Summary WS Flashcards

1
Q

What is a hydrograph?

A

Graphs showing river discharge over time, particularly during and after rainfall events.

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2
Q

Components of a hydrograph

A
  • Rising limb (increase in discharge)
  • Peak discharge
  • Falling limb (decrease in discharge).
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3
Q

Uses of a hydrograph

A

Assessing flood risk, understanding river behavior.

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4
Q

Climate factors affecting the water cycle

A

Temperature, precipitation patterns, humidity influence evaporation and precipitation rates.

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5
Q

Major stores

A

Cryosphere
Atmosphere
Lithosphere
Hydrosphere
Biosphere

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6
Q

Water cycle & affect of ice age

A
  • Milankovitch cycle
  • Glaciation (every 100,000 years)
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7
Q

What is a water budget?

A

A model which balances the inputs, outputs, and storage of water in a system. Shows surplus and deficits of water stores and the variation between evapotranspiration and precipitation

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8
Q

Human activities affecting water cycle

A

Deforestation, urbanization, irrigation alter infiltration, runoff, and evapotranspiration rates.

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9
Q

Land use change examples

A

Agriculture, urban development impact surface runoff and infiltration rates.

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10
Q

What is a river regime?

A

Seasonal variation in discharge and velocity of a river.

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11
Q

Influencing factors of a river regime

A

Precipitation patterns, temperature, drainage basin characteristics.

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12
Q

Impacts on river regime

A

Floods, droughts, erosion, sediment transport.

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13
Q

Water balance equation

A

Inputs = Outputs ± Changes in Storage.

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14
Q

Factors affecting water balance

A

Precipitation patterns, temperature, land use changes, human activities (irrigation, deforestation).

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15
Q

River regime influencing factors

A

Precipitation patterns, temperature, drainage basin characteristics.

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16
Q

Impacts if river regime

A

Floods, droughts, erosion, sediment transport.

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17
Q

Inputs of a drainage basin

A
  • Precipitation
  • Groundwater flow
  • Surface runoff
18
Q

Outputs if a drainage basin

A

River discharge, evaporation, percolation, outflow to other drainage basins

19
Q

Processes of a drainage basin

A

Precipitation, infiltration, surface runoff, evaporation, transpiration, groundwater flow.

20
Q

Water cycle stores

A

Oceans, ice caps, groundwater, rivers/lakes, soil moisture, atmospheric moisture.

21
Q

Water cycle resident times

A

Vary greatly from weeks to thousands of years, influencing the water cycle dynamics.

22
Q

Oceanic water dominance

A

Covers 72% of Earth’s surface, containing dissolved salts making it alkaline.

23
Q

Oceanic water attributes

A

Salinity, pH of 8.14, becoming more acidic due to increased atmospheric carbon.

24
Q

Cryospheric water dominance

A

1.9%

25
Q

Terrestrial Water

A

1.1%

26
Q

Significance of terrestrial water

A

Crucial for various ecological, hydrological, and biological processes.

27
Q

Terrestrial water categories

A

Surface water, groundwater, soil water, biological water.

28
Q

Atmospheric water dominance

A

0.001%

29
Q

Atmospheric water résidence time

A

10 days

30
Q

Terrestrial water résidence time

A

10,000 years

31
Q

Roles of atmospheric water

A

Absorbs, reflects, and scatters solar radiation; influences temperature and humidity.

32
Q

Cryospheric water locations

A

Sea ice, ice caps, ice sheets, alpine glaciers, permafrost.

33
Q

Cryospheric water attributes

A

Various forms of frozen water with different implications for sea level rise when melted.

34
Q

Hill slope water cycle natural factors

A

Intense precipitation and seasonal variations impact water cycle dynamics.

35
Q

Hillslipe water cycle influences

A

Deforestation, urbanization, and agricultural practices alter water movement.

36
Q

Impacts of human & natural changes

A

Alterations in inputs, transfers, or stores—via deforestation or drought—affect water movement within the basin.

37
Q

Cloud formation is controlled by

A

Amount of condensation nuclei present, temperature, high temperatures & global atmospheric circulation

38
Q

Relief as a factor

A

Water reaches the river channels more quickly in a steep sided upland river basin compared to a gentle sloping river basin. So, surface runoff is increased.

39
Q

Vegetation type/density

A

More vegetation = More interception, vegetation storage, stem flow, throughfall, transpiration and evaporation. With less surface runoff. Deciduous trees have more leaves in the summer but coniferous always have vegetation.

40
Q

Geology

A

Permeable rocks like limestone allow water to infiltrate into the soil and percolates into rocks which reduces surface runoff as throughfall, and groundwater flow are relatively slow.
Impermeable rocks like granite have higher drainage densities meaning that precipitation will reach a river very quickly causing a rapid increase in discharge.