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Part of the Aviation Weather Reference — the complete hub for METAR, TAF, SIGMETs, icing, turbulence, ISA, and weather decision-making.

Weather symbols are standardised by the World Meteorological Organization (WMO) and adopted globally through ICAO Annex 3. These symbols ensure that pilots, forecasters, and dispatchers everywhere interpret weather information consistently, regardless of language or nationality.

METAR Weather Codes

Weather phenomena in METAR reports are encoded as text codes constructed by combining up to three elements: an intensity prefix, a descriptor, and a precipitation or obscuration type. For example, +TSRA means heavy (+) thunderstorm (TS) with rain (RA).

Intensity Prefixes

PrefixMeaningNotes
-LightPrecipitation is light; visibility generally not severely reduced
(none)ModerateNo prefix indicates moderate intensity — the default
+HeavySignificant impact on visibility and operations
VCIn the vicinityWithin 8 km of the aerodrome reference point, but not at the station

Descriptor Codes

CodeMeaningUsage Notes
MIShallowUsed with FG only — fog extending less than 2 m above ground
BCPatchesUsed with FG only — patchy fog across the aerodrome
PRPartialUsed with FG only — fog covering part of the aerodrome
DRLow driftingUsed with DU, SA, SN — below eye level (below ~2 m)
BLBlowingUsed with DU, SA, SN — raised above eye level by wind
SHShower(s)Used with RA, SN, GR, GS, PL — convective precipitation
TSThunderstormMay appear alone or with precipitation types (e.g. TSRA, TSGR)
FZFreezingUsed with FG, DZ, RA — supercooled water freezing on contact

Precipitation Types

CodeMeaningNotes
RARainLiquid precipitation, droplet diameter > 0.5 mm
SNSnowFrozen precipitation in the form of ice crystals
DZDrizzleFine droplets < 0.5 mm diameter, close together
GRHailIce balls or irregular ice ≥ 5 mm diameter
GSSmall hail / snow pelletsIce particles < 5 mm; includes graupel
PLIce pelletsTransparent or translucent pellets of ice; also called sleet
SGSnow grainsVery small, white, opaque ice particles; the frozen equivalent of drizzle
ICIce crystalsAlso called diamond dust; tiny crystals suspended in air, common at very low temperatures
UPUnknown precipitationUsed at automated (AUTO) stations when the sensor cannot determine the type

Obscuration Types

CodeMeaningNotes
FGFogVisibility < 1,000 m; composed of water droplets
BRMistVisibility 1,000–5,000 m; similar to fog but less dense
HZHazeFine dry particles; visibility generally 1,000–5,000 m
FUSmokeCombustion particles suspended in air
VAVolcanic ashFine rock particles from volcanic eruption; severe hazard to engines
DUWidespread dustFine particles of earth raised by wind
SASandSand particles raised by wind; coarser than dust
PYSprayWater droplets torn from a water surface by wind

Other Weather Phenomena

CodeMeaningNotes
SQSquallSudden increase in wind speed ≥16 kt, sustained ≥22 kt for ≥1 min
SSSandstormSand raised by strong wind; visibility severely reduced. Use + for severe.
DSDuststormDust raised by strong wind; visibility severely reduced. Use + for severe.
FCFunnel cloudTornado or waterspout when preceded by +; funnel cloud (not surface) otherwise
PODust/sand whirlsWell-developed dust devils or sand pillars

Synoptic Chart Symbols

Synoptic weather charts depict large-scale weather systems using standardised symbols for fronts, pressure systems, and boundaries. The following frontal symbols are used on aviation and meteorological charts worldwide.

Frontal Symbols

Cold Front

Blue line with triangles pointing in the direction of movement. Cold air advances and undercuts warmer air, causing rapid lifting. Often associated with cumulonimbus, heavy showers, and gusty winds. Passage marked by a wind shift, pressure rise, and temperature drop.

Warm Front

Red line with semicircles pointing in the direction of movement. Warm air overrides cooler air ahead, producing a broad zone of cloud (cirrus, altostratus, nimbostratus) and prolonged, steady precipitation. Approach is signalled by lowering cloud bases.

Occluded Front

Purple line with alternating triangles and semicircles pointing in the direction of movement. Occurs when a cold front overtakes a warm front. Weather combines characteristics of both fronts — may produce heavy precipitation and embedded thunderstorms.

Stationary Front

Alternating blue triangles and red semicircles on opposite sides of the line. Neither air mass is advancing. Can persist for days, producing prolonged areas of cloud and precipitation along the boundary.

Pressure Systems

SymbolMeaningNotes
LLow pressure centreCounterclockwise circulation (N. hemisphere); associated with cloud and precipitation
HHigh pressure centreClockwise circulation (N. hemisphere); generally fair weather
TROUGHTrough of low pressureElongated area of low pressure; may trigger convection along its axis
RIDGERidge of high pressureElongated area of high pressure; generally fair weather

Cloud Type Symbols

Cloud types are classified by the WMO into ten genera, grouped into three height bands. On aviation charts and in weather reports, standard abbreviations are used to identify cloud types. Cumulonimbus (CB) and towering cumulus (TCU) are always reported in METARs when present, regardless of amount.

