摘要
卫星微波遥感的SMAP土壤水分产品可以用于大陆和全球尺度,但因为空间分辨率低,难以满足中小尺度的应用。经验性降尺度方法是空间降尺度常用方法,但因为需要依赖于光学遥感获取降尺度因子,所以易受云雾影响导致无法获得时间连续的高空间分辨率土壤水分。为了解决这个问题,我们结合机器学习和深度学习方法进行了降尺度研究。首先,获取地表温度、植被指数、反照率、土地覆盖、地形数据、土壤质地等降尺度因子。然后,利用机器学习模型(Random Forest、LightGBM、XGBoost)建立SMAP土壤水分产品数据与降尺度因子的经验降尺度模型。选择其中精度较好的XGBoost模型将SMAP-L4土壤水分产品的空间分辨率由9 km降尺度至1 km。最后,基于9 km和1 km土壤水分数据对训练DSCGAN超分辨率模型,并利用该模型获取研究区域时空连续的土壤水分数据。结果表明,降尺度得到的土壤水分与SMAP原数据之间的相关性系数R为0.96,均方根误差RMSE为0.034 m^(3)/m^(3),偏置bias为0.011 m^(3)/m^(3),无偏均方根误差ubRMSE为0.034 m^(3)/m^(3)。与实测站点之间的相关性系数R为0.696,均方根误差RMSE为0.192 m^(3)/m^(3),偏置bias为-0.171 m^(3)/m^(3),无偏均方根误差ubRMSE为0.089 m^(3)/m^(3)。本文方法为生产时空连续的更高空间分辨率的地表土壤水分提供了一个框架,可以满足区域水分调查和农业干旱监测等小尺度应用需求。
Due to the coupling effects of climatic conditions,surface and subsurface conditions,and human activities,soil moisture is highly heterogeneous on spatial and temporal scales.The SMAP soil moisture products from satellite microwave remote sensing can be used from continental to global scales,but they are not suitable for small-and medium-scale applications due to low spatial resolution.To improve the spatial resolution of soil moisture products,various downscaling methods have been developed,with the empirical downscaling method being widely used due to its relatively simple calculation.These models require downscaling factors,which are mostly obtained based on optical remote sensing and are susceptible to cloud influence.Therefore,it is impossible to obtain high spatial resolution soil moisture continuously over time using this model for downscaling.To solve this problem,we proposed a downscaling framework based on multiple data sources using machine learning and deep learning methods.The main idea is to use traditional machine learning methods in the absence of clouds and super-resolution methods to downscale soil moisture in the presence of clouds.The combination of these two methods yields time-continuous,high-resolution soil moisture.First,multi-source data were used to obtain fifteen downscaling factors,including surface temperature,normalized vegetation index,albedo,elevation,slope,slope direction,soil cover type,soil texture,etc.Then,three machine learning models(Random Forest,LightGBM,and XGBoost)were used to establish empirical downscaling models of SMAP soil moisture product data with downscaling factors.The best performing XGBoost model was chosen to downscale the spatial resolution of SMAP soil moisture products from 9 km to 1 km.Finally,the DSCGAN super-resolution model was trained based on 9 km and 1 km soil moisture data pairs.The trained models were used to obtain spatio-temporally continuous soil moisture data for the study area.The results show that,by comparing the downscaled soil moisture and original SMAP data,the R is 0.96,the RMSE is 0.034 m^(3)/m^(3),the bias is 0.011 m^(3)/m^(3),and the ubRMSE is 0.034 m^(3)/m^(3).The comparison between the downscaled soil moisture and the measured data shows that the R is 0.696,the RMSE is 0.192 m3/m,the bias is-0.171 m^(3)/m^(3),and the ubRMSE is 0.089 m^(3)/m^(3).The downscaling method proposed in this study provides a framework for generating higher resolution spatio-temporally continuous surface soil moisture that can meet the needs of small-scale applications such as regional moisture surveys and agricultural drought monitoring.
作者
王思超
蔡玉林
朱子正
黄修东
赵相伟
WANG Sichao;CAI Yulin;ZHU Zizheng;HUANG Xiudong;ZHAO Xiangwei(College of Geodesy and Geomatics,Shandong University of Science and Technology,Qingdao 266500,China;Qingdao Hydrology Bureau,Qingdao 266071,China)
出处
《地球信息科学学报》
EI
CSCD
北大核心
2024年第9期2213-2225,共13页
Journal of Geo-information Science
基金
国家重点研发计划子课题(2019YFE0126700)
山东省自然科学基金项目(ZR2022MD018)。