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Air Mass
A large body of air with generally uniform temperature and humidity.
Continental Air Masses
Air masses that originate over land and are dry.
Maritime Air Masses
Air masses that originate over oceans and are moist.
Arctic Air Masses
Air masses that originate from the arctic or antarctic and are very cold.
Polar Air Masses
Air masses that originate over high latitudes of both land and sea and are not as cold as arctic air masses.
Tropical Air Masses
Air masses that originate over the lower latitudes of both land and sea and are warm and hot.
Front
The boundary between two air masses that meet but do not mix.
Warm Front
Occurs when a warm air mass approaches a cold air mass and gradually climbs up and over it, resulting in cloudy weather with gentle steady rain.
Cold Front
Occurs when a cold air mass approaches a warm air mass, shoving the warm air up and out of the way, resulting in thunderstorms or heavy rain.
Stationary Front
Occurs when both a warm and cold air mass approach each other and stop moving, resulting in rain along the entire front.
Occluded Front
Occurs when a cold front advances and overtakes a warm front, resulting in strong wind, heavy rain, and tornadoes.
Isolines
Lines drawn on a map connecting data points of the same value.
Isotherms
Lines connecting points of equal temperature.
Isobars
Lines connecting points of equal air pressure.
Wind speeds
Wind speeds are faster when the isobars are closer.
Air Pressure
Air moves from areas of high pressure to low pressure.
High Pressure Systems
Wind moves clockwise and out due to the Coriolis effect/forces, cooler air temp, rising pressure, clear, nice weather.
Low Pressure Systems
Wind moves counterclockwise and in due to the Coriolis effect/force, warmer air temp, falling pressure, poor, humid weather.
Coriolis Effect
As the Earth spins, it causes the wind and waters to deflect; Northern hemisphere - deflects right, Southern hemisphere - deflects left.
Hurricanes
Location - over water; Duration - Days to weeks; Damage - Heavy rain, flooding, wind; Pressure - Low pressure; Peak season - June-November; Warning times - days to weeks in advance; Wind Speed - 74-157+ mph; Most affected areas - coastal states; Category system - Saffir Simpson; Call Typhoons in India and w. Pacific oceans; Hurricanes are named.
Tornadoes
Location - over land (most form when cool and warm air collide); Duration - Minutes, up to an hour; Damage - Strong winds, thunderstorms, hail; Pressure - Low pressure; Peak season - March - July; Warning times - Little to no warning; Wind Speed - up to 300 mph+; Most affected areas - Midwest/interior states; Category system - Enhanced Fujita Scale; Tornadoes are not named.
Relative Humidity
Relative Humidity - the amount of water vapor in the atmosphere compared to the amount of water vapor the air could hold.
Saturated Air
When the air is holding as much moisture as it can, it's said to be saturated. Condensation will occur at 100% relative humidity.
Units of Relative Humidity
Units - Percentage.
Dewpoint
Dewpoint - the temperature at which relative humidity is 100%. Condensation must occur.
Examples of Dewpoint
Examples - Morning Dew, Frost, Clouds - water vapor on cloud condensation nuclei.
Temperature and Dewpoint Relationship
The closer the temperature and dewpoint, the higher the relative humidity.
Units of Dewpoint
Units - Celsius (C) and Fahrenheit (F).
Finding Relative Humidity and Dewpoint
Measured using a Sling Psychrometer.
Dry Bulb Temperature
Dry Bulb Temperature = air temperature.
Wet Bulb Temperature
Wet Bulb Temperature = how much evaporation occurred.
Wet Bulb Depression
Wet Bulb Depression = the difference between dry and wet bulb temperatures.
Use of Wet Bulb Temperature
Dry Bulb temperature and Wet Bulb Depressions are used to determine relative humidity and dew point - chart.
Station Models
A station model is a representation of all the different parts of weather over a location.
Barometric Pressure
Barometric pressure is expressed in 'shorthand' millibars.
Air Pressure
This location's air pressure is currently 1019.6mb.
Wind Direction
Where the wind comes from, expressed by the direction the staff is pointing.
Wind Speed
How fast the wind is blowing, expressed in knots.
Wind Speed Measurement
Each full feather is 10 knots, each half feather is 5 knots, and each triangle is 50 knots.
Current Wind Speed
This location's wind speed is 15 knots.
Cloud Formation
Clouds form when evaporated water rises in the atmosphere, cools, attaches to small particles, condenses to form tiny water drops, which combine to form cloud droplets and ultimately clouds.
Cirrus Clouds
Wispy clouds that form at higher elevations, made mostly of ice crystals.
Stratus Clouds
Flat layered clouds that may obscure the sky, occurring at mid-low altitudes.
Cumulus Clouds
Fluffy and puffy clouds usually seen on sunny days, occurring at mid to low altitudes.
Weather Maps
Describe weather conditions at particular locations, providing information about pressure systems, fronts, air mass movement, temperature, etc.
Wind Direction on Weather Map
From what direction would the wind be blowing if you were standing on the pink dot?
Air Pressure on Weather Map
What would be the possible air pressure on the green dot?
Temperature Comparison
If the temperature at B is 79 degrees, would the temperature at A be warmer or colder?
Front Movement
Which direction is front 'X' moving?
Fastest Wind Speed
At which dot is the wind speed the fastest?
Stormy Weather Area
Which area would contain stormy weather?
Weather Map Functionality
How does this map show the weather at each particular location?
Leeward Side
Typically, as a system moves towards and over a mountain, the cloud and weather will dissipate, causing the leeward side to be considered dry.
Cup Anemometer
This instrument measures wind speed.
Barometer
Measures air pressure.
Weather Vane
Tells us wind direction and points in the direction where the wind is blowing.
Psychrometer
Allows us to find relative humidity and dew point.
Radiosonde
Collects weather data from areas in the troposphere.
Hydrologic Cycle
Describes how water moves through Earth systems.
Evaporation
Liquid water is heated into a gas and rises in the atmosphere.
Transpiration
Plants take up water from the soil and release it as gas from their leaves.
Condensation
Water vapor is cooled down (to the dew point) and becomes a liquid again.
Precipitation
Liquid water falls down from the sky as rain, snow, etc.
Surface Runoff
Liquid water on the surface travels downhill toward lower elevations.
Infiltration
Liquid water being absorbed into the ground.