Ιδρυματικό Αποθετήριο
Πολυτεχνείο Κρήτης
EN  |  EL

Αναζήτηση

Πλοήγηση

Ο Χώρος μου

Stochastic modeling of aquifer level temporal fluctuations based on the conceptual basis of the soil-water balance equation

Varouchakis Emmanouil, Spanoudaki Katerina, Christopoulos Dionysios, Karatzas Georgios, Corzo Perez Gerald A.

Απλή Εγγραφή


URIhttp://purl.tuc.gr/dl/dias/7B9F19AE-1566-4383-A7C2-8974682563A6-
Αναγνωριστικόhttps://doi.org/10.1097/SS.0000000000000157-
Αναγνωριστικόhttps://journals.lww.com/soilsci/Fulltext/2016/06000/Stochastic_Modeling_of_Aquifer_Level_Temporal.2.aspx-
Γλώσσαen-
Μέγεθος8 pagesen
ΤίτλοςStochastic modeling of aquifer level temporal fluctuations based on the conceptual basis of the soil-water balance equationen
ΔημιουργόςVarouchakis Emmanouilen
ΔημιουργόςΒαρουχακης Εμμανουηλel
ΔημιουργόςSpanoudaki Katerinaen
ΔημιουργόςChristopoulos Dionysiosen
ΔημιουργόςΧριστοπουλος Διονυσιοςel
ΔημιουργόςKaratzas Georgiosen
ΔημιουργόςΚαρατζας Γεωργιοςel
ΔημιουργόςCorzo Perez Gerald A.en
ΕκδότηςWolters Kluwer Healthen
ΠερίληψηThe formulation of a model that can reliably simulate the temporal groundwater level fluctuations of an aquifer is important for effective water resource management and for the prevention of possible desertification effects. Mires Basin at the island of Crete, Greece, is part of a major watershed with significantly reduced groundwater resources because of overexploitation during the past 30 years. In this work, the interannual variability of groundwater level is modeled with a discrete time autoregressive exogenous variable (ARX) model that is based on physical grounds (soil-water balance equation). Precipitation surplus is used as an exogenous variable in the ARX model. Three new modified versions of the original form of the ARX model are proposed and investigated: the first considers a larger time scale; the second considers a larger time delay in terms of the groundwater level input; and the third considers the groundwater level difference between the last two hydrological years, which is incorporated in the model as a third input variable. Modeling results for the time series of the spatially averaged groundwater level show very good agreement, after an initial adaptation period, with measured data. Among the three modified versions of the original ARX model considered in this work, the third model version shows significantly better agreement with measured data.en
ΤύποςPeer-Reviewed Journal Publicationen
ΤύποςΔημοσίευση σε Περιοδικό με Κριτέςel
Άδεια Χρήσηςhttp://creativecommons.org/licenses/by/4.0/en
Ημερομηνία2018-10-12-
Ημερομηνία Δημοσίευσης2016-
Θεματική ΚατηγορίαARX modelen
Θεματική ΚατηγορίαEvapotranspirationen
Θεματική ΚατηγορίαGroundwater modelen
Θεματική ΚατηγορίαMessara Valleyen
Θεματική ΚατηγορίαSoil-wateren
Θεματική ΚατηγορίαSparsely gauged basinen
Βιβλιογραφική ΑναφοράE. A. Varouchakis, K. Spanoudaki, D. T. Hristopulos, G. P. Karatzas and G. A. C. Perez, "Stochastic modeling of aquifer level temporal fluctuations based on the conceptual basis of the soil-water balance equation," Soil Sci., vol. 181, no. 6, pp. 224-231, Jun. 2016. doi: 10.1097/SS.0000000000000157en

Υπηρεσίες

Στατιστικά