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  NW European shelf under climate warming: implications for open ocean – shelf exchange, primary production, and carbon absorption

Groeger, M., Maier-Reimer, E., Mikolajewicz, U., Moll, A., & Sein, D. (2013). NW European shelf under climate warming: implications for open ocean – shelf exchange, primary production, and carbon absorption. Biogeosciences, 10, 3767-3792. doi:10.5194/bg-10-3767-2013.

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資料種別: 学術論文

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bg-10-3767-2013.pdf (出版社版), 10MB
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https://hdl.handle.net/11858/00-001M-0000-0013-AED2-A
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bg-10-3767-2013.pdf
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Final Revised Paper
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bg-10-3767-2013-supplement.zip (付録資料), 2MB
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https://hdl.handle.net/11858/00-001M-0000-0013-AEDB-7
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bg-10-3767-2013-supplement.zip
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 作成者:
Groeger, Matthias1, 著者           
Maier-Reimer, Ernst1, 著者           
Mikolajewicz, Uwe2, 著者           
Moll, Andreas, 著者
Sein, Dmitry3, 著者           
所属:
1Ocean Biogeochemistry, The Ocean in the Earth System, MPI for Meteorology, Max Planck Society, ou_913556              
2Ocean Physics, The Ocean in the Earth System, MPI for Meteorology, Max Planck Society, ou_913557              
3Climate Modelling, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_913569              

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 要旨: Shelves have been estimated to account for more than one-fifth of the global marine primary production. It has been also conjectured that shelves strongly influence the oceanic absorption of anthropogenic CO2 (carbon shelf pump). Owing to their coarse resolution, currently applied global climate models are inappropriate to investigate the impact of climate change on shelves and regional models do not account for the complex interaction with the adjacent open ocean. In this study, a global ocean general circulation model and biogeochemistry model were set up with a distorted grid providing a maximal resolution for the NW European shelf and the adjacent northeast Atlantic. Using model climate projections we found that already a~moderate warming of about 2.0 K of the sea surface is linked with a reduction by ~ 30% of the biological production on the NW European shelf. If we consider the decline of anthropogenic riverine eutrophication since the 1990s, the reduction of biological production amounts is even larger. The relative decline of NW European shelf productivity is twice as strong as the decline in the open ocean (~ 15%). The underlying mechanism is a spatially well confined stratification feedback along the continental shelf break. This feedback reduces the nutrient supply from the deep Atlantic to about 50%. In turn, the reduced productivity draws down CO2 absorption in the North Sea by ~ 34% at the end of the 21st century compared to the end of the 20th century implying a strong weakening of shelf carbon pumping. Sensitivity experiments with diagnostic tracers indicate that not more than 20% of the carbon absorbed in the North Sea contributes to the long-term carbon uptake of the world ocean. The rest remains within the ocean's mixed layer where it is exposed to the atmosphere. The predicted decline in biological productivity, and decrease of phytoplankton concentration (in the North Sea by averaged 25%) due to reduced nutrient imports from the deeper Atlantic will probably affect the local fish stock negatively and therefore fisheries in the North Sea.

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言語: eng - English
 日付: 2013-06-122013-06-12
 出版の状態: 出版
 ページ: -
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 目次: -
 査読: 査読あり
 識別子(DOI, ISBNなど): DOI: 10.5194/bg-10-3767-2013
 学位: -

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出版物 1

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出版物名: Biogeosciences
  その他 : Biogeosciences
種別: 学術雑誌
 著者・編者:
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出版社, 出版地: Katlenburg-Lindau, Germany : Copernicus GmbH on behalf of the European Geosciences Union
ページ: - 巻号: 10 通巻号: - 開始・終了ページ: 3767 - 3792 識別子(ISBN, ISSN, DOIなど): ISSN: 1726-4170
CoNE: https://pure.mpg.de/cone/journals/resource/111087929276006