aviation weather theory made easy
DESCRIPTION
Part 1 of 3, most pilots loose the basics when they start flying due to numerous reasons. Whatever your reason, don't let not coming to this seminar be one of them. This three part series will fill in the memory gaps and show you how easy it can be to understand weather systems.TRANSCRIPT
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Weather Theory Made Easy
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The basics of aviation weather, including the cases of carious weather phenomena and how they can affect the safety of flight.
For more information on aviation weather, refer to Aviation Weather for Pilots(AC 00-6A) Aviation Weather Services (AC 00-45G) Internet Communications of Aviation Weather
and NOTAMS (00-62)
Introduction
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The Atmosphere
• Composition– 78% Nitrogen– 21% Oxygen– 1% Inert
• Vertical Structure– Troposphere– Tropopause– Stratosphere– Mesosphere & thermosphere
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Variations Diurnal Seasonal Variation with Latitude Topographic Altitude
Temperature
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Atmospheric Pressure
• Measurement– Barometer
• Mercurial• Aneroid
• Variation– Altitude– Temperature
• Pressure Depiction on Chart– Isobars
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Pressure Systems Highs
H surrounded by L Lows
L surrounded by H Ridge
Elongated are of H Trough
Elongated are of L Col
Neutral area between 2 H or 2 L
Atmospheric Pressure
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Wind
• Convection• Pressure Gradient Force• Corriolis Force• Friction• Global Circulation Patterns• Jet Stream
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Land & Sea Breezes Sea Breeze Land Breeze
Mountain/Valley Winds Valley Winds Mountain Winds
Katabatic Winds Wind Shear
Local/Small Scale Winds
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Moisture
• Water Vapor– Relative Humidity– Dewpoint
• Change in State– Evaporation– Condensation– Freezing & Melting– Sublimation & Deposition
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Super-Cooled Water? Exist at temps below freezing Freeze upon impact with an exposed object
Condensation Nuclei Microscopic particles Serves as a place for condensation to form Salt, dust, by-products of combustion
Moisture
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Clouds/Cloud Formation
• Formation– Air moving over a cold surface– Air stagnating over a cold surface– Expansion cooling of upward moving air
• Classification– Fog– Low Clouds– Middle Clouds– High Clouds– Clouds with Extensive Vertical Development
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Low Clouds Almost entirely of water Super cooled water, snow, ice Surface to ±6,500’
Middle Clouds Primarily of water Most is Super cooled Bases range from ±6,500’ to ±23,000’
Classification
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Classification
• High Clouds– Almost entirely ice crystals– Base range ±16,500 to FL450
• Clouds with Extensive Vertical Development– Super cooled water above the freezing level– Tops may be ice crystals– Base range from ±1,000 to above 10K
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Particle Growth Via added condensation or sublimation Via collision of particles
Precip vs. Cloud Thickness To produce significant precip, 4000’ thick Thicker the cloud, heavier the precip
Precipitation
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Lapse Rate
The decrease in temperature with increasing altitude
Approx. 2˚C/1000’
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Resists any upward OR downward development
Unstable may grow into a vertical or convective current
Atmospheric Stability
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Temperature Inversion
An increase in temperature with an increase in altitude
Lapse rate is inverted
Usually confined to shallow layers of air
Visibility is often restricted
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Unequal heating of the Earths surface
Overlying air
heated unevenl
y
Warm air pushed
aloft
Lapse rate will determin
e the rest
Temperatures Role in Stability
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Moistures Role in Stability
Unsaturated• 3˚C/1000’• Unstable
Normal• 2˚C/1000’• Stable
Saturated
• 1.1˚ to 2.8˚C/1000’
• Unstable
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Every physical process of weather is accompanied by or is the result of a _____________.
1. Movement of air2. Pressure differential3. Heat exchange
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What causes variations in altimeter settings between weather reporting points?
1. Unequal heating of the Earth’s surface
2. Variation of terrain elevation
3. Coriolis force
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The wind at 5,000 feet AGL is southwesterly while the surface wind is southerly. The difference is direction is primarily due to?
1. Stronger pressure gradient at higher altitudes
2. Friction between the wind & the surface
3. Stronger Coriolis force at the surface
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Convective circulation patterns associated with sea breezes are
caused by?
1. Warm, dense air moving inland from over the water
2. Water, absorbing & radiating heat faster than the land
3. Cool, dense air moving inland from over the water
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The development of thermals depends upon ___________.
