在刚果中部的泥炭地模拟碳的积累和损失
Dylan M Young1, Andy J Baird1, Paul J Morris1
1School of Geography, University of Leeds, Leeds, UK.
Global change biology
|October 10, 2023
概括
热带泥炭地储存了大量的碳. 一个新的模型显示了表面湿度和缓慢的衰变控制积累,但干燥可以导致灾难性的碳损失,突出了对气候变化的脆弱性.
科学领域:
- 地球和环境科学 地球和环境科学
- 气候科学 气候科学
- 生态生态学 生态生态学
背景情况:
- 刚果中部盆地的泥炭地储存了大约29亿的碳.
- 了解泥炭碳动态和气候变化脆弱性是有限的.
研究的目的:
- 为了模拟热带泥炭地中的泥炭积累和损失.
- 确定泥炭地碳动态的关键控制.
- 评估泥炭碳储存对气候变化的脆弱性.
主要方法:
- 开发DigiBog_Congo模型用于热带泥炭地模拟.
- 模拟了超过20,000年的泥炭碳积累和损失.
- 模型年龄深度曲线与古老环境重建的比较.
主要成果:
- 模型模拟与古老环境数据保持一致.
- 表面湿度和缓慢的无氧衰变是泥炭积累的主要控制因素.
- 几千年来,大约在公元前5200年的干燥阶段导致了显著的碳损失 (57%的库存).
结论:
- 仅仅是降雨的变化就可能引发灾难性的长期泥炭碳损失.
- 热带泥炭地极易受到气候变化引起的干旱影响.
- 该模型为评估未来气候和土地利用对泥炭的影响提供了一个框架.
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