概括
在1984年,北极盆地出口弗拉姆海峡的大多数冰都是多年冰,通常是变形的. 研究人员通过雪深,核心硬度和盐度来区分冰类型,发现其年龄高达5年.
科学领域:
- 北极海洋学 北极海洋学
- 海冰物理学 海洋冰物理学
- 冰川学的冰川学
背景情况:
- 弗拉姆海峡是北极海冰的关键出口点.
- 了解从北极离开的海冰的特征对于气候研究至关重要.
- 多年冰,比第一年冰更老,更厚,在北极生态系统中起着重要作用.
研究的目的:
- 为了描述1984年6月至7月通过弗拉姆海峡从北极盆地离开的海冰.
- 根据物理性质,区分第一年冰和多年冰.
- 为了估计观察到的多年冰的年龄.
主要方法:
- 分析冰的自由板,厚度和盐度.
- 测量冰盖上的雪层深度.
- 检查冰芯的岩石图和盐度特征.
- 视觉检查冰芯硬度和透明度.
主要成果:
- 据估计,离开弗拉姆海峡的84%的冰是多年冰.
- 这个多年冰的很大一部分变形了 ().
- 雪地覆盖深度,核心硬度和透明度是区分多年和第一年冰的有效指标.
- 冰芯分析表明,多年的冰层年龄高达4-5年.
结论:
- 多年冰块主导着从北极盆地通过弗拉姆海峡的外流.
- 变形是这种流出多年冰的共同特征.
- 简单的表面和核心测量可以有效地识别多年冰,有助于大规模的冰特征.
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