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1.WEATHER
  Weather is… THE SHORT TERM CONDITION OF  THE ATMOSPHERE
Weather is the result of the interrelationship between the following 4 ATMOSPHERIC VARIABLES:TEMPERATUREHUMIDITY
AIR PRESSURE
WIND 1.Air Temperature:measures how much kinetic energy the air molecules have 2. Air Pressure: caused by the weight of atmosphere pushing down3. Wind:Horizontal     Movementof aircaused by differencesin pressure
4. Humidity:Moisture content of the atmosphere
In what layer of our atmosphere does our weather occur?Troposphere
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What is our atmosphere made of?
Argon0.93 %Carbon Dioxide0.03 %Water vapor0.0 to 4.0 %0.01 %   	Neon	Helium	Methane	Krypton	Hydrogen	Ozone	XenonOxygen21%Nitrogen78%Other1%
See Front Cover of your ESRT!!!
 1.Air Temperature:measures how much kinetic energy the air molecules have
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Each time a moleculehits the thermometer bulbenergy is transferred and the temperature rises
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Air moleculeCOLDHOT
WHICH SAMPLE HAS MOREKINETIC ENERGY?MotionCOLDHOT
WHICH SAMPLE HAS MOREKINETIC ENERGY?MotionHOTCOLDEnergy           transferred
COLDHOT
COLDHOT
COLDHOT
HOTCOLD
HOTCOLD
HOTCOLD
HOTCOLDHot air risesbecause of  increased kinetic energy
Three scales are use to measure temperature:1. Fahrenheit
2. Celsius
3. KelvinWE WILL USE THIS  THERMOMETER TO  CONVERT FROM  CELSIUS TO   FARENHEIT TO  KELVINSEE REFERENCETABLE PAGE 13
Each notchIs worth2 degreesEach notchis worth1 degree9519085355170Each notch  is worth  1 degree345150335
ALL YOU NEED TO DOIS READ ACROSS ANDUSE A STRAIGHT EDGE ICE BOILINGWATER1. FARENHEIT                  2. CELSIUS                  3. KELVIN32212 0100273373
15870 CELSIUS =         FARENHEIT			=          KELVIN343
82   180 FARENHEIT =      CELSIUS    				   =       KELVIN355
	ABSOLUTE ZERO (ZERO DEGREESKELVIN)Lowest possible temperatureNO KINETIC ENERGY       THE MOLECULES ARE NOT MOVING
Quick Energy Review!
REVIEW QUESTONS:WHICH SKIIER HAS THE GREATEST  KINETIC ENERGY?ABDC
WHICH SKIIER HAS THE GREATESTPOTENTIAL ENERGY?ABDC
DURING ENERGY CHANGES, IF ONE BODYIS LOSING ENERGY, THE OTHER IS _______ ENERGY:GainingTHE WAVE LOSESENERGY:THE SAND  GAINS   ENERGY
DURING ENERGY CHANGES, IF ONE BODYIS LOSING ENERGY THE OTHER IS GAINING ENERGY:THE WAVE LOSESENERGY:THE SAND  GAINS   ENERGY
DURING ENERGY CHANGESTHE TOTAL ENERGY REMAINS THE SAMEENERGY ALWAYS FLOWS FROM HIGH TO LOW (source to sink)
THE ENERGY WILL FLOW FROM:THE FLAME TO THEFINGER
ENERGY WILL FLOW FROMICETHE FINGER TO THE ICE
THE LIQUIDLOSES ENERGY AS THEICE GAINS ENERGY
WHEN WILL THE EXCHANGEOF ENERGY STOP?WHENEQUILIBRIUMIS REACHED THE LIQUID ANDTHE ICE REACH THE SAMETEMPERATURE
The Affects of Air Temperature
Imagine two open containers of air:One is filled with hot airand the other is filled with cold airHOTCOLD
Which container has more kinetic energy?HOTCOLD
Which container has higher air pressure?HOTCOLD
Which container has greater density?HOTCOLD
Air moleculeWater moleculeWhich container can hold more water?COLDHOT
Air moleculeWater moleculeHOTCOLD
In summary:Hot air has more kinetic energy
hot air has less pressure
hot air can hold more water
hot air is less dense
hot air rises 2. Air Pressure: caused by the weight of atmosphere pushing downAs altitudeincreasesPressuredecreases
IndirectPressureAltitude
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IndirectPressureTemperature
A barometermeasurespressure in inches of mercury or millibars see reference table page 13
Standard  pressure is1013.2 millibars or29.92 inches of mercury
Each notch is worth 1.0Each notch is worth 0.011039.030.651038.01037.0
Convert 1040.0 millibarsto inches of mercury
30.71
Atmospheric Pressure:Effected by   water vapor
Water vapor is very _________ compared to              dry air:light(Nitrogen is heavier   than hydrogen and oxygen)
SO:When water vapor is added to dry air the air pressure___________decreases
Because the air is lighterDecreases in air that is full of water vapor Pressure
IndirectpressureHumidity
SummaryHOT:COLD:less dense , lighter
less pressure
holds more water
Heavier
more dense
more pressureWhat will happen?If you add water vapor to the inside of a container and seal it, what will happen?SIT BACK AND WATCH!
