The coreless winter at Scott Base, Antarctica
Abstract The temporary early‐winter reversal of the downward trend in monthly mean surface air temperatures, which has been noted for other stations in the Ross Sea – South Pole region, is a particularly marked and persistent feature at Scott Base. An examination of temperature records shows that th...
Published in: | Quarterly Journal of the Royal Meteorological Society |
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Wiley
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crwiley:10.1002/qj.49709540413 2024-06-02T07:58:07+00:00 The coreless winter at Scott Base, Antarctica Thompson, D. C. 1969 http://dx.doi.org/10.1002/qj.49709540413 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49709540413 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49709540413 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 95, issue 404, page 404-407 ISSN 0035-9009 1477-870X journal-article 1969 crwiley https://doi.org/10.1002/qj.49709540413 2024-05-03T11:27:24Z Abstract The temporary early‐winter reversal of the downward trend in monthly mean surface air temperatures, which has been noted for other stations in the Ross Sea – South Pole region, is a particularly marked and persistent feature at Scott Base. An examination of temperature records shows that this reversal in the trend is probably due to a more frequent destruction of the low‐level surface inversion in these months, rather than a temporary increase in the level of warm air advection into the region. Article in Journal/Newspaper Antarc* Antarctica Ross Sea South pole South pole Wiley Online Library Ross Sea South Pole Scott Base ENVELOPE(166.766,166.766,-77.849,-77.849) Quarterly Journal of the Royal Meteorological Society 95 404 404 407 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract The temporary early‐winter reversal of the downward trend in monthly mean surface air temperatures, which has been noted for other stations in the Ross Sea – South Pole region, is a particularly marked and persistent feature at Scott Base. An examination of temperature records shows that this reversal in the trend is probably due to a more frequent destruction of the low‐level surface inversion in these months, rather than a temporary increase in the level of warm air advection into the region. |
format |
Article in Journal/Newspaper |
author |
Thompson, D. C. |
spellingShingle |
Thompson, D. C. The coreless winter at Scott Base, Antarctica |
author_facet |
Thompson, D. C. |
author_sort |
Thompson, D. C. |
title |
The coreless winter at Scott Base, Antarctica |
title_short |
The coreless winter at Scott Base, Antarctica |
title_full |
The coreless winter at Scott Base, Antarctica |
title_fullStr |
The coreless winter at Scott Base, Antarctica |
title_full_unstemmed |
The coreless winter at Scott Base, Antarctica |
title_sort |
coreless winter at scott base, antarctica |
publisher |
Wiley |
publishDate |
1969 |
url |
http://dx.doi.org/10.1002/qj.49709540413 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49709540413 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49709540413 |
long_lat |
ENVELOPE(166.766,166.766,-77.849,-77.849) |
geographic |
Ross Sea South Pole Scott Base |
geographic_facet |
Ross Sea South Pole Scott Base |
genre |
Antarc* Antarctica Ross Sea South pole South pole |
genre_facet |
Antarc* Antarctica Ross Sea South pole South pole |
op_source |
Quarterly Journal of the Royal Meteorological Society volume 95, issue 404, page 404-407 ISSN 0035-9009 1477-870X |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/qj.49709540413 |
container_title |
Quarterly Journal of the Royal Meteorological Society |
container_volume |
95 |
container_issue |
404 |
container_start_page |
404 |
op_container_end_page |
407 |
_version_ |
1800741386821042176 |