Jet Streams
Fast-moving rivers of air high in the atmosphere that steer weather systems.
Around Richmond: Richmond's winter storms often follow jet stream dips from Canada. When the jet stream moves south, cold air floods into Virginia, bringing potential snowstorms and ice events.
Isobars
Lines on a weather map connecting points of equal atmospheric pressure.
Around Richmond: Closely-spaced isobars = strong winds. When isobars bunch up over Richmond, you'll see gusty conditions. Wide spacing = gentle winds.
Cold Fronts
Boundary where cold air rapidly pushes into warmer air masses.
Around Richmond: A cold front moving through Richmond typically brings sudden temperature drops (10-20°F in hours), wind shifts from south to north, and thunderstorms. We track these closely for RVA.
Warm Fronts
Boundary where warm air gradually replaces cold air.
Around Richmond: Warm fronts approach Richmond more gradually, bringing steady rain or drizzle before warmer air arrives. Great for ending winter cold snaps.
Dew Point
Temperature at which air becomes saturated and moisture condenses.
Around Richmond: High dew points in Richmond summers (65°F+) = muggy, uncomfortable conditions. Low dew points (30°F-) = dry, crisp air you can feel.
Temperature Inversion
Warm air layer above cooler air, trapping weather and pollutants.
Around Richmond: Richmond experiences inversions in fall and winter, trapping cold air in the James River valley. This can create dense fog or keep pollution low to the ground.
Convection
Rising motion of warm air that creates clouds and thunderstorms.
Around Richmond: Afternoon thunderstorms in Richmond summers develop through convection—hot ground heats the air above it, causing it to rise and form storms.
Lake Effect (Virginia's Mountains)
Cold air moving over warm water creates heavy precipitation.
Around Richmond: When cold air moves across the Atlantic in winter, it can enhance moisture for Richmond. Mountain gaps channel this moisture, affecting our forecasts.