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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: TEMPERATURE ,[object Object]
AIR PRESSURE
WIND,[object Object],[object Object],[object Object]
4. Humidity:Moisture content of the atmosphere
In what layer of our atmosphere  does our weather occur? Troposphere
What is our atmosphere made of?
Argon 0.93 % Carbon Dioxide 0.03 % Water vapor 0.0 to 4.0 % 0.01 %    	Neon 	Helium 	Methane 	Krypton 	Hydrogen 	Ozone 	Xenon Oxygen 21% Nitrogen 78% Other 1%
See Front Cover of your ESRT!!!
 1.Air Temperature: ,[object Object],[object Object]
Each time  a molecule hits the  thermometer bulb energy is  transferred  and the  temperature  rises
Air molecule COLD HOT
WHICH SAMPLE HAS MORE KINETIC ENERGY? Motion COLD HOT
WHICH SAMPLE HAS MORE KINETIC ENERGY? Motion HOT COLD Energy           transferred
COLD HOT
COLD HOT
COLD HOT
HOT COLD
HOT COLD
HOT COLD
HOT COLD Hot air rises because of   increased  kinetic energy
Three scales are use to measure temperature: ,[object Object]
2. Celsius
3. Kelvin,[object Object]
Each notch Is worth 2 degrees Each notch is worth 1 degree 95 190 85 355 170 Each notch   is worth   1 degree 345 150 335
ALL YOU NEED TO DO IS READ ACROSS AND USE A STRAIGHT EDGE  ICE  BOILING WATER 1. FARENHEIT                   2. CELSIUS                   3. KELVIN 32 212  0 100 273 373
158 70 CELSIUS =         FARENHEIT 			=          KELVIN 343
82    180 FARENHEIT =      CELSIUS     				   =       KELVIN 355
	ABSOLUTE ZERO  (ZERO DEGREESKELVIN) Lowest possible temperature NO KINETIC ENERGY        THE MOLECULES ARE NOT MOVING
Quick Energy Review!
REVIEW QUESTONS: WHICH SKIIER HAS THE GREATEST   KINETIC ENERGY? A B D C
WHICH SKIIER HAS THE GREATEST POTENTIAL ENERGY? A B D C
DURING ENERGY CHANGES,  IF ONE BODYIS LOSING ENERGY,  THE OTHER IS _______ ENERGY: Gaining THE WAVE LOSES ENERGY: THE SAND   GAINS    ENERGY
DURING ENERGY CHANGES,  IF ONE BODYIS LOSING ENERGY  THE OTHER IS GAINING ENERGY: THE WAVE LOSES ENERGY: THE SAND   GAINS    ENERGY
DURING ENERGY CHANGES THE TOTAL ENERGY  REMAINS THE SAME ENERGY ALWAYS FLOWS  FROM  HIGH TO LOW (source to sink)
THE ENERGY WILL FLOW FROM: THE FLAME TO THE FINGER
ENERGY WILL FLOW FROM ICE THE FINGER TO  THE ICE
THE LIQUID LOSES ENERGY  AS THE ICE  GAINS ENERGY
WHEN WILL THE EXCHANGE OF ENERGY STOP? WHEN EQUILIBRIUM IS REACHED  THE LIQUID AND THE ICE REACH  THE SAME TEMPERATURE
The Affects of Air Temperature
Imagine two open  containers of air: One is filled with hot air and the other is  filled with cold air HOT COLD
Which container has more kinetic energy? HOT COLD
Which container has higher air pressure? HOT COLD
Which container has greater density? HOT COLD
Air molecule Water molecule Which container can hold more water? COLD HOT
Air molecule Water molecule HOT COLD
In summary: ,[object Object]
hot air has less pressure
hot air can hold more water
hot air is less dense
hot air rises,[object Object],[object Object]
Indirect Pressure Altitude
Indirect Pressure Temperature
