Cover, soil moisture, and weather conditions [27,28]. moisture, and weather circumstances [27,28]. InCover, soil moisture,

Cover, soil moisture, and weather conditions [27,28]. moisture, and weather circumstances [27,28]. In
Cover, soil moisture, and climate conditions [27,28]. moisture, and weather circumstances [27,28]. Generally, snow melting or vegetation greening causes a common decrease in surface Normally, snow melting or vegetation greening causes a typical lower in surface albedo [29]. Hence, surface albedo can broadly reflect adjustments in surface conditions, albedo [29]. Thus, surface albedo can broadly reflect adjustments in surface conditions, that is also reflected inside the partnership among NDVI and surface albedo (Figure 13). which is also reflected in the connection involving NDVI and surface albedo (Figure 13). The Pearson correlation coefficient between NDVI and surface albedo reached – along with the Pearson correlation coefficient between NDVI and surface albedo reached -0.73 0.73 and passed the significance test of 99 . We the inter-annual variations in surface albedo passed the significance test of 99 . We foundfound the inter-annual variations in surface albedo (Figure 14) fluctuated 0.18 and 0.33 and 0.33 at each and every station. to 2016, the surface (Figure 14) fluctuated betweenbetween 0.18 at each station. From 2006 From 2006 to 2016, the surface albedo at all AZD4625 References stations decreased year by year. This trend was consistent with albedo at all stations decreased year by year. This trend was constant using the findings the findings of Li et al. [30], who employed the MODIS shortwave white sky albedo product of Li et al. [30], who utilised the MODIS shortwave white sky albedo item (MOD43A3) (MOD43A3) and found that the land surface albedo has been decreasing around the Tibetan and located that the land surface albedo has been decreasing on the Tibetan Plateau from Plateau from 2000 to 2013. This paper additional supports their conclusion with real observa2000 to 2013. This paper additional supports their conclusion with actual observation information. tion information. From 2006 to 2016, the surface albedo at all stations (Z)-Semaxanib MedChemExpress showed a decreasing trend, From 2006 to 2016, the surface albedo at all stations showed a decreasing trend, and the along with the NDVI at all stations (except QOMS station) showed an growing trend. From 2016 NDVI at all stations (except QOMS station) showed an rising trend. From 2016 to to 2019, the surface albedo at BJ, MAWORS, NAMORS, and SETORS showed an increasing 2019, the surface albedo at BJ, MAWORS, NAMORS, and SETORS showed an escalating trend, plus the NDVI at these stations showed a decreasing trend. The interannual trends of surface albedo can broadly reflect the changes in surface circumstances.Water 2021, 13,(Figure 14) fluctuated between 0.18 and 0.33 at every single station. From 2006 to 2016, the surface albedo at all stations decreased year by year. This trend was constant with all the findings of Li et al. [30], who applied the MODIS shortwave white sky albedo solution (MOD43A3) and discovered that the land surface albedo has been decreasing on the Tibetan Plateau from 2000 to 2013. This paper additional supports their conclusion with real observation information. 13 of 26 From 2006 to 2016, the surface albedo at all stations showed a decreasing trend, and also the NDVI at all stations (except QOMS station) showed an escalating trend. From 2016 to 2019, the surface albedo at BJ, MAWORS, NAMORS, and SETORS showed an escalating trend, along with the NDVI at these stations showed a decreasing The interannual trends trend, as well as the NDVI at these stations showed a decreasing trend. The interannual trends of surface albedo can broadly reflect of surface albedo can broadly reflect the change.