Forecast Winds and Temps Aloft
Forecast Winds and Temperatures Aloft is a forecast of wind direction and speeds and of temperatures at different altitudes for specific locations. Data for the forecasts are gathered using a small expendable radiosonde attached to a 2 meter hydrogen or helium balloon. These balloons are released twice daily. Additional data is collected by commercial aircraft (AMDAR/MDCRS/ACARS), and a network of wind profiling radars operated by NOAA Global Systems Division (formerly known as Forecast Systems Laboratory). National Centers for Environmental Prediction (NCEP) produces scheduled wind and temperature aloft forecasts four times daily for the Continental United States, the Hawaiian Islands, Alaska and coastal waters, and the Pacific Ocean based on data collected by the weather balloon. There is no requirement to issue amendments to these forecasts. These reports were known as "FD" in the US, but are becoming known as "FB", following the World Meteorological Organization (WMO) nomenclature.
- Valid time: the specific time for which the winds and temperatures are forecast; and the
- For Use time: the time range for which the forecast values may be used.
Rules of Thumb
Winds and Temperature Aloft forecasts aids pilots with flight planning in that they forecast the existence (or absence) of head winds or cross winds which might dramatically change flight times and fuel consumption. Temperatures aloft can show temperature inversions, or unusually warm layers where climbing performance may be affected.Winds differ more than 18knts
Jack Williams, coordinator of public outreach for the American Meterological Society and frequent contributer to AOPA's Flight Training magazine wrote in the December 2007 issue that anytime the difference between two reporting altitudes is more than 18 knots, "wind shear could make a flight between those altitudes bumpy." As an aid, AvnWx.com places a dotted line between such altitudes under the wind data item, in the Winds Aloft display. You can see some examples in the above figure, such as between 30000 and 34000 in the 6hr report. It's more than just a simple 18knt difference, of course -- one has to consider the change in wind direction also. For example: 210 at 23 knts changing to 160 at 22 knts isn't a 1 knt wind shift, it is a 19 knt wind shift! Note that wind shear can happen anywhere so don't be complacent just because there isn't a dotted line at your altitude on this website.Temperature more than 3° per 1000'
Aviation Weather (page 52) gives some guidance regarding atmospheric stability, which can be estimated by observing how the temperature decreases with altitude:- When temperatures decrease uniformly and rapidly as altitude increases (approaching 3°C per 1000'), you have an indication of unstable air.
- If the temperature remains unchanged or decreases on slightly with altitude, the air tends to be stable.
- If the temperature increases with altitude through a layer -- an inversion -- the layer is stable and convection is suppressed. Air may be unstable beneath the inversion.
- When air near the surface is warm and moist, suspect instability. Surface heating, cooling aloft, converging or upslope winds, or an invading mass of colder air may lead to instability and cumuliform clouds.
- NOAA's National Weather Service, NOAA Profiler Network website
- NOAA's National Weather Service, Aviation Weather Center, Forecast Winds and Temps Aloft Help website.
- NOAA's Earth System Research Laboratory, Global Systems Division (GSD) website
- Aviation Wind and Temperature Aloft Forecasts, National Weather Service Instruction (NWSI) 10-812 (September 14, 2004).
- FAA's Aviation Weather Services : AC 00-45E
More information is available on the map's Forms and Controls, on the map's icons, and on the data sources.