A barometer measures pressure in inches  of mercury or millibars  see reference table page 13
Standard  pressure is 1013.2 millibars or 29.92 inches of mercury
Each notch is worth 1.0 Each notch is  worth 0.01 1039.0 30.65 1038.0 1037.0
Convert  1040.0 millibars to 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  lighter Decreases in air that is full of water vapor  Pressure
Indirect pressure Humidity
Summary HOT: COLD: ,[object Object]
less pressure
holds more water
Heavier
more dense
more pressure,[object Object]
equilibrium The Earth is always trying to achieve_______________
high Energy is constantly being re-distributedflowing from _______to _______ low
How can we decreasepressure without changing our elevation? Increase temperature Increase humidity
Warmer and Wet Low pressure  High pressure Cooler and Dry
Latitude…. Earth  Poles  low Temp: pressure: density:  humidity: high high low EQUATOR high temp: pressure: density: humidity: low low high
WIND:
Come from Winds are described by the direction they ___________
[object Object],high ,[object Object],low
ISOBARS White lines are
WINDS BLOW FROM HIGH TO LOW
FASTESTWINDSOCCURWHERE THE ISOBARS ARE_________________ Close together
N 30.0 29.8 W S FASTEST SPEED 29.6 NE WIND E
29.6 29.8 SW WIND 30.0 N W E FASTEST SPEED S
29.8 FASTEST SPEED L 29.6 30.0 N W E Winds blow  Toward The center S
4. Humidity and  CLOUD FORMATION
The Formation of Clouds A. Define cloud:large group of H2O  droplets suspended in air B. 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, density Warm Moist Low density
2. The air will risebecause of low density 3. Describe what the air does as it rises:        expands     cools     condenses
4. Clouds will form if this rising moist air a. 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)
Condenses Dry air cools Sinks expands Wind compresses warms Moist air rises mountain
1. The side of the mountain with the moist prevailing winds is called the _____________   Summary: Windward side moist air rises expands cools condenses Wind
2. The air descends to the otherside of the mountain which is called the      ______________________ Summary: Leeward side dry air sinks compresses warms Wind
D. Precipitation A. 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: Warm moist Rise Expand Decrease Decrease Cool Sink Compress Increase Increase
Dew Point and Relative Humidity!
Dew Point Temperature The temperature at which the air is holding the ____________ amount of water. The air is _____________ Maximum saturated
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 decrease percentage Stay the same,
The dew point and relative humidity are determined by using an instrument called a _______________________ sling psychrometer
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 _________ more lowered
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°C Air pressure = 996 mb Dew point temperature = 18 °C  Wind speed 25 knots Wind direction SW
Synoptic Weather Maps Atmospheric variables are collected from thousands of weather stations around the world four times each day.
