Articles | Volume 25, issue 4
https://doi.org/10.5194/hess-25-2009-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-25-2009-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Apr 2021
Research article |
| 15 Apr 2021
| 15 Apr 2021
The development and persistence of soil moisture stress during drought across southwestern Germany
Erik Tijdeman
CORRESPONDING AUTHOR
Hydrology and Climatology, Institute of Geography, Heidelberg University, Heidelberg, Germany
Lucas Menzel
Hydrology and Climatology, Institute of Geography, Heidelberg University, Heidelberg, Germany
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Cited
18 citations as recorded by crossref.
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- An integrated framework for non-stationary hydrological drought assessment using time-varying parameter standardized streamflow index and time-varying threshold level method M. Wang et al. 10.1016/j.ejrh.2025.102329
- Crown die-back of peri-urban forests after combined heatwave and drought was species-specific, size-dependent, and also related to tree neighbourhood characteristics H. Lv et al. 10.1016/j.scitotenv.2023.169716
- A web-based system for satellite-based high-resolution global soil moisture maps M. Khazaei et al. 10.1016/j.cageo.2022.105250
- Assessing the impact of extreme climate events on European gross primary production H. Zhang et al. 10.1016/j.agrformet.2024.110374
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- The Dynamics of Vegetation Evapotranspiration and Its Response to Surface Meteorological Factors in the Altay Mountains, Northwest China A. Aili et al. 10.3390/su16198608
- An attention-aware LSTM model for soil moisture and soil temperature prediction Q. Li et al. 10.1016/j.geoderma.2021.115651
- Adjusting line quantum sensing to improve leaf area index measurements and estimations in forests G. Battuvshin & L. Menzel 10.1016/j.mex.2022.101805
- Hydrological variability in southern Siberia and the role of permafrost degradation L. Han & L. Menzel 10.1016/j.jhydrol.2021.127203
- Different drought types and the spatial variability in their hazard, impact, and propagation characteristics E. Tijdeman et al. 10.5194/nhess-22-2099-2022
- Evaluation of flash drought under the impact of heat wave events in southwestern Germany M. Wang et al. 10.1016/j.scitotenv.2023.166815
- Deciphering the stratified distribution and evolution of deep soil drought and its environmental controls: New evidence from continuous fiber optic monitoring in 0–30 m profile Y. Tong et al. 10.1016/j.geoderma.2025.117168
- Vegetation controls on surface energy partitioning and water budget over China X. Lan et al. 10.1016/j.jhydrol.2020.125646
- Separating the impact of climate change and human activities on the connection between meteorological and hydrological drought J. Fu et al. 10.1002/hyp.15258
16 citations as recorded by crossref.
- A 1 km daily soil moisture dataset over China using in situ measurement and machine learning Q. Li et al. 10.5194/essd-14-5267-2022
- Flash droughts and their impacts—using newspaper articles to assess the perceived consequences of rapidly emerging droughts P. Henrique Lima Alencar et al. 10.1088/1748-9326/ad58fa
- An integrated framework for non-stationary hydrological drought assessment using time-varying parameter standardized streamflow index and time-varying threshold level method M. Wang et al. 10.1016/j.ejrh.2025.102329
- Crown die-back of peri-urban forests after combined heatwave and drought was species-specific, size-dependent, and also related to tree neighbourhood characteristics H. Lv et al. 10.1016/j.scitotenv.2023.169716
- A web-based system for satellite-based high-resolution global soil moisture maps M. Khazaei et al. 10.1016/j.cageo.2022.105250
- Assessing the impact of extreme climate events on European gross primary production H. Zhang et al. 10.1016/j.agrformet.2024.110374
- Compound events in Germany in 2018: drivers and case studies E. Xoplaki et al. 10.5194/nhess-25-541-2025
- Assessment of Two Drought Indices to Quantify and Characterize Drought Incidents: A Case Study of the Northern Part of Burundi J. Ndayiragije et al. 10.3390/atmos13111882
- Fungi Associated With Woody Tissues of European Beech and Their Impact on Tree Health G. Langer & J. Bußkamp 10.3389/fmicb.2021.702467
- The Dynamics of Vegetation Evapotranspiration and Its Response to Surface Meteorological Factors in the Altay Mountains, Northwest China A. Aili et al. 10.3390/su16198608
- An attention-aware LSTM model for soil moisture and soil temperature prediction Q. Li et al. 10.1016/j.geoderma.2021.115651
- Adjusting line quantum sensing to improve leaf area index measurements and estimations in forests G. Battuvshin & L. Menzel 10.1016/j.mex.2022.101805
- Hydrological variability in southern Siberia and the role of permafrost degradation L. Han & L. Menzel 10.1016/j.jhydrol.2021.127203
- Different drought types and the spatial variability in their hazard, impact, and propagation characteristics E. Tijdeman et al. 10.5194/nhess-22-2099-2022
- Evaluation of flash drought under the impact of heat wave events in southwestern Germany M. Wang et al. 10.1016/j.scitotenv.2023.166815
- Deciphering the stratified distribution and evolution of deep soil drought and its environmental controls: New evidence from continuous fiber optic monitoring in 0–30 m profile Y. Tong et al. 10.1016/j.geoderma.2025.117168
2 citations as recorded by crossref.
Latest update: 23 Apr 2025
Short summary
Low amounts of soil moisture (SM) in the root zone negatively affect crop health. We characterized the development and duration of SM stress across the croplands of southwestern Germany. Development time mainly varied within drought years and was related to the available water-holding capacity of the root zone. Duration varied both within and between drought years and was especially high in 2018. Sensitivity analyses showed that (controls on) SM stress and SM drought characteristics differ.
Low amounts of soil moisture (SM) in the root zone negatively affect crop health. We...
