222Rn in the Antarctic Peninsula During 1986
222Rn was continuously measured at the Brazilian Antarctic Station (62 oS, 58 oW) during the year of 1986. Baseline radon concentration averaged 0.02 Bq.m-3 with surges peaking at 0.4 Bq.m-3. The data exhibited a characteristic periodicity of about 25 days and a strong positive association with shor...
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fthighwire:oai:open-archive.highwire.org:rpd:24/1-4/85 2023-05-15T13:48:32+02:00 222Rn in the Antarctic Peninsula During 1986 Pereira, E.B. Setzer, A.W. Cavalcanti, I.F.A. 1988-08-01 00:00:00.0 text/html http://rpd.oxfordjournals.org/cgi/content/short/24/1-4/85 en eng Oxford University Press http://rpd.oxfordjournals.org/cgi/content/short/24/1-4/85 Copyright (C) 1988, Nuclear Technology Publishing Article TEXT 1988 fthighwire 2016-11-16T18:06:58Z 222Rn was continuously measured at the Brazilian Antarctic Station (62 oS, 58 oW) during the year of 1986. Baseline radon concentration averaged 0.02 Bq.m-3 with surges peaking at 0.4 Bq.m-3. The data exhibited a characteristic periodicity of about 25 days and a strong positive association with short term fluctuations of atmospheric temperature. No seasonal variation of radon were observed. Interpretation of the radon surges with reference to synoptic charts and weather satellite pictures showed that the continental influence of radon at the Antarctic Peninsula is very small and comes only from the tip of the South American cone. Text Antarc* Antarctic Antarctic Peninsula HighWire Press (Stanford University) Antarctic Antarctic Peninsula The Antarctic |
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HighWire Press (Stanford University) |
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fthighwire |
language |
English |
topic |
Article |
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Article Pereira, E.B. Setzer, A.W. Cavalcanti, I.F.A. 222Rn in the Antarctic Peninsula During 1986 |
topic_facet |
Article |
description |
222Rn was continuously measured at the Brazilian Antarctic Station (62 oS, 58 oW) during the year of 1986. Baseline radon concentration averaged 0.02 Bq.m-3 with surges peaking at 0.4 Bq.m-3. The data exhibited a characteristic periodicity of about 25 days and a strong positive association with short term fluctuations of atmospheric temperature. No seasonal variation of radon were observed. Interpretation of the radon surges with reference to synoptic charts and weather satellite pictures showed that the continental influence of radon at the Antarctic Peninsula is very small and comes only from the tip of the South American cone. |
format |
Text |
author |
Pereira, E.B. Setzer, A.W. Cavalcanti, I.F.A. |
author_facet |
Pereira, E.B. Setzer, A.W. Cavalcanti, I.F.A. |
author_sort |
Pereira, E.B. |
title |
222Rn in the Antarctic Peninsula During 1986 |
title_short |
222Rn in the Antarctic Peninsula During 1986 |
title_full |
222Rn in the Antarctic Peninsula During 1986 |
title_fullStr |
222Rn in the Antarctic Peninsula During 1986 |
title_full_unstemmed |
222Rn in the Antarctic Peninsula During 1986 |
title_sort |
222rn in the antarctic peninsula during 1986 |
publisher |
Oxford University Press |
publishDate |
1988 |
url |
http://rpd.oxfordjournals.org/cgi/content/short/24/1-4/85 |
geographic |
Antarctic Antarctic Peninsula The Antarctic |
geographic_facet |
Antarctic Antarctic Peninsula The Antarctic |
genre |
Antarc* Antarctic Antarctic Peninsula |
genre_facet |
Antarc* Antarctic Antarctic Peninsula |
op_relation |
http://rpd.oxfordjournals.org/cgi/content/short/24/1-4/85 |
op_rights |
Copyright (C) 1988, Nuclear Technology Publishing |
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1766249407378882560 |