Seasonal Dynamics of the Land-Surface Characteristics in Arid Regions Retrieved by Optical and Microwave Satellite Data

被引:0
|
作者
Tian, Ying [1 ]
Ackermann, Kurt [2 ]
Mccarthy, Christopher [3 ]
Sternberg, Troy [4 ]
Purevtseren, Myagmartseren [5 ]
Limuge, Che [1 ]
Hagiwara, Katsuro [6 ]
Ogawa, Kenta [1 ]
Hobara, Satoru [1 ]
Hoshino, Buho [1 ]
机构
[1] Rakuno Gakuen Univ, Coll Agr Food & Environm Sci, Hokkaido 0690836, Japan
[2] Hokusei Gakuen Univ, Junior Coll, Sapporo, Hokkaido 0040042, Japan
[3] Johns Hopkins Univ, Zanvyl Krieger Sch Arts & Sci, Baltimore, MD 21218 USA
[4] Univ Oxford, Sch Geog, Oxford OX1 3QY, England
[5] Natl Univ Mongolia, Dept Geog, Ulaanbaatar 14200, Mongolia
[6] Rakuno Gakuen Univ, Coll Vet Sci, Ebetsu, Hokkaido 0690836, Japan
关键词
integration of satellite data and field data; Sentinel-1 and Sentinel-2; linear spectral unmixing; Gobi Desert region; steppe region; Asian dust source area; Mongolia; ESTIMATING SOIL-MOISTURE; DUST OCCURRENCE; RADAR; MODEL; BACKSCATTER; ROUGHNESS; COVER; INDEX; NDVI; AREA;
D O I
10.3390/rs16173143
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Establishing a quantitative relationship between Synthetic Aperture Radar (SAR) data and optical data can facilitate the fusion of these two data sources, enhancing the time-series monitoring capabilities for remote sensing of a land surface. In this study, we analyzed the Normalized Difference Vegetation Index (NDVI) and Shortwave Infrared Transformed Reflectance (STR) with the backscatter coefficients in vertical polarization VV (sigma 0VV) and cross polarization VH (sigma 0VH) across different seasons. We used optical and microwave satellite data spanning from the southern Gobi Desert region to the steppe region in northern Mongolia. The results indicate a relatively high correlation between the NDVI derived from Sentinel-2 and sigma 0VH (RVH = 0.29, RVH = 0.44, p < 0.001) and a low correlation between the NDVI and sigma 0VV (RVH = 0.06, RVH = 0.14, p < 0.01) in the Gobi Desert region during summer and fall. STR showed a positive correlation with both sigma 0VH and sigma 0VV except in spring, with the highest correlation coefficients observed in summer (RVV = 0.45, RVV = 0.44, p < 0.001). In the steppe region, significant seasonal variations in the NDVI and sigma 0VH were noted, with a strong positive correlation peaking in summer (RVH = 0.71, p < 0.001) and an inverse correlation with sigma 0VV except in summer (RVV = -0.43, RVV = -0.34, RVV = -0.13, p < 0.001). Additionally, STR showed a positive correlation with sigma 0VH and sigma 0VV in summer (RVH = 0.40, RVV = 0.39, p < 0.001) and fall (RVH = 0.38, RVV = 0.09, p < 0.01), as well as an inverse correlation in spring (RVH= -0.17, RVV= -0.38, p < 0.001) and winter (RVH = -0.21, RVV = -0.06, p < 0.001). The correlations between the NDVI, STR, sigma 0VH, and sigma 0VV were shown to vary by season and region. In the Gobi Desert region, perennial shrubs are not photosynthetic in spring and winter, and they affect backscatter due to surface roughness. In the steppe region, annual shrubs were found to be the dominant species and were found to photosynthesize in spring, but not enough to affect the backscatter due to surface roughness.
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页数:21
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