Modelling of Hydrological Processes in the Narew Catchment [recurso electrónico] / edited by Dorota Swiatek, Tomasz Okruszko.
Tipo de material: TextoSeries Geoplanet: Earth and Planetary SciencesEditor: Berlin, Heidelberg : Springer Berlin Heidelberg, 2011Descripción: XIV, 138 p. online resourceTipo de contenido: text Tipo de medio: computer Tipo de portador: online resourceISBN: 9783642190599Tema(s): Geography | Hydraulic engineering | Agriculture | Soil conservation | Earth Sciences | Hydrogeology | Soil Science & Conservation | AgricultureFormatos físicos adicionales: Printed edition:: Sin títuloClasificación CDD: 551.4 Clasificación LoC:GB1001-1199.8Recursos en línea: Libro electrónicoTipo de ítem | Biblioteca actual | Colección | Signatura | Copia número | Estado | Fecha de vencimiento | Código de barras |
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Libro Electrónico | Biblioteca Electrónica | Colección de Libros Electrónicos | GB1001 -1199.8 (Browse shelf(Abre debajo)) | 1 | No para préstamo | 375755-2001 |
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GB1001 -1199.8 Impacts of Global Change on the Hydrological Cycle in West and Northwest Africa | GB1001 -1199.8 Groundwater Base Level Changes and Adjoining Hydrological Systems | GB1001 -1199.8 Experimental Methods in Hydraulic Research | GB1001 -1199.8 Modelling of Hydrological Processes in the Narew Catchment | GB1001 -1199.8 Groundwater in the Arab Middle East | GB1001 -1199.8 Advances in the Research of Aquatic Environment | GB1001 -1199.8 Advances in the Research of Aquatic Environment |
Operational Rainfall/Snowmelt-runoff Model for Upper Narew River -- Multi-site Calibration and Validation of the Hydrological Component of SWAT in a large Lowland Catchment -- Automatic Calibration of the WetSpa Distributed Hydrological Model for small Lowland Catchments -- Modelling Hydrological Flow Paths during Snowmelt induced high flow event.
Since climate and land use strongly affect the runoff pattern and intensity of solute export, it is likely that some observations and conclusions formulated on the basis of investigations carried out in forested catchment may not be fully adequate to describe controls on solute export from agricultural watersheds. The primary objective of the present research is to better understand the flow paths that affect the fluxes of dissolved compounds from a small agricultural catchment during snowmelt. This book focuses on spring snowmelt, because this is the dominant hydrological event in many moderate and high latitude catchments and, thus, is regarded as a prominent factor influencing the quality of surface waters
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