equilibriumThe Earth is always trying to achieve_______________
highEnergy is constantly being re-distributedflowing from _______to _______low
How can we decreasepressure without changing our elevation?Increase temperatureIncrease humidity
Warmer and WetLow pressure High pressureCooler and Dry
Latitude…. Earth Poles lowTemp:pressure:density: humidity:highhighlowEQUATORhightemp:pressure:density:humidity:lowlowhigh
WIND:
Come fromWinds are described by the direction they ___________
Winds distribute energyhighThey blow from _______ pressure  to______pressurelow
ISOBARSWhite lines are
WINDS BLOW FROMHIGH TO LOW
FASTESTWINDSOCCURWHERE THE ISOBARS ARE_________________Close together
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N30.029.8WSFASTESTSPEED29.6NE WINDE
29.629.8SW WIND30.0NWEFASTESTSPEEDS
29.8FASTESTSPEEDL29.630.0NWEWinds blow TowardThe centerS
4. Humidity and  CLOUD FORMATION
The Formation of CloudsA. Define cloud:large group of H2O droplets suspended in airB. Steps involved in cloud formation:warm moist air rises        expands            cools condenses
1. Describe the mass of air that would lead to cloud formation in terms of temperature, humidity, densityWarmMoistLow density
2. The air will risebecause oflow density3. Describe what the air does asit rises:       expands    cools    condenses
4. Clouds will form if this rising moist aira. cools to the dew point temp.b. has condensation nuclei   available.    (dust, pollutants etc..)
C. Basic Cloud Types:1. Cirrus: high and feathery      (fair weather)2. Cumulus: white and puffy      (fair weather)3. Stratus: covers the sky like a blanket     (precipitation probable)
Cirrus Clouds
Cumulus clouds
Cumulonimbus clouds
Stratus clouds with fog
D. Effects of aMountain Range:OrographicEffect(adiabatic cooling)
CondensesDry aircoolsSinksexpandsWindcompresseswarmsMoistairrisesmountain
1. The side of the mountain with the moist prevailing winds is called the_____________  Summary:Windward sidemoist airrisesexpandscoolscondensesWind
2. The air descends to the otherside of the mountain which is called the     ______________________Summary:Leeward sidedry airsinkscompresseswarmsWind
D. PrecipitationA. Describe what causes precipitation:Precipitation forms around Dust particles (pollutants) droplets combine (coalesce)become heavy and fall
B. Explain why precipitation cleans the   atmosphere:as precipitation forms around dust/pollutants…they are removed from theatmosphere as precipitation falls
When the dew point temperature    and air temperature approach    each other what happens to the    chance of precipitation and why?The chance of precipitation    increases     because the air is more    saturated
E. Complete the chart below:WarmmoistRiseExpandDecreaseDecreaseCoolSinkCompressIncreaseIncrease
Dew Point and Relative Humidity!
Dew Point TemperatureThe temperature at which the air is holding the ____________ amount of water. The air is _____________Maximumsaturated
Relative Humidity:The ratio of the amount of water vapor in the air, to the maximum amount it can hold. It is usually expressed as a __________. As the temperature increases, the maximum absolute humidity _____________ but the relative humidity will decreasepercentageStay the same,
The dew point and relative humidity are determined by using an instrument called a _______________________slingpsychrometer
The psychrometer has two thermometers, a dry bulb and a wet bulb. The psychrometer is whirled in the air so that evaporation will occur.
