frequency and duration affecting the region's temperature records and their trends. Accordingly, analysis of the region's weather and climate records and predictions of future impacts of climate change on the MDVs is incomplete without consideration of foehn winds and their influence. Copyright (c) 2012 Royal Meteorological Society Article in Journal/Newspaper Antarc* Antarctic Antarctica McMurdo Dry Valleys Ross Sea OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Antarctic The Antarctic Ross Sea McMurdo Dry Valleys International Journal of Climatology 33 4 945 958 |
institution |
Open Polar |
collection |
OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) |
op_collection_id |
ftncar |
language |
English |
description |
Warm, dry and gusty foehn winds are frequently experienced in the McMurdo Dry Valleys (MDVs), Antarctica; however, their significance in the region's climate is unknown. Foehn events in the MDVs are caused by topographic modification of southwesterly airflow which is related to the occurrence of synoptic-scale cyclones in the Amundsen/Ross Sea region. The intra- and interannual frequency and intensity of foehn events therefore varies in response to the position and frequency of cyclones in this region that are believed to be strongly influenced by the El Nino Southern Oscillation (ENSO) and the Southern Annular Mode (SAM). Here, we present a 20-year climatology of foehn winds from observational records in the MDVs. The SAM is found to significantly influence foehn wind frequency during the Antarctic summer and autumn months, whereas ENSO only holds significant correlations with winter air temperatures in the MDVs. The positive relationship between the SAM and the foehn wind regime in summer is particularly significant as foehn winds frequently cause summer temperatures to rise above 0 degrees C leading to extensive melt and thaw in MDVs. Foehn winds are a major climatological feature of the MDVs with their frequency and duration affecting the region's temperature records and their trends. Accordingly, analysis of the region's weather and climate records and predictions of future impacts of climate change on the MDVs is incomplete without consideration of foehn winds and their influence. Copyright (c) 2012 Royal Meteorological Society |
author2 |
Speirs, Johanna C. (author) McGowan, Hamish A. (author) Steinhoff, Daniel F. (author) Bromwich, David H. (author) |
format |
Article in Journal/Newspaper |
title |
Regional climate variability driven by foehn winds in the McMurdo Dry Valleys, Antarctica |
spellingShingle |
Regional climate variability driven by foehn winds in the McMurdo Dry Valleys, Antarctica |
title_short |
Regional climate variability driven by foehn winds in the McMurdo Dry Valleys, Antarctica |
title_full |
Regional climate variability driven by foehn winds in the McMurdo Dry Valleys, Antarctica |
title_fullStr |
Regional climate variability driven by foehn winds in the McMurdo Dry Valleys, Antarctica |
title_full_unstemmed |
Regional climate variability driven by foehn winds in the McMurdo Dry Valleys, Antarctica |
title_sort |
regional climate variability driven by foehn winds in the mcmurdo dry valleys, antarctica |
publishDate |
2012 |
url |
https://doi.org/10.1002/joc.3481 |
geographic |
Antarctic The Antarctic Ross Sea McMurdo Dry Valleys |
geographic_facet |
Antarctic The Antarctic Ross Sea McMurdo Dry Valleys |
genre |
Antarc* Antarctic Antarctica McMurdo Dry Valleys Ross Sea |
genre_facet |
Antarc* Antarctic Antarctica McMurdo Dry Valleys Ross Sea |
op_relation |
International Journal of Climatology--Int. J. Climatol.--08998418 articles:21497 ark:/85065/d7wd438p doi:10.1002/joc.3481 |
op_rights |
Copyright 2012 Royal Meteorological Society. |
op_doi |
https://doi.org/10.1002/joc.3481 |
container_title |
International Journal of Climatology |
container_volume |
33 |
container_issue |
4 |
container_start_page |
945 |
op_container_end_page |
958 |
_version_ |
1772821118289182720 |