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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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摘要

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 EVI>0.33. 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:为了进一步提高在广西土壤湿度的空间和时间的变化监测精度,本文采用MODIS,Landsat8,紫菀GDEM数据和测得的相对土壤湿度数据作为数据源。根据优势互补的设计理念,Landsat8图像的EVI值被分割,相对土壤水分被ATI模型方法在EVI≤0.33的区域反转,相对土壤水分被TVDI模型在该区域反转的EVI> 0.33。视在热惯量模型(ATI)和温度植被干旱指数模型(TVDI)用于反转广西相对土壤湿度。结果表明,在2017年,研究区土壤相对湿度的时间变化是从上升到下降的变化周期:上升期是1至7月,和下降期为八月至十二月,在土壤相对水分到达七月高峰。最小值是十二月;在广西北部的相对土壤湿度普遍高于广西南部高。的ATI模型的相对土壤湿度值和TVDI模型分区检索和测得的相对土壤湿度数据之间的相关性越高,相对土壤湿度检索效果更好。

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