Weather Deviation Procedures

Operational ProceduresCPL · IR · ATPL12 min readUpdated Oct 2026
Definition

A weather deviation is a departure from the cleared route to keep an aircraft clear of thunderstorms or other hazardous weather. It is normally flown with an ATC clearance; in oceanic airspace, when no clearance can be obtained in time, ICAO procedures set the broadcasts, lookout and level offsets that keep other traffic safe.

A weather deviation is a departure from the cleared route to keep an aircraft away from a thunderstorm and the hail, turbulence, icing and windshear around it. It is everyday airline flying in convective weather: a line of cumulonimbus, such as those of the intertropical convergence zone, can push every aircraft on an airway or an oceanic track off its route at once.

Deviations need procedures because separation is planned along the cleared route. Under radar the controller sees a deviating aircraft and moves other traffic out of its way. Over the ocean, separation rests largely on position reports and data link, and an aircraft that leaves its track without a clearance can fly into the traffic on the next one. ICAO's PANS-ATM (Doc 4444) therefore sets out a weather deviation procedure for oceanic airspace, which the FAA publishes in its AIP, while the FAA AIM, the manufacturers and the operators' manuals give the distances to keep from storms.

Why deviations need procedures

Oceanic tracks are close by the standards of a storm. Lateral separation between them can be 50 NM for aircraft approved for RNP 10, 30 NM with RNP 4, ADS-C and CPDLC, and 23 NM for aircraft with RNP 4 or RNP 2 and the required data link performance. The North Atlantic organized tracks reserved for such aircraft are 23 NM apart between FL340 and FL400, so there a 20 NM deviation takes an aircraft most of the way to the next track. Vertically, RVSM puts aircraft 1,000 ft apart between FL290 and FL410. A level offset smaller than that keeps a deviating aircraft away from the flight levels assigned to everyone else.

Three different procedures move an aircraft off its centerline in oceanic airspace, and exam questions often mix them up:

Strategic lateral offset (SLOP) Weather deviation Contingency procedure
Purpose Spread traffic off the centerline, against collision risk and wake Avoid weather The aircraft cannot keep its clearance and has no revised one
Lateral Right of the centerline only, up to 2 NM Either side, as far as the weather requires Turn of at least 30°, then a parallel track 5 NM away
Level Unchanged Unchanged below 5 NM off track; from 5 NM, a 300 ft change without a clearance 500 ft offset from the normal levels (1,000 ft above FL410), at the same level or after a descent below FL290

Requesting a deviation in radar airspace

In radar airspace a deviation is a request like any other, but its content matters. The FAA AIM (7-1-12) asks pilots to state a heading or a number of degrees, the direction of the deviation and the approximate number of miles, for example "requesting deviation 20 degrees left for weather", and as far as possible where the detour will begin and where the route will be resumed. Once the deviation is approved, navigation within the lateral limits given by ATC is at the pilot's discretion, but the assigned altitude is kept: a change of altitude is a separate request. Requests are best made as far in advance as possible, because the controller has to assess the traffic and may need to coordinate with other sectors.

If an immediate turn is needed for the safety of the flight, the pilot in command may deviate at once, under 14 CFR 91.3(b) in the United States, and must tell ATC as soon as possible. ICAO's Annex 2 follows the same principle: the rules of the air may be departed from only when absolutely necessary in the interests of safety, and the pilot in command has final authority over the disposition of the aircraft.

Deviations begin at the planning stage, with TAFs, SIGMETs, significant weather charts, radar imagery and extra fuel for the detours. Embedded cumulonimbus, reported as EMBD in a SIGMET or on a significant weather chart, is hidden in layer cloud, so the onboard weather radar becomes essential. Datalinked weather such as FIS-B NEXRAD mosaic imagery shows where the weather was, possibly 15 to 20 minutes older than the display indicates, so the AIM accepts it for strategic route selection around an area of storms but never as the sole means of tactical maneuvering between cells.

