exam
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Temp, wind direction and speed, Precipitation, cloud cover, humidity and barometric pressure | Weather
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Atmosphere conditions, averaged over a specific time period | Climate
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Composition of the Atmosphere(NITROGEN) | 78%(N2)
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Composition of the Atmosphere(OXYGEN) | 21%(O2)
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Composition of the Atmosphere(ARGON) | <1%(Ar)
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Composition of the Atmosphere(CARBON DIOXIDE) | 0.036%(CO2)
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Layer nearest to earth extends up to 10 km temp decreases with altitude all weather is contained within this layer upper boundary is the troposphere | ATMOSPHERIC LAYERS(TROPOSPHERE)
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Temp decreases with increasing altitude Meteorites, burn in this layer meteor shower | ATMOSPHERIC LAYERS(MESOSPHERE)
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Temp increases with increasing altitude Due to the ozone layer Jetstream in the lower part | ATMOSPHERIC LAYERS(STRATOSPHERE)
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Outermost Layer temp increases with increasing altitude Absorbing high level energy from the sun northern lights within this layer | ATMOSPHERIC LAYERS(THERMOSPHERE)
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Average Kinetic energy of the atoms of the atoms of molecules.(RELATED TO THE ABSORPTION OF SOLAR RADIATION) | Temp
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Total kinetic energy dependent on mass | Heat
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Influences the amount of solar radiation received. Rotates every 24 hours | Earth Motions
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Tilt of earth? | 23.5
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Earth is closest to the sun on? | Jan 6
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Earth is furthest from the sun in? | July
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Northern Hemisphere | Sept 22-23
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Winter Solstice | Dec 21-22
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Spring equinox | March 20-21
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Summer solstice | June 21-22
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Requires a solid mass | Conduction
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Requires liquid or gas. Density driven warm buoyant | Convection
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No mass required, cant travel through space | Radiation
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High energy | Short wavelengths
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low energy | Longer wavelengths
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Measured in calories of joules, energy required to change from liquid to gas and solid to gas | Heat energy
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Stored or hidden heat used during a phase change | Latent Heat
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LATENT HEAT OF(VAPORIZATION) | Endothermic
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LATENT HEAT OF(CONDENSATION) | Exothermic
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LATENT HEAT OF(FUSION) | Ice to water
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Amount of water vapor in the air | Humidity
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Max amount of water vapor, depending on air temp | Saturated Air
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Capacity | Is temp dependent
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Can hold more Moisture | Warmer
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Can hold less moisture | Colder
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Pressure is the mass of air under the force of gravity | Vapor Pressure
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Relative Humidity | Given as a percent
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temp at which the specific humidity is equal to saturation quality | Dew point
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Dry bulb | Actual temp
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Wet bulb | lower depending on the amount of evaporation
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Adiabatic temp changers occur when | air is compressed
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Descending air is compressed | R.H decreases
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Air will cool | R.H increases
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Cold Front coming into an area | Frontal wedging
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In areas with Mountains Forceful lifting from below | Orographic lifting
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where air is flowing together and rising | Convergence
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Lifting influenced by land surfaces. | Localized Convective
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How does the air temp change as an air parcel rises | Temp decreases, air parcel cools
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what happens to relative humidity as an air parcel rises | Relative humidity increases
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How does the air temp change as an air parcel descends | Temp increases
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What happens to relative humidity as an air parcel descends | R.H decreases
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High level or wispy or curly, completely made of ice and or crystals | Cirrus
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Blanketing an area. Moderate levels. rain associated. nimbo stratus may be associated with a warm front | Stratus
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Larger, puffy clouds. Fair weather. Evidence of differential heating. | Cumulus
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A cloud with its base at or very near the ground. | Fog
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Surface, over a large area warm moist air comes onto the land. R.H goes up until its 1oo% then fog forms | Advection fog
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Forms on cool clear nights, usually in valleys where the cool air is setting | Radiation fog
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On the windward side of a mountain range | Unslope fog
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during fall, In the evening or early morning air over the water is warmer and has more specific humidity | Steam fog
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Most common process can form rain or snow but starts as ice crystals | Bergeron Process
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Pure water can remain suspended in the air as a liquid down to -40*c. Pure water droplets | Supercoiling
