最近在格陵兰岛内陆的冰盖增长
Ola M Johannessen1, Kirill Khvorostovsky, Martin W Miles
1Mohn-Sverdrup Center for Global Ocean Studies and Operational Oceanography, Nansen Environmental and Remote Sensing Center, Bergen, 5006, Norway. ola.johannessen@nersc.no
概括
格陵兰岛 - 格陵兰岛
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 遥感 遥感 遥感 遥感
背景情况:
- 以前的研究表明,一个平衡的高海拔格陵兰冰盖.
- 据报道,冰盖边缘正在变薄.
研究的目的:
- 为了分析格陵兰冰盖高度计高度数据,从1992年到2003年.
- 为了确定内部和边缘区域的高度变化.
- 调查海拔变化和气候模式之间的联系.
主要方法:
- 对格陵兰冰盖高度计高度连续数据集的分析.
- 利用欧洲遥感卫星 (ERS-1和ERS-2) 的数据.
- 与北大西洋振荡相关的冬季海拔变化.
主要成果:
- 在1500米以上的内部区域,每年增加6.4厘米的显著增长.
- 在1500米以下的区域下降2.0厘米/年,表明边缘变薄.
- 在整个研究区域,整体平均海拔增加5.4厘米/年.
- 证明了冬季海拔变化与北大西洋振荡之间的联系.
结论:
- 格陵兰冰盖的内部不平衡,正在变厚.
- 冰盖边缘正在变薄,与之前的发现一致.
- 高度变化受到气候变化的影响,特别是北大西洋振荡.
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