Oceanic weather deviation procedure

The ICAO procedure, reproduced in ENR 7.3 of the FAA AIP and in chapter 10 of NAT Doc 007, starts with communication. The crew contact ATC by CPDLC or voice, as early as possible. A rapid response may be obtained by stating WEATHER DEVIATION REQUIRED, which asks for priority on the frequency and for the ATC reply, or by sending a CPDLC lateral deviation request; when necessary the call opens with the urgency signal PAN PAN, preferably spoken three times, or a CPDLC urgency message. They request clearance to deviate, giving the extent of the deviation, and tell ATC when the deviation is no longer required or has been completed and the aircraft is back on its cleared route.

If the controller can apply separation, the deviation is cleared. If there is conflicting traffic and the controller cannot establish separation, the controller says so, gives the conflicting traffic and asks the pilot's intentions; the FAA's phraseology is "UNABLE (requested deviation), TRAFFIC IS (call sign, position, altitude, direction), SAY INTENTIONS". The crew then either comply with the clearance or state their intentions and apply the procedure for flight without a clearance.

If a revised clearance cannot be obtained, a clearance is still to be obtained at the earliest possible time, and until then the crew:

Originally cleared track (magnetic) Deviating left Deviating right
000° to 179° Descend 300 ft Climb 300 ft
180° to 359° Climb 300 ft Descend 300 ft

On an east-west track this works out the same in both directions: an aircraft deviating to the north descends and one deviating to the south climbs. The pilot's judgment determines the sequence of actions, and ATC gives all possible assistance. The 5 NM threshold dates from Amendment 9 to PANS-ATM, applicable since 5 November 2020; older texts and exam material give 10 NM. Crews apply the version in the current AIP and, on the North Atlantic, NAT Doc 007 (see oceanic and North Atlantic operations).

Satellite view of dark blue ocean off the west coast of Africa, crossed by a broad band of white cloud clusters.
The Atlantic off West Africa from a satellite: the ITCZ runs across it as a band of convective cloud clusters. Long-haul crews deviate around such cells far from radar coverage, under the oceanic procedures.NOAA · Public domain · Wikimedia Commons

Oceanic contingency procedure

The oceanic contingency procedure covers the other cases in which an aircraft cannot continue in accordance with its clearance and cannot first obtain a revised one, such as a diversion across the traffic flow, a loss of the required navigation capability or a pressurization failure. The aircraft leaves the cleared route by turning at least 30° to the right or left to establish a parallel, same-direction track offset by 5 NM, on the side where other traffic is less likely. If possible it keeps its level until established on the offset. It then establishes a vertical offset of 500 ft from the levels normally used, 1,000 ft above FL410, either at its level or after descending below FL290, the option suited to a parallel track system or a one-way traffic flow. At FL410 itself the offset is 500 ft, to FL405 or FL415. The crew keep the transponder on and squawk 7700 when able, use MAYDAY or PAN PAN as appropriate, broadcast on 121.5 MHz and advise ATC as soon as practicable. The 45° turn and 15 NM offset of older texts no longer apply, and a deviation around weather follows the weather procedure instead.

Strategic lateral offsets

The strategic lateral offset procedure (SLOP) is approved in the North Atlantic, the Pacific and other oceanic regions. Accurate navigation puts every aircraft exactly on the centerline, so an aircraft that deviates in level meets others exactly there; SLOP spreads them out. Offsets are always to the right, up to 2 NM, flown with the FMS offset function and chosen at random. In the North Atlantic, aircraft that can program them may choose any offset in steps of 0.1 NM, where older texts allowed only the centerline, 1 NM or 2 NM. An offset also relieves wake turbulence, and two crews can agree their offsets on 123.45 MHz.

