Hydrology and Earth System Sciences
Hydrology and Earth System Sciences
HESS
Articles | Volume 25, issue 6
Articles | Volume 25, issue 6
https://doi.org/10.5194/hess-25-3519-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-25-3519-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 25, issue 6
Research article
 | 
22 Jun 2021
Research article |  | 22 Jun 2021

Deep desiccation of soils observed by long-term high-resolution measurements on a large inclined lysimeter

Markus Merk, Nadine Goeppert, and Nico Goldscheider

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Cited articles

Abichou, T., Liu, X., and Tawfiq, K.: Design Considerations for Lysimeters Used to Evaluate Alternative Earthen Final Covers, J. Geotech. Geoenviron., 132, 1519–1525, https://doi.org/10.1061/(ASCE)1090-0241(2006)132:12(1519), 2006. a
Albergel, C., Zheng, Y., Bonan, B., Dutra, E., Rodríguez-Fernández, N., Munier, S., Draper, C., de Rosnay, P., Muñoz-Sabater, J., Balsamo, G., Fairbairn, D., Meurey, C., and Calvet, J.-C.: Data assimilation for continuous global assessment of severe conditions over terrestrial surfaces, Hydrol. Earth Syst. Sci., 24, 4291–4316, https://doi.org/10.5194/hess-24-4291-2020, 2020. a
Allaire, S. E., Roulier, S., and Cessna, A. J.: Quantifying preferential flow in soils: A review of different techniques, J. Hydrol., 378, 179–204, https://doi.org/10.1016/j.jhydrol.2009.08.013, 2009. a
Augenstein, M., Goeppert, N., and Goldscheider, N.: Characterizing soil water dynamics on steep hillslopes from long-term lysimeter data, J. Hydrol., 529, 795–804, https://doi.org/10.1016/j.jhydrol.2015.08.053, 2015. a, b, c, d, e, f
Beck, H. E., Zimmermann, N. E., McVicar, T. R., Vergopolan, N., Berg, A., and Wood, E. F.: Present and future Köppen-Geiger climate classification maps at 1-km resolution, Scientific Data, 5, 180214, https://doi.org/10.1038/sdata.2018.214, 2018. a
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Soil moisture levels have decreased significantly over the past 2 decades. This decrease is not uniformly distributed over the observation period. The largest changes occur at tipping points during years of extreme drought, after which soil moisture levels reach significantly different alternate stable states. Not only the overall trend in soil moisture is affected, but also the seasonal dynamics.
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