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Calanus finmarchicus abundance, production and population dynamics in the Barents Sea in a future climate

机译:未来气候下巴伦支海的海螯虾的丰度,产量和种群动态

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摘要

Even though change in marine ecosystems due to global warming has been documented in numerous studies, the nature of change for key ecosystem components is often poorly understood. The Barents Sea is an area where strong climate changes are expected to occur, and since the area is also intensively exploited commercially, it is of particular interest to predict how primary and secondary producers which transfer energy to higher trophic levels will be affected. In the present study we have used a model approach where an individual based model that simulate the life history of Calanus finmarchicus is two-way linked to a coupled biogeochemical and ocean circulation model. Using the IPCC 20C3M control run and the A1B emission scenario, a downscaling of the GISS-AOM global climate model has been used to force the ecosystem model for a reference (1981-1999) and a future climate (2046-2064) simulation respectively. The predicted annual primary production under the future climate scenario was on average 106 g C m~(-2) y~(-1) implying a 36% increase from the reference scenario. The strongest increases occurred in the northern and eastern parts of the Barents Sea likely induced by a strong reduction in ice coverage. C. finmarchicus production also increased, but less (23%) and largely in southern and western areas where production was already high under the reference climate scenario. As a consequence, the proportion of the Barents Sea assumed to have C. finmarchicus concentrations high enough to sustain fish larval growth did not increase substantially. The results suggest that C. finmarchicus most likely are unable to take full advantage of the predicted increased Barents Sea primary production in the future, possibly due to too low temperature and a mis-match between the development and spawning of C. finmarchicus and the early primary production peak in Arctic waters. The proportion of C. finmarchicus with local overwintering and reproduction in the Barents Sea versus those adverted in from the Norwegian Sea remained unchanged at ~75%.
机译:尽管在许多研究中都记录了由于全球变暖引起的海洋生态系统变化,但人们对人们对生态系统关键组成部分的变化本质却知之甚少。巴伦支海是一个预计将发生强烈气候变化的地区,并且由于该地区也已被大量开发利用,因此特别有必要预测将能量转移到较高营养水平的初级和次级生产者将受到的影响。在本研究中,我们使用了一种模型方法,其中基于个体的模型来模拟finmarchicus的生活史,并与耦合的生物地球化学和海洋环流模型双向关联。使用IPCC 20C3M控制运行和A1B排放情景,已将GISS-AOM全球气候模型的缩减规模分别用于强迫该生态系统模型进行参考(1981-1999)和未来气候(2046-2064)模拟。在未来气候情景下,预计的年初级生产量平均为106 g C m〜(-2)y〜(-1),比参考情景增加了36%。最强烈的增加发生在巴伦支海的北部和东部,这可能是由于冰覆盖面积的大幅减少所致。 finmarchicus的产量也有所增加,但增幅较小(23%),并且大部分在南部和西部地区,在参考气候情景下,该地区的产量已经很高。结果,假定巴伦支海中的芬克梭菌浓度足以维持鱼类幼体生长的比例没有实质性增加。结果表明,C。finmarchicus最有可能无法充分利用未来巴伦支海初级产量预测的增长,这可能是由于温度太低以及C. finmarchicus的发育和产卵与早期产卵之间的不匹配所致。北极水域的初级生产高峰。在巴伦支海中局部越冬和繁殖的芬氏梭菌与从挪威海中转移过来的隐孢子虫的比例保持在〜75%。

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  • 来源
    《Progress in Oceanography》 |2014年第6期|26-39|共14页
  • 作者单位

    Institute of Marine Research, PO Box 1870, Nordnes, N-5817 Bergen, Norway;

    Institute of Marine Research, PO Box 1870, Nordnes, N-5817 Bergen, Norway;

    Institute of Marine Research, PO Box 1870, Nordnes, N-5817 Bergen, Norway,Bjerknes Centre for Climate Research, Allegt. 55, N-5007 Bergen, Norway;

    Institute of Marine Research, PO Box 1870, Nordnes, N-5817 Bergen, Norway,Bjerknes Centre for Climate Research, Allegt. 55, N-5007 Bergen, Norway;

    Institute of Marine Research, PO Box 1870, Nordnes, N-5817 Bergen, Norway;

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