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基于时空融合算法的关中地区灌溉信息遥感识别

Remote sensing identification of irrigation information in Guanzhong Region using spatiotemporal fusion algorithm

  • 摘要: 卫星遥感技术凭借快速、大范围观测的特点,在灌溉面积和灌溉频次等信息识别中具有显著优势。然而,单一遥感数据源受影像时空分辨率限制,难以满足区域尺度灌溉信息高精度动态识别需求。该研究以关中地区为研究区,构建了基于干旱指数分析与时空融合算法的灌溉信息遥感识别方法。通过干旱指数与土壤湿度相关性分析,选取温度植被干旱指数(temperature vegetation dryness index,TVDI)作为识别指标,并结合高程校正与融合策略优化,提升复杂地形条件下TVDI对土壤水分的表征能力及其时空融合精度。随后,采用增强时空自适应反射率融合模型融合Landsat与MODIS影像,生成高时空分辨率TVDI时间序列,结合阈值判别法识别2024年关中地区春灌信息。结果表明,经高程校正后的TVDI在春季作物生育阶段与土壤湿度相关性较高(相关系数最高达-0.77);TVDI融合过程中,“先融合NDVI与LST后计算TVDI”的策略融合精度更高(R2=0.76,RMSE=0.07)。灌区尺度验证结果表明,东雷二期抽黄灌区灌溉面积识别总体精度为90.8%,Kappa系数为0.80;3个验证灌区累积灌溉面积与实际灌溉面积平均识别误差分别为15.1%和14.3%。关中地区春灌信息识别结果表明,春灌活动主要集中于3—4月,灌溉次数以1~2次为主,灌溉区域主要分布于渭河平原。研究结果可为复杂地形条件下区域尺度灌溉信息识别提供方法参考。

     

    Abstract: Satellite remote sensing can identify the irrigation information, because of its rapid and wide-area observation. However, only a single source is often extracted from remote sensing data. Spatial and temporal resolution cannot fully meet the requirement for the high-accuracy and dynamic identification of irrigation information at the regional scale, especially for the strong spatial heterogeneity of agricultural activities in the complex terrain. In this study, a remote sensing framework was developed to identify the irrigation information using drought index analysis and spatiotemporal fusion. The Guanzhong Region was also taken as the study area. The temperature vegetation dryness index (TVDI) was selected as the identification index after correlation analysis between drought indices and soil moisture. Elevation correction with fusion optimization was introduced to characterize the variation in the soil moisture. Its spatiotemporal fusion accuracy was also enhanced under complex terrain conditions. Subsequently, the enhanced spatial and temporal adaptive reflectance fusion model (ESTARFM) was used to fuse high-spatial-resolution Landsat imagery and high-temporal-resolution MODIS data for the high-spatiotemporal-resolution TVDI time series. Spring irrigation information in the Guanzhong Region in 2024 was identified using the threshold method with precipitation data. The results showed that the correlations between the remote sensing drought indices and soil moisture at the 10-20 cm depth were generally higher than those with soil moisture at the 0-10 cm depth. Elevation topographic correction effectively reduced the influence of terrain on land surface temperature. There was a strong correlation between TVDI and soil moisture. Furthermore, the elevation-corrected TVDI showed a strong negative correlation with soil moisture at the 10-20 cm depth, with the maximum correlation coefficient of -0.77 during the spring crop growth period. Normalized difference vegetation index (NDVI) and land surface temperature (LST) were fused for the higher accuracy of TVDI than the strategy of first calculation and then fusion. R2and RMSE values of 0.76 and 0.07 for the former, whereas 0.44 and 0.13 for the latter, respectively. The validation showed that the overall accuracy was 90.8% for the identification in the Donglei Phase II irrigation district, with a Kappa coefficient of 0.80. The mean error was 15.1% and 14.3%, respectively, for accumulated and actual irrigated areas in the irrigation districts. Regional identification results indicated that the spring irrigation was mainly concentrated from March to April, with the irrigation frequency ranging from one to two times. Irrigated areas were distributed in the relatively flat Weihe Plain, with a spatial pattern characterized by broader irrigation extent and higher irrigation frequency in the eastern and western parts. While the central part exhibited relatively lower irrigation intensity. The spatial distribution and irrigation frequency of spring irrigation were dominated by regional topography, water supply, and cropping structure. The finding can provide a strong reference to identify the regional-scale irrigation information and water resources under complex terrains.

     

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