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Gordon de Quetteville Robin

机译:戈登·德·埃蒂特·罗宾

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摘要

Gordon de Quetteville Robin died on 21 September 2004 at the age of 83. During his life he contributed significantly and innovatively to his own academic subject of glaciology and, persuaded of the high value of cooperation between national groups at an early age, promoted actively and effectively the cause of international collaboration in Antarctica. He raised the profile and contribution to polar research of the Scott Polar Research Institute, University of Cambridge, to a new peak during his influential directorship between 1958 and 1982. Robin was best known for his pioneering contributions to the study of large ice sheets in the polar regions. He was the first to produce scientifically reliable measurements of the thickness of the Antarctic ice sheet using seismic sounding; he generated the first analysis of the temperature distribution in polar ice sheets; and, with Stan Evans, he initiated the development and implementation 40 years ago of the radio echo sounding technique to measure the thickness of ice masses using high frequency radars that remains the standard methodology, and undertook extensive airborne campaigns in Antarctica using the technique. New branches of research arose from his studies of radio echo sounding — internal layering and sub-glacial lakes. He was responsible for the first scientific proposal to measure polar ice sheets from space using satellite radar altimetry and the first to undertake an empirical study of the propagation of ocean waves into sea ice. He made a number of other significant contributions to the understanding of ice dynamics, the climate record in ice sheets, and the study of ice shelves. His written work was distinguished by innovative ideas combined with careful observation and thorough analysis.
机译:戈登·德·奎特维尔·罗宾(Gordon de Quetteville Robin)于2004年9月21日去世,享年83岁。他一生为自己的冰川学学术做出了重大贡献和创新,并由于早期国家集团之间的合作具有很高的价值,因此积极推动和发展。有效地促进了南极国际合作的事业。他在1958年至1982年间担任有影响力的董事期间,将剑桥大学斯科特极地研究所的极地研究的地位和贡献提高到一个新的高峰。极地地区。他是第一个使用地震测深仪对南极冰盖厚度进行科学可靠测量的人。他对极地冰盖的温度分布进行了首次分析。 40年前,他与斯坦·埃文斯(Stan Evans)一起开发并实施了无线电回波探测技术,该技术使用仍然是标准方法的高频雷达来测量冰块的厚度,并使用该技术在南极开展了广泛的空降战役。他对无线电回波测深的研究出现了新的研究分支-内部分层和冰下湖。他负责使用卫星雷达测高仪从太空测量极地冰盖的第一个科学建议,并且是第一个对海浪传播到海冰中进行实证研究的负责人。他在了解冰动力学,冰盖上的气候记录以及研究冰架方面做出了许多其他重大贡献。他的书面作品以创新的思想,认真的观察和彻底的分析而著称。

著录项

  • 来源
    《Polar Record》 |2005年第217期|p.177-181|共5页
  • 作者

    David J. Drewry;

  • 作者单位

    Office of the Vice-Chancellor, The University of Hull, Hull HU6 7RX;

  • 收录信息 美国《科学引文索引》(SCI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 自然地理学;
  • 关键词

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