极地研究 ›› 2003, Vol. 14 ›› Issue (2-English): 117-123.

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Remote monitoriug ice velocities of the polar record and the Dark Glaciers

 Sun Jiabing, Zhou Junqi, Huo Dongmin and Sun Zhaohui   

  1. School of remote sensing and informatics, Wuhan University, Wuhan 430079, China
  • 出版日期:1953-06-30 发布日期:1953-06-30
  • 通讯作者: Sun Jiabing

Remote monitoriug ice velocities of the polar record and the Dark Glaciers

Sun Jiabing, Zhou Junqi, Huo Dongmin and Sun Zhaohui   

  1. School of remote sensing and informatics, Wuhan University, Wuhan 430079, China
  • Online:1953-06-30 Published:1953-06-30
  • Contact: Sun Jiabing

摘要:

Measurement of ice velocities of the Antarctic glaciers is very important for studies on Antarctic ice and snow mass balance. The polar area environmental change and its influences on the global environment. Conventional methods may be used for measuring the ice velocities, but they suffer from severe weather conditions in the Polar areas. Use of satellite multi-spectral and muki-temporal images makes it easier to measure the velocities of the glacier movements. This paper discusses a new method for monitoring the glacial change by means of multi-temporal satellite images. Temporal remotely sensed images in the Ingrid Christensen coast were processed with respect to geometric rectification, registration and overlay, The average ice velocities of the Polar Record Glacier and the Dark Glacier were then calculated, with the changing characteristics analyzed and evaluated. The advantages of the method reported here include promise of all-weather operation and potentials of dynamic monitoring through suitable selection of temporal satellite images.

关键词: The Ingrid Christensea Coast, multi-temporal remotely sensed images, the Polar Record Glacier, the Dark Glacier, glacial ice velocities

Abstract:

Measurement of ice velocities of the Antarctic glaciers is very important for studies on Antarctic ice and snow mass balance. The polar area environmental change and its influences on the global environment. Conventional methods may be used for measuring the ice velocities, but they suffer from severe weather conditions in the Polar areas. Use of satellite multi-spectral and muki-temporal images makes it easier to measure the velocities of the glacier movements. This paper discusses a new method for monitoring the glacial change by means of multi-temporal satellite images. Temporal remotely sensed images in the Ingrid Christensen coast were processed with respect to geometric rectification, registration and overlay, The average ice velocities of the Polar Record Glacier and the Dark Glacier were then calculated, with the changing characteristics analyzed and evaluated. The advantages of the method reported here include promise of all-weather operation and potentials of dynamic monitoring through suitable selection of temporal satellite images.

Key words: The Ingrid Christensea Coast, multi-temporal remotely sensed images, the Polar Record Glacier, the Dark Glacier, glacial ice velocities