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where does most weather occur? |
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the layer of the atmosphere 1.5 miles thick |
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basic properties of the atmosphere |
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temperature, pressure, moisture content, wind speed and direction, significant weather (precipitation, visibility) |
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measure of the average speed that the molecules move in a substance -faster the speed of molecules, higher the temperature |
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-Temp decreases with height up to about 7 miles (Troposphere) -Above 7m temperature increases with height (Stratosphere) |
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-Boundary between Troposphere and Stratosphere -Keeps air currents out of stratosphere -Tropopause is higher up over equator and lower near the poles |
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Subtropical and Polar Jetstreams |
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circle the globe at 25 degrees and 50 degrees |
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-Above stratosphere -Temp decreases with height |
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-Above Mesosphere -Temp increases with height |
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force applied by air on earth's surface |
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-Weight of column of air above the surface area on earth at sea level |
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-Decreases with height -Measured in millibars (mb) 1000dynes/centimeter^2 -measured with barometer |
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invisible gas composed of individual water molecules |
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-force per unit area applied by only water vapor molecules -measure of the absolute amount of moisture in the air |
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-When the atmosphere cannot contain any more water vapor without condensing into cloud droplets |
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Saturation Vapor Pressure |
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the vapor pressure at which the atmosphere becomes saturated -depends on temperature |
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-the amount of water vapor in the atmosphere relative to the atmosphere's capacity for moisture -Determined by temp Relative humidity = (vapor pressure/saturation vapor pressure) x 100 |
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Temp and Relative humidity |
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As temp goes down, relative humidity goes up |
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Sat vapor pressure and temp |
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Remember, the saturation vapor pressure always increases as the air temperature increases |
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relative humidity and temp |
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-The relative humidity is high when the difference between the temperature and dewpoint temperature is small. -The relative humidity is low when the difference between the temperature and the dewpoint temperature is large |
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The energy associated with the phase changes of water |
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Heat transfer (heating vs cooling) |
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-Latent heat is released from the water to the atmosphere as water goes from a gas to a solid (top to bottom of this figure). -This causes the atmosphere to warm. -Latent heat is absorbed by the water and removed from the atmosphere as water goes from a solid to a gas (bottom to top of this figure). -This causes the atmosphere to cool |
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Universal Time Coordinate |
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-UTC is based on a 24 hour clock -UTC never switches from standard time to daylight savings time |
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converting UTC to mountain time |
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MST = UTC - 7 hours MDT = UTC - 6 hours |
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Pressure Temperature Dewpoint Temperature Wind direction and speed Precipitation amount Precipitation type Present weather condition Visibility Cloud cover Cloud types Cloud ceiling (height) |
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a balloon-borne instrumentation system that measures pressure, temperature, dewpoint temperature, wind direction, and wind speed |
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A depiction of the vertical structure of the atmosphere |
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what determines how much microwave energy is returned to the radar? |
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Size of precipitation particles Number of precipitation particles Type of precipitation particles (rain, snow, hail, etc.) |
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Decibel Radar Reflectivity dBZ |
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logarithmic scale used when plotting radar reflectivity data to indicate the intensity of the microwave energy returned to the radar from targets (raindrops, hail, snow, etc) |
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Position of precipitation Intensity of precipitation |
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indicates the position and intensity of precipitation (like a regular radar) but can also estimate the radial wind speed from the Doppler shift of the transmitted and received signal. |
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•Temperature (deg F) •Dewpoint Temperature(deg F) •Coded SLP •Wind speed and direction •Cloud cover •Significant Weather |
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Decoding sea level pressure |
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-If coded SLP is greater than 500: Put a 9 in front of the 3 digit coded SLP -If coded SLP is less than 500: Put a 10 in front of the 3 digit coded SLP |
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change in pressure over a given distance |
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change in temperature over a given distance |
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contour lines of constant dewpoint temperature |
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an imaginary surface above the ground where the pressure has a constant value |
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area of low heights on a constant pressure map |
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area of high heights on a constant pressure map |
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-a measure of the local rotation (spin) in a flow -Positive vorticity indicates counterclockwise spin. Negative vorticity indicates clockwise spin. |
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contour line of constant wind speed |
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band of strong winds that circle the earth at mid-latitudes |
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region of exceptionally strong winds embedded in the jetstream |
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How do weather forecasters make forecasts? |
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-Observations of the atmosphere -Use computer model forecasts -Knowledge of local weather and experience |
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Numerical Weather Prediction NWP |
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the science of predicting the future weather with computer models |
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a set of mathematical equations, coded into a computer program, that describe the behavior of the atmosphere |
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Regional models - cover a limited portion of the atmosphere Global models - cover the entire atmosphere |
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an NWP model is run repeatedly with slight changes to the initial conditions or model formulation |
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the average forecast of all the ensemble members |
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the lowest temperature to which air can be cooled at constant pressure before saturation occurs |
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lines of constant pressure on a map |
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-exists where the pressure changes over distance. -Strong pressure gradient = fast winds |
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lines of constant temperature |
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Lines of constant dew point temperature |
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a surface above the ground where the pressure has a specific value |
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difference between the temperature and the dewpoint temperature -smaller value = more saturated |
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-useful for identifying fronts (boundaries between large airmasses) -Winds flow parallel to height contours |
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moisture distribution is prevalent on this map |
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-used to determine the location of short waves and long waves associated with the ridges and troughs in the air-flow pattern |
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-located near top of troposphere -jetstreams are prevalent |
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