EXOSPHERE
(480 -+ KM)
ATMOSPHERE
THERMOSPHERE
( 80 - 480 KM)
IONOSPHERE
can be
divided
into
LAYERS
include
MESOSPHERE
(50 - 80 KM)
FRONTS
OZONE LAYER
contains
TROPOSHPERE
(0 - 10 KM)
is heated by
OXYGEN
21%
BAROMETER
ARGON
.93%
is heated unevenly
causing transfer
of heat by
CARBON DIOXIDE
.03%
varies along
is the
is where
MOST DENSE
LAYER
NITROGEN
78%
EARTH'S
SURFACE
exerts
STRATOSPHERE
(10 - 50 KM)
is mostly
made up of
WEATHER
OCCURS
is closest to
is measured by
CONDUCTION
RADIATION
is influenced by
TOPOGRAPHIC
FEATURES OF
EARTH'S SURFACE
can be drawn
close together
indicating
RAPID CHANGE
IN PRESSURE
can be drawn
far apart
indicating
SLOW CHANGE
IN PRESSURE
EARTH
causes
can be explained in terms of
AIR PRESSURE
is related to
can be
OTHER GAS
LAWS
CONVECTION
is presented by
BERNOULLI'S
PRINCIPLE
HIGH
PRESSURE
ATMOSPHERE
WIND
LOW
PRESSURE
LINES CALLED
ISOBARS
moves
moves air
connect
CLOCKWISE
COUNTERCLOCKWISE
AREAS OF EQUAL
ATMOSPHERIC
PRESSURE
includes as
an example
HURRICANES