An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring

Abstract

An effective soil moisture retrieval method for FY-3E (Fengyun-3E) GNOS-R (GNSS occultation sounder II-reflectometry) is developed in this paper. Here, the LAGRS model, which is totally oriented for GNOS-R, is employed to estimate vegetation and surface roughness effects on surface reflectivity. Since the LAGRS (land surface GNSS reflection simulator) model is a space-borne GNSS-R (GNSS reflectometry) simulator based on the microwave radiative transfer equation model, the method presented in this paper takes more consideration on the physical scattering properties for retrieval. Ancillary information from SMAP (soil moisture active passive) such as the vegetation water content and the roughness coefficient are investigated for the final algorithm’s development. At first, the SR (surface reflectivity) data calculated from GNOS-R is calculated and then calibrated, and then the vegetation roughness factor is achieved and used to eliminate the effects on both factors. After receiving the Fresnel reflectivity, the corresponding soil moisture estimated from this method is retrieved. The results demonstrate good consistency between soil moisture derived from GNOS-R data and SMAP soil moisture, with a correlation coefficient of 0.9599 and a root mean square error of 0.0483 cm3/cm3. This method succeeds in providing soil moisture on a global scale and is based on the previously developed physical LAGRS model. In this way, the great potential of GNOS-R for soil moisture estimation is presented.

Assessing the Freeze/Thaw States in Arctic Circle Using FengYun-3E GNOS-R: An Initial Demonstration and Analysis

“…In order to do the following discrimination for surface soil F/T detection, we will employ the peak values of DDM. While we call this value as SR, its equation for the final calculation is like the following [19]:…”

“…Launched on July 10, 2021, GNOS-II consists of eight reflection channels, capable of receiving signals from GPS, Beidou Navigation System (BDS), and Galileo navigation satellites simultaneously. While GNOS-R has been utilized for studying ocean state parameters, soil moisture, and sea ice thickness, its application in studying surface F/T states is relatively unexplored [17], [18], [19], [20]. This article employs GNOS-R data from July 10, 2021, to September 27, 2022, to investigate the F/T state of the Arctic Circle.…”