Features of visibility variation at Great Wall Station, Antarctica
The variation of visibility at Great Wall Station (GWS) was analyzed using manual observational data for the period of 1986 to 2012. Results show that the frequencies of occurrence of high (≥10 km) and low visibility (0―1 km) are 61.0% and 8.0%, respectively. Visibility at GWS shows an evident seaso...
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ftarcticportal:oai:generic.eprints.org:2497 2023-10-29T02:29:43+01:00 Features of visibility variation at Great Wall Station, Antarctica Qinghua, Yang Lejiang, Yu Lixin, Wei Benzheng, Zhang Shang, Meng 2013-09 application/pdf http://library.arcticportal.org/2497/ http://library.arcticportal.org/2497/1/A20130308.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2497/1/A20130308.pdf Qinghua, Yang and Lejiang, Yu and Lixin, Wei and Benzheng, Zhang and Shang, Meng (2013) Features of visibility variation at Great Wall Station, Antarctica. Advances in Polar Science, 24 (3). pp. 188-193. Atmosphere Cryosphere Oceans Article PeerReviewed 2013 ftarcticportal 2023-10-04T22:54:12Z The variation of visibility at Great Wall Station (GWS) was analyzed using manual observational data for the period of 1986 to 2012. Results show that the frequencies of occurrence of high (≥10 km) and low visibility (0―1 km) are 61.0% and 8.0%, respectively. Visibility at GWS shows an evident seasonal variation: The highest visibility between November and March, and the lowest visibility from June to October. Sea fog and precipitation are the main factors for low visibility during summer, whereas frequent adverse weather, such as falling snow, blowing snow, or blizzards, are responsible for low visibility in winter. The frequency of occurrence of low visibility has decreased significantly from 1986 to 2012. Conversely, the frequency of occurrence of high visibility has shown a significant increasing trend, especially during winter. The decreasing tendencies of fog, blowing snow, and snowfall have contributed to the increasing trend of high visibility during winter. Visibility at GWS exhibits significant synoptic-scale (2.1 to 8.3 d), annual, and inter-annual periods (2 a, 4.1 a, and 6.9 a to 8.2 a), among which the most significant period is 4.1 a. The visibility observed during 2012 indicates that instrumental observation can be applied in the continuous monitoring of visibility at GWS. Article in Journal/Newspaper Advances in Polar Science Antarc* Antarctica Polar Science Polar Science Arctic Portal Library |
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Arctic Portal Library |
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ftarcticportal |
language |
English |
topic |
Atmosphere Cryosphere Oceans |
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Atmosphere Cryosphere Oceans Qinghua, Yang Lejiang, Yu Lixin, Wei Benzheng, Zhang Shang, Meng Features of visibility variation at Great Wall Station, Antarctica |
topic_facet |
Atmosphere Cryosphere Oceans |
description |
The variation of visibility at Great Wall Station (GWS) was analyzed using manual observational data for the period of 1986 to 2012. Results show that the frequencies of occurrence of high (≥10 km) and low visibility (0―1 km) are 61.0% and 8.0%, respectively. Visibility at GWS shows an evident seasonal variation: The highest visibility between November and March, and the lowest visibility from June to October. Sea fog and precipitation are the main factors for low visibility during summer, whereas frequent adverse weather, such as falling snow, blowing snow, or blizzards, are responsible for low visibility in winter. The frequency of occurrence of low visibility has decreased significantly from 1986 to 2012. Conversely, the frequency of occurrence of high visibility has shown a significant increasing trend, especially during winter. The decreasing tendencies of fog, blowing snow, and snowfall have contributed to the increasing trend of high visibility during winter. Visibility at GWS exhibits significant synoptic-scale (2.1 to 8.3 d), annual, and inter-annual periods (2 a, 4.1 a, and 6.9 a to 8.2 a), among which the most significant period is 4.1 a. The visibility observed during 2012 indicates that instrumental observation can be applied in the continuous monitoring of visibility at GWS. |
format |
Article in Journal/Newspaper |
author |
Qinghua, Yang Lejiang, Yu Lixin, Wei Benzheng, Zhang Shang, Meng |
author_facet |
Qinghua, Yang Lejiang, Yu Lixin, Wei Benzheng, Zhang Shang, Meng |
author_sort |
Qinghua, Yang |
title |
Features of visibility variation at Great Wall Station, Antarctica |
title_short |
Features of visibility variation at Great Wall Station, Antarctica |
title_full |
Features of visibility variation at Great Wall Station, Antarctica |
title_fullStr |
Features of visibility variation at Great Wall Station, Antarctica |
title_full_unstemmed |
Features of visibility variation at Great Wall Station, Antarctica |
title_sort |
features of visibility variation at great wall station, antarctica |
publisher |
Polar Research Institute of China - PRIC |
publishDate |
2013 |
url |
http://library.arcticportal.org/2497/ http://library.arcticportal.org/2497/1/A20130308.pdf |
genre |
Advances in Polar Science Antarc* Antarctica Polar Science Polar Science |
genre_facet |
Advances in Polar Science Antarc* Antarctica Polar Science Polar Science |
op_relation |
http://library.arcticportal.org/2497/1/A20130308.pdf Qinghua, Yang and Lejiang, Yu and Lixin, Wei and Benzheng, Zhang and Shang, Meng (2013) Features of visibility variation at Great Wall Station, Antarctica. Advances in Polar Science, 24 (3). pp. 188-193. |
_version_ |
1781058847360679936 |