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dc.contributor.authorVaheddoost Babak:: Mohammadi Babak:: Safari Mir Jafar Sadegh
dc.date.accessioned2024-04-06T12:16:57Z
dc.date.available2024-04-06T12:16:57Z
dc.date.issued2023
dc.identifier.urihttp://dx.doi.org/10.3390/su152115675
dc.identifier.urihttps://dspace.yasar.edu.tr/handle/20.500.12742/19368
dc.description.abstractThis study addressed the intricate interplay between meteorological droughts and groundwater level fluctuations in the vicinity of Mount Uludag in Bursa Turkey. To achieve this an exhaustive analysis encompassing monthly precipitation records and groundwater level data sourced from three meteorological stations and eight groundwater observation points spanning the period from 2007 to 2018 was performed. Subsequently this study employed the Standard Precipitation Index (SPI) and Standard Groundwater Level (SGL) metrics meticulously calculating the temporal extents of drought events for each respective time series. Following this a judicious application of both the Thiessen and Support Vector Machine (SVM) methodologies was undertaken to ascertain the optimal groundwater observation wells and their corresponding SGL durations aligning them with SPI durations tied to the selected meteorological stations. The SVM technique in particular excelled in the identification of the most pertinent observation wells. Additionally the Elman Neural Network (ENN) and its optimized version through the Firefly Algorithm (ENN-FA) demonstrated their prowess in accurately predicting SPI durations based on SGL durations. The results were favorable as evidenced by the commendable performance metrics of the Normalized Root Mean Square Error (NRMSE) the Nash-Sutcliffe Efficiency (NSE) the product of the coefficient of determination and the slope of the regression line (bR2) and the Kling-Gupta Efficiency (KGE). Consequently the favorable simulation results were construed as evidence supporting the presence of a discernible association between SGL and the duration of the SPI. As we substantiate the concordance between the temporal extent of meteorological droughts and the perturbations in groundwater levels this unmistakably underscores the fact that the historical fluctuations in groundwater levels within the region were predominantly attributable to climatic influences rather than being instigated by anthropogenic activities. Nevertheless it is imperative to underscore that this revelation should not be misconstrued as an endorsement of future heedless exploitation of groundwater resources.
dc.titleThe Association between Meteorological Drought and the State of the Groundwater Level in Bursa Turkey
dc.typeArticle
dc.relation.journalSUSTAINABILITY
dc.identifier.doi10.3390/su152115675
dc.relation.volume15
dc.relation.issue21
dc.identifier.issue21
dc.identifier.volume15


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