2,454
Views
3
CrossRef citations to date
0
Altmetric
Research Article

Early validation study of the photochemical reflectance index (PRI) and the normalized difference vegetation index (NDVI) derived from the GCOM-C satellite in Mongolian grasslands

, ORCID Icon, , , , ORCID Icon & ORCID Icon show all
Pages 5145-5172 | Received 24 Jan 2022, Accepted 16 Sep 2022, Published online: 12 Oct 2022

Figures & data

Figure 1. The national-scale target area and the locations of the ground sites (red triangles). The backdrop image is a GCOM-C/SGLI false colour image, with the water bodies painted in sky blue.

Figure 1. The national-scale target area and the locations of the ground sites (red triangles). The backdrop image is a GCOM-C/SGLI false colour image, with the water bodies painted in sky blue.

Figure 2. Satellite and on-site camera images of the ground sites: (a) Baganuur: BGN, (b) Delgertsogt: DGT, and (c) Khar yamaat: KYM. Satellite images were created from Sentinel-2A true colour images with the red squares representing the 500 m × 500 m areas covering the sites.

Figure 2. Satellite and on-site camera images of the ground sites: (a) Baganuur: BGN, (b) Delgertsogt: DGT, and (c) Khar yamaat: KYM. Satellite images were created from Sentinel-2A true colour images with the red squares representing the 500 m × 500 m areas covering the sites.

Table 1. Descriptions of the ground sites and the dates of in-situ and satellite observations.

Figure 3. Transect lines and satellite pixels () corresponding to the in-situ spectral observation points at the (a) BGN, (b) DGT, and (c) KYM sites. Black dots denote the spectral observation points. Black lines denote the transect lines. Blue and orange squares denote the 250 m × 250 m area around the pixel centres of the SGLI and MODIS images, respectively. (d) a picture of an in-situ spectral observation.

Figure 3. Transect lines and satellite pixels (Table 4) corresponding to the in-situ spectral observation points at the (a) BGN, (b) DGT, and (c) KYM sites. Black dots denote the spectral observation points. Black lines denote the transect lines. Blue and orange squares denote the 250 m × 250 m area around the pixel centres of the SGLI and MODIS images, respectively. (d) a picture of an in-situ spectral observation.

Table 2. Satellite data used in this study.

Figure 4. Relative spectral response (RSR) of SGLI (blue) and MODIS (yellow) in the wavelength between 500 nm 900 nm, along with typical examples of spectral reflectance of ground covers: grass canopy, dry grass canopy, dry soil, and wet soil. The reflectances of grass (LAI = 1.05) and dry grass (LAI = 0.18) canopies were measured at the Khar yamaat and Baganuur sites, respectively (in this study). The “dry grass canopy” means that the ground was covered with dry soil and sparse grass. The reflectance of the forest canopy was measured at a deciduous broad-leaved forest in Takayama, Japan (obtained from the Phenological Eyes Network, Nasahara and Nagai, Citation2015). The reflectance data from dry soil and wet soil was obtained from the literature (Baumgardner et al., Citation1986).

Figure 4. Relative spectral response (RSR) of SGLI (blue) and MODIS (yellow) in the wavelength between 500 nm 900 nm, along with typical examples of spectral reflectance of ground covers: grass canopy, dry grass canopy, dry soil, and wet soil. The reflectances of grass (LAI = 1.05) and dry grass (LAI = 0.18) canopies were measured at the Khar yamaat and Baganuur sites, respectively (in this study). The “dry grass canopy” means that the ground was covered with dry soil and sparse grass. The reflectance of the forest canopy was measured at a deciduous broad-leaved forest in Takayama, Japan (obtained from the Phenological Eyes Network, Nasahara and Nagai, Citation2015). The reflectance data from dry soil and wet soil was obtained from the literature (Baumgardner et al., Citation1986).

Table 3. The satellite products used for deriving the satellite vegetation index (VI) and band reflectance (BR).

Table 4. Coordinate of the pixels within the satellite product tile (04, 25) (vertical tile number, horizontal tile number) used in this study.

Figure 5. Workflow to acquire the in-situ vegetation index (VI, PRI, and NDVI).

Figure 5. Workflow to acquire the in-situ vegetation index (VI, PRI, and NDVI).

