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Advanced Radar Imaging of Geophysical Flows

机译:地球物理流动的先进雷达成像

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摘要

The dynamics of geophysical flows such as snow avalanches and pyroclastic flows are of great interest, not least due to their potential for catastrophic consequences, and have received substantial attention over recent years. A variety of models have been formulated to predict the behaviour of such flows but there is currently a lack of suitable experimental data to validate these models and inform the choice of model or coefficients for a given situation. Radar measurements are useful in, for instance, observation of snow avalanches in order to provide velocity vector information of the movements of snow below the powder cloud, thus providing information that is not available using optical instruments. Simple radar observations, consisting of a one-dimension range profile of low resolution, have been made of snow avalanches. This work sets out to develop and utilize a more sophisticated radar instrument able to perform high resolution 3-D images of, in particular, snow avalanches but also pyroclastic flows, in order to provide a step improvement in the observational data with which to compare with a range of flow laws.
机译:诸如雪雪崩和发球流的地球物理流动的动态具有很大的兴趣,并非最不重要的是由于他们对灾难性后果的潜力,并且近年来受到了大量关注。已经制定了各种模型以预测这种流的行为,但目前缺乏合适的实验数据来验证这些模型,并为特定情况提供选择模型或系数。雷达测量在例如雪崩观察中是有用的,以便在粉末云下方提供雪的运动的速度矢量信息,从而提供使用光学仪器不可用的信息。简单的雷达观测,包括低分辨率的一维范围剖面,已经由雪崩组成。该工作计划开发和利用更复杂的雷达仪器,能够执行高分辨率3-D图像,特别是雪崩,而且还可以在与之比较的观察数据中提供步骤改进一系列流法。

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