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R.H gets above 100% S.C and S.S= rapid formation of ice crystals | Super saturation
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On a global scale | Convection
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warm air rises at the equator. low pressure center develops near the equator. Doldrums air flow | Hudley cell
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Instrument used to measure air pressure | Barometer
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Result of variations in atmosphere pressure related to differential heating. | wind
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Blows fro areas of higher pressure to areas of lower pressure. similar to water flowing down hill | wind
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Lines on a map connecting points of equal air pressure. | isobars
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Moves from high to low | wind
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sinking and warming due to pressure and adiabatic warming | cool dry air
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downward and out from high pressure center | air flow
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Continental Polar | CP, Midwest cold air from canada
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Mavitime Polar | MP, over the pacific ocean
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Mavitime Tropical | MT, humid and warm
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Continental Tropical | CT, dry air and warm
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over takes warm air(CP->MT) | Cold air
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forces warm air upward | cold air
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(cold fronts)- cumulonimbus clouds higher relative humidity likely to have precipitation lower air pressures | ahead
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(cold Fronts)- clearing skies rising pressure lower relative humilities. | behind
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vertical profile | warm front
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usually results in stratus clouds | warm front
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cold front over takes a warm front | occluded front
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may develop a low pressure center | occluded front
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associated with mid-latitude cyclone | occluded front
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cold air flows in one direction warm air flows in opposite direction can cause flooding | stationary
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violent wind storm, rotating column of air that extends down from a cumulonimbus cloud. | tornadoes
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combined winds with thunderstorm(cold front) and down draft heavy rain or hail. | Microbursts
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caused by the rapid expansion of air around a lightning bolt | thunder
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controls on global climate change | Climate variabilty
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Sunspot cycle little ice age in Europe | solar output
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maunder minimum | solar output
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associated with warming | green house
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saw tooth pattern- precessive, obliquity-tilt, eccentricity | milankovitch cycles
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long term | plate tectonics
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influences the temp range | precipitation
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vertical growth R.H is higher as air mass is forced upward and cooling | cumulonimbus clouds
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occurs between oppositely charged particles within a cloud | Sheet lightning
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Occurring between the cloud and something on the land surface (trees, and high buildings) | forked lightning
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low pressure, wind speed 0-38? | tropical depression
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wind speeds 38-74 mph with lots of rain | tropical storm
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rotating wall of cumulonimbus clouds often with lighting | wall cloud
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center of a very strong hurricane | eye
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arms of clouds with great amount of precipitation | rain bands
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Airflow that is most common with severe weather | Airflow inwards and upwards
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What cloud type is most common with severe weather | cumulonimbus
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Tornadoes is the Midwest are when | Spring and summer
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Southeast Tornadoes occur when | summer to fall
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Two characteristic of hurricanes that cause the most damage | High winds and Flooding
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What does the self-ionization of water cause that is related to severe weather | lighting
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amount of incoming solar radiation | latitude
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Temp decreases with increasing elevation | elevation
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At 12 on Feb 7, the sun is directly overhead at | Some point between the tropic of Capricorn and the equator, heading northward
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The normal change in temp with altitude for a given location is the | environmental lapse rate
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What is the 3 most abundant gases in the atmosphere | Nitrogen, oxygen, argon
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When warm moist air moves over a cold surface as a commonly occurs in san Francisco this type of fog will occur | Advection fog
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If fair weather is approaching the air pressure tendency would probably be | rising
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Airflow near the equator is dominated by these wind patterns | doldrums
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A typhoon is the same as a | hurricane
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What is the range of wind speed for a tropical storm | 38-74 mph
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If an observer sees cirrus clouds, followed later by cirrostratus and then altostratus, he or she is witnessing the approach of an | Warm front
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Location near a large body of water generally have moderated climates due to the high specific heat of water | True
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