Linked from

The 22 pages that link to Wind shear, each with the reason it gives.

• Tropical cycloneRelated: Strong vertical wind shear can tilt and disrupt the cyclone’s organized thunderstorms.

• Wind turbineRelated: Wind shear means blades encounter different wind speeds across their swept area.

• TornadoRelated: Vertical wind shear helps thunderstorms develop organized, persistent rotation.

• ThunderstormRelated: Vertical wind shear can organize storms and keep their updrafts separated from downdrafts.

• Aviation meteorologyRelated: Rapid wind changes near the ground can alter airspeed and flight path during takeoff or landing.

• Dynamic soaringRelated: Strong shear creates the velocity differences exploited during each soaring cycle.

• Lake-effect snowRelated: Changes in wind with height can disrupt or reshape lake-effect snowbands.

• TyphoonRelated: Strong vertical shear can tilt a typhoon and disrupt its organized core.

• Cirrus cloudRelated: Upper-level wind shear stretches and reshapes cirrus into long filaments.

• Atlantic hurricaneRelated: Strong vertical wind shear can disrupt the organized circulation Atlantic hurricanes need.

• SupercellRelated: Vertical wind shear helps create the storm rotation that a supercell organizes.

• VirgaRelated: Downdrafts associated with virga can create dangerous wind shear for aircraft.

• Atmospheric instabilityRelated: Wind shear organizes storms but is distinct from the buoyant instability that feeds them.

• Cumulonimbus cloudRelated: Vertical wind shear can organize a storm and prolong its severe-weather potential.

• Tropical cyclogenesisCompared with: Strong vertical shear tilts and disrupts the convection that cyclogenesis needs.

• DownburstRelated: Downburst outflow creates abrupt wind shifts and shear near the ground.

• GustnadoRelated: Sharp wind changes near the gust front can contribute to horizontal rotation that becomes a whirlwind.

• Funnel cloudRelated: Wind shear can create horizontal rotation that a thunderstorm updraft tilts and strengthens.

• Altostratus undulatusRelated: Differences in airflow through the cloud layer can organize its undulations.

• Fractus cloudRelated: Shearing winds can distort cloud edges into ragged fragments.

• Prevailing windsRelated: A regional prevailing direction provides context for local directional changes.

• Vertical draftCompared with: Shear describes variation in airflow rather than vertical displacement itself.