新西兰高频的全新纪冰川波动与北方的特征不同
Joerg M Schaefer1, George H Denton, Michael Kaplan
1Geochemistry, Lamont-Doherty Earth Observatory (LDEO), Palisades, NY 10964, USA. schaefer@ldeo.columbia.edu
概括
新西兰的全新纪冰川波动.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 气候科学 气候科学
背景情况:
- 在全新世纪期间半球间气候变化的时间和原因尚不清楚.
- 重建过去的气候动态需要高分辨率的古气候记录.
研究的目的:
- 为了研究新西兰南部阿尔卑斯山的Holocene冰川波动.
- 建立这些事件的高分辨率时间表.
- 了解这些气候变化的驱动因素.
主要方法:
- 高分辨率-10 (10Be) 时间表.
- 对过去7000年的冰川波动进行分析.
- 与北半球气候模式的比较.
主要成果:
- 在过去的千年里,至少发生了五次冰川前进事件.
- 冰川的延伸从中期到晚期的全新纪减少了.
- 新西兰冰川的进步与北半球温暖时期相吻合.
结论:
- 新西兰的全新纪冰川动态与北半球的模式形成鲜明对比.
- 区域机制可能影响了新西兰的气候.
- 西南太平洋大气循环的变化可能导致了这些波动.
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