CIVE 634 - Surface-water Hydrology - Videos - Fall 2020
- Water balance I: Water balance using catchment wetting.
- Water balance II: Why is the cybernetic hydrologic balance better suited for yield hydrology
than the conventional approach?
- Evaporation I: The psychrometric constant.
- Evaporation II: The Penman-Monteith method.
- Infiltration I: My conversation with Vic Mockus.
- Infiltration II: Initial abstraction revisited.
- Overland flow I: Water does not flow uphill!
- Hydroclimatology I: Signal or noise.
- Hydroclimatology II: Q&A on the return period to be used for design.
- Hydroclimatology III: The ford bridge: Sustainable river crossings in arid regions.
- Hydroclimatology IV: [A drought] Every four years.
- Hydroclimatology V: The untimely drought.
- Catchment routing I: The Pfafstetter coding system for watershed identification.
- Catchment routing II: The true source of the Missouri river.
- Catchment routing III: Runoff diffusion reexamined.
- Catchment routing IV: Synthetic unit hydrographs explained.
- Catchment routing V: A general dimensionless unit hydrograph.
- Catchment routing VI:
Cascade and convolution: One and the same.
- Catchment routing VII: Creager and flood wave diffusion.
- Catchment routing VIII: A channel in the middle of the street.
- Catchment routing IX: A hydrodynamic watershed model.
- Catchment routing X: Comparison of two types of Clark unit hydrographs.
- Channel routing I: Muskingum-Cunge method explained.
- Channel routing II: Analytical verification of Muskingum-Cunge routing.
- Channel routing III: The Att-Kin model.
- Channel routing IV: Steady vs unsteady flow with HEC-RAS.
- Channel routing V: The Thomas problem with online computation.
- Channel routing VI: Causes of runoff diffusion.
- Climate change I: Plants and animals: How many are they?
- Climate change II: Effect of global climate change on the White Range of Peru.
- Climate change III: Milestones in global climate change.
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