西南极洲的一个活跃的冰下水系统,从太空绘制出地图
Helen Amanda Fricker1, Ted Scambos, Robert Bindschadler
1Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA. hafricker@ucsd.edu
概括
科学家们使用卫星激光测高仪在西南极洲发现了动态的冰下水系统. 这些系统,包括一个大排水湖,显著影响冰流的流动和质量平衡.
科学领域:
- 冰川学的冰川学
- 水文学 水文学
- 遥感 遥感 遥感 遥感
背景情况:
- 冰下水系统在冰流动力学和南极冰盖稳定性方面发挥着关键作用.
- 了解冰下水的运动和储存对于预测冰流和海平面上升至关重要.
研究的目的:
- 为了调查南极西部冰川下水系统的存在和行为.
- 为了量化水的运动和储存在威伦斯和默塞尔冰流下.
- 评估冰下水对冰的动态和质量平衡的影响.
主要方法:
- 利用2003-2006年的卫星激光高度测量数据来绘制海拔变化.
- 分析了14个区域的时间海拔变化,表明了亚冰川水的运动.
- 采用卫星图像差异化来确认关键特征的垂直运动和空间范围.
- 确定并监测了位于惠兰斯冰流接地线附近的主要冰下湖.
主要成果:
- 确定了14个区域的动态海拔变化,解释为亚冰川水的运动.
- 通过使用卫星图像差异化,确认了两个大区域的垂直运动和空间范围.
- 观察到一个以前未知的地下冰川湖,在3年内排出了2.0立方公里的水.
- 其他地方有记录的冰下水储存,其体积与排水湖相当.
结论:
- 揭示了西南极洲广泛和动态的冰下水系统.
- 亚冰川水的运动,包括湖泊排水和储存,显著影响冰川流动力学.
- 观察到的冰下水系统可能对冰流和南极冰盖的质量平衡产生重要控制.
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