1. A counterclockwise circulation of air
2. Temperature inversions3. Solar heating
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Air Masses
• What is an air mass?– Large body of air with fairly uniform
• Temperature• Moisture content
– Forms when air remains stationary and takes on the characteristics of the underlying surface
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Temp & moisture content of the underlying surface
Tropical oceans & large deserts Middle latitudes are poor regions
Source Regions
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Classifications
• Temp– Polar– Tropical
• Moisture content– Continental– Maritime
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As it moves from its source region, it begins to change
Warming from below can cause instability Cooling from below may result in stability
May also cause poor visibility from fog and low clouds
Modification
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Fronts
Boundaries between air masses
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Change in temp May be abrupt or gradual
Change in wind direction or velocity Always shifts to the right in the Northern
Hemisphere Change in pressure
Usually a drop as you approach it Always reset your altimeter
Frontal Passage Detection
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Cold Fronts
Hugs the ground as it
moves due to gravity
Forces warmer less
dense air aloft
Movement is usually in an
easterly direction
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Cumulus Clouds
Turbulence
Showery Precipitati
on
Gusty Winds
Good Visibility
Speed Will Dictate the Weather
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Fast Moving Cold Fronts
Moved along by intense high pressure system
Surface friction causes a steep frontal slope
Wide difference between temp & moisture between the two masses
Squall lines will precede if the air is moist and unstable. Usually 50 to 300 miles ahead.
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Fast Moving Cold Front
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Slow Moving Cold Front
• Much shallower frontal slop
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Occurs when warm air overtakes cooler air Move at much slower rates Frontal slope is very gradual
Warm Fronts
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Generalizations
• Stratus clouds• Smooth air• Steady precipitation• Poor visibility
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Occurs when two air masses are equally balanced
A mix of both air masses may be present for several days
Stationary Fronts
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Frontal Occlusions
• Occurs when a fast moving cold front catches up to a slow moving warm front
• The difference in temperature determines the front that is produced (warm or cold front occlusion)
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Weather Hazards
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Thunderstorms
• 3 conditions necessary– Unstable lapse rate– High moisture content– Some form of lifting action
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3 stages Cumulus or building stage
Continuous updrafts Mature stage
Rain at the surface Dissipating stage
Downdrafts Anvil top
Thunderstorms
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Types of T-Storms
• Air Mass– Convection on hot summer days
• Frontal– Collision of 2 AM’s
• Orographic– Mountainous areas
• Converging Air flow from 2 active storms• Squall lines
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Turbulence Lightning Microburst Hail
Hazards
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Do’s & Don’ts
DO NOT• Take off or land in the
face of a storm• Fly under a storm• Fly in a cloud mass
without airborne radar• Trust the outward
appearance of a cloud
DO• Avoid by 20 miles• Clear the tops by 1000’
for each knot wind• Circumnavigate the area
for 6/10th coverage• Avoid lightning areas• Regard tops of 35K or
higher as hazadous
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Tighten your seatbelt & secure loose items Plan & hold your course for minimum time
through the storm Plan to enter below the freezing level Pitot heat & carb heat on Set power to establish Va Turn up flight deck lighting Turn off autopilot
If You Can’t Avoid
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During Penetration
• DO keep you eyes on your instruments• DO maintain maneuvering speed• DO Allow the aircraft to “Ride the Waves”• DO Maintain Course for a minimum time
through the storm
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Can take place at any altitude Can be caused by wind shear, convection
currents, & obstructions to airflow Often found near the jet stream
CAT
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Wake Turbulence
• Caused by wing tip vortices• Cup in a cup
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Icing
• Rime Ice– Tiny rain droplets or drizzle– Milky in color
• Clear Ice– Large water droplets– Cumulous clouds– Above the freezing level
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Restrictions to Visibility
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Fog
• Gets its name by how its formed– Radiation or ground– Advection– Upslope– Steam
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Haze Airborne dust particles
Smoke Combustion materials
Smog Smoke & Fog mixed
Haze, Smoke, Smog
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Cooling from aloft tends to make an air mass more…
1 2
50%50%
1. Stable
2. Unstable
Countdown
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When an air mass is warmed from below, its stability is…
1 2
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1. Increased2. Decreased
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Transition zone between two different air masses…
33%
33%
33%
1 2 3
1. Frontal zone
2. Trade wind
3. Trough
Countdown
20
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This will always change when flying across a front…
33%
33%
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1. Wind Direction
2. Type of precipitation
3. Stability of the air mass
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Cold fronts in the US generally move to the…
1. East-Northeast
2. East-Southeast
3. West-Southwest
4. South
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What type of front generally produces the most violent flying
weather?
1. Warm2. Cold3. Fast-moving cold front4. Stationary
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What type of cloud is associated with fast-moving cold fronts?
1. Cirrus
2. Altostratus
3. Altocumulus
4. Cumulonimbus
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