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NIU H L, REN H R. Spatio-temporal variations in non-photosynthetic vegetation cover on the Qinghai-Tibet Plateau grassland. Pratacultural Science, 2022, 39(8): 1521-1530. doi: 10.11829/j.issn.1001-0629.2021-0624
Citation: NIU H L, REN H R. Spatio-temporal variations in non-photosynthetic vegetation cover on the Qinghai-Tibet Plateau grassland. Pratacultural Science, 2022, 39(8): 1521-1530. doi: 10.11829/j.issn.1001-0629.2021-0624

Spatio-temporal variations in non-photosynthetic vegetation cover on the Qinghai-Tibet Plateau grassland

  • Estimating the fractional cover of non-photosynthetic vegetation (fNPV) is of great importance for managing grassland resources, calculating carbon balance, and adapting to climate change. The Qinghai-Tibet Plateau has unique climatic characteristics and rich vegetation types that play an important role in the global ecosystem. In this study, we first developed a method for estimating fNPV using a dimidiate pixel model and normalized difference tillage index (NDTI) without field measurements. The model assumes that a mixed pixel is a linear combination of non-photosynthetic vegetation and bare soil, and their coefficients represent the proportion of the area occupied by non-photosynthetic vegetation and bare soil in that pixel. The model was then used to estimate the grassland fNPV on the Qinghai-Tibet Plateau from the year 2000 to 2020 using MODIS surface reflectance data at 500 m resolution (MOD09A1). Statistical analyses were used to further examine the spatio-temporal variations in grassland fNPV on the Qinghai-Tibet Plateau and their relationship with climatic factors. The results showed that the proposed dimidiate pixel model was capable of estimating fNPV of the Qinghai-Tibet Plateau grasslands. The grassland fNPV on the Qinghai-Tibet Plateau gradually increased from northwest to southeast. This trend was closely related to the topography and climatic factors of the Qinghai-Tibet Plateau. The grassland fNPV on the Qinghai-Tibet Plateau was positively correlated with precipitation, and negatively correlated with precipitation in parts of the southwest. Temperature and fNPV were positively correlated in the central and eastern parts of the study area, whereas in the south, southeast, and southwest, fNPV was negatively correlated with temperature. The correlation between fNPV and temperature in the study area was not significantly affected by precipitation, the correlation between fNPV and precipitation was almost unaffected by temperature, and fNPV was significantly affected by the mean precipitation received between May and September and the accumulated precipitation received between January and December. Our study provides a new approach for estimating the fNPV and a new idea for the dynamic monitoring of non-photosynthetic vegetation on the Qinghai-Tibet Plateau.
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