首页> 外文期刊>Geoscience and Remote Sensing, IEEE Transactions on >Validation of Airborne FMCW Radar Measurements of Snow Thickness Over Sea Ice in Antarctica
【24h】

Validation of Airborne FMCW Radar Measurements of Snow Thickness Over Sea Ice in Antarctica

机译:机载FMCW雷达测量南极海冰厚度的验证

获取原文
获取原文并翻译 | 示例

摘要

Antarctic sea ice and its snow cover are integral components of the global climate system, yet many aspects of their vertical dimensions are poorly understood, making their representation in global climate models poor. Remote sensing is the key to monitoring the dynamic nature of sea ice and its snow cover. Reliable and accurate snow thickness data are currently a highly sought after data product. Remotely sensed snow thickness measurements can provide an indication of precipitation levels, predicted to increase with effects of climate change in the polar regions. Airborne techniques provide a means for regional-scale estimation of snow depth and distribution. Accurate regional-scale snow thickness data will also facilitate an increase in the accuracy of sea ice thickness retrieval from satellite altimeter freeboard estimates. The airborne data sets are easier to validate with in situ measurements and are better suited to validating satellite algorithms when compared with in situ techniques. This is primarily due to two factors: better chance of getting coincident in situ and airborne data sets and the tractability of comparison between an in situ data set and the airborne data set averaged over the footprint of the antennas. A 2–8-GHz frequency modulated continuous wave (FMCW) radar loaned by the Center for Remote Sensing of Ice Sheets to the Australian Antarctic Division is used to measure snow thickness over sea ice in East Antarctica. Provided with the radar design parameters, the expected performance parameters of the radar are summarized. The necessary conditions for unambiguous identification of the air/snow and snow/ice layers for the radar are presented. Roughnesses of the snow and ice surfaces are found to be dominant determinants in the effectiveness of layer identification for this radar. Finally, this paper presents the first in situ validated snow thickness estimates over sea ice in Antarctica derived from an FMCW radar on a helicopterborne pla-n-ntform.
机译:南极海冰及其积雪是全球气候系统不可或缺的组成部分,但对其垂直尺寸的许多方面却知之甚少,因此它们在全球气候模型中的代表性很差。遥感是监测海冰及其积雪动态特征的关键。可靠,准确的积雪厚度数据是目前急需的数据产品。遥感积雪厚度测量可以提供降水水平的指示,预计会随着极地地区气候变化的影响而增加。机载技术为区域范围的积雪深度和分布估计提供了一种手段。准确的区域尺度积雪厚度数据也将有助于提高卫星高度计干舷估计值反演海冰厚度的准确性。与现场技术相比,机载数据集更易于通过现场测量进行验证,并且更适合于验证卫星算法。这主要是由于两个因素造成的:获得原位和机载数据集重合的机会更大,以及在整个天线覆盖范围内对原位数据集和机载数据集进行比较的比较的可处理性。冰盖遥感中心借给澳大利亚南极局的2-8 GHz调频连续波(FMCW)雷达用于测量南极东部海冰上的积雪厚度。提供了雷达设计参数,总结了雷达的预期性能参数。提出了明确识别雷达的空气/雪和雪/冰层的必要条件。人们发现,雪和冰表面的粗糙度是该雷达层识别有效性的主要决定因素。最后,本文介绍了从直升机载平台上的FMCW雷达得出的南极洲海冰上的第一个经过现场验证的雪厚估计。

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