Climate Flashcards

1
Q

Synoptic Scale

A

Anti cyclones, depressions, tropical cyclones, trade winds

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2
Q

Layers of the atmosphere

A

troposphere (0-12km), stratosphere (12km-48km), mesosphere (48km-85km), thermosphere (87km-100km)

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3
Q

Ozone layer

A

20-30km

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4
Q

What are the non variant and variant gases and their percentages

A
Non variant
Nitrogen -78%
Oxygen- 20.1% 
Argon- 1%
Variant
Water vapour, carbon dioxide, ozone
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5
Q

Meaning of non variant and variant gases

A

Non variant- same concentration throughout the atmosphere

variant- different concentrations throughout the atmosphere

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6
Q

Irradiance

A

the amount of solar radiation on a surface perpendicular to the solar beam

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7
Q

Difference between global energy balance and radiation budget

A

Global energy balance: balance between incoming energy from the sun and outgoing heat from earth. It regulates the state of the earth’s climate. It is energy balance on a smaller, more local
Radiation Budget: balance between incoming energy from the sun and outgoing long wave (thermal) and reflected shortwave energy from the earth.

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8
Q

Difference between global energy balance and radiation budget (symbols)

What do these symbols mean?

A

Energy Balance: Q= Qg+ Qe+Qh
Qh= sensible heat
Qg=conduction of heat from soil
Qe= latent heat
Radiation Budget:
Q
=K+L (day)
Q=L (night)
Q= decrease K- increase K+ decrease L− increase L (daytime and positive)
Q
= decrease L −increase L (noncturnal and negative)
Q*= global distribution of net radiation or principle energy source which drives the circulation system
K= short wave radiation, L= long wave radiation

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9
Q

What are the factors that influence net radiation?

A

Diurnal, seasonal, and latitudinal variability, composition of the atmosphere, surface types, solar variability

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10
Q

Definition of shortwave and long wave r

A

Short wave radiation- energy from the sun

Long wave radiation- energy that is reflected from the earth

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11
Q

Planacks Law

A

the electromagnetic radiation emitted by a black body on thermal equilibrium at a definite temperature

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12
Q

Factors affecting temperature

A
Pressure gradient force 
Elevation
Latitude 
Season 
Proximity to bodies of water
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13
Q

Global atmospheric circulation

A
  1. Subtropical or Hadley Cell
  2. The mid-latitude or ferrel cell
  3. High latitude or polar cell
  4. Intertropical convergence zone
  5. Polar front
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14
Q

Major forces generating air motion

A
  1. Pressure Gradient Force- force between low and high pressure systems- drives air from high pressure to low pressure
  2. Coriolis Force- deflection by earth’s rotation left in southern hemisphere, right in northern hemisphere
  3. Centripetal Force- curved motion of air
  4. Friction- retarding influence on the surface of the earth
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15
Q

What is an anticyclone

A
  • Closed high pressure system with a general west-east trending axis
  • Associated with upper and lower level convergence and subsidence
  • Weather typically fine, with light winds
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16
Q

What is a depression

A
  • Forms in association with fronts
  • Rotate clockwise
  • Air in these system ascends, rather than subsiding in high pressure systems, cools and condenses forming clouds
  • associated with intense rain cold temperatures
  • east coast lows
17
Q

What is a front

A
  • Convergence zone of two airbuses with distinctly different temperature and humidity characteristics
  • Warm air rises over cool air, moisture vapour condenses to produce cloud, and precipitation
18
Q

Warm front

A

Warm air replacing cold air

Precipitation is typically observed often with nimbostratus before clearing weather

19
Q

Cold front

A

Cold air replacing warm air

Precipitation associated with rearward sloping ascent in concentrated close to the frontal zone

20
Q

Monsoon

A

A collection of low pressure systems which are persistent in the tropical north in summertime
Driven by trough
Important for rainfall- 80% of annual rainfall in northern Australia between dec and mar