AVIATION WEATHER STUDY · 6JJ

Aviation Weather & Clouds

Read the sky — identify, interpret, decide
SOURCES: PHAK Ch.12 (FAA-H-8083-25) · Aviation Weather Handbook (FAA-H-8083-28) · AC 00-6 · AIM · Helicopter Flying Handbook
Study Block
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Read-aloud: tap Play to listen, hands-free. (Cloud pictures aren't read.)
00· How To Use

The goal: call the cloud, know the weather

Clouds are the sky's instrument panel. Each type is the visible result of what the air is doing — rising or sinking, stable or unstable, wet or drying. Learn the shape and you read the air.

Work the Guide with the cloud galleries open, hit Play to hear it on a drive, then drill Flashcards and the Quiz. The single most useful habit: every time you're outside, name what's overhead before you do anything else.

01· How Clouds Form

The recipe

A cloud is just water vapor that cooled to its dew point and condensed onto tiny particles. Four ingredients:

  • Moisture — water vapor in the air.
  • Cooling to the dew point — almost always by lifting (air expands and cools as it rises, about 3°C per 1,000 ft when dry).
  • Condensation nuclei — dust, salt, smoke for vapor to condense on.
  • Stability decides the shape (see next section).

What lifts the air (4 mechanisms)

  • Convective — sun heats the surface, warm bubbles rise → cumulus.
  • Orographic — wind pushed up a mountain slope → clouds on the windward side, often lenticulars and rotors.
  • Frontal — one air mass lifted over another along a front.
  • Convergence — air flowing together has nowhere to go but up.
Pilot tie-inThe temperature/dew point spread tells you how close the air is to saturating. A small, shrinking spread means fog or low cloud is likely. Cloud bases over a hot day roughly equal spread ÷ 4.4 × 1,000 ft AGL.
02· Stability: The Master Key

Stable vs. unstable air

Stability is whether lifted air keeps rising or sinks back. It is the single biggest predictor of what you'll fly through, and it sorts every cloud into one of two families.

Stable airUnstable air
CloudsStratiform (layered, flat)Cumuliform (heaped, puffy)
RideSmoothTurbulent / bumpy
VisibilityPoor (haze, fog trapped)Good (mixing clears the air)
PrecipSteady, widespreadShowery, localized
Memory hookStratus = stable & smooth. Cumulus = convective & choppy. If you see puffy, expect bumps; if you see flat gray sheets, expect smooth air but low ceilings and reduced visibility.
03· The Cloud Decoder

Latin roots + altitude = the name

Every cloud name is built from a few Latin words plus an altitude prefix. Learn these and you can construct or decode any cloud:

RootMeansLooks like
Cirrus"curl of hair"Wispy, thin, icy
Cumulus"heap"Puffy, cotton, lumpy
Stratus"layer"Flat sheets, featureless
Nimbus"rain"Precipitating (nimbo-/-nimbus)

Altitude prefixes (the "étage" or family):

FamilyPrefixHeight (temperate)
Highcirro-~16,500–45,000 ft — ice crystals
Middlealto-~6,500–23,000 ft
Low(none)surface–6,500 ft
VerticalBase low, tops to the stratosphere
Decode it"Altocumulus" = alto (middle) + cumulus (heap) = mid-level puffy patches. "Nimbostratus" = nimbus (rain) + stratus (layer) = a rain-bearing flat gray layer. "Cirrostratus" = high, thin layer. The system always works.
04· High Clouds

Cirro- family · ice crystals, ~16,500–45,000 ft

Cirrus Ci

High · thin wisps & streaks
Spot itThin white feathery streaks or hooks ("mare's tails"), made of ice. No shading.
MeansFair now, but often the first sign of an approaching warm front or change 24–48 hr out.

Cirrocumulus Cc

High · tiny ripples ("mackerel sky")
Spot itSmall white grains or ripples in rows, like fish scales. No shadows on the elements.
MeansUnstable air aloft; can precede unsettled weather. Often short-lived.

