The breakup in early July 2010 occurred on the northern tributary to Jakobshavn Glacier.
2010年7月初在雅各布港冰川北部支流发生了一起崩裂。
In 2001, Jakobshavn glacier extends westward, showing typical features of a glacier, including flow stripes and crevasses.
2001年的时候，雅各布港冰川向西延伸，呈现出包括流动条纹和裂隙在内的冰川的典型特征。
These images acquired by the Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite show Jakobshavn Glacier in 2001 (top) and 2010 (bottom).
这两张由美国航太总署的地球观测1号(EO-1)卫星上的高级陆地成像仪(ALI)拍摄的图片显示的是2001年（上图）与2010年（下图）的雅各布港冰川。
These images acquired by the Advanced Land Imager (ALI) on NASA's Earth Observing-1 (EO-1) satellite show Jakobshavn Glacier in 2001 (top) and 2010 (bottom).
这两张由美国航太总署的地球观测1号(EO - 1)卫星上的高级陆地成像仪(ALI)拍摄的图片显示的是2001年(上图)与2010年(下图)的雅各布港冰川。
In 2001, Jakobshavn was already the fastest glacier in the world, flowing from land to sea at 7 kilometers per year.
2001年时，雅各布港冰川已是世界上流动速度最快的冰川，它以每年7公里的速度从陆地向海洋流动。
When an ice tongue such as the Jakobshavn calves, the glacier feeding that ice tongue typically accelerates.
当诸如雅各布港冰川之类的冰舌崩离时，冰川为了补给冰舌通常会加速流动。
When an ice tongue such as the Jakobshavn calves, the glacier feeding that ice tongue typically accelerates.
当诸如雅各布港冰川之类的冰舌崩离时，冰川为了补给冰舌通常会加速流动。
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