从观察到的海平面最小值计算出最后一个冰川最大值的时间
Yokoyama1, Lambeck, De Deckker P
1Research School of Earth Sciences, The Australian National University, Canberra, ACT.
Nature
|August 30, 2000
概括
最后一个冰川最大期出现了巨大的冰盖,超过今天的5250万立方公里. 这一时期大约在19000年前结束,冰的体积迅速减少了10%.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 海洋地质 海洋地质学
背景情况:
- 最后的冰川最大期 (LGM) 的特点是广泛的冰盖和较低的全球温度.
- 对LGM冰盖体积和融化动态的直接估计很少.
研究的目的:
- 为了估计LGM期间陆地冰的最大容量.
- 为了确定LGM冰盖初始融化阶段的时间.
- 为了重建海平面变化和冰盖质量平衡.
主要方法:
- 在澳大利亚波纳帕特湾 (Bonaparte Gulf) 分析了四种不同的沉积面.
- 使用动物组合和沉积物保存来识别海洋和盐条件.
- 放射性碳年代测定和冰川-水分-静态建模以估计冰的体积和时间.
主要成果:
- 陆地冰的数量在现在之前的22000到19000个日历年之间达到峰值.
- LGM冰的体积超过了当前的地面冰盖52.5 x 10^6 km3.
- 大约19,000 +/- 250年前,冰量迅速减少了10%,这标志着LGM的结束.
结论:
- 波拿巴湾为重建LGM冰动态提供了有价值的记录.
- LGM以一个显著且相对较快的脱冰事件结束.
- 了解过去的冰盖行为对于预测未来气候变化影响至关重要.
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