Global Temperatures Flashcards

1
Q

What kind of system is Earth?

A

Open system

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2
Q

Average energy output for Earth?

A

240 W/m^2

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3
Q

Insolation in Tropics

A
  • high angle
  • constant year round
  • little seasonal variation
  • energy SURPLUS
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4
Q

Insolation in Polar Regions

A
  • low angle insolation (1/2 the year)
  • light surfaces
  • energy DEFICIT
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5
Q

Where is there an energy balance, latitude wise?

A

40 degress

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6
Q

Sensible Heat Flux-> symbol and definition

A
  • H
  • transfer of heat between surface and air
  • conduction and convection
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7
Q

Heat flux is LOW when…

A

Temperature surface > temperature of air

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8
Q

Heat flux is ZERO when…

A

surface temp = air temp

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9
Q

Heat Flux is HIGH when

A

Temperature surface < temperature of air

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10
Q

Ground Heat Flux -> symbol definition

A
  • energy which flows out/into the ground

- through conduction

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11
Q

Ground Flux is LOW when…

A

Temperature surface > temperature deep soil

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12
Q

Ground Flux is ZERO when…

A

temperature surface = temperature deep soil

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13
Q

Ground Flux is HIGH when

A

temperature surface < temperature deep soil

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14
Q

Urban Heat Islands

A
  • regular 1-6 degrees Celsius > surrounding
  • similar desert surface energy characteristics
  • max and min temps > surroundings
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15
Q

Temperature Controls: Latitude

A
  • insolation
  • different latitudes, different insolation angle
  • polar (deficit of energy, cooler), tropics (surplus, hotter)
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16
Q

Temperature Controls: Cloud Cover

A
  • high albedo
  • moderate temperatures
  • cooler days, warmer nights
17
Q

Temperature Controls: Altitude/Elevation

A
  • temperature decreases with increasing altitude
  • density decreases with increasing altitude
  • less dense air cannot absorb or radiate sensible heat easily
  • daily temperature range INCREASES with altitude
18
Q

Land-Water Heating Differences

A
  • evaporation and transparency
  • water has higher heat capacity than soil
  • fluid motion and mixing reduces water temperature differences
19
Q

Specific heat

A

-amount of energy required to raise a unit of mass by 1 degrees celcius

20
Q

heat capacity

A

mass * specific heat

21
Q

Maritime effect

A

locations exhibit moderating influences of the ocean

-stable relatively consistent weather

22
Q

Continental effect

A

-areas less affected by the sea have greater temperature range

23
Q

Wind Chill

A
  • cold & wind speed

- stronger wind, lower wind chill (more cold)

24
Q

Humidex

A
  • heat and humidity

- higher humidity, higher heat