Atmosphere 2 (lecture 20) Flashcards

1
Q

Phases of water on earth

A

water vapour (gas), liquid water (aerosol), and solid ice (aerosol)

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2
Q

Amount of water vapour in the atmosphere

A

0.3% to 4%

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3
Q

Dalton’s law of partial pressures

A

the pressures of a mixture of gases can be expressed as the sum of the partial pressures of all the components

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4
Q

Latent heat

A

the energy that is released/absorbed when water changes state

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5
Q

Saturation pressure

A

the partial pressure of water at saturation and represents the maximum amount of water vapour that air can hold at equilibrium at a particular temperature

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6
Q

relative humidity

A

the partial pressure of water divided by the saturation pressure

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7
Q

Condensation occurs when relative humidity is

A

100%

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8
Q

Adiabatic time-lapse rate

A

as air masses rise, the pressure falls and they cool at a constant rate of 10degrees per km

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9
Q

The adiabatic cooling of rising air causes condensation because

A

colder air has less capacity for moisture

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10
Q

Condenstation releases energy as ______

A

latent heat

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11
Q

Moist adiabatic lapse rate

A

6 degrees per km

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12
Q

moist adiabatic lapse rate is different from lapse rate due to

A

Adiabatic cooling of rising air causes condensation that releases energy as latent heat. This offsets adiabatic cooling

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13
Q

Condensation occurs when

A

water vapor forms liquid water or ice

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14
Q

The first nucleus of a new waterdrop or ice crystal required energy input called ______

A

nucleation energy

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15
Q

Nucleation is easier on a ____ surface

A

solid

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16
Q

Bergeron process

A

the process by which supercooled water droplets release vapour that condenses on ice crystals and clouds of water and ice forms

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17
Q

Below ___ degrees, water droplets are all ice in clouds

A

-20

18
Q

The process of forming clouds

A
  1. air rises
  2. adiabatic cooling reduces the temperature of an air mass
  3. cooling air increases the relative humidity until condensation occurs
19
Q

4 basic ways air is forced to rise and cool to form clouds

A

density lifting, frontal lifting, orographic lifting, and convergence lifting

20
Q

Convergence lifting

A

occurs where masses of air collide forcing them to rise (such as at an island)

21
Q

Density lifting

A

occurs when warm and low-density air rises and expands

22
Q

Frontal lifting

A

occurs when the movement of air masses drives warm air over cold

23
Q

Orographic lifting

A

occurs where a mountain range forces air masses to rise and where dry ar descends down the other side of the mountain

24
Q

Cloud types

A

cumulus, stratus, and cirrus

25
Q

Clouds are classified based on their:

A

shape and altitude/position, and sometimes: origin and the amount of possible rain/snow coming from them.

26
Q

Cumulus clouds

A

have a flat base and a domed top that is typical of rising warm air. The flat base at the surface is where the water reaches its condensation point.

27
Q

Cumulus clouds generally form at ____ altitudes

A

lower (2-6 km)

28
Q

Stratus Clouds

A

form horizontally extensive flat layers, and are typical of frontal lifting where warm air spreads over cold.

29
Q

Stratus clouds generally form at ____ altitudes

A

lower (2km)

30
Q

Cirrus clouds

A

wispy, high altitude made of ice particles in the upper troposphere

31
Q

Cirrus clouds generally form at ___ altitudes

A

high - above 6km in the troposphere

32
Q

Names for higher elevation cumulus clouds

A

altocumulus and cirrocumulus

33
Q

Names for higher elevation stratus clouds

A

altostratus, and cirrostratus

34
Q

Cloud variants

A

cumulonimbus, nimbostratus, and stratocumulus

35
Q

Cumulonimbus cloud variants

A

are associated with heavy rain and lightning. This cloud can hit the top of the troposphere as the release of latent heat during condensation allows air masses to rise.

36
Q

Nimbostratus cloud variants

A

Stratus clouds that cover the entire sky, and are associated with heavy rain and snow

37
Q

Stratocumulus cloud variants

A

Occurs when cumulus clouds emerge to form a semi-continuous layer in the atmosphere with little precipitation.

38
Q

Solar radiation

A

the ultimate driving force of atmospheric circulation, weather, and climate, as well as ocean currents including deep circulation

39
Q

Solar energy flux

A

the amount of energy in an electromagnetic wave that passes a perpendicular surface per unit time (measured in W/m^2)

40
Q

Flux from the sun

A

1370 W/m^2

41
Q

Solar flux is lower at the equator because

A

radiation hits at a higher angle, distributing energy over a wider area

42
Q

Precession

A

determines which hemisphere points towards the sun at certain points in the orbit