Climate Flashcards
Synoptic Scale
Anti cyclones, depressions, tropical cyclones, trade winds
Layers of the atmosphere
troposphere (0-12km), stratosphere (12km-48km), mesosphere (48km-85km), thermosphere (87km-100km)
Ozone layer
20-30km
What are the non variant and variant gases and their percentages
Non variant Nitrogen -78% Oxygen- 20.1% Argon- 1% Variant Water vapour, carbon dioxide, ozone
Meaning of non variant and variant gases
Non variant- same concentration throughout the atmosphere
variant- different concentrations throughout the atmosphere
Irradiance
the amount of solar radiation on a surface perpendicular to the solar beam
Difference between global energy balance and radiation budget
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.
Difference between global energy balance and radiation budget (symbols)
What do these symbols mean?
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
What are the factors that influence net radiation?
Diurnal, seasonal, and latitudinal variability, composition of the atmosphere, surface types, solar variability
Definition of shortwave and long wave r
Short wave radiation- energy from the sun
Long wave radiation- energy that is reflected from the earth
Planacks Law
the electromagnetic radiation emitted by a black body on thermal equilibrium at a definite temperature
Factors affecting temperature
Pressure gradient force Elevation Latitude Season Proximity to bodies of water
Global atmospheric circulation
- Subtropical or Hadley Cell
- The mid-latitude or ferrel cell
- High latitude or polar cell
- Intertropical convergence zone
- Polar front
Major forces generating air motion
- Pressure Gradient Force- force between low and high pressure systems- drives air from high pressure to low pressure
- Coriolis Force- deflection by earth’s rotation left in southern hemisphere, right in northern hemisphere
- Centripetal Force- curved motion of air
- Friction- retarding influence on the surface of the earth
What is an anticyclone
- 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