Distances from thunderstorms

No single rule applies everywhere. EASA sets no figure in regulation, and operators publish their minima in the operations manual, normally from manufacturer guidance. The figures most often quoted are these:

Source Lateral Vertical and other
FAA AIM 7-1-27 and AC 00-24C At least 20 NM from any storm identified as severe or giving an intense radar echo, especially beneath the anvil; heavy or extreme echoes at least 40 NM apart before flying between them Treat tops of 35,000 ft or more as extremely hazardous; never fly under a thunderstorm or its anvil
FAA AIM 7-1-26 Severe turbulence can be expected up to 20 NM from a severe storm, about 10 NM from a less severe one
UK CAA airborne radar criteria Below 20,000 ft, 10 NM from echoes with hooks, fingers, scalloped edges, strong intensity, sharp gradients or rapid change; above 20,000 ft, 20 NM from all echoes
Airbus briefing note on weather radar 20 NM, preferably upwind; in cruise, from every cell with green or stronger returns 5,000 ft

Two severe or intense cells less than 40 NM apart therefore leave no gap to fly through, and the AIM adds that no path between strong echoes 20 to 30 NM apart or less can be considered free of severe turbulence. Hail can fall from the anvil into clear air several miles from the cell, and the threat is greater on the downwind side, which is why a deviation goes upwind of a storm whenever there is a choice. The visual appearance of a storm says nothing reliable about the turbulence inside it.

A towering white storm cloud with a flat anvil top spreading out to the left over clear sky, above a rural road, fence and distant hills.
A cumulonimbus with a spreading anvil, seen from Canberra. Hail can fall from the anvil into clear air downwind of the storm, which is why deviations are made on the upwind side and never beneath the anvil.Karen Hedley · Public domain · Wikimedia Commons
A cumulonimbus is most dangerous in its mature stage, and the plan view shows why deviations go upwind: hail and turbulence spread downwind under the anvil. The distances drawn are general guidance; the FAA AIM's 20 NM applies to any storm identified as severe or giving an intense radar echo, and operators publish their own minima. v1prep schematic.
A cumulonimbus is most dangerous in its mature stage, and the plan view shows why deviations go upwind: hail and turbulence spread downwind under the anvil. The distances drawn are general guidance; the FAA AIM's 20 NM applies to any storm identified as severe or giving an intense radar echo, and operators publish their own minima. v1prep schematic.Illustration © v1prep

Using weather radar

Weather radar sees precipitation, not cloud or turbulence. Wet hail gives the strongest return, while the dry upper part of a storm and its anvil, made of ice, may give almost none. The tilt keeps the beam on the wet, reflective part of the storm, below the freezing level, without overscanning the tops or painting ground clutter. Airbus gives a rule of thumb for the height of a cell top relative to the aircraft, about 100 ft per NM of range per degree of tilt: an echo that disappears at 40 NM with 1° of down-tilt has its top about 4,000 ft below. The gain normally stays in AUTO or CAL and is changed only to evaluate a cell, reduced to find the strongest core or increased at high altitude, where cloud is less reflective, then reset.

The areas to avoid by a wide margin are the steepest color gradients, where the zones crowd together, and the hooks, fingers, U-shapes and scalloped edges that suggest hail. Heavy rain attenuates the beam, so a cell behind another paints weaker than it is, and a black shadow behind a red return must be treated as potentially very active. A deviation is planned on a long range and flown on a short one, and never into a shadow or an area the beam has not scanned; Airbus wants the decision made while still 40 NM from a large storm. The HOLD function freezes the picture; comparing it with the live image a little later shows how the cells are moving relative to the aircraft, a help in choosing the side to deviate. Weak returns at cruise level above strong returns lower down mark a very turbulent area and can mean high concentrations of ice crystals, a threat to engines and air data probes even where the display shows little.

