首页> 外文期刊>The Science of the Total Environment >Remote sensing of diffuse attenuation coefficient patterns from Landsat 8 OLI imagery of turbid inland waters: A case study of Dongting Lake
【24h】

Remote sensing of diffuse attenuation coefficient patterns from Landsat 8 OLI imagery of turbid inland waters: A case study of Dongting Lake

机译:基于内陆浑浊水域Landsat 8 OLI影像的漫反射衰减系数模式的遥感研究-以洞庭湖为例

获取原文
获取原文并翻译 | 示例
           

摘要

The diffuse attenuation coefficient, K_d(λ), is an important optical property. Environmental change and anthropogenic activities, however, have made it challenging to accurately assess K_d(λ) patterns in the extremely turbid inland waters. We addressed this challenge by using new Landsat 8 Operational Land Imager (OU) imagery. For the bio-optical complexity of water, we proposed an empirical band-ratio algorithm for estimating K_d(490) using our in situ measurements. Based on the acceptable performance of an OLI image-based atmospheric correction and K_d(490) validation, the algorithm was then applied to OLI images to estimate K_d(490) patterns from April 2013 to April 2016, leading to several key findings: (1) Spatial-temporal patterns of K_d(490) varied significantly in Dongting Lake. The temporal heterogeneity of K_d(490) could be explained primarily by surface-runoff changes driven by regional precipitation. The spatial heterogeneity was due to sediment resuspension, resulting from sand dredging and shipping activities; (2) K_d(490) values that were inversed at the intersection of Dongting Lake and Yangtze River were observed for the first time near the Chengliji site and resulted from the opposing temporal cycle of K_d(490) variations between Dongting Lake and the Yangtze River; (3) There was a significant positive correlation between K_d(490) and total suspended matter (TSM). This confirms that TSM often plays a principal role in the attenuation of light in extremely turbid water bodies; (4) The empirical band-ratio algorithm worked well, not only for the broader Landsat archives, but also for the narrower Sentinel-2/3 for K_d(490) estimation, which demonstrates that the algorithm could be used to quantitatively monitor multi-decade records of Landsat observations and future applications of inland water quality in turbid inland waters, such as Dongting Lake and Poyang Lake.
机译:漫射衰减系数K_d(λ)是重要的光学特性。然而,环境变化和人为活动使准确评估极端浑浊的内陆水域的K_d(λ)模式面临挑战。我们通过使用新的Landsat 8 Operational Land Imager(OU)影像解决了这一挑战。对于水的生物光学复杂性,我们提出了一种实地带比率算法,用于使用我们的原位测量估算K_d(490)。基于基于OLI图像的大气校正和K_d(490)验证的可接受性能,然后将该算法应用于OLI图像,以估算2013年4月至2016年4月的K_d(490)模式,得出以下几个主要发现: )洞庭湖K_d(490)的时空格局变化很大。 K_d(490)的时间异质性主要可以由区域降水驱动的地表径流变化来解释。空间异质性是由于泥沙疏shipping和运输活动造成的沉积物再悬浮所致; (2)首次在洞里湖站点附近观测到洞庭湖与长江交汇处的K_d(490)值,这是由于洞庭湖与长江之间K_d(490)变化的时间周期相反造成的; (3)K_d(490)与总悬浮物(TSM)之间存在显着正相关。这证实了TSM在极其浑浊的水体中通常在光的衰减中起主要作用。 (4)经验带比率算法不仅适用于更广泛的Landsat档案,而且适用于较窄的Sentinel-2 / 3的K_d(490)估计,效果都很好,这表明该算法可用于定量监测多Landsat观测的十年记录以及在内陆水域(如洞庭湖和Po阳湖)中内陆水质的未来应用。

著录项

  • 来源
    《The Science of the Total Environment》 |2016年第15期|39-54|共16页
  • 作者单位

    Key Laboratory of Virtual Geographic Environment, Ministry of Education, College of Geographic Science, Nanjing Normal University, Nanjing 210023, China ,School of Geography and Planning, Gannan Normal University, Ganzhou 341000, China ,State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China ,Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China;

    Key Laboratory of Virtual Geographic Environment, Ministry of Education, College of Geographic Science, Nanjing Normal University, Nanjing 210023, China ,School of Geography and Planning, Gannan Normal University, Ganzhou 341000, China;

    Key Laboratory of Virtual Geographic Environment, Ministry of Education, College of Geographic Science, Nanjing Normal University, Nanjing 210023, China ,State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China ,Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China;

    Key Laboratory of Virtual Geographic Environment, Ministry of Education, College of Geographic Science, Nanjing Normal University, Nanjing 210023, China ,State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China ,Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China;

    Key Laboratory of Virtual Geographic Environment, Ministry of Education, College of Geographic Science, Nanjing Normal University, Nanjing 210023, China;

    Key Laboratory of Virtual Geographic Environment, Ministry of Education, College of Geographic Science, Nanjing Normal University, Nanjing 210023, China;

    Key Laboratory of Virtual Geographic Environment, Ministry of Education, College of Geographic Science, Nanjing Normal University, Nanjing 210023, China ,State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China ,Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Diffuse attenuation coefficient; Landsat 8 OLI; Dongting Lake; Total suspended matter (TSM); Surface runoff; Sand dredging;

    机译:漫射衰减系数;Landsat 8 OLI;洞庭湖总悬浮物(TSM);地表径流;挖沙;

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