Chapter 4 Moisture and Atmospheric Stability This chapter covers: Water Water states of matter...
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Transcript of Chapter 4 Moisture and Atmospheric Stability This chapter covers: Water Water states of matter...
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Chapter 4Chapter 4Moisture and Atmospheric Moisture and Atmospheric
StabilityStabilityThis chapter covers:This chapter covers: WaterWater
states of matterstates of matter heat capacity and latent heatheat capacity and latent heat
Humidity and dew pointHumidity and dew point Adiabatic temperature changes in Adiabatic temperature changes in
the atmospherethe atmosphere Atmospheric stabilityAtmospheric stability
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The Hydrologic CycleThe Hydrologic Cycle
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States of Matter: Solid, Liquid and VaporStates of Matter: Solid, Liquid and Vapor
Water’s Changes of State
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Gas (Vapor)Gas (Vapor)
widely spaced moleculeswidely spaced molecules no bonding between moleculesno bonding between molecules molecules move at high speedsmolecules move at high speeds very compressiblevery compressible
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LiquidLiquid Closely spaced moleculesClosely spaced molecules Moderate bonding between Moderate bonding between
moleculesmolecules molecules move at medium molecules move at medium
speedsspeeds Slightly compressibleSlightly compressible
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Solid (i.e., ice)Solid (i.e., ice)
closely spaced moleculesclosely spaced molecules Strong, rigid bonding between Strong, rigid bonding between
moleculesmolecules No molecule movement – only No molecule movement – only
vibrationsvibrations Fairly incompressibleFairly incompressible
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Solid Water: Ice
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Liquid Water
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Water Vapor
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Heat Capacity and Latent Heat of Water
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SaturationSaturation
Condition in which the air is holding Condition in which the air is holding the maximum amount of water the maximum amount of water vapor possiblevapor possible
Amount of water vapor present at Amount of water vapor present at saturation depends onsaturation depends on Temperature; more vapor at higher Temperature; more vapor at higher
temp. Very strong effecttemp. Very strong effect Pressure; more vapor at higher Pressure; more vapor at higher
pressure.pressure.
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Absolute HumidityAbsolute Humidity
Amount of water vapor present in Amount of water vapor present in airair
Given as grams water vapor per Given as grams water vapor per cubic meter of aircubic meter of air
Value is affected by air pressureValue is affected by air pressure
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Mixing RatioMixing Ratio
Amount of water vapor present Amount of water vapor present in air, but more useful than in air, but more useful than absolute humidityabsolute humidity
Given as grams water vapor per Given as grams water vapor per kilogram of airkilogram of airTypically ranges from 0 to 4%Typically ranges from 0 to 4%
Value is Value is notnot affected by air affected by air pressurepressure
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SaturationSaturation
Air is limited in how much water Air is limited in how much water vapor it can hold without water vapor it can hold without water droplets formingdroplets forming
SaturationSaturation is the point at which air is the point at which air can’t hold more water vaporcan’t hold more water vapor
Mixing ratio at saturation depends on Mixing ratio at saturation depends on temperature, and somewhat on temperature, and somewhat on pressurepressure
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Contrail: engine exhaust contains water vapor, exhaust cools, becomes saturated
with water vapor and condensation occurs
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Contrail: engine exhaust contains water vapor, exhaust cools, becomes saturated
with water vapor and condensation occurs
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Saturation Mixing-Ratio:Saturation Mixing-Ratio:How much water vapor can be present in air How much water vapor can be present in air
at different temperaturesat different temperatures
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Relative HumidityRelative Humiditythe humidity we feelthe humidity we feel
Amount of water vapor in air relative to maximum possible
amount (saturation mixing ratio)
Example
Temperature: 20oC
Saturation mixing ratio=14g vapor per 1 kg air
Actual vapor content = 7 g per 1 kg air
Relative humidity = 7 g / 14 g x 100% = 50%
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Dew PointDew Point Temperature to which air must Temperature to which air must
be cooled to become saturatedbe cooled to become saturated Assumes no change in mixing ratioAssumes no change in mixing ratio Relative humidity is 100% in air Relative humidity is 100% in air
that’s at its dew pointthat’s at its dew point Stating air’s dew point is Stating air’s dew point is
essentially the same as stating its essentially the same as stating its mixing ratiomixing ratio
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Air’s saturation mixing ratio and relative humidity change with temperature
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Which has larger mixing ratio?
Which has higher relative humidity?
Antarctica
Death Valley
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Hotter:Higher mixing ratio,Lower relative humidity
Colder:Lower mixing ratio Higher relative humidity
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Relative Humidity, Mixing Ratio Relative Humidity, Mixing Ratio and Air Temperatureand Air Temperature
Hotter air can hold much more Hotter air can hold much more
water vapor than cold airwater vapor than cold air
Hotter air can have more vapor in it Hotter air can have more vapor in it
than cold air, yet have lower than cold air, yet have lower
relative humidityrelative humidity
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Relative Humidity Changes with Relative Humidity Changes with Temperature DailyTemperature Daily
Rel
ativ
e H
um
idit
y
Tem
per
atu
re
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Air Temp, Dew Pt. & Relative Air Temp, Dew Pt. & Relative Humidity in HeberHumidity in Heber
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Dew Point Temperatures
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Adiabatic Temperature ChangesAdiabatic Temperature Changes
• Air cools when it expands, warms Air cools when it expands, warms when its compressedwhen its compressed
• Rising air expands and coolsRising air expands and cools
• Sinking air is compressed and warmsSinking air is compressed and warms
• Adiabatic refers to temperature Adiabatic refers to temperature changes w/o heat transferchanges w/o heat transfer
Very important!