The lower the moisture content of the air, the ________ evaporation will occur from the wet bulb and the wet bulb temperature will be _________morelowered
Use your ESRT to fill in the chart…The answer the questions
Do Now:Read the “Structure of the atmosphere notes” and answer questions 1 through 6 using your reference tables.
Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mbDew point temperature = 18 °C Wind speed 25 knotsWind direction SW
Synoptic Weather MapsAtmospheric variables are collected from thousands of weather stations around the world four times each day.
1. Station ModelProvides a summary of the current atmospheric conditions in an area.
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Additional symbols used on weather maps and station models
The circle represents the actual weather station at its location
The shaded portion of the circle represents the % cloud.
The line represents the direction the wind is coming from.
The feathers represent the wind speed.  Each whole feather is 10 knots and each half feather is 5 knots.  1 knot = 1.15 m/hr.
The number in the upper left represents the current temperature in Fahrenheit degrees.
The symbol * represents the present weather.
The number to the left of present weather is visibility in miles.
The bottom left number represents the dew point in degrees Fahrenheit.
The top right number represents the barometric pressure in short hand millibars.  196 = 1019.6 millibars.
The middle right number represents the barometric trend. A steady 1.9mb rise in the past 3 hours.
Bottom right is the amount of precipitation in the last 6 hoursWeather Station Models196286*+1.9/   27.25
The Barometric Pressure on a Station Map is in code… The number 9 or 10 has been omitted from the front
Rule for converting the code into millibars:1088.7887= ___________Because if the first digit is 5 or greater add _________ and place a decimal point before the last digit. A 10 in front
Rule for converting the code into millibars:916.52. 165= ___________Because if the first digit is less than 5 add ________ and place a decimal point before the last digit. a 9 in front
Change the following to abbreviated form:956.4:______________1014.3: _____________564143
Change from abbreviated form:964:______________126: _____________996.41014.3
Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°C =  Air pressure = 996 mbDew point temperature = 18 °C Wind speed 25 knotsWind direction SW68°F68
Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mb =Dew point temperature = 18 °C Wind speed 25 knotsWind direction SW099668960
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Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mbDew point temperature = 18 °C =64 °FWind direction SW Wind speed 25 knots96068
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Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mbDew point temperature = 18 °C =64Wind direction SW Wind speed 25 knots9606864
Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mbDew point temperature = 18 °C Wind direction SWWind speed 25 knots9606864
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Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mbDew point temperature = 18 °C Wind direction SW Wind speed 25 knots9606864
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Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mbDew point temperature = 18 °C Wind direction SW Wind speed 25 knotsAdd sleet9606864
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Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mbDew point temperature = 18 °C Wind direction SW Wind speed 25 knotsAdd sleet9606864
Construct a Station Model Using the following Weather Data:Cloud cover: 50 %Air temp = 20°CAir pressure = 996 mbDew point temperature = 18 °C Wind direction SW Wind speed 25 knotsAdd Raina steady 1.9mbrise in the past3 hours96068+1.9/64
Construct a Station Model Using the following Weather Data:75% cloudswinds  from  the  N.W.wind speed 35 knotsair temperature 28F, dew point temp. 20Fvisibility 5 milesbarometric pressure 1032.5barometric trend 1.1 falling steadilypresent weather is snow325285*-1.1\20
5. The Greenhouse EFFECT
Video:The Greenhouse EffectHandout: label the diagrams
THE GREENHOUSE EFFECT
THE GREENHOUSE EFFECTHEAT ISTRAPPED BY THE GLASS OFTHE GREENHOUSEIncoming isShort waveoutgoing isLonger waveEnergy absorbed
What are the Greenhouse gases?CO2H20 VAPORINFRAREDMETHANE GAS
The Earth  Receives Energy    from          two sources:
SUN
 RadioactiveEnergy CORE
ElectromagneticAll matter radiates some__________________________Energy
