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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




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


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
Content:
Front Matter....Pages i-xiv
Operational Rainfall/Snowmelt-Runoff Model for Upper Narew River....Pages 1-13
Multi-Site Calibration and Validation of the Hydrological Component of SWAT in a Large Lowland Catchment....Pages 15-41
Automatic Calibration of the WetSpa Distributed Hydrological Model for Small Lowland Catchments....Pages 43-62
Modeling Hydrological Flow Paths During Snowmelt Induced High Flow Event in a Small Agricultural Catchment....Pages 63-78
Modelling of Groundwater Fluctuations in the Area Between the Narew and Suprasl Rivers....Pages 79-87
Groundwater Modelling and Hydrological System Analysis of Wetlands in the Middle Biebrza Basin....Pages 89-109
Aspiration-Reservation Decision Support System for Siemianowka Reservoir....Pages 111-121
Hydraulic Conditions of Flood Wave Propagation in the Valley of the Narew River after the Siemianowka Dam Overtopping Failure....Pages 123-136
Back Matter....Pages 137-138


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
Content:
Front Matter....Pages i-xiv
Operational Rainfall/Snowmelt-Runoff Model for Upper Narew River....Pages 1-13
Multi-Site Calibration and Validation of the Hydrological Component of SWAT in a Large Lowland Catchment....Pages 15-41
Automatic Calibration of the WetSpa Distributed Hydrological Model for Small Lowland Catchments....Pages 43-62
Modeling Hydrological Flow Paths During Snowmelt Induced High Flow Event in a Small Agricultural Catchment....Pages 63-78
Modelling of Groundwater Fluctuations in the Area Between the Narew and Suprasl Rivers....Pages 79-87
Groundwater Modelling and Hydrological System Analysis of Wetlands in the Middle Biebrza Basin....Pages 89-109
Aspiration-Reservation Decision Support System for Siemianowka Reservoir....Pages 111-121
Hydraulic Conditions of Flood Wave Propagation in the Valley of the Narew River after the Siemianowka Dam Overtopping Failure....Pages 123-136
Back Matter....Pages 137-138
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