Climate change has been partially mitigated by an increasing net land carbon sink in the
terrestrial biosphere; understanding the processes that drive this sink is thus essential for …

Light use efficiency (LUE) models have been widely used to estimate terrestrial gross
primary production (GPP) at local, regional, and global scales, which is vital for …

Water availability plays a critical role in sha** terrestrial ecosystems, particularly in low-
and mid-latitude regions. The sensitivity of vegetation growth to precipitation strongly …

Climate extremes such as droughts and heatwaves have a large impact on terrestrial carbon
uptake by reducing gross primary production (GPP). While the evidence for increasing …

The time required for an ecosystem to recover from severe drought is a key component of
ecological resilience. The phenology effects on drought recovery are, however, poorly …

Global warming delays the autumn date of foliar senescence (DFS) in recent decades, with
positive implications for growing season length and therefore global carbon storage …

Climatic warming has greatly increased vegetation productivity in the extratropical Northern
Hemisphere since the 1980s, but how long this positive relationship will continue remains …

In the context of global warming, the advancement of spring phenology in northern and
temperate regions due to increased temperatures has been widely reported. Early and …

Although our observing capabilities of solar‐induced chlorophyll fluorescence (SIF) have
been growing rapidly, the quality and consistency of SIF datasets are still in an active stage …

Vegetation changes in karst areas are controlled by the soil formation rate (SFR) and soil
moisture (SM). However, little is known about their thresholds and global control patterns. To …