ALLThe sun emits energy in _____ wavelengthsof the electromagneticspectrum
ELECTROMAGNETIC SPECTRUM:REFERENCE TABLE PAGE 1410-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
infraredThe Earth radiates_____________      (heat)
Each type of energy differs in its    __________wavelength10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
ELECTROMAGNETIC SPECTRUM:REFERENCE TABLE PAGE 1410-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
SHORT WAVE LENGTHS ARE: MOSTLY ABSORBED byTHE OZONE GAMMAOZONE
ELECTROMAGNETIC SPECTRUM:REFERENCE TABLE PAGE 1410-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
SHORT WAVE LENGTHS ARE MOSTLYABSORBED by THE OZONE IN THE STRATOSPHERE   gamma,X-RAYSOZONE
ELECTROMAGNETIC SPECTRUM:REFERENCE TABLE PAGE 1410-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
SHORT WAVE LENGTHS ARE MOSTLYABSORBED by THE OZONE IN THE STRATOSPHERE  gamma, x-rays,UVOZONE
ELECTROMAGNETIC SPECTRUM:REFERENCE TABLE PAGE 1410-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
OZONEVISIBLE LIGHT :PASSES THROUGHTHE ATMOSPHEREWITH THE GREATEST INTENSITY
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ELECTROMAGNETIC SPECTRUM:REFERENCE TABLE PAGE 1410-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
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10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
Sun emits allwavelengths(heat)infraredEarth re-radiates
Interactions between Electromagnetic Energy & The Environment:
1.2.3.4.5.ABSORBTION- UV ABSORBED by OZONE IN STRATOSPHEREINFRARED ABSORBED BYCO2&H2O vapormethane, nitrous oxideREFLECTIONSCATTERINGREFRACTIONTRANSMISSION- BY CLOUDS, ICE, SNOW &  WATER- BY AEROSOLS, WATER DROPLETS, ICE CRYSTALS,AIR POLLUTANTS, DUST, POLLENLIGHT IS BENT AS ITMOVES THROUGH VARIED DENSITIESWHEN ENERGY PASSES THROUGH A MEDIUM
1. ABSORPTION2. REFLECTION3.SCATTERING4. REFRACTION5. TRANSMISSION
halfLess than ______of the incoming solar radiationis receivedby the Earth’s  surface
Surface properties of the Earth and Absorption of Energy:
Reflection vs. Absorption & RadiationColor:Texture:Light (white) reflectsdark (black) absorbsRough surface absorbssmooth surface reflects
ELECTROMAGNETIC SPECTRUM:				LAB10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4gammaX rayMicrowavesUltra violetInfraredRadio wavesIncreasingwavelengthDecreasingwavelengthvisibleViolet  Blue   Green  Yellow  Orange   Red
6. How does tooMuch      contribute to Global warming?CO2CO2H20 VAPORINFRAREDMETHANE GASCO2 absorbsinfrared
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I. Air Masses-
A. Air Mass:    large amount    of air with    the same     temperature    and humidity
B. List the characteristics    that an air mass picks up     from its place of origin:  1.   2. temperaturehumidity
C. Types of Air Masses:Describe the Air MassOriginSymbolcOver LandDry - HeavierContinentalmOver WaterMoist - LighterMaritimeLow LatitudesTWarm - Less DenseTropicalHigh LatitudesPCool - More DensePolarVery High LatitudesAArcticCold - Very Dense
Name and DescriptionDescribe the Air MassSymbolContinentalTropicalcTDry and WarmmTMoist and WarmMaritimeTropicalContinental PolarcPDry and CoolMaritime PolarmPMoist and CoolContinental ArcticcADry and Very Cold
E. Types of Air Masses:cPmPmPcPcTmTmT
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Local windCaused by the unequal heating of land and water.
This creates density difference.
Draw the diagrams in your notes.Planetary Wind BeltsReference TablesPage 14
Planetary wind Pattern If The Earth Didn’t Rotate
	Cold air would_______ at the poles and flow along the surface of the     Earth toward the__________sinkequator
riselow	Air would then warm atthe equator and_____________(due to ___________ density) and flow back to the_____________poles
	this would create two great _________ cells over the Earthconvection
	II. Earth’s Rotation Effect On Wind Patterns:convection
Coriolis (Rotation)right___________________ effect causesthe winds to deflect to the __________ in theNorthern Hemisphere
Right in the Northern HemisphereIntendedActual dueTo coriolis(rotation)
Left in the Southern HemisphereIntendedActual dueTo coriolis(rotation)
Left    And to the __________ in theSouthernHemisphere
 two convection cells tobreak into ________convection cells6
Planetary Wind and Moisture Belts in the TroposphereDryNEWet60°NSW                Dry                                    30°NHorse latitudesNEDoldrums               Wet                                         0°SE               Dry                                 30°SHorse latitudesNNWWet60°SWESEDryS
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