Cirrostratus Cs

High · thin milky veil
Spot itA transparent whitish sheet over the whole sky — the giveaway is a halo ring around the sun or moon (ice crystals).
MeansMoisture moving in aloft; a warm front and rain may be 12–24 hr away.
05· Middle Clouds

Alto- family · ~6,500–23,000 ft

Altocumulus Ac

Middle · rolls/patches with shading
Spot itRounded mid-level clumps in groups or rows, with grey shading underneath (bigger than cirrocumulus). "Sheep in the sky."
MeansMoisture and some instability at mid-levels. Altocumulus on a warm humid morning can warn of afternoon thunderstorms.

Altostratus As

Middle · grey-blue sheet
Spot itA uniform grey/blue sheet covering the sky; the sun shows weakly as if through ground glass, with no halo and no sharp shadows on the ground.
MeansA warm front's mid stage — thickening to nimbostratus and steady rain is common next.
06· Low Clouds

Surface–6,500 ft

Stratus St

Low · featureless grey layer
Spot itA low, flat, uniform grey deck with no texture — like fog that didn't reach the ground. May produce drizzle.
HazardLow ceilings and poor visibility — the classic VFR-into-IMC trap. Stable but you can't see.

Stratocumulus Sc

Low · lumpy rolls with breaks
Spot itLow, grey-and-white rounded rolls or patches with blue sky showing in the gaps. Lumpier than stratus, flatter than cumulus.
MeansWeak instability under a stable layer; usually little or no precip.

Nimbostratus Ns

Low/middle · thick dark rain layer
Spot itA thick, dark, shapeless grey layer that blots out the sun, with continuous steady rain or snow falling from it.
HazardWidespread IFR, icing in the cold season, and ragged scud beneath. Steady — not showery.
07· Vertical Development

The cumulus family · unstable air, the action clouds

Cumulus Cu

Vertical · puffy, flat base, fair weather
Spot itDetached white cotton-balls with flat bases and cauliflower tops, clear sky between them. "Fair-weather cumulus."
HazardLow-level turbulence and updraft/downdraft bumps. Harmless small — but watch them grow.

Towering Cumulus TCU

Vertical · tall cauliflower, still growing
Spot itA cumulus taller than it is wide, with hard, bright cauliflower tops surging upward — but no anvil yet.
HazardStrong updrafts and turbulence; a thunderstorm in the making. Give it room — it can become a Cb in minutes.

Cumulonimbus Cb

Vertical · base low, anvil top to 45,000+ ft
Spot itA towering dark thunderstorm cloud with a flat, spreading anvil top, dark rain base, and lightning. The king of clouds.
HazardEverything dangerous at once: severe turbulence, hail, lightning, icing, microbursts, low-level wind shear, tornadoes. Avoid by 20 NM. Never fly under, through, or near.
08· Special & Hazard Clouds

The ones that signal danger

Standing Lenticular ACSL

Mountain wave · smooth lens / "UFO" stack
Spot itSmooth, lens- or almond-shaped clouds that stay still over or downwind of mountains, sometimes stacked like plates.
HazardA flag for mountain-wave activity — severe turbulence and strong up/downdrafts nearby, even though the cloud itself looks calm.

Rotor Cloud

Mountain wave · ragged, churning roll
Spot itA ragged, turbulent-looking roll cloud sitting below the lenticulars, near mountain-top height on the lee side, that appears to churn in place.
HazardThe most violent part of a mountain wave — extreme turbulence. Especially dangerous for helicopters at low level near terrain.

Mammatus

Pouches hanging under a storm anvil
Spot itRound pouch-like bulges hanging down from the underside of a cloud, usually a thunderstorm anvil. Eerie, lumpy ceiling.
HazardA marker of a strong/severe thunderstorm nearby with violent up- and downdrafts. Stay well clear.

