Skydiving Weather Guide

Weather can change faster than forecasts update. Check more than one source, look at how old the data is, and don't make the call off a single forecast or a single station report.

How Windy Is Too Windy to Skydive?

There's no single number for everyone. It depends on who's jumping and on the dropzone.

Gusts matter as much as the average. 12 mph steady is a very different day from 8 gusting 20. A big gap between the steady wind and the gusts means bumpy, unpredictable air right where you're flaring.

Winds aloft matter too. Strong upper winds push you a long way in freefall, make the spot more critical, and mean groups need more time between exits on jump run. If you open in the wrong place on a big upper-wind day, you may not make it back.

Rules change, so check the current USPA SIM and your DZ's limits. If it's a hold for students, it's worth asking yourself why you'd go.

Weather Decision Framework (Go or No-Go)

When the weather is borderline, break the decision into four questions:

If you're newer to the sport, keep your personal limits conservative and don't be shy about asking an instructor or experienced jumper what they think before you get on the plane.

Green Sources agree, conditions steady Steady winds, small gusts, and no storms building nearby.
Amber Mixed signals or getting worse Gusts picking up, wind direction swinging around, or storms nearby with unclear timing.
Red Hazardous and changing fast Storm outflow, thunderstorms close by, strong shear, dust devils, or rotor over the landing area.
Pilots learn this as Aeronautical Decision-Making (ADM). The FAA's chapter on it, linked in the references below, is worth reading for skydivers too.

Wind Structure by Altitude

The wind on the ground, the wind where you fly your canopy, and the wind in freefall are often blowing different directions at different speeds. Each layer affects a different part of the jump.

When the wind direction changes a lot with altitude, you won't drift in a straight line. A spot that works for a belly group can be wrong for a freefly group or a tandem, because they spend different amounts of time in each layer and open at different altitudes.

Arrows show where the wind blows to N 12,000 ft exit 34 kt from 280° 9,000 ft freefall 29 kt from 265° 6,000 ft freefall 21 kt from 245° 3,000 ft opening 14 kt from 215° Surface landing 8 kt from 180°
A common day: the wind turns from south at the ground to west at exit altitude and gets stronger with height. Each layer pushes your spot, freefall drift, and canopy a different way.

Thermal Turbulence and Rotor

Thermal Turbulence

Thermals are rising bubbles/columns of warm air and are usually strongest during sun-driven heating cycles. They can produce abrupt vertical and lateral changes under canopy, especially over mixed terrain (asphalt, fields, buildings, and dry patches).

A canopy can feel floaty in the thermal core, then lose lift after crossing the edge into sinking air. That "pop up then sink" transition is one of the classic thermal-turbulence surprises on final.

Rising Sinking Sinking lift… …then sink Hot pavement or dry field
Air rises over hot ground and sinks around it. Fly from rising air into sinking air on final and the canopy can balloon up, then drop.

Mechanical Turbulence and Rotor

Flow over and around terrain or obstacles can create wake turbulence and rotor on the lee side. This is common near hangars, tree lines, ridges, and large structures and can persist downwind.

Wind HANGAR Rotor final Low down, air rolls back toward the hangar
Wind goes over the hangar and tumbles down behind it. A canopy on final through the downwind side can get bounced or partly collapse close to the ground.

What this means under canopy

Gust Fronts, Outflow, and Storm Influence

Thunderstorms push out a wall of cold air called an outflow boundary or gust front. It can bring sudden wind shifts and strong gusts miles away from the rain.

Rain Cold outflow Gust front light wind now DZ often miles ahead of the rain Wind can flip direction and gust hard in seconds
Cold air pouring out of a storm spreads along the ground ahead of it. The gust front can reach the DZ well before any rain, often while people are in the pattern.
If you're not sure when the storm will arrive, wait. There's always another load.

Wind Shear and Directional Change

Wind shear is a significant change in wind speed and/or direction over a short distance. Under canopy, you feel it as a sudden change in groundspeed or a push off your heading, often during opening or low in the pattern.

Upper wind ⚠ Shear zone Lower wind, opposite direction pushed off heading
When the wind changes direction or speed sharply at one altitude, a canopy flying through that layer suddenly gets pushed a different way. If you only check the surface wind, it can surprise you on opening or on final.

Dust Devils and Dirt Devils

Dust devils are spinning columns of rising air that form over hot, dry ground, usually on sunny days with fairly light wind. Most are small and only last a minute or two, but they can still collapse a canopy close to the ground.

Dust devil stay well clear Hot, dry ground · light wind · sunny afternoon
Dust devils show up on hot, clear afternoons over dry open ground, which is often exactly when and where skydivers land. Even a small one can collapse a canopy near the ground.

Collapses, Surges, and Deformation Risk

In turbulent air, a ram-air canopy can surge forward, rock, turn on its own, or partly collapse for a moment. Up high that's usually just uncomfortable. Close to the ground there's no time to recover.

On bumpy days, keep your landing simple, fly a predictable pattern, and stay away from obstacles. If you haven't taken a canopy course, it's the single best thing you can do to handle these days well. They teach you what turbulence feels like and how to fly through it. Find one through USPA.

Weather Checks Before You Board

Students and newer jumpers: ask questions, and if the weather feels off, it's always OK to sit a load down.

Use With winDZaloft Tools

Trusted References

Sources used for this page, if you want to go deeper.

FAA PHAK Chapter 2: Aeronautical Decision-Making

Core framework for risk and decision behavior in aeronautical operations.

FAA PHAK Chapter 12: Weather Theory

Meteorology fundamentals relevant to thermals, turbulence, instability, and wind behavior.

FAA PHAK Chapter 13: Aviation Weather Services

How flight crews use weather products and why product timing/validity matter operationally.

NOAA Aviation Weather Center (AWC)

Primary U.S. aviation weather products and data interfaces.

AWC Graphical Forecasts for Aviation (GFA)

Graphical view for winds, hazards, and forecast context across altitude/time.

NOAA JetStream Weather School

Educational weather modules for turbulence, atmospheric structure, and storm processes.

NWS Wind Safety

Safety context for hazardous wind events, gust potential, and strong wind impacts.

NWS Dust Storm and Haboob Safety

Dust-related wind hazard context relevant to dry, convective, and visibility-limited environments.

USPA Skydiver's Information Manual (SIM)

Sport-specific operational and safety context to pair with meteorological guidance.

USPA Canopy Courses and Educational Programs

Find formal canopy training opportunities to build safer weather and landing decision-making skills.

SKYbrary: Windshear

Aviation safety reference on wind shear hazards and operational implications.