The Global Ensemble Forecast System (GEFS) is a probabilistic weather prediction system managed by NOAA.
It utilizes multiple ensemble members to generate a range of possible outcomes, enhancing the ability to
assess weather uncertainties and probabilities. The ensemble approach helps to capture the range of possible
weather scenarios by running slightly different initial conditions or model configurations, which are
referred to as ensemble members or components.
The GEFS Atmos Ensemble Mean is a statistical aggregation of all atmospheric ensemble members, providing a single, representative forecast from the GEFS system. This mean forecast smooths out the variability inherent in individual ensemble members, offering a balanced
and reliable view of expected atmospheric conditions such as temperature, wind, and precipitation. The ensemble mean is commonly used as a baseline in risk management, operational planning, and research, giving users a robust and stable prediction while still
acknowledging underlying forecast uncertainties.
Aggregates the outcomes of multiple ensemble members to produce a mean forecast, smoothing out extreme variations and providing a more stable prediction.
Facilitates improved decision-making in weather-sensitive sectors by offering a balanced view of expected atmospheric conditions.
Incorporates extensive meteorological data from global measurement networks and satellites.
Resolution: 0.25° global grid.
Temporal Coverage: Updated four times daily, with forecasts extending up to 10 days.
Primary Use Cases: General weather forecasting, agricultural planning, emergency management, and public safety.
Parameters
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Convective Available Potential Energy (CAPE) quantifies buoyant energy available to rising air parcels. Larger values generally imply stronger potential updrafts and greater convective intensity.
Units: J/kg.
Often used with CIN and lifting mechanisms to assess thunderstorm potential.
Convective Inhibition (CIN) measures the energy barrier that must be overcome to initiate convection. More negative values indicate a stronger cap that can suppress storms.
Units: J/kg.
When CIN is weak and CAPE is high, convection is more likely.
Geopotential height is the altitude of a pressure surface in the atmosphere. It is the primary field for identifying ridges, troughs, and large‑scale flow patterns.
Storm-relative helicity measures the potential for streamwise vorticity to be ingested by a storm updraft. Higher values suggest a greater likelihood of rotating updrafts.
Units: m^2/s^2.
Commonly evaluated in the lowest 1 to 3 km layer.
Level
Info
Horizon
Introduced
Selector
3000-0 m above ground
ens mean
0h-240h
2020-10-01
{"name":"HLCY","level":"3000-0 m above ground","info":"ens mean"}