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首页> 外文期刊>International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences >REMOTE SENSING RETRIEVAL OF SOIL MOISTURE IN GUANGXI BASED ON ATI AND TVDI MODELS
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REMOTE SENSING RETRIEVAL OF SOIL MOISTURE IN GUANGXI BASED ON ATI AND TVDI MODELS

机译:基于ATI和TVDI模型的广西土壤水分遥感检索

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In order to further to improve the monitoring accuracy of soil moisture spatial and temporal changes in Guangxi, this paper uses MODIS, Landsat8, ASTER GDEM data and measured relative soil moisture data as data sources. According to the design idea of complementary advantages, the EVI value of Landsat8 image is partitioned, and the relative soil moisture is inverted by ATI model method in the area of EVI≤0.33, and the relative soil moisture is inverted by TVDI model in the area of EVI0.33. The apparent thermal inertia model (ATI) and the temperature vegetation drought index model (TVDI) was used to invert the relative soil moisture in Guangxi. The results show that the temporal variation of relative soil moisture in the study area in 2017 is the change cycle from rising to falling: the rising period is from January to July, and the falling period is from August to December, in which the relative soil moisture reaches the peak in July. The minimum value are December; the relative soil moisture in the north of Guangxi are generally higher than that in southern Guangxi. The correlation between the relative soil moisture value of the ATI model and the TVDI model partition retrieval and the measured relative soil moisture data is higher, and the relative soil moisture retrieval effects is better.
机译:为了进一步提高广西土壤水分空间和时间变化的监测准确性,本文使用MODIS,LANDSAT8,ASTER GDEM数据和测量的相对土壤湿度数据作为数据源。根据互补优势的设计思想,陆地上的ATI模型方法在EVI≤0.33面积中倒​​置的陆地湿度水分的EVI值,在该地区的TVDI模型反转了相对土壤水分EVI> 0.33。表观热惯性模型(ATI)和温度植被干旱指数模型(TVDI)用于颠倒广西相对土壤水分。结果表明,2017年研究区域中相对土壤水分的时间变化是从上升到下降的变化周期:上升期为1月至7月,下降期为8月至12月,其中相对土壤湿度在7月份达到了高峰。最低价值是12月;广西北部的相对土壤水分一般高于广西南部的土壤水分。 ATI模型的相对土壤湿度值与TVDI模型分区检索与测量的相对土壤水分数据之间的相关性更高,并且相对土壤水分检索效果更好。

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