Fog

Stratus cloud at the surface · visibility < 5/8 SM
Spot itCloud touching the ground — the same thing as stratus, just at the surface, dropping visibility below 5/8 statute mile.
HazardSudden IFR/below-minimums conditions. See the next section for the types and how each forms.
09· Fog Types

Same cloud, five ways to make it

  • Radiation (ground) fog — clear, calm night; ground cools, air above it cools to dew point. Forms in low spots, burns off after sunrise.
  • Advection fog — warm, moist air blows over a cooler surface (coastlines). Needs wind, so it's persistent and can move inland.
  • Upslope fog — moist air pushed up rising terrain, cooling adiabatically. Needs wind too.
  • Steam fog ("sea smoke") — cold air over warm water; water evaporates and recondenses. Low-level turbulence/icing possible.
  • Precipitation-induced (frontal) fog — warm rain falls through cool air and saturates it, often near a warm front.
Pre-flight habitA small temperature/dew point spread (within ~4°F / 2°C) plus clear, calm, cooling conditions = expect radiation fog by dawn.
10· Sky Cover & Ceilings

Reading coverage like a METAR

Sky cover is reported in eighths (oktas) — how much of the sky a layer fills:

CodeNameCoverage
SKC/CLRClear0/8
FEWFew1/8 – 2/8
SCTScattered3/8 – 4/8
BKNBroken5/8 – 7/8
OVCOvercast8/8
CeilingThe ceiling is the height of the lowest broken or overcast layer (or vertical visibility into an obscuration). FEW and SCT layers are not ceilings. In a METAR, sky condition reads as code + height in hundreds of feet AGL, e.g. BKN025 = broken at 2,500 ft AGL = a 2,500-ft ceiling.
11· Air Masses & Fronts

Why the weather changes

An air mass takes on the temperature and moisture of its source region. A front is the boundary where two air masses meet — and that's where clouds and weather concentrate.

FrontClouds & weather
ColdFast; steep lift → cumulus/Cb, showers & thunderstorms, gusty wind shift, then clearing. Narrow band.
WarmSlow; gentle lift → the classic sequence Ci → Cs → As → Ns with steady widespread rain and low ceilings ahead. Wide band.
StationaryBoundary stalls; prolonged clouds and precip over one area.
OccludedCold front overtakes warm; mix of both — can bring widespread, heavy weather.
Cloud sequence = forecastThat high-cloud progression (cirrus thickening to cirrostratus to altostratus to nimbostratus) is a warm front announcing itself hours ahead. Reading clouds is forecasting.
12· Thunderstorms

The cumulonimbus, broken down

Three things it needs

  • Sufficient moisture.
  • An unstable lapse rate.
  • A lifting trigger (heating, front, terrain, convergence).

Three life-cycle stages

  • Cumulus (building) — updrafts only; cloud grows rapidly.
  • Mature — rain reaches the ground; up- and downdrafts side by side = the most violent stage. Starts when precip begins falling out.
  • Dissipating — downdrafts dominate, rain tapers, anvil remains.
HazardsSevere/extreme turbulence, hail (thrown out the top, can fall in clear air), lightning, severe icing, and — deadliest at low altitude — the microburst: a violent downdraft (up to 6,000 fpm) causing low-level wind shear. Avoid all storms by at least 20 NM; never take off or land into a microburst-risk storm. A squall line of storms ahead of a cold front can't be flown through — go around or wait.
13· Icing & Turbulence

Two more cloud-borne hazards

Structural icing

  • Needs visible moisture (cloud/rain) and a surface at 0°C or colder.
  • Clear ice — large supercooled drops, freezes slowly into a heavy glaze (most dangerous). Rime ice — small drops, freezes fast, rough/milky. Mixed — both.
  • Helicopter concern: ice on rotor blades destroys lift and balance fast — most light helicopters are placarded against flight into known icing.

