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来自西伯利亚融湖的甲泡,作为气候变暖的积极反
K M Walter1, S A Zimov, J P Chanton
1Institute of Arctic Biology, University of Alaska Fairbanks, Alaska 99775, USA. ftkmw1@uaf.edu
Nature
|September 8, 2006
概括
西伯利亚融化湖泊的甲排放量高于此前的预期,原因是永久土的泡和融化. 这一发现显著影响了气候变化预测,因为它揭示了大量的古代碳排放.
科学领域:
- 环境科学 环境科学
- 气候科学 气候科学
- 地质化学 地质化学
背景情况:
- 大气中的甲是一种强大的温室气体,其不确定的排放预算会影响气候预测.
- 北西伯利亚的融化湖是已知的甲来源,但通过沸 (泡) 量化排放是具有挑战性的,因为它的变化.
研究的目的:
- 量化北西伯利亚解湖的甲排放量,使用一种新的沸测量方法.
- 评估沸对甲总流量的贡献及其对区域和全球预算的影响.
主要方法:
- 开发和应用一种新的方法来测量融化湖中的甲沸.
- 在北西伯利亚的两个融化湖中实地测量了甲流量.
- 对甲年龄的分析,以确定碳来源.
主要成果:
- 沸占研究的融化湖的甲排放量的95%.
- 估计这些湖泊的甲流量比以前报告的高出五倍.
- 北西伯利亚的融湖每年可能会排放3.8千克的甲,使目前北方湿地的估计增加10-63%.
结论:
- 湖边的永久土融化是这些湖泊释放的甲的主要来源.
- 解湖扩张 (1974-2000年) 与变暖相关,区域甲排放量增加了58%.
- 从永久土解中释放的古代碳 (普世时代的甲) 代表了气候变暖的显著积极反.
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