Non-rainfall water (NRW), defined here as dew, hoar frost, fog, rime and water vapor adsorption, might be a relevant water source for ecosystems, especially during summer drought periods. These water inputs are often not considered in ecohydrological studies, because water amounts of NRW events are rather small and therefore difficult to measure. Here we present a novel micro-lysimeter (ML) system and its application which allows to quantify very small water inputs from NRW with an unprecedented high accuracy of ±0.25 g, which corresponds to ±0.005 mm water input. This is possible with an improved ML design paired with individual ML calibrations in combination with high-frequency measurements at 3.3 Hz and an efficient low-pass filtering to...
The vegetation water potential (VWP) indicates the level of water stress anticipating eventually dro...
Weighing lysimeters are a well-established means of accurately obtaining local-scale estimates of ac...
The surface layer of soil as transition zone between pedosphere and atmosphere plays a crucial role ...
Non-rainfall water (NRW), defined here as dew, hoar frost, fog, rime, and water vapour adsorption, m...
Climate change scenarios for Switzerland predict a decline in summer precipitation by the end of the...
Non-rainfall events like dew or hoar frost formation are often neglected in the water budget, becaus...
Dew, fog/mist and water vapour adsorption, the 3 vectors by which non-rainfall water can be added to...
The measurement of non-rainfall atmospheric water input (NRWI) in arid environments requires instrum...
The Community Land Model (CLM4.0) was extended to account for an alternative root water uptake model...
The input of liquid water to terrestrial ecosystems is composed of rain and non-rainfall water (NRW)...
In the semi-arid regions of South Africa, the efficiency of water use by natural grazing plants is i...
Leaf wetness is an important and frequent phenomenon for the surface¿atmosphere exchange of some atm...
Aims We aimed at assessing the influence of above- and below-ground environmental conditions over th...
Weighing lysimeters are a well-established means of accurately obtaining local-scale estimates of ac...
Climate measurements are needed at a scale at which organisms live and die. Currently available clim...
The vegetation water potential (VWP) indicates the level of water stress anticipating eventually dro...
Weighing lysimeters are a well-established means of accurately obtaining local-scale estimates of ac...
The surface layer of soil as transition zone between pedosphere and atmosphere plays a crucial role ...
Non-rainfall water (NRW), defined here as dew, hoar frost, fog, rime, and water vapour adsorption, m...
Climate change scenarios for Switzerland predict a decline in summer precipitation by the end of the...
Non-rainfall events like dew or hoar frost formation are often neglected in the water budget, becaus...
Dew, fog/mist and water vapour adsorption, the 3 vectors by which non-rainfall water can be added to...
The measurement of non-rainfall atmospheric water input (NRWI) in arid environments requires instrum...
The Community Land Model (CLM4.0) was extended to account for an alternative root water uptake model...
The input of liquid water to terrestrial ecosystems is composed of rain and non-rainfall water (NRW)...
In the semi-arid regions of South Africa, the efficiency of water use by natural grazing plants is i...
Leaf wetness is an important and frequent phenomenon for the surface¿atmosphere exchange of some atm...
Aims We aimed at assessing the influence of above- and below-ground environmental conditions over th...
Weighing lysimeters are a well-established means of accurately obtaining local-scale estimates of ac...
Climate measurements are needed at a scale at which organisms live and die. Currently available clim...
The vegetation water potential (VWP) indicates the level of water stress anticipating eventually dro...
Weighing lysimeters are a well-established means of accurately obtaining local-scale estimates of ac...
The surface layer of soil as transition zone between pedosphere and atmosphere plays a crucial role ...