High Clouds
Above FL200 (approx. 20,000 ft / 6,000 m) — composed of ice crystals
CICirrus — thin, wispy, fibrous
CCCirrocumulus — small white patches, rippled
CSCirrostratus — thin, whitish veil, halo phenomena
Medium Clouds
6,500–20,000 ft (2,000–6,000 m) — water droplets and/or ice crystals
ACAltocumulus — white/grey patches, rounded masses
ASAltostratus — greyish sheet, sun visible as through ground glass
NSNimbostratus — thick, dark grey layer, continuous rain/snow
Low Clouds
Surface–6,500 ft (0–2,000 m) — predominantly water droplets
SCStratocumulus — grey/white layer with rounded masses
STStratus — uniform grey layer, may produce drizzle
CUCumulus — detached, dense, vertical development
CBCumulonimbus — heavy, dense, great vertical extent; thunderstorms

METAR cloud reporting: Cloud amounts are given in oktas (eighths of sky) using the codes FEW (1–2), SCT (3–4), BKN (5–7), OVC (8/8). Heights are in hundreds of feet AGL. The suffixes CB and TCU are appended when cumulonimbus or towering cumulus are observed — e.g. BKN040CB.

Wind Symbols

Station model wind barbs are used on synoptic charts and significant weather (SIGWX) charts to depict wind speed and direction. The barb points in the direction the wind is coming from, with speed indicated by half barbs, full barbs, and pennants attached to the end of the shaft.

Calm
0 knots — no wind
5 Knots
Half barb = 5 kt
10 Knots
Full barb = 10 kt
25 Knots
2 full + 1 half barb
50 Knots
Pennant (triangle) = 50 kt
75 Knots
1 pennant + 2 full + 1 half
ElementValueAppearance
Circle onlyCalm (0 kt)Empty circle at station position
Half barb (short line)5 ktShort tick on the shaft
Full barb (long line)10 ktFull-length tick on the shaft
Pennant (filled triangle)50 ktSolid triangular flag on the shaft

Wind barbs are additive — combine pennants, full barbs, and half barbs to read the total wind speed. For example: one pennant + one full barb + one half barb = 50 + 10 + 5 = 65 knots.

Visibility and Ceiling Symbols

The following codes appear in METAR and TAF reports to indicate special visibility or cloud conditions. These codes replace the standard cloud and visibility groups when applicable.

CodeMeaningConditions
CAVOK Ceiling and Visibility OK Visibility ≥10 km, no cloud below 5,000 ft or below minimum sector altitude (whichever higher), no CB or TCU, and no significant weather
SKC Sky Clear No cloud at any level; used at manual observation stations
NSC No Significant Cloud No cloud below 5,000 ft or below MSA, no CB/TCU; used when CAVOK criteria are not fully met (e.g. significant weather present)
NCD No Cloud Detected Automated station (AUTO) — ceilometer detected no cloud; does not guarantee clear sky beyond sensor range
VV Vertical Visibility Sky obscured; followed by a three-digit height in hundreds of feet. Example: VV005 = vertical visibility 500 ft. Used when a ceiling cannot be determined due to obscuration (fog, heavy snow, etc.)

IFR ceiling definition: A ceiling exists when the lowest layer is reported BKN (broken) or OVC (overcast), or when vertical visibility (VV) is reported. For IFR planning, the ceiling is the height of the lowest BKN/OVC layer or the VV value.

Turbulence and Icing Symbols

Turbulence and icing are reported on Significant Weather (SIGWX) prognostic charts, PIREPs (pilot reports), and AIRMETs/SIGMETs. The following intensity scales and type classifications are standardised by ICAO.

Turbulence Intensity

IntensityPIREP CodeEffect on Aircraft
Light LGT Slight, erratic changes in altitude/attitude; occupants may feel slight strain against belts. Unsecured objects displaced slightly.
Moderate MOD Changes in altitude/attitude occur, but aircraft remains in positive control. Occupants feel definite strain against belts. Unsecured objects dislodged.
Severe SEV Large, abrupt changes in altitude/attitude. Large airspeed variations. Aircraft may be momentarily out of control. Occupants forced violently against belts.
Extreme EXTRM Aircraft is violently tossed about and practically impossible to control. May cause structural damage.

Turbulence Types on Charts

TypeAbbreviationDescription
Clear Air TurbulenceCATOccurs in clear air, typically near the jet stream or in areas of strong wind shear at high altitude
MechanicalMECHCaused by terrain or obstructions disrupting airflow; common at low levels near mountains
ConvectiveCONVAssociated with cumulonimbus and thunderstorms; updrafts/downdrafts
Mountain waveMTWStanding waves on the lee side of mountains; may extend to great heights and include rotor turbulence at lower levels

Icing Intensity

IntensityPIREP CodeAccumulation Rate / Effect
Trace TRACE Ice becomes perceptible. Rate of accumulation slightly greater than sublimation. Not hazardous unless encountered for extended period.
Light LGT Rate of accumulation may create a problem for prolonged flight (>1 hour). Occasional use of de-icing equipment removes accumulation.
Moderate MOD Rate of accumulation is such that even short encounters become potentially hazardous. Use of de-icing/anti-icing or diversion is necessary.
Severe SEV Rate of accumulation is such that de-icing/anti-icing equipment fails to reduce or control the hazard. Immediate exit from the icing environment is required.

Icing Types

TypeDescriptionTypical Conditions
Rime ice Rough, milky-white, opaque ice formed by rapid freezing of small supercooled droplets Stratiform cloud, temperatures -10 to -20 °C, small droplets
Clear ice (glaze) Smooth, transparent, dense ice formed by slow freezing of large supercooled droplets Cumuliform cloud or freezing rain, temperatures 0 to -10 °C, large droplets
Mixed ice Combination of rime and clear ice, rough and irregular Mixed droplet sizes; varying temperature zones within cloud
SLD (Supercooled Large Droplets) Freezing drizzle or rain; droplets > 50 microns. Extremely hazardous — ice can accumulate aft of protected surfaces. Warm layer aloft producing rain that becomes supercooled below; also in deep convective cloud

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