Concentration and Size Distribution of Fungi Aerosol over Oceans along a Cruise Path during the Fourth Chinese Arctic Research Expedition
Bioaerosol can act as nuclei and thus may play an important role in climate change. During the Fourth Chinese National Arctic Research Expedition (CHINARE 2010) from July to September 2010, the concentrations and size distributions of airborne fungi, which are thought to be one of important bioaeros...
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ftmdpi:oai:mdpi.com:/2073-4433/4/4/337/ 2023-08-20T04:03:52+02:00 Concentration and Size Distribution of Fungi Aerosol over Oceans along a Cruise Path during the Fourth Chinese Arctic Research Expedition Juan Yu Qihou Hu Zhouqing Xie Hui Kang Ming Li Zheng Li Peipei Ye agris 2013-11-05 application/pdf https://doi.org/10.3390/atmos4040337 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/atmos4040337 https://creativecommons.org/licenses/by/3.0/ Atmosphere; Volume 4; Issue 4; Pages: 337-348 fungi concentration size distribution marine boundary layer the Arctic Ocean Text 2013 ftmdpi https://doi.org/10.3390/atmos4040337 2023-07-31T20:34:37Z Bioaerosol can act as nuclei and thus may play an important role in climate change. During the Fourth Chinese National Arctic Research Expedition (CHINARE 2010) from July to September 2010, the concentrations and size distributions of airborne fungi, which are thought to be one of important bioaerosols, in the marine boundary layer were investigated. The concentrations of airborne fungi varied considerably with a range of 0 to 320.4 CFU/m3. The fungal concentrations in the marine boundary layer were significantly lower than those in most continental ecosystems. Airborne fungi over oceans roughly displayed a decreasing trend with increasing latitudes. The mean concentrations of airborne fungi in the region of offshore China, the western North Pacific Ocean, the Chukchi Sea, the Canada Basin, and the central Arctic Ocean were 172.2 ± 158.4, 73.8 ± 104.4, 13.3 ± 16.2, 16.5 ± 8.0, and 1.2 ± 1.0 CFU/m3, respectively. In most areas airborne fungi showed a unimodal size distribution pattern, with the maximum proportion (about 36.2%) in the range of 2.1~3.3 µm and the minimum proportion (about 3.5%) in the range of 0.65~1.1 µm, and over 50% occurred on the fine size (<3.3 µm). Potential factors influencing airborne fungal concentrations, including the origin of air mass, meteorological conditions, and sea ice conditions, were discussed. Text Arctic Arctic Ocean canada basin Central Arctic Chukchi Chukchi Sea Climate change Sea ice MDPI Open Access Publishing Arctic Arctic Ocean Chukchi Sea Canada Pacific Atmosphere 4 4 337 348 |
institution |
Open Polar |
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MDPI Open Access Publishing |
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ftmdpi |
language |
English |
topic |
fungi concentration size distribution marine boundary layer the Arctic Ocean |
spellingShingle |
fungi concentration size distribution marine boundary layer the Arctic Ocean Juan Yu Qihou Hu Zhouqing Xie Hui Kang Ming Li Zheng Li Peipei Ye Concentration and Size Distribution of Fungi Aerosol over Oceans along a Cruise Path during the Fourth Chinese Arctic Research Expedition |
topic_facet |
fungi concentration size distribution marine boundary layer the Arctic Ocean |
description |
Bioaerosol can act as nuclei and thus may play an important role in climate change. During the Fourth Chinese National Arctic Research Expedition (CHINARE 2010) from July to September 2010, the concentrations and size distributions of airborne fungi, which are thought to be one of important bioaerosols, in the marine boundary layer were investigated. The concentrations of airborne fungi varied considerably with a range of 0 to 320.4 CFU/m3. The fungal concentrations in the marine boundary layer were significantly lower than those in most continental ecosystems. Airborne fungi over oceans roughly displayed a decreasing trend with increasing latitudes. The mean concentrations of airborne fungi in the region of offshore China, the western North Pacific Ocean, the Chukchi Sea, the Canada Basin, and the central Arctic Ocean were 172.2 ± 158.4, 73.8 ± 104.4, 13.3 ± 16.2, 16.5 ± 8.0, and 1.2 ± 1.0 CFU/m3, respectively. In most areas airborne fungi showed a unimodal size distribution pattern, with the maximum proportion (about 36.2%) in the range of 2.1~3.3 µm and the minimum proportion (about 3.5%) in the range of 0.65~1.1 µm, and over 50% occurred on the fine size (<3.3 µm). Potential factors influencing airborne fungal concentrations, including the origin of air mass, meteorological conditions, and sea ice conditions, were discussed. |
format |
Text |
author |
Juan Yu Qihou Hu Zhouqing Xie Hui Kang Ming Li Zheng Li Peipei Ye |
author_facet |
Juan Yu Qihou Hu Zhouqing Xie Hui Kang Ming Li Zheng Li Peipei Ye |
author_sort |
Juan Yu |
title |
Concentration and Size Distribution of Fungi Aerosol over Oceans along a Cruise Path during the Fourth Chinese Arctic Research Expedition |
title_short |
Concentration and Size Distribution of Fungi Aerosol over Oceans along a Cruise Path during the Fourth Chinese Arctic Research Expedition |
title_full |
Concentration and Size Distribution of Fungi Aerosol over Oceans along a Cruise Path during the Fourth Chinese Arctic Research Expedition |
title_fullStr |
Concentration and Size Distribution of Fungi Aerosol over Oceans along a Cruise Path during the Fourth Chinese Arctic Research Expedition |
title_full_unstemmed |
Concentration and Size Distribution of Fungi Aerosol over Oceans along a Cruise Path during the Fourth Chinese Arctic Research Expedition |
title_sort |
concentration and size distribution of fungi aerosol over oceans along a cruise path during the fourth chinese arctic research expedition |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2013 |
url |
https://doi.org/10.3390/atmos4040337 |
op_coverage |
agris |
geographic |
Arctic Arctic Ocean Chukchi Sea Canada Pacific |
geographic_facet |
Arctic Arctic Ocean Chukchi Sea Canada Pacific |
genre |
Arctic Arctic Ocean canada basin Central Arctic Chukchi Chukchi Sea Climate change Sea ice |
genre_facet |
Arctic Arctic Ocean canada basin Central Arctic Chukchi Chukchi Sea Climate change Sea ice |
op_source |
Atmosphere; Volume 4; Issue 4; Pages: 337-348 |
op_relation |
https://dx.doi.org/10.3390/atmos4040337 |
op_rights |
https://creativecommons.org/licenses/by/3.0/ |
op_doi |
https://doi.org/10.3390/atmos4040337 |
container_title |
Atmosphere |
container_volume |
4 |
container_issue |
4 |
container_start_page |
337 |
op_container_end_page |
348 |
_version_ |
1774714296382521344 |