极地研究 ›› 2011, Vol. 23 ›› Issue (2): 138-148.DOI: 10.3724/SP.J.1084.2011.00138

• 研究进展 • 上一篇    下一篇

ICESat与ICESat-2应用进展与展望

杨帆1 温家洪1 Weili Wang2   

  1. 1上海师范大学地理系 2NASA Goddard Space Flight Center
  • 收稿日期:2010-11-18 修回日期:2010-12-16 出版日期:2011-06-30 发布日期:2011-06-30
  • 通讯作者: 杨帆
  • 基金资助:

    南极Amery冰架底部界面过程与冰架变化研究

ICESat AND ICESAT-2 APPLICATIONS: PROGRESS AND PROSPECT

  • Received:2010-11-18 Revised:2010-12-16 Online:2011-06-30 Published:2011-06-30

摘要:

近十年来,格陵兰和南极冰盖消融增速,两极地区显著变化。美国国家航空航天管理局(NASA)的冰、云和陆地高程卫星(ICESat)自2003年发射至2009年的在轨期间,用于定量分析冰盖和海冰变化速率,并对这些变化的驱动机制进行检测与监测。ICESat在极地冰雪遥感应用等方面展示出了无可比拟的优势。对精确估算冰盖对海平面上升的年贡献,南北极海冰物质平衡量和计算全球生物总量具有重要的科学意义。冰、云和陆地高程卫星2号(ICESat-2)将在2015年发射,该卫星在ICESat的技术基础上,测高技术和精准度都有了很大的提高。本文评述了ICESat运行情况和应用优势,详尽的介绍了ICESat-2的任务目标、运行参数和技术改进,为其将来在极地科学的巨大应用前景进行展望。

关键词: ICESat-2

Abstract:

The Ice, Cloud, and land Elevation Satellite, whose primary mission was the global monitoring of the polar ice change. ICESat placed in a 91-day exact repeat orbit with 33 days sub-cycles at 600 km altitude and prescribed ground tracks for measuring elevations of ice sheet, sea ice and forest canopy. The global observation systems are being enhanced by ICESat’s precise measurement. With big three missions, it has obvious superiority in pole ice and snow remote sensing. Firstly, ICESat is specifically intended to estimate the change of polar ice-sheet contributions to current and future sea-level rise. ICESat can make different in not only assessing mass balance and mechanisms that driving those changes, but improving predictive ice sheet models. Secondly, as a new and powerful tool, ICESat is designed to measure changes in the spatial patterns of freeboard and thickness of sea-ice by improving narrow lead detection. Finally, it will contribute much to the vegetation and ecosystem science in terms of forest canopy height estimation as well as topographic relief and vegetation vertical structure description. ICESat-2, which is the successor of the ICESat, is a following mission planed by NASA. ICESat-2 will be launched in late 2015 and will follow the ICESat orbit. Compare to the ICESat’s design, ICESat-2 will provide a micro-pulse multi-beam method. ICESat-2 will apply dense cross-track sampling to solve the influence of surface slope. The sensor will have a high laser repetition rate of 10 kHz which are spaced along-track sampling of about 0.7m. The sensor has 9 beams with unequal energy. In contrast to the predecessor, ICESat-2’s elevation measures over high slope areas and very rough areas will be precise.

Key words: ICESat-2