Turbulence sources

  • Convective (rising thermals/cumulus), mechanical (wind over terrain/buildings), frontal (along the boundary), wind shear / clear-air turbulence (often near the jet stream, no cloud warning), and mountain wave (lenticular/rotor clouds).
14· Numbers Worth Knowing

The standard atmosphere & quick anchors

ItemValue
Std sea-level temp15°C / 59°F
Std sea-level pressure29.92 inHg / 1013.2 hPa
Avg temp lapse rate~2°C per 1,000 ft
Dry adiabatic lapse rate3°C (5.4°F) per 1,000 ft
Fog/IFR thresholdVis < 5/8 SM
Storm avoidance20 NM from any Cb
Where weather livesEssentially all weather happens in the troposphere (surface to ~36,000 ft at mid-latitudes). The boundary above it, the tropopause, is where thunderstorm anvils flatten out — which is why a Cb top spreading sideways tells you it has hit the ceiling of the weather layer.
Sources & how this was built

Content aligned to FAA references: PHAK (FAA-H-8083-25) Ch.12 Weather Theory & Ch.13 Weather Services; the Aviation Weather Handbook (FAA-H-8083-28, which absorbed AC 00-6 and AC 00-45); the AIM (sky cover/ceiling definitions); and the Helicopter Flying Handbook (FAA-H-8083-21B) for rotorcraft-specific notes on mountain wave, icing, and wind shear.

Every cloud picture is a hand-built vector illustration (drawn into this file), chosen to highlight the identifying shape rather than any single photograph — so the tool stays fully offline and self-contained. Compare them against real photos as you study; the shapes are what you're training your eye on.

The Brief

A plain-language overview of this tool, and the four clouds worth memorizing first.

This is your Aviation Weather & Clouds tool — the read-aloud deck (cloud pictures are skipped so it only narrates the words), a 5-minute study timer, and a Source/copy tab. It carries your 6JJ callsign.

What's inside: 15 guide sections grounded in PHAK / Aviation Weather Handbook / AIM / HFH. The heart of it is a cloud gallery — every cloud type drawn as a custom illustration with a Spot it / Means / Hazard breakdown so you train your eye on the identifying shape: high (Ci, Cc, Cs), middle (Ac, As), low (St, Sc, Ns), vertical (Cu, TCu, Cb), plus the danger clouds (lenticular, rotor, mammatus, fog). Then sky cover & ceilings, fog types, fronts, thunderstorms, icing/turbulence, and the standard-atmosphere numbers. 36 flashcards, 22 quiz questions.

The drawings teach the silhouette — but your CFI pointed at a real cloud. Burn these four into memory first.

Know these four on sight

Cumulonimbus Cb

The one that can kill you. Flat anvil top, dark base, the king of clouds. Avoid by 20 NM.

Standing Lenticular ACSL

Smooth lens / "UFO" stack that sits still over mountains. Looks calm, warns of severe mountain-wave turbulence.

Cirrus Ci

The mild one. Thin white feathery streaks high up, no shading — usually the first hint a warm front is coming.

Mammatus

Droopy pouches hanging under a storm anvil. A sign a severe thunderstorm is right there.

Three of these four are hazard flags. Pair each drawing with the real photos below until your eye knows them cold.

See the real thing — public domain

This file is kept fully self-contained and offline, so the web photos from our chat aren't baked in — those are copyrighted, and embedding them in a file you host or share would be a copyright problem (and they'd break offline). Instead, here are public-domain / open-license photo libraries. Tap to open when you're online and compare them to the illustrations above.

Tip: on Wikimedia Commons or the NOAA library, just search the cloud's name (e.g. "cumulonimbus," "lenticular," "mammatus") to pull up galleries of real photos.

Want them embedded?If you'd rather have real photos baked into this tab so they work offline too, save a few you like from the NWS or NOAA links (both public domain) and send them to me — I'll embed them permanently as offline-safe pictures.
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