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Advective Flows. Surface Water Flow Options. Specified river, tributary flows (net flow) Specified lake, estuary flows (separate flows) Calculated flows using internal kinematic wave equations Calculated flows from external hydrodynamic model. Surface Water Flow Options – WASP Screen.
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Surface Water Flow Options • Specified river, tributary flows (net flow) • Specified lake, estuary flows (separate flows) • Calculated flows using internal kinematic wave equations • Calculated flows from external hydrodynamic model
Transport Flow Fields • Type 1 - Water Column flow carries both dissolved and particulate material • Type 2 - Pore Water flow carries dissolved material only • Type 3,4,5 – Solids “i” settling/resuspension carries particulate fraction only • Type 6 – Water evaporation/precipitation adjusts water volume only
WASP Transport Scheme • Each Flow Field can have multiple flow patterns and time functions. • WASP sums the individual flows for each segment to determine overall transport
10 cms 10 cms 10 cms 5cms 5 cms 5 cms 5 cms WASP uses each flow separately WASP sums and uses net flow Surface Flow Options 1. Net Flow Option + = 2. Gross Flow Option + =
WASP internally calculates flows, volumes, depths, widths Surface Flow Options 3. Kinematic Wave
Surface Flow Options 4. Hydrodynamic Linkage Hydrodynamic Interface Hydro WASP
0 1 0 Flow through Simple Pond Flow Path Continuity Function Flow Time Function Time, days
0 0 1 2 3 4 5 6 Upstream Flow Through River Flow Path Continuity Function Flow Time Function Time, days
7 0 0 1 2 3 4 5 6 Flow through River with Tributary Flow Path Continuity Functions Flow Time Function Time, days
4 0 0 1 2 3 6 7 Flow Path Continuity Function Flow Time Function 5 Time, days Branched Flow through River
Kinematic Wave Option • Applicable to 1-dimensional, branching streams, rivers • Calculates flow wave propagation and resulting variable flows, volumes, depths, and velocities throughout the network • Default rectangular channel shape unless user specifies hydraulic coefficients
Kinematic Wave Equations Continuity equation (mass balance): Momentum equation (momentum balance): gravity friction
Kinematic Wave Equations Substitute in Manning’s equation: Kinematic wave differential equation:
Kinematic Wave Input Data • Time-variable upstream and tributary inflows (m3/sec) • Continuity flow paths for main stem and each tributary (IQ, JQ, BQ) • Channel properties: • length (m), width (m), initial depth (m) • hydraulic exponents set to 0 • bottom slope (m/m) • Manning’s roughness coefficient
River Brandywine Flows – Annuminas • Flow Pattern • Average Flow, m3/sec
River Brandywine Flows – Hobbiton • Flow Pattern • Average Flow, m3/sec