古老的永久土和一个未来,更温暖的北极
Duane G Froese1, John A Westgate, Alberto V Reyes
1Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB T5M 0M3, Canada. duane.froese@ualberta.ca
概括
加拿大的古老的永久土,年龄超过70万年,在过去的温暖时期中幸存下来. 这一发现挑战了气候模型,这些气候模型预测全球变暖导致永久土广泛融化.
科学领域:
- 地球科学 地球科学 地球科学
- 古气候学 古气候学
- 气候科学 气候科学
背景情况:
- 气候模型预测,在全球变暖下,永久土的退化显著,可能会释放大量储存的碳.
- 由于对过去温暖的气候期间永久土的历史行为的理解有限,因此评估这些模型具有挑战性.
研究的目的:
- 调查永久土的长期稳定性及其对过去冰川间变暖事件的弹性.
- 为完善气候模型对永久土对变暖反应的预测提供经验数据.
主要方法:
- 地质调查和分析加拿大亚北极地区的残骸地下冰沉积物.
主要成果:
- 发现了超过70万年历史的残骸地下冰.
- 有证据表明,这种古老的地面冰在过去的多次间冰期中一直存在.
结论:
- 这个地区的永久土表现出比当前气候模型预测的更大的稳定性.
- 过去的温暖的间冰期比现在更长,并没有导致这个古老的地面冰完全融化.
- 这些发现需要重新评估气候变化预测中的永久土碳反机制.
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