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  • 1
    Online Resource
    Online Resource
    Informa UK Limited ; 2021
    In:  Hydrological Sciences Journal Vol. 66, No. 5 ( 2021-04-04), p. 888-903
    In: Hydrological Sciences Journal, Informa UK Limited, Vol. 66, No. 5 ( 2021-04-04), p. 888-903
    Type of Medium: Online Resource
    ISSN: 0262-6667 , 2150-3435
    Language: English
    Publisher: Informa UK Limited
    Publication Date: 2021
    detail.hit.zdb_id: 2180448-5
    detail.hit.zdb_id: 625713-6
    SSG: 14
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  • 2
    Online Resource
    Online Resource
    Cellule MathDoc/Centre Mersenne ; 2024
    In:  Comptes Rendus. Géoscience Vol. 356, No. G1 ( 2024-06-18), p. 67-82
    In: Comptes Rendus. Géoscience, Cellule MathDoc/Centre Mersenne, Vol. 356, No. G1 ( 2024-06-18), p. 67-82
    Type of Medium: Online Resource
    ISSN: 1778-7025
    Language: English
    Publisher: Cellule MathDoc/Centre Mersenne
    Publication Date: 2024
    detail.hit.zdb_id: 2079109-4
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  • 3
    Online Resource
    Online Resource
    Copernicus GmbH ; 2021
    In:  Hydrology and Earth System Sciences Vol. 25, No. 10 ( 2021-10-14), p. 5447-5471
    In: Hydrology and Earth System Sciences, Copernicus GmbH, Vol. 25, No. 10 ( 2021-10-14), p. 5447-5471
    Abstract: Abstract. Drainage systems are currently implemented on agricultural plots subjected to temporary or permanent waterlogging issues. Drained plots account for 9 % of all arable soils in France. As such, the need for accurate hydrological modeling is crucial, especially in an unstable future context affected by climate change. The aim of this paper is to assess the capacity of the SIDRA-RU hydrological drainage model to represent the variability in pedoclimatic conditions within French metropolitan areas and to demonstrate the utility of this model as a long-term management tool. The model is initially calibrated using the KGE′ criterion as an objective function (OF) on a large and unique database encompassing 22 plots spread across France and classified according to three main soil textures (silty, silty–clay, and clayey). The performance of SIDRA-RU is evaluated by monitoring both the set of KGE′ calibration values and the quality of simulations on each plot with respect to high and low discharges, as well as the annual drained water balance. Next, the temporal robustness of the model is assessed by conducting, on selected plots, the split-sample test capable of satisfying the data requirements. Results show that the SIDRA-RU model accurately simulates drainage discharge, especially on silty soils. The performance on clayey soils is slightly weaker than that on silty soils yet remains acceptable. Similarly, the split-sample test indicates that SIDRA-RU is temporally robust on all three soil textures. Consequently, the SIDRA-RU model closely replicates the diversity of French drained soil and could be used for its long-term management potential.
    Type of Medium: Online Resource
    ISSN: 1607-7938
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2021
    detail.hit.zdb_id: 2100610-6
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  • 4
    Online Resource
    Online Resource
    Copernicus GmbH ; 2022
    In:  Hydrology and Earth System Sciences Vol. 26, No. 8 ( 2022-04-28), p. 2147-2159
    In: Hydrology and Earth System Sciences, Copernicus GmbH, Vol. 26, No. 8 ( 2022-04-28), p. 2147-2159
    Abstract: Abstract. The increasing air temperature in a changing climate will impact actual evaporation and have consequences for water resource management in energy-limited regions. In many hydrological models, evaporation is assessed using a preliminary computation of potential evaporation (PE), which represents the evaporative demand of the atmosphere. Therefore, in impact studies, the quantification of uncertainties related to PE estimation, which can arise from different sources, is crucial. Indeed, a myriad of PE formulations exist, and the uncertainties related to climate variables cascade into PE computation. To date, no consensus has emerged on the main source of uncertainty in the PE modeling chain for hydrological studies. In this study, we address this issue by setting up a multi-model and multi-scenario approach. We used seven different PE formulations and a set of 30 climate projections to calculate changes in PE. To estimate the uncertainties related to each step of the PE calculation process, namely Representative Concentration Pathway (RCP) scenarios, general circulation models (GCMs), regional climate models (RCMs) and PE formulations, an analysis of variance (ANOVA) decomposition was used. Results show that mean annual PE will increase across France by the end of the century (from +40 to +130 mm y−1). In ascending order, uncertainty contributions by the end of the century are explained by PE formulations (below 10 %), RCPs (above 20 %), RCMs (30 %–40 %) and GCMs (30 %–40 %). However, under a single scenario, the contribution of the PE formulation is much higher and can reach up to 50 % of the total variance. All PE formulations show similar future trends, as climatic variables are co-dependent with respect to temperature. While no PE formulation stands out from the others, the Penman–Monteith formulation may be preferred in hydrological impact studies, as it is representative of the PE formulations' ensemble mean and allows one to account for the coevolution of climate and environmental drivers.
    Type of Medium: Online Resource
    ISSN: 1607-7938
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2022
    detail.hit.zdb_id: 2100610-6
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