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| 001 | 888981 | ||
| 005 | 20201230100831.0 | ||
| 024 | 7 | _ | |a 2128/26596 |2 Handle |
| 037 | _ | _ | |a FZJ-2020-05368 |
| 041 | _ | _ | |a English |
| 100 | 1 | _ | |a Ma, Yueling |0 P:(DE-Juel1)176840 |b 0 |e Corresponding author |u fzj |
| 111 | 2 | _ | |a AGU 2020 Fall Meeting |c Online |d 2020-12-01 - 2020-12-17 |w Online |
| 245 | _ | _ | |a An optimized indirect method to estimate groundwater table depth anomalies over Europe based on Long Short-Term Memory networks |
| 260 | _ | _ | |c 2020 |
| 336 | 7 | _ | |a Conference Paper |0 33 |2 EndNote |
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| 520 | _ | _ | |a Long Short-Term Memory (LSTM) networks are a deep learning technology to exploit long-term dependencies in the input-output relationship, which has been observed in the response of groundwater dynamics to atmospheric and land surface processes. We introduced an indirect method based on LSTM networks to estimate monthly water table depth anomalies (wtd_a) across Europe from monthly precipitation anomalies (pr_a). The network has further been optimized by including supplementary hydrometeorological variables, which are routinely measured and available at large scales. The data were obtained from daily integrated hydraulic simulation results over Europe from 1996 to 2016, with a spatial resolution of 0.11° (Furusho-Percot et al., 2019), and separated into a training set, a validation set and a test set at individual pixels. We compared test performances of the LSTM networks locally at selected pixels in eight PRUDENCE regions with random combinations of monthly pr_a, evapotranspiration anomaly, and soil moisture anomaly (θ_a) as input variables. The optimal combination of input variables was pr_a and θ_a, and the networks with this combination achieved average test R^2 between 47.88% and 91.62% in areas with simulated wtd ≤ 3 m. Moreover, we found that introducing θ_a improved the ability of the trained networks to handle new data, indicating the substantial contribution of θ_a to explain groundwater state variation. Therefore, including information about θ_a is beneficial, for instance in the estimation of groundwater drought, and the proposed optimized method may be transferred to a real-time monitoring of groundwater drought at the continental scale using remotely sensed soil moisture observations.Furusho-Percot, C., Goergen, K., Hartick, C., Kulkarni, K., Keune, J. and Kollet, S.: Pan-European groundwater to atmosphere terrestrial systems climatology from a physically consistent simulation, Sci. data, 6(1), 320, doi:10.1038/s41597-019-0328-7, 2019. |
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| 700 | 1 | _ | |a Montzka, Carsten |0 P:(DE-Juel1)129506 |b 1 |u fzj |
| 700 | 1 | _ | |a Bayat, Bagher |0 P:(DE-Juel1)177038 |b 2 |u fzj |
| 700 | 1 | _ | |a Kollet, Stefan |0 P:(DE-Juel1)151405 |b 3 |u fzj |
| 856 | 4 | _ | |u https://agu2020fallmeeting-agu.ipostersessions.com/default.aspx?s=C2-0F-E6-B5-74-26-9F-0B-3B-44-C8-A2-D3-74-AA-81# |
| 856 | 4 | _ | |u https://juser.fz-juelich.de/record/888981/files/IPoster.pdf |y OpenAccess |
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