Title: Meteorology 3
1Meteorology 3
2FRONTS
Pg 6-7
3Warm
Colder
Cold
Warm
Colder
Cold
Warm
Cold
Colder
4Precipitation
- Precipitation occurs when water droplets grow
sufficiently in size and weight and then fall due
to gravity. - Showery precipitation Cumulus
- Steady precipitation Stratus
- Condensation Nuclei
- Smoke, sea salt, etc.
5MOISTURE CONTENT
_at_40OC one cubic metre of air can hold 50 grams of
water vapour. One M3 of air weighs about 1.35
kg. This represents about 3.5 by weight.
Pg 1-3
6- CLOUDS
- PRECIPITATION
- THUNDERSTORMS
- FOG
- ICING
- VFR MVFR IFR WEATHER
- UPPER WINDS
7CLOUDS
- CLOUDS ARE FORMED IN TWO WAYS
- air is cooled to its saturation point and
condensation occurs OR - Air absorbs additional water vapour until
saturation is reached. - LIFTING AGENTS
- Convection
- Orographic lift
- Frontal Lift
- Convergence
- Mechanical turbulence
8UNSTABLE vs. STABLE
9UNSTABLE
Steep lapse rate Cumulus type cloud Precipitation
in showers Thunderstorms Good visibility Bumpy
conditions
Shallow lapse rate Stratus type
cloud Precipitation is steady and
lighter Fog Poor visibility Smooth conditions
STABLE
10Precipitation
.
Pg 8-17
- Any precipitation, in order to form, requires
condensation nuclei. - Temperature to dew point
spread must be small
11Precipitation
Pg 9-2
12THUNDERSTORMS
- Requirements
- Unstable air to high levels
- High relative humidity
- Lifting agent
- The three stages
- Cumulus
- Mature
- Dissipation
13THUNDERSTORMS
Pg 15-2
14- Cumulus Stage
- Cloud driven upward by the latent heat as water
vapour condenses - Temperatures in cell are higher than outside
temperature at the same level. - No precipitation as water and ice are suspended.
- Strong updrafts prevail throughout.
- Mature Stage
- Heights may reach 60,000 feet
- Updrafts up to 6,000 ft/min or over 100 km/hr.
- As the water droplets grow large enough to fall,
they drag air down with them. - Downdraft starts in the middle region of the
cloud. - Lightning, microburst, hail, wind shear.
- Arrival of precipitation on the ground in mature
stage. - Dissipation stage
- Downdraft spreads throughout the cell (except
top) - Gradual cessation of rainfall and the passing
rain may cool the lower regions - Anvil shape
- Total cycle
- Can form in 15-20 minutes although whole process
usually 1 to 3 hours
15Thunderstorm Types
- Air Mass
- Form singly or in clusters on hot days.
- Usually VFR weather around them
- Convection and/or orographic lifting
- Frontal
- Usually advancing cold front
- Squall line very turbulent and slows front
- NOTE
- Either type can penetrate the tropopause which
can be based from 28,000 feet at poles to 54,000
feet at equator
16Convective Thunderstorms
Pg 15-11
17Orographic Lift
Pg 8-15
18Pgs 15-9,10,11
19Thunderstorm Weather
- Turbulence has potential to overstress a/c max
turb. near mid-levels 12,000 to 20,000 feet - Lightning may blow out electrical fuses
blindness structural damage ignite fuel cells
greatest potential between -5/5 - Hail encountered between 10,000 and 30,000 ft
may be encountered in clear air downwind of
storm airframe damage - Icing heaviest icing occurs just above
freezing level where droplets are super cooled.
Severe in the mature stage near cloud top. - Pressure rapid barometric changes, altimeter
may be unreliable. - Rain reduced visibility, refraction on
windscreen, hydroplane
20Dos and Donts of Thunderstorms
Pg 15-18
21Gust Front Hazards
Pg 15-18
22Anvil, Multi-Cell Lightning
Positive build up in top and negative build up in
cloud base is usual
Pgs 15-3,5,7
23FOG
24FOG
- Fog is a cloud (usually stratus) that is in
contact with the ground. - forms in relatively stable air where the
temperature - to dew point spread is small, wind may be
present - requires condensation nuclei
- Usually needs a cooling process
- Types of Fog
- Radiation Advection
- Upslope Steam
- Frontal Ice
25Radiation Fog clear night, light wind, high
humidity, often a high pressure area.
Pg 10-7
26Radiation Fog at CYKZ
27Advection Fog warm moist air moving over colder
land, horizontal movement, warm fronts/oceans,
sometimes strong winds (25kts)
Pg 10-8
28Upslope Fog
Pg 10-9
29Ice Fog Byproduct of engine is wateradded to
cold crisp air. (sublimation vapour to ice)
Pg 10-10
30WATER VAPOUR WATER - ICE
Pg 1-2
31Frontal Fog vapour addition raises the dew point
under a warm front
Pg 10-10
32Steam fog cold air moving over a warm surface
Pg 10-9
33Steam Fog at Collingwood
34ICEpart 9
- Clear Ice skin warms to 0 while droplets freeze
- large super cooled water droplets
- bottom layers of cold clouds or tops of unstable
clouds - freeze just below 0 to -15
- tend to hit wing
- high collection efficiency
- large spreading droplets
- Rime Ice skin temperature lt 0
- small super cooled droplets can exist down to
-40 - stable clouds, usually rime only -25 to -40
- tend to flow around wing
- low collection efficiency
- leading edge only (no spread)
35Heaviest Icing Rate of Catch
- Skin temperature at or below freezing
- High water content held up in updrafts
- Large droplets
- Collection efficiency is inversely proportional
to the surface geometry - thick vs. thin wings
Pg 9-10
36Ice Formation - Stability
Pg 9-4
37ICING
- Cumulus
- icing distributed vertically
- top of mature stage
- In 5000 ft above 0 level
- large droplets to -25
- Stratus
- icing distributed horizontally
- if turbulent, top of cloud will have the
heaviest. - snow means less icing
Warm clouds have more droplets with
altitude. Colder clouds have fewer droplets
with altitude.
Pg 9-5
38WEATHER TERMINOLOGY
- SKY CONDITION
- Clear 0/8
- Few 1/8 to 2/8
- Scattered 3/8 to 4/8
- Broken 5/8 to 7/8
- Overcast 8/8
- IFR less than 1000 ft 3 miles
- MVFR 1000-3000 ft 3-5 miles
- VFR greater than 3000 ft better than 5
39Clear 0/8
40Few 1/8 to 2/8
41Scattered 3/8 to 4/8
42Broken 5/8 to 7/8
43Overcast 8/8
44UPPER AIR CHARTS standard pressure levels
- 850 mb 5000 feet asl
- 700 10000
- 500 18000
- 400 24000
- 300 30000
- 250 34000
- 200 40000
- 150 45000
- 100 53000
45STEEP PRESSURE GRADIENT GIVES HIGHER WIND SPEEDS
46JET STREAM
Pg 12-11
Pg 12-13
47Low Level Nocturnal Jet
Pg 11-13
40 KNOTS