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在最近的变暖期间,泛北极泥地已经扩大.

J Handley1, R E Fewster1,2,3, T G Sim4

  • 1Department of Geography, University of Exeter, Exeter, UK.

Global change biology
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概括

由于气候变暖,北极泥炭地正在迅速扩张,自1950年以来,每年通常超过1米. 这种泥炭地扩张正在进行中,可能是一个泛北极现象,影响碳循环.

关键词:
北极地区的泥炭地.碳 碳 碳 碳 碳 碳环境变化 环境变化横向扩张 横向扩张peatland 泥炭地面积的范围

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科学领域:

  • 地球科学 地球科学 地球科学
  • 气候科学 气候科学
  • 生态生态学 生态生态学

背景情况:

  • 由于气候变化对永久土和碳循环的影响,北极泥炭地中的碳命运是不确定的.
  • 北极泥炭地面积的变化不太清楚,这限制了对陆地碳储存的准确预测.
  • 全北极泥炭地范围的变化可能会显著改变陆地北极碳的命运.

研究的目的:

  • 调查北极泥炭地的横向扩张,以应对最近的变暖.
  • 量化这个泥炭地扩张的速度.
  • 确定泥炭地扩张的区域差异.

主要方法:

  • 收集了来自欧洲和加拿大北极跨度的12个泥炭地站点的数据.
  • 通过14C和210Pb约会限制的年龄深度模型分析了91个泥炭核心.
  • 检查了从泥炭边缘到泥炭中心的泥炭芯,横跨度梯度.

主要成果:

  • 泥炭地已经扩大,一些地点显示自公元1950年以来的扩张速度超过每年1米.
  • 1990年以后,在三分之二 (8/12) 的研究地点观察到新的泥炭形成.
  • 泥炭地扩张正在进行中,很可能是一个泛北极现象,尽管地形等区域因素可能会对其施加约束.

结论:

  • 由于近期的气候变暖,北极泥炭地正在积极扩张.
  • 这种扩张对北极碳循环有重大影响.
  • 需要进一步的研究来估计泛北极泥炭地扩张及其对气候变化的全部影响.