Physical Geography 101
Global Energy System
Global Energy System
A system is defined as:
Open System: A system that does interact with other systems or items outside of the system.
Closed System: A system that does not interact with other systems of items outside of the closed system.
Incoming and Outgoing Radiation
100 units - energy recieved from the sun (not important what type of units are used - could be joules, watts, calories, etc.)
Albedo is the percent of radiation scattered and reflected from a surface.
Of the 100 units of incoming radiation, 3 units are reflected back by the atmosphere, 19 units by the clouds, and 9 units by the ground. Total reflected = 31 units
Notice that the amount reflected by the clouds is two times greater than the amount reflected by the ground. Why?
It should be noted at this point that "ground" is used here to indicate the surface of the Earth - land and water surfaces.
Of the 100 units of incoming radiation, 17 units are absorbed by the atmosphere, 3 units are absorbed by the clouds, and 49 units are absorbed by the ground. Total absorbed = 69 units
69 units + 31 units = 100 units
Starting with the radiation from the ground - the ground absorbs 49 units from insolation - it absorbs another 95 units of energy from counterradiation that has been re-emitted from the atmosphere.
49 units + 95 units = 144 units total absorption by the ground.
Radiation is then re-emitted from the ground as 114 units of infrared radiation. Of this 114 units, 102 units are absorbed by the atmosphere and 12 units are lost directly to space.
144 units - 114 units = 30 units remaining
23 units are moved from the ground to the atmosphere through Latent Heat Transfer (Heat is removed from the surface during evaporation)
7 units are moved from the ground to the atmosphere through Sensible Heat Transfer (the air is in contact with the ground and heat is transfered directly from one material to the other)
23 units + 7 units = 30 units
The Atmosphere directly absorbs 20 units of insolation, 102 units are absorbed from the ground, 23 units absorbed from latent heat transfer and 7 units from sensible heat transfer. Total = 152 units absorbed by the atmosphere.
Of this 152 units, 95 units are re-emitted to and absorbed by the ground, and 57 units are lost directly to space.
Of the total outgoing radiation lost to space, 31 units are reflected insolation, 12 units are radiated from the ground and 57 units are radiated from the atmosphere.
31 units + 12 units + 57 units = 100 units.
The amount of incoming radiation equals the amount of outgoing radiation. Global Radiation Balance
This equation is not constant and is not always balanced.
Variations in the amount of energy recieved, energy lost, ground cover, composition of the atmosphere can all affect the this equation.
The Earth's energy system is dynamic and is always changing and adjusting to new conditions.
As a result the global is either warming up or cooling down.
Global Energy Balance is a global average.
Radiation is only received on one hemisphere.
Energy is lost from both hemispheres.
Equatorial regions receive more radiation than polar regions.
Polar regions loose more radiation than received.
Excess energy at equator must move to polar regions.