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地中海大气循环的区域综合在最后的冰川最大期间
J Kuhlemann1, E J Rohling, I Krumrei
1Institute for Geosciences, University of Tuebingen, Sigwartstrasse 10, D-72076 Tuebingen, Germany. kuhlemann@uni-tuebingen.de
概括
重建过去的大气循环是具有挑战性的. 这项研究揭示了在最后的冰川最大期期间地中海海域放大了冷极空气入侵和的温度梯度,为古代气候动态提供了洞察力.
科学领域:
- 古气候学 古气候学
- 大气科学 大气科学
- 地中海气候研究 地中海气候研究
背景情况:
- 由于地质证据有限,重建过去的大气循环是很困难的.
- 了解过去的大气动态对于理解气候系统变化至关重要.
研究的目的:
- 综合古老代理数据,用于地中海地区大气循环的重建.
- 详细介绍从最后一个冰川最大期到现在的大气循环的三维结构.
主要方法:
- 从海面到阿尔卑斯山高度的古老代理数据的区域综合.
- 对三维大气循环模式的分析.
主要成果:
- 有证据表明,频繁的寒冷极地空气入侵引入了地中海西北部.
- 由于地中海中部的垂直温度梯度导致了局部对流降水的影响.
- 相似的,虽然放大了,LGM循环模式与马恩德最小值相比.
结论:
- 最后的冰川最大期出现了放大大气循环模式,包括显著的冷空气入侵.
- 古老代理数据合成为了解地中海过去大气动态提供了一个强大的框架.
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