Soil Moisture Retrieval Using Microwave Remote Sensing Data and a Deep Belief Network in the Naqu Region of the Tibetan Plateau

Soil moisture plays an important role in the land surface model. In this paper, a method of using VV polarization Sentinel-1 SAR and Landsat optical data to retrieve soil moisture data was proposed by combining the water cloud model (WCM) and the deep belief network (DBN). Since the simple combinati...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Zhihui Yang, Jun Zhao, Jialiang Liu, Yuanyuan Wen, Yanqiang Wang
Formato: article
Lenguaje:EN
Publicado: MDPI AG 2021
Materias:
Acceso en línea:https://doaj.org/article/bf9d0c331ef5403db51de6dedb27aa71
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:bf9d0c331ef5403db51de6dedb27aa71
record_format dspace
spelling oai:doaj.org-article:bf9d0c331ef5403db51de6dedb27aa712021-11-25T19:02:50ZSoil Moisture Retrieval Using Microwave Remote Sensing Data and a Deep Belief Network in the Naqu Region of the Tibetan Plateau10.3390/su1322126352071-1050https://doaj.org/article/bf9d0c331ef5403db51de6dedb27aa712021-11-01T00:00:00Zhttps://www.mdpi.com/2071-1050/13/22/12635https://doaj.org/toc/2071-1050Soil moisture plays an important role in the land surface model. In this paper, a method of using VV polarization Sentinel-1 SAR and Landsat optical data to retrieve soil moisture data was proposed by combining the water cloud model (WCM) and the deep belief network (DBN). Since the simple combination of training data in the neural network cannot effectively improve the accuracy of the soil moisture inversion results, a WCM physical model was used to eliminate the effect of vegetation cover on the ground backscatter, in order to obtain the bare soil backscatter coefficient. This improved the correlation of ground soil backscatter characteristics with soil moisture. A DBN soil moisture inversion model based on the bare soil backscatter coefficients as the foundation training data combined with radar incidence angle and terrain factors obtained good inversion results. Studies in the Naqu area of the Tibetan Plateau showed that vegetation cover had a significant effect on the soil moisture, and the goodness of fit (R<sup>2</sup>) between the backscatter coefficient and soil moisture before and after the elimination of vegetation cover was 0.38 and 0.50, respectively. The correlation between the backscatter coefficient and the soil moisture was improved after eliminating the vegetation cover. The inversion results of the DBN soil moisture model were further improved through iterative parameters. The model prediction reached its highest level of accuracy when the restricted Boltzmann machine (RBM) was set to seven layers, the bias and R were 0.007 and 0.88, respectively. Ten-fold cross-validation showed that the DBN soil moisture model performed stably with different data. The prediction was further improved when the bare soil backscatter coefficient was used as the training data. The mean values of the root mean square error (RMSE), the inequality coefficient (TIC), and the mean absolute percent error (MAPE) were 0.023, 0.09, and 11.13, respectively.Zhihui YangJun ZhaoJialiang LiuYuanyuan WenYanqiang WangMDPI AGarticledeep belief networkwater cloud modelsoil moistureSentinel-1Environmental effects of industries and plantsTD194-195Renewable energy sourcesTJ807-830Environmental sciencesGE1-350ENSustainability, Vol 13, Iss 12635, p 12635 (2021)
institution DOAJ
collection DOAJ
language EN
topic deep belief network
water cloud model
soil moisture
Sentinel-1
Environmental effects of industries and plants
TD194-195
Renewable energy sources
TJ807-830
Environmental sciences
GE1-350
spellingShingle deep belief network
water cloud model
soil moisture
Sentinel-1
Environmental effects of industries and plants
TD194-195
Renewable energy sources
TJ807-830
Environmental sciences
GE1-350
Zhihui Yang
Jun Zhao
Jialiang Liu
Yuanyuan Wen
Yanqiang Wang
Soil Moisture Retrieval Using Microwave Remote Sensing Data and a Deep Belief Network in the Naqu Region of the Tibetan Plateau
description Soil moisture plays an important role in the land surface model. In this paper, a method of using VV polarization Sentinel-1 SAR and Landsat optical data to retrieve soil moisture data was proposed by combining the water cloud model (WCM) and the deep belief network (DBN). Since the simple combination of training data in the neural network cannot effectively improve the accuracy of the soil moisture inversion results, a WCM physical model was used to eliminate the effect of vegetation cover on the ground backscatter, in order to obtain the bare soil backscatter coefficient. This improved the correlation of ground soil backscatter characteristics with soil moisture. A DBN soil moisture inversion model based on the bare soil backscatter coefficients as the foundation training data combined with radar incidence angle and terrain factors obtained good inversion results. Studies in the Naqu area of the Tibetan Plateau showed that vegetation cover had a significant effect on the soil moisture, and the goodness of fit (R<sup>2</sup>) between the backscatter coefficient and soil moisture before and after the elimination of vegetation cover was 0.38 and 0.50, respectively. The correlation between the backscatter coefficient and the soil moisture was improved after eliminating the vegetation cover. The inversion results of the DBN soil moisture model were further improved through iterative parameters. The model prediction reached its highest level of accuracy when the restricted Boltzmann machine (RBM) was set to seven layers, the bias and R were 0.007 and 0.88, respectively. Ten-fold cross-validation showed that the DBN soil moisture model performed stably with different data. The prediction was further improved when the bare soil backscatter coefficient was used as the training data. The mean values of the root mean square error (RMSE), the inequality coefficient (TIC), and the mean absolute percent error (MAPE) were 0.023, 0.09, and 11.13, respectively.
format article
author Zhihui Yang
Jun Zhao
Jialiang Liu
Yuanyuan Wen
Yanqiang Wang
author_facet Zhihui Yang
Jun Zhao
Jialiang Liu
Yuanyuan Wen
Yanqiang Wang
author_sort Zhihui Yang
title Soil Moisture Retrieval Using Microwave Remote Sensing Data and a Deep Belief Network in the Naqu Region of the Tibetan Plateau
title_short Soil Moisture Retrieval Using Microwave Remote Sensing Data and a Deep Belief Network in the Naqu Region of the Tibetan Plateau
title_full Soil Moisture Retrieval Using Microwave Remote Sensing Data and a Deep Belief Network in the Naqu Region of the Tibetan Plateau
title_fullStr Soil Moisture Retrieval Using Microwave Remote Sensing Data and a Deep Belief Network in the Naqu Region of the Tibetan Plateau
title_full_unstemmed Soil Moisture Retrieval Using Microwave Remote Sensing Data and a Deep Belief Network in the Naqu Region of the Tibetan Plateau
title_sort soil moisture retrieval using microwave remote sensing data and a deep belief network in the naqu region of the tibetan plateau
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/bf9d0c331ef5403db51de6dedb27aa71
work_keys_str_mv AT zhihuiyang soilmoistureretrievalusingmicrowaveremotesensingdataandadeepbeliefnetworkinthenaquregionofthetibetanplateau
AT junzhao soilmoistureretrievalusingmicrowaveremotesensingdataandadeepbeliefnetworkinthenaquregionofthetibetanplateau
AT jialiangliu soilmoistureretrievalusingmicrowaveremotesensingdataandadeepbeliefnetworkinthenaquregionofthetibetanplateau
AT yuanyuanwen soilmoistureretrievalusingmicrowaveremotesensingdataandadeepbeliefnetworkinthenaquregionofthetibetanplateau
AT yanqiangwang soilmoistureretrievalusingmicrowaveremotesensingdataandadeepbeliefnetworkinthenaquregionofthetibetanplateau
_version_ 1718410361921601536