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Global estimates of snow water equivalent from passive microwave instruments: history, challenges and future developments

机译:无源微波仪器对雪水当量的全球估算:历史,挑战和未来发展

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摘要

Snow properties have been retrieved from satellite data for many decades. While snow extent is generally felt to be obtained reliably from visible-band data, there is less confidence in the measurements of snow mass or water equivalent derived from passive microwave instruments. This paper briefly reviews historical passive microwave instruments and products, and compares the large-scale patterns from these sources to those of general circulation models and leading reanalysis products. Differences are seen to be large between the datasets, particularly over Siberia. A better understanding of the errors in both the model-based and measurement-based datasets is required to exploit both fully. Techniques to apply to the satellite measurements for improved large-scale snow data are suggested.
机译:数十年来,已经从卫星数据中获取了降雪特性。通常认为从可见带数据可以可靠地获得降雪程度,但对无源微波仪器产生的积雪或水当量的测量却缺乏信心。本文简要回顾了历史悠久的无源微波仪器和产品,并将这些来源的大规模模式与一般循环模型和领先的再分析产品进行了比较。数据集之间的差异很大,尤其是在西伯利亚地区。为了充分利用两者,需要更好地理解基于模型的数据集和基于测量的数据集中的错误。提出了适用于卫星测量的技术,以改进大型雪数据。

著录项

  • 来源
    《International journal of remote sensing》 |2010年第14期|P.3707-3726|共20页
  • 作者

    DEBBIE CLIFFORD;

  • 作者单位

    National Centre for Earth Observation, Department of Meteorology, University of Reading, Earley Gate, PO Box 243, Reading RG6 6BB, UK;

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

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