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SIZE DISTRIBUTION OF AEROSOLS AT BARROW IN ALASKA : A CASE STUDY IN SPRING
https://doi.org/10.15094/00002865
https://doi.org/10.15094/00002865a7c9510a-725f-4c8d-8313-5902403295aa
名前 / ファイル | ライセンス | アクション |
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KJ00002364375 (1.1 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1998-11-01 | |||||
タイトル | ||||||
タイトル | SIZE DISTRIBUTION OF AEROSOLS AT BARROW IN ALASKA : A CASE STUDY IN SPRING | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002865 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | SIZE DISTRIBUTION OF AEROSOLS AT BARROW IN ALASKA : A CASE STUDY IN SPRING | |||||
著者名よみ |
ザイゼン, ユウジ
× ザイゼン, ユウジ× オカダ, キクオ× イケガミ, ミワコ× アオキ, テルオ× サワ, ヨウスケ× ニシオ, フミヒコ× タチバナ, ヨシヒロ |
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著者名(英) |
ZAIZEN, Yuji
× ZAIZEN, Yuji× OKADA, Kikuo× IKEGAMI, Miwako× AOKI, Teruo× SAWA, Yousuke× NISHIO, Fumihiko× TACHIBANA, Yoshihiro |
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著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Hokkaido University of Education | ||||||
著者所属(英) | ||||||
en | ||||||
Research Institute of Civilization, Tokai University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Concentration, size distribution and morphological features of aerosol particles were observed at Barrow in Alaska during the period 13-28 April 1997 together with concentrations of gaseous species (SO_2,NO and NO_2). The concentrations of gaseous species were less than 50 pptv except for locally polluted air. Aerosol size distributions suggested the occurrence of new particle formation from the gas phase in spite of very low concentrations of gaseous species, especially in the air mass from lower latitudes during the latter part of the observational period. In the air mass from higher latitudes, new particle formation was assumed to be not active. The largest maximum was found at 0.1-0.2μm radius in most of the observation periods, suggesting that the size distributions have been influenced by wellaged particles. The dominant component of aerosol particles in this size range is considered to be sulfate-containing particles. Another maximum was found occasionally at 0.02-0.05μm radius. This kind of air mass was possibly influenced by air from lower latitudes. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1129795X | |||||
書誌情報 |
Polar meteorology and glaciology 巻 12, p. 40-48, 発行日 1998-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |