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

被引:3
|
作者
Bayarsaikhan, Undrakh [1 ]
Akitsu, Tomoko Kawaguchi [2 ]
Tachiiri, Kaoru [3 ]
Sasagawa, Taiga [4 ]
Nakano, Tomoko [5 ]
Uudus, Bayar-Saikhan [6 ]
Nasahara, Kenlo Nishida [7 ]
机构
[1] Informat & Res Inst Meteorol Hydrol & Environm IR, Dept Environm Database, Ulaanbaatar, Mongolia
[2] Japan Aerosp Explorat Agcy, Earth Observat Res Ctr, 2-1-1 Sengen, Tsukuba, Ibaraki 3058505, Japan
[3] Japan Agcy Marine Earth Sci & Technol, Res Inst Global Change, Yokohama, Kanagawa, Japan
[4] Univ Tsukuba, Grad Sch Sci & Technol, Tsukuba, Ibaraki, Japan
[5] Chuo Univ, Fac Econ, Hachioji, Tokyo, Japan
[6] Natl Univ Mongolia, Sch Arts & Sci, Dept Biol, Div Nat Sci, Ulaanbaatar, Mongolia
[7] Univ Tsukuba, Fac Life & Environm Sci, Tsukuba, Ibaraki, Japan
关键词
GCOM-C; SGLI; PRI; NDVI; Grasslands; LIGHT-USE EFFICIENCY; MODIS; PHENOLOGY; PRODUCTS; ALGORITHM; RESPONSES; DROUGHT; QUALITY;
D O I
10.1080/01431161.2022.2128923
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
The Global Change Observation Mission-Climate (GCOM-C), launched in 2017, has suitable bands matching the photochemical reflectance index (PRI) definition. It also has the bands for the normalized difference vegetation index (NDVI). The PRI has a unique capability to detect plant stress caused by excessive light and drought. However, no moderate-resolution satellites had suitable bands for the PRI, requiring two narrow bands in green light in the definition. In this study, we conducted the early validation study of PRI and NDVI derived from the GCOM-C satellite and demonstrated those accuracies and characteristics in Mongolian grassland. The Mongolian Steppes (dry grasslands) are widely distributed on the plateau and therefore suitable for satellite validation. It is particularly suitable for the PRI validation because Mongolian grasslands have water stress due to the small amount of precipitation in summer. Therefore, we carried out field campaigns at three study sites in Mongolia. In this study, we found the seasonal pattern of PRI suggesting the potential to detect the water stress of vegetation, which is essential information for informed management of the grasslands. However, the correlation between the satellite-derived PRI and the in-situ PRI was negative because of the dependence of GCOM-C PRI on the soil moisture at sparse vegetation. For the accuracy assessment of PRI, which depends on rapidly changing light and soil moisture in a day, more exact synchronization of in-situ and satellite observation is required. On the other hand, we found that the NDVI derived from GCOM-C was highly accurate: The correlation coefficient (R) between the satellite-derived NDVI and the in-situ NDVI was 0.988 (RMSE=0.052). GCOM-C NDVI has enough similarities with MODIS NDVI in terms of accuracy, spatial resolution, and frequency. For example, we demonstrated that GCOM-C NDVI could detect the phenology with the same or better accuracy than MODIS NDVI. We also demonstrated their difference: the soil moisture dependence in sparse vegetation. The less dependency of GCOM-C NDVI on the soil moisture leads to a better classification of vegetation and non-vegetation in the sparse grassland than MODIS NDVI.
引用
收藏
页码:5145 / 5172
页数:28
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