首页> 外文期刊>The Cryosphere Discussions >Multi-channel and multi-polarization radar measurements around the NEEM site
【24h】

Multi-channel and multi-polarization radar measurements around the NEEM site

机译:NEEM站点周围的多通道和多极化雷达测量

获取原文
       

摘要

Ice properties inferred from multi-polarization measurements, such as birefringence and crystal orientation fabric (COF), can provide insight into ice strain, viscosity, and ice flow. In 2008, the Center for Remote Sensing of Ice Sheets (CReSIS) used a ground-based VHF (very high frequency) radar to take multi-channel and multi-polarization measurements around the NEEM (North Greenland Eemian Ice Drilling) site. The system operated with 30 MHz bandwidth at a center frequency of 150 MHz. This paper describes the radar system, antenna configurations, data collection, and processing and analysis of this data set. Within the framework derived from uniaxial ice crystal model, we found that ice birefringence dominates the power variation patterns of co-polarization and cross-polarization measurements in the area of 100 kmsup2/sup around the ice core site. The phase shift between ordinary and extraordinary waves increases nonlinearly with depth. The ice optic axis lies in planes that are close to the vertical plane and perpendicular or parallel to the ice divide depending on depth. The ice optic axis has an average tilt angle of about 11.6° vertically, and its plane may rotate either clockwise or counterclockwise by about 10° across the 100 kmsup2/sup area, and at a specific location the plane may rotate slightly counterclockwise as depth increases. Comparisons between the radar observations, simulations, and ice core fabric data are in very good agreement. We calculated the effective colatitude at different depths by using azimuth and colatitude measurements of the c?axis of ice crystals. We obtained an average effective c?axis tilt angle of 9.6° from the vertical axis, very comparable to the average optic axis tilt angle estimated from radar polarization measurements. The comparisons give us confidence in applying this polarimetric radio echo sounding technique to infer profiles of ice fabric in locations where there are no ice core measurements.
机译:从多偏振测量得出的冰属性,例如双折射和晶体取向织物(COF),可以提供对冰应变,粘度和冰流的了解。 2008年,冰原遥感中心(CReSIS)使用了地面甚高频(甚高频)雷达在NEEM(北格陵兰Eemian冰钻)站点附近进行多通道和多极化测量。该系统在150 MHz的中心频率下以30 MHz带宽运行。本文介绍了雷达系统,天线配置,数据收集以及该数据集的处理和分析。在单轴冰晶模型推导的框架内,我们发现冰双折射在冰芯中心周围100 km 2 的区域中主导着共极化和交叉极化测量的功率变化模式。普通波和异常波之间的相移随深度非线性增加。冰视轴位于接近垂直平面且垂直或平行于冰块的平面中,取决于深度。冰视轴在垂直方向的平均倾斜角度约为11.6°,其平面可以在100 km 2 区域内顺时针或逆时针旋转大约10°,并且在特定位置,该平面可以随着深度增加,逆时针方向略微旋转。雷达观测,模拟和冰芯织物数据之间的比较非常吻合。我们通过使用冰晶偏角的方位角和清晰度测量来计算不同深度的有效清晰度。我们从垂直轴获得的平均有效c轴倾斜角为9.6°,与从雷达极化测量估计的平均光轴倾斜角相当。这些比较使我们有信心使用这种极化无线电回波探测技术来推断没有冰芯测量位置的冰布轮廓。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号