Anticyclones
, HP El S bysouth Africa
not
p gYfroggT
Itoh EE
afft
r
n Maa e
H
919ha HP
SouthAtlantic Hp South Indian HP
1 General Characteristics
large 3000km 4000km
3 cells always present theymove oKalaharipushedintoupperatmosphere
anticyclonic airflow aroundHPcenter anti clockwise in South
onshorewinds from SAAct SIAC jonverging subsiding air warms
air subsides atcenter diverges air
subsiding air
subsiding as a result relativehumidity
sinkingairwarms
Tempinversionabove surface of the decreases
Earth normally temp decreases w
altitude oturnedupside
down w tempinversions
peppy a i associatedw
dryair
temp increases w height
a
inversion
B tempincrw altitudes adiabatic warming
É temp increase associated w subsiding air as it's
compressed loweraltitudes wherepressure is incr
temp
in a subtropical anticyclones temp inversion result of adiabatic warming as air subsides
, HP El S bysouth Africa
not
p gYfroggT
Itoh EE
afft
r
n Maa e
H
919ha HP
SouthAtlantic Hp South Indian HP
1 General Characteristics
large 3000km 4000km
3 cells always present theymove oKalaharipushedintoupperatmosphere
anticyclonic airflow aroundHPcenter anti clockwise in South
onshorewinds from SAAct SIAC jonverging subsiding air warms
air subsides atcenter diverges air
subsiding air
subsiding as a result relativehumidity
sinkingairwarms
Tempinversionabove surface of the decreases
Earth normally temp decreases w
altitude oturnedupside
down w tempinversions
peppy a i associatedw
dryair
temp increases w height
a
inversion
B tempincrw altitudes adiabatic warming
É temp increase associated w subsiding air as it's
compressed loweraltitudes wherepressure is incr
temp
in a subtropical anticyclones temp inversion result of adiabatic warming as air subsides