Sierra Nevada Flashcards

1
Q

What is the difference between permeability vs. porosity?

A

Permeability: ability to allow water to flow through rock

Porosity: refers to ability to store water within holes (pores) within rock

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2
Q

What is a confined aquifer?

A
  • Water is stored in porous rock surrounded by impermeable rock
  • Means water can’t flow away or aquifer be replenished
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3
Q

What is an unconfined aquifer?

A
  • Porous rock surrounded by permeable
  • means water can percolate and flow out of aquifer
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4
Q

What do the Rockies act as?

A
  • a watershed (AKA drainage basin)
    • Colorado River basin flows into West -> Mexico
    • Great Plains basin is in East
      • Includes Ogallala Aquifer
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5
Q

What inputs are there into river basins?

A
  • Rainfall (convectional or frontal)
    • Location determined by proximity to ocean (frontal) or topography (convectional)
      • eg. Mountains create rain shadows
  • Rocky Mountain snowpack meltwater feeds river seasonally
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6
Q

What affects the output from river basins?

A
  • Level of interception (may vary due to extent of deforestation)
  • Level of runoff
    • eg. Caliche in Great Plains reduces infiltration
  • Geology
    • Only unconfined aquifers will be replenished
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7
Q

What are the reasons for variation in hydrological balance of river basins?

A
  • Anthropogenic:
    • Eg. Human extraction of water from confined aquifers
  • Secular: LT climate change (reduction of water in Colorado Basin and Great Plains)
  • Periodity:
    • Annual, seasonal, monthly, diurnal changes to water flow
  • Stochastic:
    • random factors eg. localised thunderstorms
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8
Q

What is the main input of water into the Colorado River basin?

A
  • Rain from North Pacific Ocean front systems
    • cold frontal systems leave snow on the Sierra Nevada
    • Rain shadow effect on east side of SN (Death Valley/Mojave desert)
    • snowmelt during summer provides runoff
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9
Q

What is caliche?

A
  • impermeable layer of calcium carbonate on bottom of aquifer
    • prevents it from being recharged
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10
Q

What has happened to the water table in the Great Plains?

A
  • dropped by 1.5m/yr
    • wells have been deepened to access water
  • in some places water has been totally drained
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11
Q

What sort of aquifer is the High Plains aquifer?

A
  • unconfined
  • parts of the aquifer is covered by a caliche layer
  • permeability is allowed by playa lakes
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12
Q

What are the main uses of water in the Colorado River Basin?

A

Irrigation:
- 2.1m acres to 15.5m acres in 2015

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13
Q

What is grown in the Colorado River Basin?

A
  • wheat (largest in US)
  • ethanol
  • cotton
  • cheese (largest in world)
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14
Q

Why is there water insecurity in the Colorado River Basin?

A
  • The High Plains aquifer is unconfined for now
    • deterioration of playa soils is increasing though
  • region is semi-arid, evaporation rate is high
    • steady winds are also present —> evaporation
  • increased evaporation is increasing amount of caliche in soil
    • making aquifer more confined
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15
Q

What are Playa Lakes?

A
  • lakes which have soil that does not contain caliche
    • allows for aquifer to be recharged
  • farming destroys playa
    • creates layer of caliche as soil moisture evaporates
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16
Q

What strategies are states using to allow water levels to recover?

A
  • usage of more efficient irrigation systems (centre pivot)
  • farmers use more recycled water
  • plant crops that use less water (sunflowers)