Snow Grain Size Estimates from Airborne Ka-Band Radar Measurements

Jilu Li, B. Camps-Raga, F. Rodríguez‐Morales, D. Gomez-Garcia, J. Paden, C. Leuschen
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引用次数: 1

Abstract

We designed a Ka-band prototype radar altimeter operated at a center frequency of 35 GHz with a 6 GHz bandwidth. The instrument was intended for fine-resolution verification and validation of space borne altimetry datasets. We installed it onboard the NASA C-130 aircraft in conjunction with two other wideband microwave instruments and collected airborne altimetry data over Greenland land ice and arctic sea ice during the 2015 NASA Operation IceBridge arctic campaign. Apart from the major application of verification and calibration of satellite-based measurements, data from this instrument can be used to derive snow grain size because of the dominant effect of volume scattering in radar signatures. In this paper, we briefly describe the system design and the installation on the NASA C-130, discuss the observed penetration depths of Ka-band signals into the snowpack, present sample results of optical-equivalent snow grain size estimates from radar measurements over the dry snow zone using a simplified snowpack model. We show that the observed penetration depths and the snow grain size estimates from the airborne Ka-band radar retrievals agree well with the model and in-situ snow-pit measurements.
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从机载ka波段雷达测量估计雪粒大小
我们设计了一个ka波段原型雷达高度计,工作在35 GHz的中心频率和6 GHz的带宽。该仪器旨在对空间载测高数据集进行精细分辨率验证和验证。我们将其安装在NASA C-130飞机上,与另外两台宽带微波仪器一起,在2015年NASA冰桥行动北极运动期间收集格陵兰陆地冰和北极海冰的机载高度数据。除了主要应用于卫星测量的验证和校准之外,由于雷达特征中的体积散射的主导作用,该仪器的数据可用于推导雪粒度。本文简要介绍了该系统的设计和在NASA C-130上的安装,讨论了观测到的ka波段信号进入积雪的穿透深度,给出了使用简化积雪模型从干雪区雷达测量中估计光学等效雪粒度的样本结果。通过机载ka波段雷达反演得到的穿透深度和雪粒大小与模型和现场雪坑测量值吻合较好。
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