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太阳变化和阿曼的季风在9至6千年前之间有很强的连贯性
1Heidelberg Academy of Sciences, Im Neuenheimer Feld 229, Heidelberg, Germany D-69120.
Nature
|May 18, 2001
概括
太阳辐射变化对热带降雨和季风强度在百年到十年的规模上产生了重大影响. 这项研究将太阳活动的变化与阿曼古老的气候变化联系起来,使用石氧同位素.
科学领域:
- 古气候学 古气候学
- 气候科学 气候科学
- 地质化学 地质化学
背景情况:
- 假设太阳辐射变化会影响地球的气候,但它们对千年到十年时间尺度的影响仍然不确定.
- 之前的气候记录显示了与太阳周期的相关性,但绝对太阳强度的变化很小,太阳流动的影响尚未得到充分证实.
- 奥曼的斯塔拉格米特形成提供了过去热带融合区 (ITCZ) 转移的记录.
研究的目的:
- 为了重建过去的热带循环和季风降雨变化,使用高分辨率的石氧同位素记录.
- 为了将氧同位素记录与树环放射性碳数据进行比较,这是太阳活动的代理.
- 调查太阳辐射变化与热带地区百年至十年规模的气候变化之间的关系.
主要方法:
- 在阿曼北部的Th-U日期的岩石中分析氧同位素变化 (delta18O).
- 使用- (Th-U) 方法对石的高分辨率约会.
- 斯塔拉格米特的delta18O记录与来自树环的Delta14C记录的比较.
主要成果:
- 一个高分辨率的氧同位素记录跨越9.6至6.1 kyr之前的现实,从一个阿曼斯塔拉格米特.
- 反映热带循环和季风降雨的delta18O记录与来自树环的Delta14C记录有很好的相关性.
- 这种相关性表明,太阳辐射的变化是热带降雨和季风强度百年至十年规模变化的主要驱动因素.
结论:
- 太阳辐射变化是控制热带降雨和季风强度的一个主要因素,在研究期间 (9.6-6.1 kyr BP) 在百年到十年的时间尺度上.
- 奥曼石石为重建过去的太阳气候联系提供了有价值的代理.
- 这项研究加强了对太阳对区域气候模式的影响的理解.
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