冰川的影响限制了山的高度
D L Egholm1, S B Nielsen, V K Pedersen
1Department of Earth Sciences, Aarhus University, DK-8000 Aarhus, Denmark. david@geo.au.dk
Nature
|August 14, 2009
概括
山脉的高度主要是由气候控制的,而不是构造力. 冰川侵蚀和静态升起,由气候影响的雪线驱动,决定了山脉的最大高度.
科学领域:
- 地球科学 地球科学 地球科学
- 地质地质地质地质地质地
- 气候学 气候学 气候学
背景情况:
- 山脉的高度是由于构造上升,地强度和表面剥光之间的平衡造成的.
- 构造变形,排泄和气候之间的相互作用是科学辩论的关键领域.
- 气候,特别是降雨和冰川,影响了排泄率和山地地形.
研究的目的:
- 研究气候,特别是雪线高度与全球山脉的最大高度之间的关系.
- 为了测试冰川侵蚀通过"冰川"机制影响山脉高度的假设.
- 要确定气候或构造力是否是控制山脉高度的主导因素.
主要方法:
- 对地形数据的全球分析.
- 在最大山峰高度和气候控制的雪线高度梯度之间的相关性分析.
- 数字建模以模拟侵蚀和静态过程.
主要成果:
- 在多种山脉的最大山高度和气候控制的雪线高度梯度之间发现了强烈的相关性.
- 数字模型表明,冰川在雪线以上的侵蚀和随后的静态升起可以将山脉的高度推向雪线以下的窗口.
- 该模型成功地复制了与冰川刀机制相关的低度特征.
结论:
- 气候,通过冰川和其对脱皮和静止的影响,是最大山脉高度的主要驱动因素.
- 与气候相比,构造力在确定山脉的最终高度方面发挥的作用较小.
- "冰川"是一种有效的机制,塑造了山脉的地形,并限制了最大的高度.
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