United States thermal forecast
Scan the broader pattern of afternoon thermal potential across the contiguous United States. Compare nearby flying areas and follow the forecast through the day.
Open the United States soaring map →Hourly soaring outlook • United States
Explore areas favorable for thermaling with animated, hourly maps of thermal potential, approximate thermal-top height and overdevelopment screening. See how daytime heating changes across your flying region.

Start with the national soaring outlook, then choose any state map for county boundaries and cities. Step through forecast hours to see where potential rises, peaks and fades.
Scan the broader pattern of afternoon thermal potential across the contiguous United States. Compare nearby flying areas and follow the forecast through the day.
Open the United States soaring map →Use the layer selector on a map to compare the broad thermal pattern, its approximate vertical extent and the possibility of convective overdevelopment.

An experimental 0-100 index showing areas more favorable for daytime surface heating and thermal development. Compare regions and times; the number is neither a climb rate nor a probability.

Boundary-layer height offers a rough estimate of how high daytime mixing may reach, shown in feet above ground level. Usable lift may stop below this height.

An experimental index highlights where growing convection could complicate soaring. It is not a thunderstorm probability or an official hazard alert.
USAIRNET processes NOAA HRRR weather-model fields into hourly experimental soaring layers. Its grid describes broad atmospheric conditions, not the exact field, hillside or cloud where a thermal will form.
Forecast colors help glider, hang glider and paraglider pilots compare possible soaring conditions over time.
What the shading means: Forecast colors highlight broad areas with more favorable thermal lift conditions. They do not pinpoint an individual thermal, promise a climb rate, or replace current weather observations and official aviation forecasts.
No. Thermals can form and detach on a smaller scale than the model can resolve. The map shows areas favorable for lift, not the position of individual rising columns.
No. The potential layer is an experimental 0-100 screening index. It is not a forecast of feet per minute, and the site does not assign a measured climb rate to each colored area.
AGL means above ground level. This layer approximates the height of the daytime boundary layer, which may differ from the actual top of usable soaring lift.
No. The current thermal soaring maps use a weather-model grid for the contiguous United States. Alaska and Hawaii would need separate model data and maps, and are not available in this forecast yet.
Not currently. The three map layers cover thermal potential, approximate thermal top and overdevelopment screening. Look at current sky conditions and other weather products to evaluate clouds.