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南極海の海氷から大気へのブロモホルム放出
https://nipr.repo.nii.ac.jp/records/11683
https://nipr.repo.nii.ac.jp/records/116836906a957-e603-4fc9-9476-a398e2ced613
名前 / ファイル | ライセンス | アクション |
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OM_NomuraDaiki_3.pdf (409.5 kB)
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Item type | 会議発表用資料 / Presentation(1) | |||||
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公開日 | 2016-12-28 | |||||
タイトル | ||||||
タイトル | 南極海の海氷から大気へのブロモホルム放出 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Bromoform emission over the Antarctic sea ice | |||||
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_c94f | |||||
資源タイプ | conference object | |||||
著者 |
野村, 大樹
× 野村, 大樹× 大木, 淳之× G.S., Dieckmann× E., Damm× K., Meiners× 田村, 岳史× Daiki, Nomura× Atsushi, Ooki× Gerhard, S. Dieckmann× Ellen, Damm× Klaus, M. Meiners× Takeshi, Tamura |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Bromoform is one of the volatile organic compounds emitted from the ocean surface to the atmosphere, and it is believed to affect ozone depletion in the atmosphere through photochemical reactions. While estimates of air−sea flux of bromoform are well examined in open ocean areas, fluxes have rarely been estimated in ice-covered seas, and so far, no observations have been made to evaluate the bromoform flux between the sea ice surface and atmosphere. Here, we present the first direct measurements of the air−sea ice bromoform flux obtained from first-year sea ice off east Antarctica. Measurements were made in early austral spring (September to November 2012) as part of the Sea Ice Physics and Ecosystem Experiment II (SIPEX-2). Vertical profiles of bromoform concentrations in snow and sea ice indicated that high concentrations were mainly found in the bottom of the snow and the surface layers of the sea ice (Figure 1) (including slush and brine) ranging from 281−1360 pM. Sea ice–atmosphere bromoform fluxes measured by the chamber method ranged from +0.3 to +7.5 nmol CHBr3 m–2 day–1 (positive value indicates the emission of the bromoform from ice surface to the atmosphere), and flux values increased with increasing bromoform concentrations at the surface layers (Figure 2). The mean flux estimate (+2.4 nmol CHBr3 m–2 day–1) obtained in this study was consistent with the flux estimate for the ice-free part of the Southern Ocean (+2.6 nmol CHBr3 m–2 day–1; Quack and Wallace, 2003). Our results suggest that the bromoform emitted from the sea ice surface to the atmosphere may account for an important fraction of the global bromine budget. | |||||
会議概要(会議名, 開催地, 会期, 主催者等) | ||||||
内容記述タイプ | Other | |||||
内容記述 | 第4回極域科学シンポジウム 個別セッション:[OM] 気水圏 11月14日(木) 統計数理研究所 3階セミナー室1(D305) |
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発表年月日 | ||||||
日付 | 2013-11-14 | |||||
日付タイプ | Issued |