The Wüstebach catchment belongs to the German TERENO (Terrestrial Environmental Observatories) network and was partially deforested (~21%) by the Eifel National Park in 2013. In this data paper, we provide 11‐year precipitation and stream water isotope data and the corresponding runoff discharge rates recorded in the Wüstebach catchment (from 2009 to 2019). In addition, we provide an overview of available datasets and access information for environmental data of the Wüstebach catchment that are discoverable with associated metadata at the Web‐based TERENO data portal. We anticipate that this comprehensive data set will give new insights in how deforestation influences the hydrological system, for exampole, in terms of transit time distribut...
Although the hydrological effects of land use change have been studied extensively, only few dataset...
Time series of the natural isotopic composition (2H, 18O) of precipitation and streamwater can provi...
The young water fraction Fyw, defined as the proportion of catchment outflow younger than approximat...
Over the past decades, interpretation of changes in stable isotope signatures of catchment waters ha...
Knowledge about water flow paths is essential for understanding biogeochemical fluxes in developed a...
The transport of precipitation water through a catchment to its outlet is influenced by many factors...
The mean water residence time (MRT) in a catchment gives information about storage,flow pathways, so...
The Weierbach experimental catchment (0.45 km2) is the most instrumented and studied sub-catchment i...
Stable isotopes of water are often used as tracers of water movement at the catchment scale. Previou...
Knowledge of catchment response times to a precipitation forcing and of isotope tracer transit times...
The stable isotopes of oxygen and hydrogen, 18O and 2H, provide information on water flow pathways a...
In mountainous headwater catchments, with their high variability of hydrological processes and catch...
Time series of the natural isotopic composition (2H, 18O) of precipitation and streamwater can provi...
A dual stable water isotope (d2H and d18O) study was conducted in the developed (managed) landscape ...
Quantifying how vegetation mediates water partitioning at different spatial and temporal scales in c...
Although the hydrological effects of land use change have been studied extensively, only few dataset...
Time series of the natural isotopic composition (2H, 18O) of precipitation and streamwater can provi...
The young water fraction Fyw, defined as the proportion of catchment outflow younger than approximat...
Over the past decades, interpretation of changes in stable isotope signatures of catchment waters ha...
Knowledge about water flow paths is essential for understanding biogeochemical fluxes in developed a...
The transport of precipitation water through a catchment to its outlet is influenced by many factors...
The mean water residence time (MRT) in a catchment gives information about storage,flow pathways, so...
The Weierbach experimental catchment (0.45 km2) is the most instrumented and studied sub-catchment i...
Stable isotopes of water are often used as tracers of water movement at the catchment scale. Previou...
Knowledge of catchment response times to a precipitation forcing and of isotope tracer transit times...
The stable isotopes of oxygen and hydrogen, 18O and 2H, provide information on water flow pathways a...
In mountainous headwater catchments, with their high variability of hydrological processes and catch...
Time series of the natural isotopic composition (2H, 18O) of precipitation and streamwater can provi...
A dual stable water isotope (d2H and d18O) study was conducted in the developed (managed) landscape ...
Quantifying how vegetation mediates water partitioning at different spatial and temporal scales in c...
Although the hydrological effects of land use change have been studied extensively, only few dataset...
Time series of the natural isotopic composition (2H, 18O) of precipitation and streamwater can provi...
The young water fraction Fyw, defined as the proportion of catchment outflow younger than approximat...