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  Modelling terrestrial vegetation dynamics and carbon cycling for an abrupt climatic change event

Scholze, M., Knorr, W., & Heimann, M. (2003). Modelling terrestrial vegetation dynamics and carbon cycling for an abrupt climatic change event. The Holocene, 13(3), 327-333. doi:10.1191/0959683603hl625rp.

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資料種別: 学術論文

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BGC0638.pdf (出版社版), 511KB
 
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 作成者:
Scholze, M., 著者
Knorr, W.1, 著者           
Heimann, M.2, 著者           
所属:
1Department Biogeochemical Synthesis, Prof. C. Prentice, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497753              
2Department Biogeochemical Systems, Prof. M. Heimann, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497755              

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キーワード: Younger Dryas; modelling; vegetation dynamics; terrestrial biosphere; carbon cycle; abrupt climatic change Younger dryas event; north-atlantic; atmospheric CO2; ocean; circulation; enrichment; increase; storage; record; system
 要旨: Abrupt climatic changes have occurred several times in the past, leading to large-scale modifications of vegetation patterns with important consequences for the global carbon cycle. Dynamic global vegetation models (DGVM) constitute an advanced tool for reconstructing past or predicting future shifts in vegetation distributions in response to climatic change on a global scale. The Land-Potsdam-Jena (LPJ) model is a DGVM that also includes a complete description of terrestrial-vegetation carbon cycling. Here, it is used for a longtime integration simulating terrestrial ecosystem responses to an abrupt climatic change event. Climate data from an 850- year-long coupled ocean-atmosphere model (ECHAM3/LSG) experiment representing a highly idealized Younger Dryas (c. 12 ka BP) like event are used to study the reactions of the vegetation distribution and changes in terrestrial carbon storage. The main feature of the Younger Dryas simulation experiment is the suppression of the Atlantic thermohaline circulation leading to a significant cooling of the Northern Hemisphere accompanied by a large-scale precipitation decrease. The simulation exhibits a significant shift of the vegetation distribution in the Northern Hemisphere during the cold period in conjunction with a change in global total terrestrial carbon stocks of 180 x 10(12) kg C as a consequence of the climatic change event. The response time of the terrestrial biosphere lags the climatic changes by about 250 years for vegetation and 400 years for soil-carbon pools.

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 日付: 2003
 出版の状態: 出版
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 識別子(DOI, ISBNなど): その他: BGC0638
DOI: 10.1191/0959683603hl625rp
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出版物 1

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出版物名: The Holocene
種別: 学術雑誌
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出版社, 出版地: Los Angeles, CA : Sage Publications
ページ: - 巻号: 13 (3) 通巻号: - 開始・終了ページ: 327 - 333 識別子(ISBN, ISSN, DOIなど): ISSN: 1477-0911
CoNE: https://pure.mpg.de/cone/journals/resource/954925578075_1