Navigation display with a magenta track line and, to the right, a patch of radar returns in green, yellow and red.
Weather radar returns from cumulonimbus to the right of track on a Boeing 737NG navigation display, with the wind 234°/50 kt at top left. Green is light, yellow moderate and red heavy precipitation; with the wind from the left, a deviation here would go left, upwind of the cells.Shawn from Airdrie, Canada · CC BY-SA 2.0 · Wikimedia Commons

Communication failure during a deviation

The oceanic weather deviation procedure is written for the case where no clearance can be obtained, including when ATC cannot be reached at all. The crew deviate as safety requires, broadcast on 121.5 MHz, or 123.45 MHz as a backup, keep the lookout and the lights, apply the 300 ft change from 5 NM off track and keep trying to obtain a clearance. On the North Atlantic every aircraft is required to monitor 121.5 MHz and asked to monitor 123.45 MHz as well when possible, so other crews hear the broadcasts and can relay. CPDLC, satellite voice and HF offer further channels.

If two-way radio has failed altogether, the crew set 7600 and, once clear of the weather, return to the cleared route at the assigned level, which the weather procedure has them regain before 5 NM from the centerline. They then follow the regional radio communication failure procedure; on the North Atlantic, after a loss of communications inside the region, the current NAT Doc 007 has the crew maintain the cleared route, flight level and speed to the oceanic exit point, changing them earlier only when the pilot in command judges it necessary for safety.

Exam tip: in the oceanic weather deviation procedure, less than 5 NM off track means no level change; 5 NM or more without a clearance means 300 ft, descending when deviating left on a track of 000° to 179°. Do not confuse it with the contingency procedure (30° turn, 5 NM offset, 500 ft or 1,000 ft) or with SLOP (right only, up to 2 NM).

Frequently asked questions

What is the oceanic weather deviation procedure?

The crew first request a clearance, starting the call with WEATHER DEVIATION REQUIRED, or PAN PAN if necessary. If no clearance can be obtained, they deviate away from organized tracks if possible, broadcast their level, position and intentions on 121.5 MHz, watch for traffic visually and on ACAS and turn on the exterior lights. For a deviation of less than 5 NM they keep their level; from 5 NM off track they climb or descend 300 ft according to track direction and deviation side.

How far should you stay away from a thunderstorm?

The FAA AIM advises avoiding any thunderstorm identified as severe or giving an intense radar echo by at least 20 NM, especially under the anvil, and AC 00-24C wants such echoes at least 40 NM apart before flying between them. Airbus gives 20 NM laterally, preferably upwind, and 5,000 ft vertically. UK CAA radar criteria call for 10 NM from significant echoes below 20,000 ft and 20 NM from all echoes above. Operators publish their own minima.

How do you request a weather deviation from ATC?

Ask early and be specific: give a heading or a number of degrees, the direction and the approximate distance, and say where you expect to rejoin the route, for example requesting a deviation 20 degrees left for weather. A change of altitude needs its own clearance. If an immediate turn is needed for safety, the pilot in command may deviate at once and must tell ATC as soon as possible.

What is the difference between SLOP and a weather deviation?

The strategic lateral offset procedure is a small, planned offset of up to 2 NM, always to the right of the centerline, used in oceanic airspace where it is authorized to reduce collision risk and wake encounters. A weather deviation is a tactical departure, to either side and as far as the weather requires, normally cleared by ATC and, if it cannot be cleared, flown under the weather deviation procedure.

What do you do if you must deviate for weather and cannot contact ATC?

Deviate as safety requires and keep trying to obtain a clearance at the earliest possible time. Over the ocean, the weather deviation procedure covers this case: broadcast on 121.5 MHz, with 123.45 MHz as backup, watch for traffic, show exterior lights and apply the 300 ft level change from 5 NM off track. If the radio has failed altogether, squawk 7600, rejoin the clearance once clear and follow the regional radio failure procedure.

Test yourself on Weather Deviation Procedures

The v1prep banks cover this topic in Operational Procedures (070), with a worked explanation for every answer. EASA ATPL, PPL, IR and CPL, the FAA written tests and type ratings for the A320, 737, A220, 787, ATR 72 and E-Jet.

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