Recent decades have been characterized by increasing temperatures worldwide, resulting
in an exponential climb in vapor pressure deficit (VPD). VPD has been identified as an …

Climate change can directly affect forest hydrology by altering precipitation,
evapotranspiration, and streamflow generation, or indirectly by changing disturbance …

Irrigation is an important adaptation to reduce crop yield loss due to water stress from both
soil water deficit (low soil moisture) and atmospheric aridity (high vapor pressure deficit …

Accurate measurement or estimation of plant transpiration (T) is of great significance for
understanding crop water use, predicting crop yield and designing irrigation schedule in …

Plant transpiration links physiological responses of vegetation to water supply and demand
with hydrological, energy and carbon budgets at the land-atmosphere interface. However …

Soil moisture (VWC) and atmospheric dryness (vapor pressure deficit, VPD) have an
increasing impact on tree transpiration and productivity with climate change. However, the …

To accurately quantify tree transpiration and determine related hydrologic and physiological
processes, it is important to have reliable information on environmental and physiological …

Total daily water use is a key factor influencing the growth of many terrestrial plants, and
reflects both day-time and nocturnal water fluxes. However, while nocturnal sap flow (E n) …

In many regions of the world, drought is projected to increase under climate change, with
potential negative consequences for forests and their ecosystem services (ES). Forest …

Tree transpiration contributes to the forest water budget and its environmental responses
differ between daytime and nighttime. Elucidating these divergent responses separately …