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Relevant bibliographies by topics / Wüstebach Catchment

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Journal articles

Academic literature on the topic 'Wüstebach Catchment'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Wüstebach Catchment"

1

Płaczkowska, Eliza, Karolina Mostowik, Heye Reemt Bogena, and Michael Leuchner. "The Impact of Partial Deforestation on Solute Fluxes and Stream Water Ionic Composition in a Headwater Catchment." Water 15, no. 1 (2022): 107. http://dx.doi.org/10.3390/w15010107.

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To ensure the good chemical status of surface water across Europe, it is necessary to increase research on the comprehensive impact of land use and land cover changes, i.e., deforestation, on the natural environment. For this reason, we used data from 9-year environmental monitoring in the Wüstebach experimental catchment of the TERENO (Terrestrial Environmental Observatories) network to determine the impact of partial deforestation on solute fluxes and stream water ionic composition. In 2013, a partial deforestation experiment was conducted in the study area using a cut-to-length logging meth

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2

Hrachowitz, Markus, Michael Stockinger, Miriam Coenders-Gerrits, et al. "Reduction of vegetation-accessible water storage capacity after deforestation affects catchment travel time distributions and increases young water fractions in a headwater catchment." Hydrology and Earth System Sciences 25, no. 9 (2021): 4887–915. http://dx.doi.org/10.5194/hess-25-4887-2021.

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Abstract. Deforestation can considerably affect transpiration dynamics and magnitudes at the catchment scale and thereby alter the partitioning between drainage and evaporative water fluxes released from terrestrial hydrological systems. However, it has so far remained problematic to directly link reductions in transpiration to changes in the physical properties of the system and to quantify these changes in system properties at the catchment scale. As a consequence, it is difficult to quantify the effect of deforestation on parameters of catchment-scale hydrological models. This in turn leads

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3

Heistermann, Maik, Heye Bogena, Till Francke, et al. "Soil moisture observation in a forested headwater catchment: combining a dense cosmic-ray neutron sensor network with roving and hydrogravimetry at the TERENO site Wüstebach." Earth System Science Data 14, no. 5 (2022): 2501–19. http://dx.doi.org/10.5194/essd-14-2501-2022.

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Abstract. Cosmic-ray neutron sensing (CRNS) has become an effective method to measure soil moisture at a horizontal scale of hundreds of metres and a depth of decimetres. Recent studies proposed operating CRNS in a network with overlapping footprints in order to cover root-zone water dynamics at the small catchment scale and, at the same time, to represent spatial heterogeneity. In a joint field campaign from September to November 2020 (JFC-2020), five German research institutions deployed 15 CRNS sensors in the 0.4 km2 Wüstebach catchment (Eifel mountains, Germany). The catchment is dominantl

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4

Strebel, Lukas, Heye R. Bogena, Harry Vereecken, and Harrie-Jan Hendricks Franssen. "Coupling the Community Land Model version 5.0 to the parallel data assimilation framework PDAF: description and applications." Geoscientific Model Development 15, no. 2 (2022): 395–411. http://dx.doi.org/10.5194/gmd-15-395-2022.

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Abstract. Land surface models are important for improving our understanding of the Earth system. They are continuously improving and becoming better in representing the different land surface processes, e.g., the Community Land Model version 5 (CLM5). Similarly, observational networks and remote sensing operations are increasingly providing more data, e.g., from new satellite products and new in situ measurement sites, with increasingly higher quality for a range of important variables of the Earth system. For the optimal combination of land surface models and observation data, data assimilati

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5

Katsanou, Konstantina, Alessandro Cattapan, Raymond Venneker, Roland Bol, and Jochen Wenninger. "Can high-resolution monitoring provide a better understanding of the hyporheic zone in Groundwater Dependent Ecosystems?" ARPHA Conference Abstracts 8 (May 28, 2025): e155243. https://doi.org/10.3897/aca.8.e155243.

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The hyporheic zone is an essential component of river ecosystems, yet it is often overlooked in environmental studies. A comprehensive understanding of the interactions between surface water (SW) and groundwater (GW), as well as the role of Groundwater Dependent Ecosystems (GDEs) in providing essential ecosystem services, is crucial for informed and effective land and water management (Yang and 2017).GDEs are influenced by local hydrogeology and climate, necessitating detailed spatial and temporal monitoring of the physical and chemical interactions occurring within these systems. Traditional

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6

Robinson, Kerri-Leigh, Heye R. Bogena, Qiqi Wang, Erik Cammeraat, and Roland Bol. "Effects of deforestation on dissolved organic carbon and nitrate in catchment stream water revealed by wavelet analysis." Frontiers in Water 4 (November 10, 2022). http://dx.doi.org/10.3389/frwa.2022.1003693.

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Deforestation can lead to an increase in the availability of nutrients in the soil and, in turn, have an impact on the quality of water in receiving water bodies. This study assesses the impact of deforestation by evaluating the in-stream concentrations of dissolved organic carbon (DOC) and nitrate, their internal relationship, and those with stream discharge in the Wüstebach headwater catchment (Germany). This catchment has monitored stream water and associated environmental parameters for over a decade as part of the TERENO initiative. Additionally, there is a paired undisturbed forested cat

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7

Wang, Qiqi, Yuquan Qu, Kerri-Leigh Robinson, et al. "Deforestation alters dissolved organic carbon and sulfate dynamics in a mountainous headwater catchment—A wavelet analysis." Frontiers in Forests and Global Change 5 (November 7, 2022). http://dx.doi.org/10.3389/ffgc.2022.1044447.

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Deforestation has a wide range of effects on hydrological and geochemical processes. Dissolved organic carbon (DOC) dynamics, a sensitive environmental change indicator, is expected to be affected by deforestation, with changes in atmospheric sulfur (S) deposition compounding this. However, how precisely anthropogenic disturbance (deforestation) under a declining atmospheric S input scenario affects the underlying spatiotemporal dynamics and relationships of river DOC and sulfate with hydro-climatological variables e.g., stream water temperature, runoff, pH, total dissolved iron (Fetot), and c

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8

Bogena, Heye R., Michael P. Stockinger, and Andreas Lücke. "Long‐term stable water isotope and runoff data for the investigation of deforestation effects on the hydrological system of the Wüstebach catchment, Germany." Hydrological Processes, December 18, 2020. http://dx.doi.org/10.1002/hyp.14006.

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9

Katsanou, Konstantina, Alessandro Cattapan, Raymond Venneker, Roland Bol, and Jochen Wenninger. "Can high-resolution monitoring provide a better understanding of the hyporheic zone in Groundwater Dependent Ecosystems?" ARPHA Conference Abstracts 8 (May 28, 2025). https://doi.org/10.3897/aca.8.e155243.

Full text

Abstract:

The hyporheic zone is an essential component of river ecosystems, yet it is often overlooked in environmental studies. A comprehensive understanding of the interactions between surface water (SW) and groundwater (GW), as well as the role of Groundwater Dependent Ecosystems (GDEs) in providing essential ecosystem services, is crucial for informed and effective land and water management (Yang and 2017). GDEs are influenced by local hydrogeology and climate, necessitating detailed spatial and temporal monitoring of the physical and chemical interactions occurring within these systems. Traditional

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