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Factors controlling sea salt modification and dry deposition of nonsea-salt components to the ocean
http://hdl.handle.net/2237/23081
http://hdl.handle.net/2237/2308116bff72a-a390-410f-aa5d-0dac10650e67
名前 / ファイル | ライセンス | アクション |
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Kawakami_et_al-2008-Journal_of_Geophysical_Research_Atmospheres_1984-2012.pdf (864.0 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2015-11-04 | |||||
タイトル | ||||||
タイトル | Factors controlling sea salt modification and dry deposition of nonsea-salt components to the ocean | |||||
言語 | en | |||||
著者 |
Kawakami, N.
× Kawakami, N.× Osada, K.× Nishita, C.× Yabuki, M.× Kobayashi, H.× Hara, K.× Shiobara, M. |
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アクセス権 | ||||||
アクセス権 | open access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
権利 | ||||||
言語 | en | |||||
権利情報 | ©2008. American Geophysical Union. | |||||
抄録 | ||||||
内容記述 | [1] Modification of sea salt aerosol particles (SSA particles) by HNO3 and SO2 is an important process for changing phase partitioning of acidic gases from industrial regions to the ocean. During 12–29 September 2005, size-segregated aerosol particles and acidic gases were sampled around the western part of the Japanese Islands to elucidate controlling factors of modification of SSA particles by acidic gases and to estimate dry deposition flux over the ocean. For coarse (>2 μm diameter) SSA particles, the amount of Cl− deficiency from the seawater ratio was comparable to the sum of the equivalent concentrations of NO3− and nonsea-salt (nss) SO42−, suggesting Cl− displacement of SSA particles by acidic gases such as HNO3 and SO2. The Cl− deficiency of SSA particles varied according to the size range and wind speed. Decreasing modification occurred with increasing wind speed for particles of 2–8 μm. Under high (low) wind conditions, the NO3− concentration per unit surface area of coarse SSA particles was lower (higher) for particles >8 μm than for those of 2–8 μm diameter. The respective dry deposition fluxes (Fdry) of NO3−, nss-SO42−, HNO3, and SO2 were estimated according to the wind speed and size of aerosol particles. On average, the Fdry of particulate NO3− was 10 times larger than that of HNO3, but Fdry of nss-SO42− was almost equal to that of SO2. Phase partitioning of dry deposition for NO3− and nss-SO42− over the ocean differs from that of coastal marine areas. | |||||
言語 | en | |||||
内容記述タイプ | Abstract | |||||
出版者 | ||||||
言語 | en | |||||
出版者 | Wiley | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプresource | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | journal article | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
DOI | ||||||
関連タイプ | isVersionOf | |||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.1029/2007JD009410 | |||||
ISSN | ||||||
収録物識別子タイプ | PISSN | |||||
収録物識別子 | 2169-897X | |||||
書誌情報 |
en : Journal of Geophysical Research: Atmospheres 巻 113, 号 D14, p. D14216-D14216, 発行日 2008-07 |
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著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://dx.doi.org/10.1029/2007JD009410 | |||||
識別子タイプ | DOI | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/23081 | |||||
識別子タイプ | HDL |