A cloud is a visible mass of tiny liquid droplets and/or ice crystals hanging in the air, each clinging to a condensation nucleus (dust, salt, pollen, smoke). It is not a gas — the invisible part is the water vapouraround the droplets. White or grey? Sunlight scatters off zillions of droplets; when the cloud is thick enough, light cannot punch through, so the base looks dark even on a sunny day.
🧪 SCALE
A small fair-weather puffy can hold hundreds of tonnes of liquid water if you add all those micro-drops — still lighter-than-air as a whole parcel of rising, buoyant air.
FLOAT!
DROPLET
Droplet sizes: mostly tiny, so they float with the wind
ICE
High and cold: crystals & hazy wispy structure
PAGE 2 OF 5, THE AIR MUST RISE (OR LOSE HEAT)
LIFTING MECHANISMS
COOL UNTIL SATURATION
To get a cloud, you need cooling to the dew point. That usually means air rising, because it expands and chills adiabatically in the thinner upper sky. Convection (bubbling thermals) builds puffy clouds. Mountains force wind upward — orographic clouds. Fronts slide air masses, lifting warm over cold or ploughing cold under warm. At night, the ground cools and can fog the surface — same physics, just not rising very far. No lift, no story — or a very thin one.
UP!
THERMALS
Heated ground → buoyant columns → cumulus family
RIDGE
Wind hits slopes — forced ascent, banner clouds possible
SLIDE
Frontal lift: one air mass rides over or wedges under another
PAGE 3 OF 5, HIGH, WISPY, USUALLY ICE
CIRRUS
Feathery — ice crystals falling slowly, sometimes sheared into hooks
CIRRO-
Veil or patch high up — often first hint of a warm front in mid-latitudes
6–12 KM UP
READ THE CIRRUS TEA LEAVES
Cirrus, cirrostratus, cirrocumulus live in the high troposphere where it is cold, so ice dominates. Wispy mares' tails and thin veils do not mean a picnic every time — but spreading cirrostratus can signal moisture riding ahead of a system in many regions. Contrails are human-made cirrus where jet exhaust provides nuclei. Watch shape change over hours — the sky is a slow-motion map.
WISPY!
PAGE 4 OF 5, FLAT, GREY, STEADY
STRATIFORM LAYERS
DRIZZLE HOURS, NOT A MINUTE BURST
Stratus & stratocumulus form wide sheets — stable air lifted just enough to smear moisture across a layer. Nimbostratus is the thick, dark, sad blanket that brings hours of light-to-moderate rain or snow, not a dramatic thunder clap. Altostratus in mid levels can dim the sun into a hazy disc (often a front is close). Character: low drama on the convective scale, high duration on the human calendar.
SOAK!
FOG =
Stratus on the ground — same droplets, your shoes get wet
MASH
Stratocumulus: bumpy underbelly, often dry gaps between clumps
NIMBO-
"Nimbo-" = rain-bearer; thick layer = long wet afternoon
PAGE 5 OF 5, TOWERS, ANVILS, & STORMS
CUMULUS → CUMULONIMBUS
PUFF, TOWER, THEN ANVIL
Fair-weather cumulus = gentle convection, short lives. Towering cumulus = strong updraft; watch vertical growth. Cumulonimbus hits the tropopause and spreads an anvil of ice — that is a thunder factory: rain, lightning, maybe hail, microbursts. Shape = energy. After this topic, Topic 4 (on the hub) looks at the whole atmosphere in layers — the stage where all these clouds act out their play.
☁️ READER TIP
Once a day, name three cloud types you see. Trend beats one snapshot — weather is a movie.
LOOK!
ANVIL
Flat icy top: cloud hits the "ceiling" of the troposphere