对"全球变暖导致的土壤碳流"的评论的回应
Caitlin E Hicks Pries1,2, C Castanha3, R Porras3
1Climate Sciences Department, Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, MS 74R316C, Berkeley, CA 94720, USA. caitlin.e.h.pries@dartmouth.edu mstorn@lbl.gov.
概括
深层土壤和表面土壤的温度是相同的, 我们的分析证实土壤深度对变暖的反应,
科学领域:
- 土壤科学
- 气候变化研究
- 地质学
背景情况:
- 最近的研究已经讨论了深层土壤因气候变化而变暖的速度.
- 了解土壤热力学对于预测碳循环反至关重要.
研究的目的:
- 解决有关土壤变暖速度和Q10分析的批评.
- 为了证明深层土壤与表面土壤相比温暖.
主要方法:
- 对温度记录和模型预测的分析.
- 在Q10分析中包含所有数据点以验证结果.
主要成果:
- 温度记录和模型预测显示深层土壤和表面土壤的温度是相同的.
- 在包括所有数据的情况下,整个土壤概况中的Q10值始终超过2.
结论:
- 所有的土壤深度都表现出对变暖的反应.
- 这些发现驳斥了表面土壤和深层土壤之间的变暖速度差异的说法.
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