Item type |
学術雑誌論文 / Journal Article(1) |
公開日 |
2022-05-20 |
タイトル |
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タイトル |
Long-term changes in aerosol radiative properties over Ny-Ålesund: Results from Indian scientific expeditions to the Arctic |
タイトル |
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言語 |
en |
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タイトル |
Long-term changes in aerosol radiative properties over Ny-Ålesund: Results from Indian scientific expeditions to the Arctic |
言語 |
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言語 |
eng |
キーワード |
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言語 |
en |
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主題Scheme |
Other |
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主題 |
Black carbon |
キーワード |
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言語 |
en |
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主題Scheme |
Other |
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主題 |
Aerosol scattering coefficient |
キーワード |
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言語 |
en |
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主題Scheme |
Other |
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主題 |
Single scattering albedo |
キーワード |
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言語 |
en |
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主題Scheme |
Other |
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主題 |
Aerosol size distribution |
キーワード |
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言語 |
en |
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主題Scheme |
Other |
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主題 |
Aerosol chemical composition |
キーワード |
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言語 |
en |
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主題Scheme |
Other |
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主題 |
Radiative forcing |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
journal article |
アクセス権 |
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アクセス権 |
metadata only access |
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アクセス権URI |
http://purl.org/coar/access_right/c_14cb |
著者 |
Gogoi, Mukunda M.
Pandey, Santosh K.
Arun, B.S.
Nair, Vijayakumar S.
Thakur, Roseline C.
Chaubey, Jai Prakash
Tiwari, Anoop
Manoj, M.R.
Kompalli, Sobhan Kumar
Vaishya, Aditya
Prijith, S.S.
Hegde, Prashant
Babu, S. Suresh
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抄録 |
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内容記述タイプ |
Abstract |
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内容記述 |
Continuous long-term monitoring of black carbon (BC) mass concentration and aerosol light scattering coefficient (σSCA), supplemented by number size distribution and chemical composition, are utilized in this study to understand the temporal changes in aerosol properties, associated source processes and radiative effects at Ny-Ålesund (79 oN) in the Svalbard Archipelago. A statistically significant decreasing trend in BC (- 24.7 ng m−3 decade−1) is observed during spring of 2010–2019. In contrast, σSCA depicted a general increasing trend (5.2 Mm−1 decade−1) during 2011–2016. BC and σSCA were higher during winter and spring. Aerosol single scattering albedo was highest in May ~ 0.95 (during spring) and lowest in September ~ 0.87 (during summer). Fractional share of BC to total aerosol mass was higher in winter and summer. Anthropogenic SO42− and NO3− (after ssNa+) species dominated the summer, when total number and mass concentrations of aerosols were at their minimum. Elemental Carbon (EC) and Organic Carbon (OC) showed higher concentrations in spring with EC-to-OC ratio ~ 0.08 - 0.22. The columnar AOD varied between 0.01 and 0.20 (annual mean ~ 0.09), resulting in aerosol radiative forcing (in the top of the atmosphere) ~ 0.15 - 2.69 Wm-2 in the month of April (during spring). Potential source contribution function (PSCF) revealed the dominant source areas to be over Europe and Russia in terms of contributing to the seasonal high BC mass concentrations at Ny-Ålesund. Our study has also revealed an unusual impact of biomass burning aerosols (advected from the Alaska wildfire) during July 2015. |
書誌情報 |
en : Polar Science
巻 30,
p. 100700,
発行日 2021-12
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ISSN |
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収録物識別子タイプ |
ISSN |
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収録物識別子 |
18739652 |
DOI |
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識別子タイプ |
DOI |
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関連識別子 |
https://doi.org/10.1016/j.polar.2021.100700 |
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関連名称 |
10.1016/j.polar.2021.100700 |