| نویسندگان | Mohammad Ghasem Akbari |
| نشریه | Journal of Groundwater Science and Engineering |
| شماره صفحات | 83-99 |
| شماره سریال | 14 |
| شماره مجلد | 3 |
| نوع مقاله | Full Paper |
| تاریخ انتشار | 2026 |
| نوع نشریه | چاپی |
| کشور محل چاپ | ایران |
| نمایه نشریه | Scopus |
| کلید واژه ها | Birjand aquifer; Data, scarce regions; Fuzzy, based approach; Groundwater table; Novel statistical model; Soft computing |
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چکیده مقاله
Groundwater modeling remains challenging due to heterogeneity and complexity of aquifer
systems, necessitating endeavors to quantify Groundwater Levels (GWL) dynamics to inform policymakers
and hydrogeologists. This study introduces a novel Fuzzy Nonlinear Additive Regression (FNAR) model to
predict monthly GWL in an unconfined aquifer in eastern Iran, using a 19-year (1998–2017) dataset from
11 piezometric wells. Under three distinct scenarios with progressively increasing input complexity, the
study utilized readily available climate data, including Precipitation (Prc), Temperature (Tave), Relative
Humidity (RH), and Evapotranspiration (ETo). The dataset was split into training (70%) and validation
(30%) subsets. Results showed that among three input scenarios, Scenario 3 (Sc3, incorporating all four
variables) achieved the best predictive performance, with RMSE ranging from 0.305 m to 0.768 m, MAE
from 0.203 m to 0.522 m, NSE from 0.661 to 0.980, and PBIAS from 0.771% to 0.981%, indicating low
bias and high reliability. However, Sc2 (excluding ETo) with RMSE ranging from 0.4226 m to 0.9909 m,
MAE from 0.3418 m to 0.8173 m, NSE from 0.2831 to 0.9674, and PBIAS from −0.598% to 0.968% across
different months offers practical advantages in data-scarce settings. The FNAR model outperforms conventional
Fuzzy Least Squares Regression (FLSR) and holds promise for GWL forecasting in data-scarce
regions where physical or numerical models are impractical. Future research should focus on integrating
FNAR with deep learning algorithms and real-time data assimilation expanding applications across diverse
hydrogeological settings.