首页> 外文会议>30th Asian conference on remote sensing 2009 >Remote Sensing Retrieval of Soil Moisture in the Wetland Area of a Flood Plain——a case study of Honghe National Nature Reserve
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Remote Sensing Retrieval of Soil Moisture in the Wetland Area of a Flood Plain——a case study of Honghe National Nature Reserve

机译:洪泛区湿地土壤水分的遥感反演-以红河国家自然保护区为例

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摘要

Soil moisture is an important indicator for wetland degradation. It is significant to do research on spatial and time variability of soil moisture and on how to monitor soil moisture by remote sensing in wetland, which is still a lack of research at present. In this paper, the Honghe National Nature Reserve is taken as an example. After analyzing all kinds of information about soil moisture reversion and comparing different quantitative remote sensing models, we introduce Ts/NDVI model and rectify it by many monitoring data to adapt to the soil moisture retrieving in the wetland study area. Supported by Landsat TM data and other high-resolution data, we inverse the factors (e.g. the vegetation index, the surface temperature, the albedo and so on) needed in the model by remote sensing techniques. And further on, the process of soil moisture is modulated and described quantitavely. Then we use the new model to monitor soil moisture in Honghe National Nature Reserve in June、July、 August and September of 2008. Based on the monitoring data of some typical fields, the retrieved information is validated and the result show that the model is very well to obtain the depth soil moisture in wetland. The results of this study show that the improved TS/EVI space can extract more accurate spatial/temporal distribution of soil moisture information in wetland. It is useful for the quantitative investigation of the four typical growing season's soil moisture variations as well as analysis of habitat characteristics of the humidity gradient.
机译:土壤水分是湿地退化的重要指标。研究湿地土壤水分的时空变异性以及如何通过遥感监测湿地土壤水分具有重要意义,目前仍缺乏研究。本文以红河国家自然保护区为例。在分析了有关土壤水分恢复的各种信息并比较了不同的定量遥感模型之后,我们引入了Ts / NDVI模型,并通过许多监测数据对其进行了校正,以适应湿地研究区的土壤水分恢复。在Landsat TM数据和其他高分辨率数据的支持下,我们通过遥感技术逆转了模型中所需的因素(例如植被指数,地表温度,反照率等)。进而,对土壤水分的过程进行了调制和定量描述。然后利用新模型对红河国家自然保护区的土壤水分进行监测,分别于2008年6月,7月,8月和9月进行。根据一些典型田间的监测数据,对检索到的信息进行验证,结果表明该模型非常有效。很好地获得湿地的深度土壤水分。这项研究的结果表明,改进的TS / EVI空间可以提取湿地中土壤水分信息的更准确的时空分布。它对四个典型生长期土壤湿度变化的定量研究以及湿度梯度的栖息地特征分析很有用。

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  • 来源
  • 会议地点 Beijing(CN);Beijing(CN)
  • 作者单位

    Key Laboratory of 3D Information Acquisition and Application of Ministry of Education,Beijing 100048, China;

    Key Laboratory of 3D Information Acquisition and Application of Ministry of Education,Beijing 100048, China;

    Key Laboratory of 3D Information Acquisition and Application of Ministry of Education,Beijing 100048, China;

    Key Laboratory of 3D Information Acquisition and Application of Ministry of Education,Beijing 100048, China;

    Key Laboratory of 3D Information Acquisition and Application of Ministry of Education,Beijing 100048, China;

  • 会议组织
  • 原文格式 PDF
  • 正文语种
  • 中图分类 遥感技术;
  • 关键词

    soil moisture; remote sensing; TS/EVI space; Honghe National Nature Reserve;

    机译:土壤湿度遥感TS / EVI空间红河国家自然保护区;

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