Meteorology 1 Flashcards

1
Q

Standard Atmosphere

A
  • Air is a perfectly dry gas
  • MSL pressure of 29.92 inches of mercury
  • MSL temperature of 15ºC
  • Lapse rate of 1.98ºC/1000 ft
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2
Q

Principle Properties of the Atmosphere

A
  • Expansion
  • Compression
  • Mobility
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3
Q

Sources of Moisture in Atmosphere

A
  • Evaporation from oceans and lakes
  • Transpiration from vegetation
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4
Q

Heating Processes - Conduction

A
  • Heating through contact
  • Air is poor conductor so limited in effect
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5
Q

Heating Processes - Convection

A
  • Air that is warmed becomes less dense and tends to rise
  • Rising continues until density (temp) is same as surrounding air
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6
Q

Heating Processes - Turbulent Mixing

A
  • Friction causes eddies to form as air moves over surfaces
  • Disruption is proportionate to terrain (rough terrain = more mixing)
  • Can rise high into troposphere when combined with convection
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7
Q

Heating Processes - Advection

A
  • Horizontal movement of air masses
  • If it travels over a warm surface, the air mass will be warmed
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8
Q

Heating Processes - Compression

A
  • Descending (subsiding) air increases in pressure, in turn increasing temperature
  • Can occur along ridges of high pressure or over mountain ranges
  • Known as adiabatic heating
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9
Q

Heating Processes - Release of Latent Heat

A

Changing state down an energy level releases heat energy and vice versa

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10
Q

Cooling Processes - Expansion Cooling

A
  • Rising air expands, which causes a decrease in temperature (adiabatic cooling)
  • Dry or saturated adiabatic lapse rate
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11
Q

Cooling Processes - Orographic and Upslope Lift

A
  • Air flowing over topographical features causing it to rise
  • Slope of terrain not important
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12
Q

Cooling Processes - Frontal Lift

A

Expansion cooling when warm air is forced up along a frontal surface

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13
Q

Cooling Processes - Mechanical Turbulence

A

Friction causes eddies to form as air moves over surfaces

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14
Q

Cooling Processes - Convection

A

Rising air cools according to the appropriate lapse rate

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15
Q

Cooling Processes - Convergence

A

Air at the centre of a low pressure area rises, causing cooling

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16
Q

Inversions

A

Generally associated with a layer of haze with a very sharp top typically found 1000 ft AGL

17
Q

Factors Affecting Inversions

A
  • Wind
  • Cloud Affect
  • Topographical Effect
  • Maritime Effect
18
Q

Dew Point Lapse Rate

A

0.5ºC/1000 ft

19
Q

Vertical Development Clouds

A
  • Bases range from 1000 ft or lower to 10,000 ft or higher
  • Composed of water droplets or ice crystals
  • Usually contain super-cooled water above the freezing level
20
Q

Requirements for Formation of Fog

A
  • High Relative Humidity
  • Abundance of Condensation Nuclei
  • Mixing Action
  • Fog dissipates as air temp rises
21
Q

Radiation Fog

A

Formed on cool clear nights with high relative humidity

22
Q

Advection Fog

A
  • Formed in coastal areas when warm moist air moves over a cold land surface
  • Does not burn off, requires a change in wind direction
23
Q

Steam Fog

A
  • Formed when cool air moves over warm water surfaces
  • Found over rivers and small lakes
  • Evaporation occurs and saturates the air
24
Q

Ice Fog

A
  • Forms on very cold days
  • Consists of very small ice crystals
  • Associated with hoar frost
25
Q

Difference between fog and mist

A
  • Fog is less than 5/8 SM vis
  • Mist is more than 5/8 SM vis
26
Q
A