Earth’s Energy Balance (slide 3) Flashcards
Radiation
is when energy travels as waves
Ex- Ultraviolet (U.V.) radiation from the sun
Conduction
is when energy is transferred through contact
Ex- The handle of a metal pan getting hot when it is heated
Convection
is when energy is transferred because of
differences in temperatures in a liquid or gas
Ex- ocean currents, or warm air rising and cool air falling
Earth maintains a relatively constant global temperature-
a unique quality that
allows it to be able to maintain life
Planets such as Mercury can be heated up 450 degrees Celsius from the Sun
Why doesn’t Earth get scorching hot?
earth has an atmosphere and it is further away from the sun
incoming solar energy
100%
reflected by atmosphere
6%
refleceted by clouds
20%
reflected by earth’s surface
4%
absorbed by atmosphere and clouds
19%
absorbed by land and oceon
51%
reflected back into space
30%
energy is absorbed onto Earth
70%
If there is an energy balance then that would mean:
the amount of energy absorbed = the amount of energy released
The absorbed 70% of
energy is actually
converted
to heat
The oceans and land begin
to radiate that heat
back
out into the atmosphere
and eventually back to
space
Energy absorbed by living
things will also radiate
thermal energy
back into
space
Other planets like Mercury do not have an atmosphere therefore it is unable to
reflect light (450 degrees C)
during the day and retain heat during the night (-170 degrees C)
It is important for the energy to be converted to thermal energy because
it allows Earth to stay warm
It is important for the energy to be immediately reflected back into space and have the thermal energy
slowly radiate back into space so
Earth does not reach scorching hot temperatures