Figure 6. Comparison of the in-situ NDVI and the satellite NDVI: (a) GCOM-C/SGLI and (b) Terra/MODIS. The satellite NDVI was taken on the closest sunny day to the day of the in-situ observation. The RMSE for all data was calculated using 1) BGN, DGT (satellite data on 2019-08-09), and KYM data and 2) BGN, DGT (satellite data on 2019-08-10), and KYM data. For the DGT site, the satellite NDVI of two days (the closest sunny day for both SGLI and MODIS: 2019-08-10 and the same day with the in-situ observation: 2019-08-09, cloudy for SGLI and sunny for MODIS) was demonstrated. The bar denotes the uncertainty of the in-situ mean PRI calculated by EquationEq. 6.

Figure 6. Comparison of the in-situ NDVI and the satellite NDVI: (a) GCOM-C/SGLI and (b) Terra/MODIS. The satellite NDVI was taken on the closest sunny day to the day of the in-situ observation. The RMSE for all data was calculated using 1) BGN, DGT (satellite data on 2019-08-09), and KYM data and 2) BGN, DGT (satellite data on 2019-08-10), and KYM data. For the DGT site, the satellite NDVI of two days (the closest sunny day for both SGLI and MODIS: 2019-08-10 and the same day with the in-situ observation: 2019-08-09, cloudy for SGLI and sunny for MODIS) was demonstrated. The bar denotes the uncertainty of the in-situ mean PRI calculated by EquationEq. 6(6) σ=2yx+y2σx2+σy2.(6) .

Table 5. The correlation coefficient and the root-mean-square error between the in-situ vegetation index (VI) and satellite VI at each observation site.

Table 6. Comparison of NDVISGLI and NDVIMODIS simulated using the spectral reflectance of a forest canopy, grass, dry grass, wet soil, and dry soil, which is described in .

Figure 7. Time-Series of temperature, precipitation, NDVI, and PRI (a) at the BGN site in 2018, (b) at the DGT site in 2019, and (c) at the KYM site in 2019. The in-situ data (shown by the large circles and the large triangles) are the mean of NDVI or PRI within a target area (shown in ) at each study site. The bars of the vegetation index and band reflectance denote the uncertainty of the mean (calculated by EquationEq. 6) and the standard error, respectively.

Figure 7. Time-Series of temperature, precipitation, NDVI, and PRI (a) at the BGN site in 2018, (b) at the DGT site in 2019, and (c) at the KYM site in 2019. The in-situ data (shown by the large circles and the large triangles) are the mean of NDVI or PRI within a target area (shown in Fig. 3) at each study site. The bars of the vegetation index and band reflectance denote the uncertainty of the mean (calculated by EquationEq. 6(6) σ=2yx+y2σx2+σy2.(6) ) and the standard error, respectively.

Figure 8. Comparison of NDVISGLI with NDVIMODIS on (a) the relationship between NDVI and the ratio of the soil surface to vegetation cover in wet and dry soils (b) the difference in NDVI on dry and wet soils. The simulation was conducted using the spectral reflectance of grass, wet soil, and dry soil, which are described in .

Figure 8. Comparison of NDVISGLI with NDVIMODIS on (a) the relationship between NDVI and the ratio of the soil surface to vegetation cover in wet and dry soils (b) the difference in NDVI on dry and wet soils. The simulation was conducted using the spectral reflectance of grass, wet soil, and dry soil, which are described in Fig. 4.

Figure 9. Comparison of the in-situ PRISGLI and the satellite PRISGLI at all sites. The satellite PRI was taken on the closest sunny day to the day of the in-situ observation. For the DGT site, the satellite PRI of two days (the closest sunny day: 2019-08-10 and the same day with the in-situ observation but cloudy: 2019-08-09) was demonstrated. The RMSE for all data was calculated using 1) BGN, DGT (satellite data on 2019-08-09), and KYM data and 2) BGN, DGT (satellite data on 2019-08-10), and KYM data.

Figure 9. Comparison of the in-situ PRISGLI and the satellite PRISGLI at all sites. The satellite PRI was taken on the closest sunny day to the day of the in-situ observation. For the DGT site, the satellite PRI of two days (the closest sunny day: 2019-08-10 and the same day with the in-situ observation but cloudy: 2019-08-09) was demonstrated. The RMSE for all data was calculated using 1) BGN, DGT (satellite data on 2019-08-09), and KYM data and 2) BGN, DGT (satellite data on 2019-08-10), and KYM data.

