PPL Meteorology
8.24 Atmospheric Moisture to Clouds
Requirements for cloud to form: Saturated Air – Temperature equals Dew Point or below. Condensation Nuclei – Dust, smoke etc. Lifting Processes: Orthographic – mountains.
8.26 Visibility and Fog
Clouds that touch the ground are fog. Warm Moist air moving over a cold surface can create fog. 8.26 Visibility and Fog
8.28.12 SLEET SNOW AND FREEZING RAIN EXPLAINED
Drizzle – Fine and close together droplets. Droplets can be suspended due to small size causing bad visibility. Snow – Ice crystals. Remains frozen Sleet –
8.28.14 Carburettor Icing
Most common in cool summer or early fall days when there is high moisture Can happen at warm temperatures as Venturi effect in the carburetor
8.28.4 How Does Frost Form?
Ice is formed through deposition (Gas directly to Solid). Cold moist air will form into hoar frost when passing over a very cold surface i.e
8.30 How a thunderstorm is formed
Three conditions are required for the development of thunderstorms: Rising Air Moisture Unstable Air 8.30.2 State the three conditions required for the development of thunderstorms.
8.32 Mountain Wave Time Lapse
8.32.6 Describe the mountain lee-wave (standing wave) development process
8.32.12 Flying around Thunderstorms
Three stages in the life-cycle of a thunderstorm: Cumulus/ Growing Stage – Strong updrafts, often suspending all water or ice Mature Stage – Heavy water
8.32.2 Fohn Wind And How It Works Simple
Warm moist air rises over a mountain. Air expands and cools adiabatically on the way up. Reaches dew point and rains. Air is compressed and
8.36 Cold Fronts and Warm Fronts
A front marks the boundary between two air-masses, and appears on the weather map as a line with triangles or semicircles attached. Cold – Cold
8.4.2 How to read a Synoptic Chart
Isobars – lines of equal pressure marked as lines around highs and lows. The closer the isobars, the stronger the winds Anticyclone (“high”) – Shown as
8.40 The Ups and Downs of Air Turbulence
Wind forced over the mountain ridge will rise over the terrain and then sink after, this continues oscillating for a large distance. Beneath the oscillations
as an example,
from uTube Video’s URL of https://www.youtube.com/watch?v=Nqv-0qd7sBg
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