geog 209 Flashcards

1
Q

Air Pressure

A

Pressure is force applied per unit area
Density is mass per unit volume
Gas law (P=TpC)

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2
Q

Vertical Comp of atmosphere

A

1.Troposphere
2.Stratosphere
3.Mesosphere
4.Thermosphere

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3
Q

Energy 2 types

A

Changing internal energy requires ‘work’ & everything else.
Internal stored energy
Kinetic ( movement relative to centre of mass )
Potential ( Energy that holds bonds together)

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4
Q

Energy transfer types

A

Conduction-when molecules collide and transfer heat
Convection heat by fluid ( water or air vertically)
Advection (by transport i.e. wind horizontally)
Radiation ( electromagnetic waves )

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5
Q

Radiation laws

A

Radiant energy (electromagnetic radiation from sun)

Stefan boltzmann’s law (Proportional energy emitted to temp)

Weins law
3000(K)/T(K)

Kirchhoff’s Law
good absorbers are good emitters, and poor absorbers are poor emitters

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6
Q

Earths radiative balance

A
  • Earth emits long term radiation
  • Water vapour condenses releasing heat
  • Air in contact with earth gains energy
  • Balance between incoming shortwave and emitted long wave
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7
Q

Frost

A

Sources : inversion
Mitigation: wind, heat

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8
Q

Saturation

A
  • Evaporating and Condensing molecules are equal
  • Impacted by temp ( easier with cold air)
  • Water vapour required to saturate air at any temp
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9
Q

Dew Point Definition

A

temperature to which the air would be cooled (with no change in water vapour or air pressure) for saturation to occur

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10
Q

Measures of humidity

A

Absolute: mass of water vapour per volume of air
Specific (mass of water vapour per total mass of air (kg/g)
Saturation, Mixing, Vapour

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11
Q

Pressure types

A

Partial pressure: total pressure inside a parcel due to molecule collisions
Vapour pressure: atmospheric pressure exerted by water vapour
Saturation vapour pressure: total pressure when saturation ( more temp needs more water for saturation)

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12
Q

Formation of dew and frost

A

Dew
- Clear
- Cool ground
- Air at dew point
Frost
- White frost forms on freezing surface past dew point

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13
Q

Fog

A
  • Formed on condensation nuclei by cooling air below saturation point or by evaporation and mixing
  • Maintained by new droplets forming
    Fog Types
  • Mixing fog from two air pockets of different temps
  • Upslope fog air rises cools and forms fog
  • Advection fog Warm air moving over cold surface such as ocean
  • Radiation fog (moist air with cold ground
    Fog Mitigation
  • Warm fog
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14
Q

Basic cloud types

A

Basic types of clouds
* Cirrus ( wispy)
* Stratus (layer)
* Cumulus (puffy)
* Nimbus (rain cloud)

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15
Q

Cloud classifications

A

High clouds (Cirrus)
- Thin
- Ice
- Elevation

Middle clouds (Cirrostratus)
- Water droplets
- Puffer
- 1k thick or less
Nimbostratus - low clouds
- Blanket of clouds low down in atmosphere
- Can be one thick layer
-
Clouds with vertical development (cumulus)
- Fair weather
- Puffs of cotton
- Typical short duration
- Height changes

Lenticular clouds
* Air forced up creates cloud
* Flat and rounded like a ufo/saucer
* Created by air moving over cloud

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