Human impact: Lowland hydrology

15 important questions on Human impact: Lowland hydrology

Lowlands are often induced by humans. True or false?

True

What are lowland catchments?

Not really a definition of a lowland areas.
Claudia: Areas where hydrological processes are influenced by shallow (less than 3 m below surface) GW.

What are differences between freely draining lowlands and polders (see slide!) - both are lowland catchments.

Freely:
  • Gradients are flow, so flow is slow but flow is gravity-driven
  • Are influenced by people, but natural system
  • Slightly sloping
  • Drained by brooks

Polder:
  • below land surface, water flow is pumped/levels are managed
  • Manmade
  • More stable GW level
    
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What are similarities between freely draining lowlands and polders?

Limited slope
Often located in river deltas
Shallow GW
Agriculturally productive
Attractive for settlement (often densely populated)

What are challenges in lowland catchments (advantages leading to challenges):

  • Floods
  • Climate change
  • Land use change (has to do with urbanisation and agri expansion)
  • Water quality detoriation (extensive agri use and population density)
  • Land subsidence (peat oxidation)
  • Increasing deman for information

Name (dis)advantages of parametric models (min 16)

Advantage:
  • Representation of processes by parameters
  • Easy to use
  • Relatively fast
  • Smaller risk of overparameterisastion than physicall

Disadvantage:
  • Need for calibration of parameters  
  • Over-parameterization (but not as bad with physically based models, in principle you shouldnt have to calibrate your model, but in theory you do)
  • No spatial information



Often used at catchment scale

What was a major problem until 2013?

Complex, spatially distributed models for lowland catchments OR simple, parametric models for sloping catchments

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Fill the gap: WALRUS    ....SEE SLIDE

Maximum soil moisture content (min 22/23)

Storage deficit: air part - lack of water in the soil
Brown part: soil particles
Water = water part

There's a strong relation in GW depth and SM content in lowland areas. True/False?

True (see above)

Which lessons were learned (min 41)

In lowland areas, there's a strong coupling between GW-unsaturated zone

dV indicates how dry it is = storage deficit
dG indicates GW depth = GW table

.....

What is lesson 2: wetnes-dependent flowroutes

  • Drainpipe flow
  • Ponding & overland flow
  • Macropore flow

How does this work in the model?

W is related to vadose zone and dV.
...
Relation between wetness index (W)

GW - SW feedback, has to do with SWlvl management. Name two ways in which SW lvls are managed?  SW = surface water

  1. Supply water from upstream
  2. Changing weir elevations

What is the 4-step effect of SW lvl management?

See slide 60

What is lesson 3: GW-SW feedback & how is this modelled in WALRUS?

Drainage: GW to SW
Infiltration: SF to GW

WALRUS: Part P is led to SW and GS and SW interact. Water can also be supplied/extracted externally from SW.

What do the external fluxes fXG and fXS represent?

Flow over catchment boundaries that occurs often

Draw graph
fxG = upward...

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