A novel global grid model for soil moisture retrieval considering geographical disparity in spaceborne GNSS-R

Abstract Spaceborne global navigation satellite system-reflectometry has become an effective technique for Soil Moisture (SM) retrieval. However, the accuracy of global SM retrieval using a single model is limited due to the complexity of land surface. Introducing redundant ancillary data may also result in over-reliance problems. Therefore, we propose a method for SM retrieval that considers geographical disparities using the data from Cyclone GNSS (CYGNSS) observations and Soil Moisture Active and Passive (SMAP) product. Based on the CYGNSS effective reflectivity and ancillary datasets of SMAP, we establish five models for each grid with different parameters to achieve global SM retrieval. Subsequently, an optimal model, determined by the performance indicator, is used for SM retrieval. The results show that the root mean square error $$S_{\mathrm{RMSE}}$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:msub> <mml:mi>S</mml:mi> <mml:mi>RMSE</mml:mi> </mml:msub> </mml:math> with the improved method is decreased by 9.1% using SMAP SM as reference with the $$S_{\mathrm{RMSE}}$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:msub> <mml:mi>S</mml:mi> <mml:mi>RMSE</mml:mi> </mml:msub> </mml:math> = 0.040 cm 3 /cm 3 compared with using single reflectivity-temperature-vegetation method. Additionally, using the in-situ SM of International Soil Moisture Network as reference, the overall correlation coefficient $$R$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mi>R</mml:mi> </mml:math> and $$S_{\mathrm{RMSE}}$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:msub> <mml:mi>S</mml:mi> <mml:mi>RMSE</mml:mi> </mml:msub> </mml:math> values with the improved method are 0.80 and 0.064 cm 3 /cm 3 , respectively. The average $$R$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mi>R</mml:mi> </mml:math> of the chosen sites is increased by 22.7%, and the average $$S_{\mathrm{RMSE}}$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:msub> <mml:mi>S</mml:mi> <mml:mi>RMSE</mml:mi> </mml:msub> </mml:math> is decreased by 8.7%. The results indicate that the improved method can better retrieve SM in both global and local scales without redundant auxiliary data.

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Publication Details

Journal
Satellite Navigation
Published
2024-09-02
DOI
https://doi.org/10.1186/s43020-024-00150-9
Citations
17
Primary Topic
Soil Moisture and Remote Sensing
Type
article
Field-Weighted Citation Impact
3.50

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article

A novel global grid model for soil moisture retrieval considering geographical disparity in spaceborne GNSS-R

Fade Chen, Liangke Huang, Fei Guo, Haojun Li et al.
17 citations
Satellite Navigation
Soil Moisture and Remote Sensing
3.50
article

A novel global grid model for soil moisture retrieval considering geographical disparity in spaceborne GNSS-R

Fade Chen, Liangke Huang, Fei Guo, Haojun Li, Lilong Liu, Anrong Pan
article en
17 citations

Abstract

Abstract Spaceborne global navigation satellite system-reflectometry has become an effective technique for Soil Moisture (SM) retrieval. However, the accuracy of global SM retrieval using a single model is limited due to the complexity of land surface. Introducing redundant ancillary data may also result in over-reliance problems. Therefore, we propose a method for SM retrieval that considers geographical disparities using the data from Cyclone GNSS (CYGNSS) observations and Soil Moisture Active and Passive (SMAP) product. Based on the CYGNSS effective reflectivity and ancillary datasets of SMAP, we establish five models for each grid with different parameters to achieve global SM retrieval. Subsequently, an optimal model, determined by the performance indicator, is used for SM retrieval. The results show that the root mean square error $$S_{\mathrm{RMSE}}$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:msub> <mml:mi>S</mml:mi> <mml:mi>RMSE</mml:mi> </mml:msub> </mml:math> with the improved method is decreased by 9.1% using SMAP SM as reference with the $$S_{\mathrm{RMSE}}$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:msub> <mml:mi>S</mml:mi> <mml:mi>RMSE</mml:mi> </mml:msub> </mml:math> = 0.040 cm 3 /cm 3 compared with using single reflectivity-temperature-vegetation method. Additionally, using the in-situ SM of International Soil Moisture Network as reference, the overall correlation coefficient $$R$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mi>R</mml:mi> </mml:math> and $$S_{\mathrm{RMSE}}$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:msub> <mml:mi>S</mml:mi> <mml:mi>RMSE</mml:mi> </mml:msub> </mml:math> values with the improved method are 0.80 and 0.064 cm 3 /cm 3 , respectively. The average $$R$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mi>R</mml:mi> </mml:math> of the chosen sites is increased by 22.7%, and the average $$S_{\mathrm{RMSE}}$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:msub> <mml:mi>S</mml:mi> <mml:mi>RMSE</mml:mi> </mml:msub> </mml:math> is decreased by 8.7%. The results indicate that the improved method can better retrieve SM in both global and local scales without redundant auxiliary data.

Satellite NavigationVol. 5(1)
Tongji University (CN), Wuhan University (CN), Guilin University of Technology (CN)
National Natural Science Foundation of China
Life in Land
Openalex Percentile: Top 7%
Soil Moisture and Remote Sensing
3.50
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