概括
格陵兰岛的冰盖正在变厚,积累了多余的冰,并可能降低全球海平面. 这表明降水量增加,可能与温暖的极地气候有关.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 海平面研究研究 海平面研究
背景情况:
- 格陵兰冰盖的质量平衡对于了解全球海平面变化至关重要.
- 以前的研究集中在冰的损失上,但冰的增加也是一个重要的因素.
研究的目的:
- 量化格陵兰岛冰盖最近的加厚情况.
- 评估这种加厚对全球海平面的影响.
- 探索增加冰积累的潜在气候驱动因素.
主要方法:
- 使用观测数据分析冰盖厚度变化的分析.
- 冰的积累速度与冰流量的建模.
- 基于冰块质量平衡的全球海平面影响的计算.
主要成果:
- 观察到冰盖每年厚度为0.23米.
- 超过余额的冰积累超过余额要求的25%至45%.
- 全球海平面的隐性减退为0.2至0.7毫米/年,取决于所考虑的时间尺度和区域.
结论:
- 冰厚增加表明降水量增加,这可能是温暖极地气候的特征.
- 格陵兰冰盖的加厚对全球海平面有可测量的,尽管目前很小的影响.
- 需要进一步的研究来证实极地降水的长期趋势和驱动因素.
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