Effects of different climatic conditions on soil water storage patterns
<p>The soil water storage (SWS) defines the crop productivity of a soil and varies under different climatic conditions.</p> <p>Pattern identification and quantification of these variations in SWS remain difficult due to the non-linear behaviour of SWS changes over time. Wave...
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Copernicus Publications
2025-01-01
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| Series: | Hydrology and Earth System Sciences |
| Online Access: | https://hess.copernicus.org/articles/29/313/2025/hess-29-313-2025.pdf |
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| author | A. Ehrhardt A. Ehrhardt J. Groh J. Groh J. Groh H. H. Gerke |
| author_facet | A. Ehrhardt A. Ehrhardt J. Groh J. Groh J. Groh H. H. Gerke |
| author_sort | A. Ehrhardt |
| collection | DOAJ |
| description | <p>The soil water storage (SWS) defines the crop productivity of a soil and varies under different climatic conditions.</p>
<p>Pattern identification and quantification of these variations in SWS remain difficult due to the non-linear behaviour of SWS changes over time. Wavelet analysis (WA) provides a tool to efficiently visualize and quantify these patterns by transferring the time series from the time domain into the frequency domain.</p>
<p>We applied WA to an 8-year time series of SWS, precipitation (<span class="inline-formula"><i>P</i></span>), and actual evapotranspiration (ET<span class="inline-formula"><sub>a</sub></span>) in similar soils of lysimeters in a colder and drier location and in a warmer and wetter location within Germany. Correlations between SWS, <span class="inline-formula"><i>P</i></span>, and ET<span class="inline-formula"><sub>a</sub></span> at these sites might reveal the influence of altered climatic conditions but also of subsequent wet and dry years on SWS changes.</p>
<p>We found that wet and dry years exerted an influence over SWS changes by leading to faster or slower response times of SWS changes in relation to precipitation with respect to normal years. The observed disruption of annual patterns in the wavelet spectra of both sites was possibly caused by extreme events. Extreme precipitation events were visible in SWS and <span class="inline-formula"><i>P</i></span> wavelet spectra. Time shifts in correlations between ET<span class="inline-formula"><sub>a</sub></span> and SWS became smaller at the wetter and warmer site over time in comparison to at the cooler and drier site, where they stayed constant. This could be attributed to an earlier onset of the vegetation period over the years and, thus, to an earlier ET<span class="inline-formula"><sub>a</sub></span> peak every year. This reflects the impact of different climatic conditions on soil water budget parameters.</p> |
| format | Article |
| id | doaj-art-0cc40428da56407a9bc323d72a03a8fe |
| institution | Kabale University |
| issn | 1027-5606 1607-7938 |
| language | English |
| publishDate | 2025-01-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Hydrology and Earth System Sciences |
| spelling | doaj-art-0cc40428da56407a9bc323d72a03a8fe2025-01-17T09:56:10ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382025-01-012931333410.5194/hess-29-313-2025Effects of different climatic conditions on soil water storage patternsA. Ehrhardt0A. Ehrhardt1J. Groh2J. Groh3J. Groh4H. H. Gerke5Working group “Isotope Biogeochemistry and Gas Fluxes”, Research Area 1 “Landscape Functioning”, Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, GermanyInstitute for Drilling Technology and Fluid Mining, TU Bergakademie Freiberg, Agricolastraße 22, 09599 Freiberg, GermanyWorking group “Isotope Biogeochemistry and Gas Fluxes”, Research Area 1 “Landscape Functioning”, Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, GermanyInstitute of Crop Science and Resource Conservation (INRES) – Soil Science and Soil Ecology, University of Bonn, Nußallee 13, 53115 Bonn, Germany Institute of Bio- and Geoscience IBG-3: Agrosphere, Forschungszentrum Jülich GmbH, 52425 Jülich, GermanyWorking group “Silicon Biogeochemistry”, Research Area 1 “Landscape Functioning”, Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, Germany<p>The soil water storage (SWS) defines the crop productivity of a soil and varies under different climatic conditions.</p> <p>Pattern identification and quantification of these variations in SWS remain difficult due to the non-linear behaviour of SWS changes over time. Wavelet analysis (WA) provides a tool to efficiently visualize and quantify these patterns by transferring the time series from the time domain into the frequency domain.</p> <p>We applied WA to an 8-year time series of SWS, precipitation (<span class="inline-formula"><i>P</i></span>), and actual evapotranspiration (ET<span class="inline-formula"><sub>a</sub></span>) in similar soils of lysimeters in a colder and drier location and in a warmer and wetter location within Germany. Correlations between SWS, <span class="inline-formula"><i>P</i></span>, and ET<span class="inline-formula"><sub>a</sub></span> at these sites might reveal the influence of altered climatic conditions but also of subsequent wet and dry years on SWS changes.</p> <p>We found that wet and dry years exerted an influence over SWS changes by leading to faster or slower response times of SWS changes in relation to precipitation with respect to normal years. The observed disruption of annual patterns in the wavelet spectra of both sites was possibly caused by extreme events. Extreme precipitation events were visible in SWS and <span class="inline-formula"><i>P</i></span> wavelet spectra. Time shifts in correlations between ET<span class="inline-formula"><sub>a</sub></span> and SWS became smaller at the wetter and warmer site over time in comparison to at the cooler and drier site, where they stayed constant. This could be attributed to an earlier onset of the vegetation period over the years and, thus, to an earlier ET<span class="inline-formula"><sub>a</sub></span> peak every year. This reflects the impact of different climatic conditions on soil water budget parameters.</p>https://hess.copernicus.org/articles/29/313/2025/hess-29-313-2025.pdf |
| spellingShingle | A. Ehrhardt A. Ehrhardt J. Groh J. Groh J. Groh H. H. Gerke Effects of different climatic conditions on soil water storage patterns Hydrology and Earth System Sciences |
| title | Effects of different climatic conditions on soil water storage patterns |
| title_full | Effects of different climatic conditions on soil water storage patterns |
| title_fullStr | Effects of different climatic conditions on soil water storage patterns |
| title_full_unstemmed | Effects of different climatic conditions on soil water storage patterns |
| title_short | Effects of different climatic conditions on soil water storage patterns |
| title_sort | effects of different climatic conditions on soil water storage patterns |
| url | https://hess.copernicus.org/articles/29/313/2025/hess-29-313-2025.pdf |
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