water budgets

    Cards (35)

    • What is the water budget?
      The annual balance between precipitation, evapotranspiration, and runoff
    • How is the water budget calculated?
      Using the formula P=P =E+ E +R±S R \pm S
    • What do the variables in the water budget formula represent?
      P is precipitation, E is evapotranspiration, R is runoff, and S represents changes in storage
    • At what scales can the water budget be calculated?
      From global to local scales
    • What does a national or regional water budget indicate?
      The amount of water available for human use
    • What is available soil water?
      The amount of water that can be stored in the soil and is available for growing crops
    • How can farmers use available soil water information?
      To identify when irrigation might be required and how much
    • What is a river regime?
      The annual variation in the discharge or flow of a river at a particular point
    • What factors influence the character of a river's regime?
      Size of the river, precipitation, temperatures, geology, vegetation cover, and human activities
    • How is river discharge usually measured?
      In cumecs
    • What do storm hydrographs show?
      Discharge changes over a short period of time, often no more than a few days
    • What are the main features of a hydrograph?
      Rising limb, peak discharge, lag time, falling limb, and base flow
    • What is lag time in a hydrograph?
      The time interval between peak rainfall and peak discharge
    • How does the shape of a storm hydrograph vary?
      It varies from one rain event to the next and from one river to another
    • What are 'flashy' hydrographs characterized by?
      Short lag time, high peak discharge, and steep rising limbs
    • What are 'delayed' hydrographs characterized by?
      Long lag time, low peak discharge, and gently inclined limbs
    • What is the impact of urbanization on storm hydrographs?
      It increases the flood risk and changes the characteristics of the land surface
    • How does construction work affect hydrological processes?
      It leads to the removal of vegetation cover, exposing soil and increasing runoff
    • What happens to rainwater in urban areas?
      It is swiftly fed into drains by gutters and pipes
    • How do drains and sewers affect rainwater?
      They reduce the distance and time rainwater travels before reaching a stream or river channel
    • What is the effect of channelization of urban rivers?
      It guards against flooding but can lead to more devastating floods
    • Why is urbanization a concern for flood risk?
      Many towns and cities are located close to rivers, increasing flood risk
    • What role do planners play in managing flood risk?
      They help manage the impacts of urbanization on flood risk
    • What actions are involved in flood risk management?
      Strengthening embankments, implementing flood emergency procedures, and steering development away from high-risk areas
    • What are the interacting factors affecting the shape of storm hydrographs?
      • Weather/climate: Intense storms vs. steady rainfall
      • Rock type: Impermeable vs. permeable rocks
      • Soils: Low vs. high infiltration rates
      • Relief: High steep slopes vs. low gentle slopes
      • Basin size: Small basins vs. larger basins
      • Shape: Circular vs. elongated basins
      • Drainage density: High vs. low drainage density
      • Pre-existing conditions: Wet vs. dry basins
      • Vegetation: Bare/low density vs. dense vegetation
      • Human activity: Urbanization vs. reforestation
    • How do impermeable rocks affect storm hydrographs?
      They restrict percolation and encourage rapid surface runoff
    • How do permeable rocks affect storm hydrographs?
      They allow percolation and limit rapid surface runoff
    • How does soil type influence storm hydrographs?
      Clay soils have low infiltration rates, while sandy soils have high infiltration rates
    • How does relief affect storm hydrographs?
      High, steep slopes promote surface runoff, while low, gentle slopes allow infiltration
    • How does basin size affect storm hydrographs?
      Small basins tend to have flashy hydrographs, while larger basins have more delayed hydrographs
    • How does the shape of a basin influence storm hydrographs?
      Circular basins have shorter lag times, while elongated basins tend to have delayed hydrographs
    • How does drainage density affect storm hydrographs?
      High drainage density means water moves quickly to the measuring point, while low density means slower movement
    • How do antecedent conditions affect storm hydrographs?
      Wet basins lead to low infiltration, while dry basins allow high infiltration
    • How does vegetation affect storm hydrographs?
      Bare or low-density vegetation leads to low interception, while dense vegetation increases interception
    • How does human activity influence storm hydrographs?
      Urbanization creates impermeable surfaces, while reforestation increases interception
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