...
首页> 外文期刊>Arctic: Journal of the Arctic Institute of North America >Lake and river ice investigations in northern Manitoba using airborne SAR imagery
【24h】

Lake and river ice investigations in northern Manitoba using airborne SAR imagery

机译:利用机载SAR图像对马尼托巴北部的湖泊和河流冰层进行调查

获取原文

摘要

Multichannel airborne SAR data were collected over northern Manitoba in April 1989 and January 1990. During the week of the SAR flights, several reconnaissance helicopter flights were undertaken, and ground calibration sites were visited to collect ice, snow, and water data. A total of six SAR image passes were flown in April 1989 and seven in January 1990, in order to collect a data set with numerous incidence angle, frequency, polarization, and look direction combinations. The data have been qualitatively assessed, with specific emphasis on C-band horizontally polarized imagery - the proposed SAR configuration for Radarsat. Results of the analysis have shown that airborne SAR can be used to identify various freshwater ice features, such as juxtaposition ice, refrozen slush, river ice runs, and lake ice. Open water leads were also successfully identified. A careful interpretation of the airborne SAR imagery in conjunction with the ground truth data has shown that the unusually bright returns characterizing the Burntwood River and the west portion of Split Lake were caused by a layer of refrozen slush that was generated during the initial formation of the ice cover. Although the results reported here focused exclusively on a qualitative analysis of C-HH data, preliminary analysis of the digital data suggests that changes in frequency and polarization produce measurable differences and can be used to develop classification algorithms for freshwater ice.
机译:1989年4月和1990年1月在马尼托巴北部收集了多通道机载SAR数据。在SAR飞行的一周中,进行了几次侦察直升机飞行,并访问了地面校准站点,以收集冰,雪和水数据。 1989年4月总共飞行了6次SAR图像,1990年1月飞行了7次,以收集具有众多入射角,频率,极化和视线方向组合的数据集。已对数据进行了定性评估,尤其侧重于C波段水平极化图像-Radarsat的SAR配置建议。分析结果表明,机载SAR可用于识别各种淡水冰特征,例如并置冰,再冻雪泥,河道和湖冰。开水引线也被成功识别。对机载SAR图像和地面真相数据的仔细解释表明,表征伯恩伍德河和斯普利特湖西段的异常明亮的回波是由冰层的最初形成过程中产生的一层重新冻融引起的。冰盖。尽管此处报告的结果仅集中于C-HH数据的定性分析,但对数字数据的初步分析表明,频率和极化的变化会产生可测量的差异,可用于开发淡水冰的分类算法。

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