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Adiabatic Temperature ChangesAdiabatic Temperature Changes
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Dry & Wet Adiabatic RatesDry & Wet Adiabatic Rates• Saturated air cools less as it rises
because condensation of water releases heat
• Dry adiabatic rate = 10Dry adiabatic rate = 10ooC / C / 1000m = 5.51000m = 5.5ooF / 1000 feetF / 1000 feet
• Wet adiabatic rate = 5 to Wet adiabatic rate = 5 to 99ooC / 1000m C / 1000m (2.75 to 5(2.75 to 5ooF/1000ft)F/1000ft)
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Dry & Wet Adiabatic RatesDry & Wet Adiabatic Rates
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Lifting Condensation LevelLifting Condensation Level As air rises, it expands and coolsAs air rises, it expands and cools Level (altitude) at which it is cooled Level (altitude) at which it is cooled
to its dew point is theto its dew point is the lifting lifting condensation levelcondensation level
– Clouds form Clouds form above this level above this level if air is risingif air is rising
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Causes of LiftingCauses of Lifting Orographic – wind blows over Orographic – wind blows over
mountainsmountains Frontal wedging – warm air forced Frontal wedging – warm air forced
over colder airover colder air Convergence – winds blowing Convergence – winds blowing
togethertogether Convection – solar heating creates Convection – solar heating creates
hot air that riseshot air that rises
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Orographic LiftingOrographic Lifting
Important along Wasatch Front, much of Western U.S.
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Frontal WedgingFrontal Wedging“Storm Fronts”
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ConvergenceConvergence
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ConvectionConvection
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Cause of Rain Shadow DesertCause of Rain Shadow Desert
Rising air cools at
wet adiabatic
rate
sinking air warms at
dry adiabatic rate
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Atmospheric StabilityAtmospheric Stability
Stable Air = Air that tends to not Stable Air = Air that tends to not riserise
Unstable Air = Air that tends to Unstable Air = Air that tends to keep rising keep rising (regardless of orographics, (regardless of orographics, fronts, etc.)fronts, etc.)
Importance – rising air cools, Importance – rising air cools, makes clouds, precipitation, even makes clouds, precipitation, even tornadostornados
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What Controls StabilityWhat Controls Stability
Depends on adiabatic cooling Depends on adiabatic cooling
rate (dry and wet) vs. rate (dry and wet) vs.
Environmental Lapse RateEnvironmental Lapse Rate
Environmental Lapse Rate = the Environmental Lapse Rate = the
actual, existing decrease in air actual, existing decrease in air
temperature with altitudetemperature with altitude
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Atmospheric Stability, Atmospheric Stability, cont.cont.
Three types of stability:Three types of stability:Absolute stabilityAbsolute stability
Absolute instabilityAbsolute instabilityConditional instabilityConditional instability
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Absolute StabilityAbsolute Stability
Environmental Lapse rate is Environmental Lapse rate is less than wet adiabatic rateless than wet adiabatic rate As air rises, it cools so much (even if As air rises, it cools so much (even if
its saturated) that it becomes cooler its saturated) that it becomes cooler than surrounding air so it stops than surrounding air so it stops risingrising
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Absolute stabilityAbsolute stability
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Absolute instabilityAbsolute instability Environmental lapse rate is Environmental lapse rate is
greater than dry adiabatic greater than dry adiabatic raterate As air rises, despite cooling at As air rises, despite cooling at
dry adiabatic rate, it becomes dry adiabatic rate, it becomes progressively warmer than progressively warmer than surrounding air and rises surrounding air and rises fasterfaster
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Absolute InstabilityAbsolute Instability
Absolute instabilityAbsolute instability
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Conditional InstabilityConditional Instability
Environmental Lapse rate is Environmental Lapse rate is greater than wet adiabatic rate, greater than wet adiabatic rate, less than dry adiabatic rateless than dry adiabatic rate As air rises, if it is unsaturated it As air rises, if it is unsaturated it
tends to not rise, but once its tends to not rise, but once its saturated it keeps risingsaturated it keeps rising
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Conditional StabilityConditional Stability
Conditional InstabilityConditional Instability
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NWS Storm Prediction NWS Storm Prediction CenterCenter
Focuses on dangerous thunderstormsFocuses on dangerous thunderstorms Produces estimates of convective stability Produces estimates of convective stability
for locations across the country twice dailyfor locations across the country twice daily Main website: Main website: http://www.spc.noaa.govhttp://www.spc.noaa.gov Soundings (weather balloon data which Soundings (weather balloon data which
provide information on environmental lapse provide information on environmental lapse rate and more) with stability analysis rate and more) with stability analysis (somewhat advanced scientifically): (somewhat advanced scientifically): http://http://www.spc.noaa.gov/exper/soundingswww.spc.noaa.gov/exper/soundings//
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Chapter 4Chapter 4
ENDEND