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Pressure systems
Anticyclones & Cyclones
Global circulation:
Part 1
Part 2
Part 3
Global circulation
Seasonal pressure movement
Seasonal pressure movement
Anticyclone
• High pressure area or ”high”
• Subsidence dissolving clouds.
Types of highs
Ridge
Blocking anticyclone
Cyclone
Low pressureareas or ”low”.
Convectiveweather, CU, CB
Types of lows
Trough
Non-Frontal Depressions
• Thermal
• Orographic
• Polar Air Depression
• Secondary Depression
Thermal Depression
• Over land in the
summer
• Balochistan low
Orographic Depression
Wind flows around the
edge rather than the top.
Polar Air Depressions
• Extremely cold Arctic
air moves south,
leading to convection.
• Only during winter.
• Different from Polar
Front Depressions!
Secondary depressions
1) On a trailing front from
an occluded primary.
2) On a trailing cold front
well within the primary
circulation.
Secondary depressions
3) At the tip of the
warm sector of a partly
occluded depressions.
Cols
Cols in frontal systems
Air masses
Air masses
• An airmass is a large body of air with the same properties.
• Develop in source regions.
Source regions
Moving air masses
Moves over warmersurface =
Defined as cold air mass!
• Becomes warmer in lowerlayers
• Becomes more unstable
• RH decreases
Moves over colder
Surface =
Defined as warm air mass!
• Becomes cooler in lower
layers
• Becomes more stable
• RH increases
Typical weather - Warm Air mass
Inversion
Typical weather - Cold Air mass
Air mass classification
C = Cold
W = Warm
Examples:
cTw
mAc
UK
Fronts and Occlusions
Fronts• Border between 2 air masses
Front Definitions
• Warm front: Warm air displacing cold air.
• Cold front: Cold air displacing warm air.
• Occluded front: Forms when the cold front overtakes the warm front.
• Warm front occlusion: The air ahead of the occluded front is the coldest.
• Cold front occlusion: The air behind the occluded front is the coldest.
• Stationary front: Essentially no movement acrossthe frontal zone.
Fronts Definitions
The warm front is red
The cold front is blue
The occluded front is violet
The Quasi stationary front is
grey. One cold and warm front
opposing each other
Warm Front
Warm front movement
• 2/3 of geostrophic
wind
• At right angles to itself
Ahead of the warm front
At the warm front
Cold front
Cold front movement
• Geostrophic wind
• At right angles to itself
At the cold front
Behind the cold front
Squall Lines
10 - 50 ( 150 ) NM
CB
CB
Gust front Warm humid
air
Ahead of a cold front
or a trough line the
outflow of cold air can
be fairly uniform and
at about the same
distance from the
mother clouds a line of
new CB clouds forms –
a squall line (SQL).
Warm sector
The area between the fronts
Stationary front
• No or little movement
• Calm but long lasting weather
Occluded fronts
Occlusions – General
• The cold front
catches up to the
warm front
• Warm sector raised
off the ground
• Hard to predict
movement and
weather
Warm occlusion
Cold occlusion
Polar front depressionsA hemispheric sea level
pressure chart reveals the
presence of several
extratropical cyclones around
the middle latitudes.
Extratropical
cyclones develop
near the polar front. They have a
significantly smaller scale than
features of the global circulation.
Frontal Development
A disturbance causes a bulge of mTw air in the mPc
air, cerating an area of relatively lower pressure.
Air starts to blow towards the low pressure centre,
but is reflected to the right due to the Coriolis force.
The low pressure centre moves east due to the
general circulation. The fronts follow accordingly.
The cold front will eventually catch up to the warm
front, creating an occluded front.
The two cold airmasses start to mix, effectively
removing the frontal zone.