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Vocabulary practice flashcards covering atmospheric pressure, upper-air forces, geostrophic winds, scales of motion, meteorological instruments, jet streams, ENSO cycles, and air mass classifications.
Atmospheric Pressure
The mass of air above a given level, which always decreases with increasing elevation and is interrelated with air density and temperature.
Vertical Atmospheric Coupling
The dynamic principle analogous to "wag the dog," wherein atmospheric conditions at high altitudes are intrinsically linked to and influence conditions down to the Earth's surface.
Constant Pressure Charts
Upper-level meteorological maps (also called confidence peak charts) that illustrate atmospheric conditions across distinct vertical boundaries using seven standard pressure levels updated twice daily.
Ridge
An elongated area of high atmospheric pressure, which is meteorologically synonymous with an anticyclone.
Trough
An elongated area of low atmospheric pressure.
Wind Direction Reporting Rule
The standard meteorological convention requiring wind direction to be recorded and reported by the direction from which the air originates, rather than where it is blowing.
Pressure Gradient Force (PGF)
The fundamental driving force behind wind velocity and acceleration, generated by differences in horizontal atmospheric pressure.
Geostrophic Wind
An upper-level, "earth-turning" wind resulting from a balance between the pressure gradient force and the Coriolis force.
Zonal Flow
An atmospheric flow regime characterized by straight, parallel isobars aligned west-to-east, resulting in calm, tranquil, and stable weather.
Meridional Flow
An atmospheric flow regime characterized by sharp bends, sinusoidal curves, and waves in isobars, instigating agitated atmospheric states and severe storm formation.
Surface Friction
Terrestrial boundary drag that slows ground-level wind speeds, thereby reducing the Coriolis force and preventing true geostrophic balance near the surface.
Cyclonic Action (Low-Pressure Center)
A pressure system acting as "nature's vacuum cleaner," characterized by surface convergence, vertical ascent promoting cloud formation, and upper-level divergence.
Anticyclonic Action (High-Pressure Center)
A pressure system characterized by surface divergence, subsiding dry air that suppresses cloud formation, and upper-level convergence.
Sea-Level Pressure Standardization
The mathematical normalization of raw barometric pressure observations from varying station elevations to standard sea-level pressure to allow valid synoptic comparisons.
Planetary Scale
The largest scale of atmospheric motion, spanning 10,000km (≈6213.71mi) and larger, lasting a week or more, including longwaves in the westerlies.
Synoptic Scale
Atmospheric motion spanning 500–2000km (≈1242.74mi) and lasting days to weeks, including hurricanes and high- and low-pressure systems.
Mesoscale
Atmospheric phenomena ranging from a few kilometers to 500km (≈310.69mi) and lasting hours to a few days, including fronts and severe thunderstorms.
Microscale
Atmospheric motions spanning less than 1km and lasting a few minutes to an hour, including tornadoes and turbulent eddies.
Planetary Boundary Layer (PBL)
The lowest 1000m (3000ft) of the atmosphere, also known as the friction or atmospheric boundary layer, where surface friction significantly influences airflow.
Viscosity
The internal friction of fluid flow.
Eddies
Irregular, random turbulent whirls forming in viscous flow that produce rapid changes in wind speed and direction, wind gusts, and internal friction.
Wind Shear
An abrupt change in wind speed or wind direction over a short distance.
Clear Air Turbulence (CAT)
Strong wind shear that occurs without any visible cloud formations or dust.
Prevailing Wind
The wind direction most frequently observed during a given period of time.
Wind Vane
A weather instrument that rotates freely on a post until its arrow points directly into the wind, measuring direction only.
Anemometer
An instrument equipped with cups mounted on a vertical pole that spin faster with increasing wind velocity, measuring wind speed only.
Aerovane
An instrument (also called a sky vane) with a fin that aligns into the wind to indicate direction and a propeller that spins to measure speed.
Wind Profiler
A vertically pointing radar that emits pulses of microwave radiation to detect backscattered energy from moisture and temperature irregularities, plotting how wind changes with height.
Radiosonde
An instrument package carried aloft by a weather balloon to measure temperature, humidity, pressure, and wind.
Conduction
Thermal energy transfer occurring at the ground surface level through direct molecular contact, warming the immediate overlying air layer.
Convection
The vertical transport of thermal energy driven by the rising of warm air parcels, often forming localized whirlwinds or vortexes.
Intertropical Convergence Zone (ITCZ)
The equatorial latitudinal zone where trade winds converge and rising motion produces active tropical weather.
Polar Jet Stream
An upper-level jet stream located in northern latitudes that drags cold, dry air southward.
Subtropical Jet Stream
An upper-level jet stream that meanders through southern latitudes, transporting warm, moist air northward.
Low-Level Jet (LLJ)
A high-velocity wind feature positioned near the Earth's surface rather than the upper troposphere, strongly influencing weather patterns across the Midwest and Central Plains.
El Niño
A warm ocean current in the South Pacific characterized by low pressure over the Eastern Pacific, high pressure over the Western Pacific, altered trade winds, increased Atlantic wind shear, and suppressed Atlantic hurricanes.
La Niña
The inverse phase of El Niño characterized by high pressure and cold upwelling over the Eastern Pacific, low pressure over the Western Pacific, an active polar jet, and cold, wet, snowy winters across regions like Missouri.
Air Mass
An extensive body of air whose physical properties of temperature and moisture are homogeneous horizontally across thousands of miles at any given altitude.
Air Mass Source Region
A flat, uniform, and vast geographic region dominated by light winds and persistent high pressure, allowing an overlying air mass to acquire its characteristic temperature and moisture.
Maritime Arctic (mA) Air Mass
A theoretical air mass that does not exist in nature because frigid arctic air lacks the thermodynamic moisture capacity required to maintain high moisture content.