Figure 10. Relationship between PRISGLI and the ratio of the soil surface to vegetation cover on dry and wet soils. The simulation was conducted using the spectral reflectance of grass, wet soil, and dry soil, which are described in .

Figure 10. Relationship between PRISGLI and the ratio of the soil surface to vegetation cover on dry and wet soils. The simulation was conducted using the spectral reflectance of grass, wet soil, and dry soil, which are described in Fig. 4.

Figure 11. Spatial distribution of PRI derived from SGLI in (a) the area including three study sites on (b) August 23, 2018 (the peak of greenness), and (c) October 03, 2018 (the end of the growing season). (d) Subtraction of (b) from (c).

Figure 11. Spatial distribution of PRI derived from SGLI in (a) the area including three study sites on (b) August 23, 2018 (the peak of greenness), and (c) October 03, 2018 (the end of the growing season). (d) Subtraction of (b) from (c).

Figure 12. Comparison of the band reflectance between the SGLI (satellite data) and the MS-720 spectroradiometer (in-situ data) at the (a) BGN, (b) DGT, and (c) KYM sites. The daily SGLI band reflectance data were taken on the closest sunny day to the day of the in-situ observation. For the DGT site, the SGLI data of two days (the closest sunny day: 2019-08-10 and the same day with the in-situ observation but cloudy: 2019-08-09) was demonstrated. The bars for the band reflectance and the VI denote the standard error of the mean and the uncertainty of the mean (calculated by Eq. Equation6) within the target area at each observation site, respectively. The *, **, and *** indicate p-values less than 0.05, 0.01, and 0.001, respectively (Welch’s t-test).

Figure 12. Comparison of the band reflectance between the SGLI (satellite data) and the MS-720 spectroradiometer (in-situ data) at the (a) BGN, (b) DGT, and (c) KYM sites. The daily SGLI band reflectance data were taken on the closest sunny day to the day of the in-situ observation. For the DGT site, the SGLI data of two days (the closest sunny day: 2019-08-10 and the same day with the in-situ observation but cloudy: 2019-08-09) was demonstrated. The bars for the band reflectance and the VI denote the standard error of the mean and the uncertainty of the mean (calculated by Eq. Equation6(6) σ=2yx+y2σx2+σy2.(6) ) within the target area at each observation site, respectively. The *, **, and *** indicate p-values less than 0.05, 0.01, and 0.001, respectively (Welch’s t-test).

Figure 13. Dates of phenological events (DPE) detected from the in-situ observation (time-lapse camera) and the satellite time-series NDVI at the BGN site in 2018. The time-lapse camera images, shown above the graphs, were taken on the DPE detected from three sources (camera, NDVISGLI, and NDVIMODIS). The blue line denotes the NDVISGLI, and the orange line is the NDVIMODIS.

Figure 13. Dates of phenological events (DPE) detected from the in-situ observation (time-lapse camera) and the satellite time-series NDVI at the BGN site in 2018. The time-lapse camera images, shown above the graphs, were taken on the DPE detected from three sources (camera, NDVISGLI, and NDVIMODIS). The blue line denotes the NDVISGLI, and the orange line is the NDVIMODIS.

Figure 14. Comparison of the annual maximum NDVI of SGLI and MODIS in 2019 in each natural zone [delineated in (a)] of Mongolia (Dash, Citation2005): (b) the entire of Mongolia, (c) mountain-taiga and forest-steppe, (f) steppe, (e) semi-desert, and (f) desert. The colour bar denotes the number of pixels. The dashed line in a scatter diagram is the 1:1 line. (g)–(j) Images of typical vegetation cover of each natural zones.

Figure 14. Comparison of the annual maximum NDVI of SGLI and MODIS in 2019 in each natural zone [delineated in (a)] of Mongolia (Dash, Citation2005): (b) the entire of Mongolia, (c) mountain-taiga and forest-steppe, (f) steppe, (e) semi-desert, and (f) desert. The colour bar denotes the number of pixels. The dashed line in a scatter diagram is the 1:1 line. (g)–(j) Images of typical vegetation cover of each natural zones.

Figure 15. Spatial distributions of the annual maxima of (a) NDVISGLI, (b) NDVIMODIS, and (c) the difference in 2019.

Figure 15. Spatial distributions of the annual maxima of (a) NDVISGLI, (b) NDVIMODIS, and (c) the difference in 2019.

Data availability statement

The observed spectral data that support the findings of this study are available from the corresponding author, Akitsu T.K., upon reasonable request.