由于相邻的冰湖泊加快了欧亚大陆的冰盖增长
G Krinner1, J Mangerud, M Jakobsson
1LGGE, CNRS-UJF Grenoble, BP 96, F-38402 Saint Martin d'Hères, France. krinner@ujf-grenoble.fr
Nature
|January 30, 2004
概括
大型欧亚亚洲前冰川湖通过减少冰盖融化,显著降低了区域夏季气候的降温. 这种冷却加速了冰盖的增长和延迟了衰变,影响了过去的气候动态.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 大气科学 大气科学
背景情况:
- 大型前冰期湖泊通过热容量和大气反影响区域气候.
- 约9万年前形成的欧亚大陆的冰湖泊,在最后一个冰川时期阻塞了俄罗斯的河流.
研究的目的:
- 调查欧亚前冰期湖泊对巴伦茨-卡拉冰盖的影响.
- 量化这些湖泊对冰盖融化和区域气候的影响.
主要方法:
- 使用大气一般循环模型的高分辨率模拟.
- 冰盖表面质量平衡的明确模拟.
主要成果:
- 欧亚亚洲的前冰河湖泊导致俄罗斯地区的夏季显著降温.
- 这种降温导致南部边缘的冰盖融化大幅减少.
- 夏季的冷却效应超过了由于湿度降低而降雪的减少.
结论:
- 冰川湖引起的冷却加速了欧亚冰盖的增长,并延迟了衰退.
- 这种机制可能也影响了北美冰盖.
- 冰川前期的湖泊是冰川动态和古气候重建的关键因素.
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