Developing Guretolimod custom synthesis season vegetation greenness was positively correlated with the developing season precipitation,season vegetation greennessthe expanding season temIn common, the developing and negatively correlated with was positively correlated with perature and vapor stress deficit (Figure 7). The interannual dynamics of vegetation in the growing season precipitation, and negatively correlated using the developing season the two high-elevation stations correlate small with temperature, precipitation, or VPD, temperature and vapor stress deficit (Figure 7). The interannual dynamics of vegetation suggesting that elements other than temperature and moisture handle interannual vegetaat the two high-elevation stations correlate tiny with temperature, precipitation, or VPD, tion dynamics there. suggesting that factorsair temperature was negativelymoisture manage interannual vegetation The developing season besides temperature and correlated with the increasing seadynamics there. son vegetation greenness, as well as the correlation coefficients had been statistically insignificant exceptThe expanding on grassland. This suggestswas negatively correlatedvegetation expanding at 1 station season air temperature that warming did not drive using the season vegetation greenness, and this region, and coefficients have been statistically insignificant growth at the interannual time scale inthe correlation inversely, vegetation development may have cooled the near-surface air temperature (Figure S2) that warming did not drive vegetation except at one station on grassland. This suggests with all the enhanced evapotranspiration from the interannual time scale within this area, and inversely, vegetation growth may development at the vegetation green-up. Additionally, the magnitudes on the correlation amongst temperature and vegetation greenness had been typically much smaller than these of your correlation between humidity (i.e., ML-SA1 Purity & Documentation precipitation and VPD) and vegetation greenness. This suggests that the interannual vegetation dynamics within this region may possibly be driven by soil moisture and atmospheric humidity–that is, precipitation and VPD, if we assume that precipitation is related to soil moisture, and VPD represents air humidity.4.four. Interannual Covariation among the Vegetation Greenness and Climatic FactorsRemote Sens. 2021, 13,10 ofRemote Sens. 2021, 13,have cooled the near-surface air temperature (Figure S2) using the enhanced evapotranspiration in the vegetation green-up. Furthermore, the magnitudes of your correlation amongst temperature and vegetation greenness have been frequently a great deal smaller than those in the correlation involving humidity (i.e., precipitation and VPD) and vegetation greenness. This suggests that the interannual vegetation dynamics within this region may possibly be driven by 11 of 20 soil moisture and atmospheric humidity–that is, precipitation and VPD, if we assume that precipitation is related to soil moisture, and VPD represents air humidity.Figure 7. Correlation coefficients amongst the detrended growing season NDVI along with the detrended Figure 7. Correlation coefficients involving the detrended growing season NDVI and also the detrended growing season temperature, precipitation, too as atmospheric vapor stress deficit (VPD) developing season temperature, precipitation, too as atmospheric vapor stress deficit (VPD) at at the meteorological stations in the the period from 2000 to 2016. NDVI meteorological station the nine nine meteorological stations in period from 2000 to 2016. NDVI at aat a me.
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