1. Station Model Provides a summary of the current atmospheric conditions in an area.
Additional symbols used on weather maps and station models
[object Object]
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 Models 196 28 6 * +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: 1088.7 887= ___________ 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: 916.5 2. 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: _____________ 564 143
Change from abbreviated form: 964:______________ 126: _____________ 996.4 1014.3
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C =   Air pressure = 996 mb Dew point temperature = 18 °C  Wind speed 25 knots Wind direction SW 68°F 68
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb = Dew point temperature = 18 °C  Wind speed 25 knots Wind direction SW 0 996 68 960
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C =64 °F Wind direction SW  Wind speed 25 knots 960 68
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C =64 Wind direction SW  Wind speed 25 knots 960 68 64
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C  Wind direction SW Wind speed 25 knots 960 68 64
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C  Wind direction SW  Wind speed 25 knots 960 68 64
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C  Wind direction SW  Wind speed 25 knots Add sleet 960 68 64
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C  Wind direction SW  Wind speed 25 knots Add sleet 960 68 64
Construct a Station Model  Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C  Wind direction SW  Wind speed 25 knots Add Rain a steady 1.9mb rise in the past 3 hours 960 68 +1.9/ 64
Construct a Station Model  Using the following Weather Data: 75% clouds winds  from  the  N.W. wind speed 35 knots air temperature 28F,  dew point temp. 20F visibility 5 miles barometric pressure 1032.5 barometric trend 1.1  falling steadily present weather is snow 325 28 5 * -1.1br />20
5. The Greenhouse  EFFECT
Video: The Greenhouse Effect Handout: label the diagrams
THE GREENHOUSE EFFECT
THE GREENHOUSE EFFECT HEAT IS TRAPPED BY  THE GLASS OF THE GREENHOUSE Incoming is Short wave outgoing is Longer wave Energy absorbed
What are the Greenhouse gases? CO2 H20 VAPOR INFRARED METHANE GAS
The Earth  Receives Energy    from          two sources:
SUN
 Radioactive Energy  CORE
Electromagnetic All matter radiates some__________________________ Energy
ALL The sun emits energy in _____ wavelengthsof the electromagneticspectrum
ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
infrared The Earth radiates_____________      (heat)
Each type of energy differs  in its    __________ wavelength 10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
SHORT WAVE LENGTHS ARE:  MOSTLY ABSORBED by THE OZONE  GAMMA OZONE
ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
SHORT  WAVE LENGTHS ARE MOSTLY ABSORBED by THE OZONE IN  THE STRATOSPHERE    gamma, X-RAYS OZONE
ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
SHORT  WAVE LENGTHS ARE MOSTLY ABSORBED by THE OZONE IN  THE STRATOSPHERE   gamma, x-rays, UV OZONE
ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
OZONE VISIBLE LIGHT : PASSES THROUGH THE ATMOSPHERE WITH THE  GREATEST  INTENSITY
ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
Sun emits all wavelengths (heat) infrared Earth re-radiates
Interactions between Electromagnetic Energy & The Environment:
1. 2. 3. 4. 5. ABSORBTION - UV ABSORBED by  OZONE IN STRATOSPHERE INFRARED ABSORBED BY CO2&H2O vapor methane, nitrous oxide REFLECTION SCATTERING REFRACTION TRANSMISSION - BY CLOUDS, ICE,  SNOW &  WATER - BY AEROSOLS,  WATER DROPLETS, ICE CRYSTALS, AIR POLLUTANTS, DUST, POLLEN LIGHT IS BENT AS IT MOVES THROUGH  VARIED DENSITIES WHEN ENERGY  PASSES THROUGH  A MEDIUM
1. ABSORPTION 2. REFLECTION 3.SCATTERING 4. REFRACTION 5. TRANSMISSION
half Less than ______of the incoming solar radiationis receivedby the Earth’s  surface
Surface properties of the Earth and Absorption of Energy:
Reflection vs. Absorption & Radiation Color: Texture: Light (white) reflects dark (black) absorbs Rough surface absorbs smooth surface reflects
ELECTROMAGNETIC SPECTRUM: 				LAB 10-10      10-8      10-6       10-4       10-2        10 0       10 2        10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet  Blue   Green  Yellow  Orange   Red
6. How does too Much      contribute to  Global warming? CO2 CO2 H20 VAPOR INFRARED METHANE GAS CO2 absorbs infrared
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.  temperature humidity
C. Types of Air Masses: Describe the  Air Mass Origin Symbol c Over Land Dry - Heavier Continental m Over Water Moist - Lighter Maritime Low  Latitudes T Warm - Less Dense Tropical High  Latitudes P Cool - More Dense Polar Very High  Latitudes A Arctic Cold - Very Dense
Name and Description Describe the Air Mass Symbol ContinentalTropical cT Dry and Warm mT Moist and Warm MaritimeTropical Continental Polar cP Dry and Cool Maritime Polar mP Moist and Cool Continental Arctic cA Dry and Very Cold
E. Types of Air Masses: cP mP mP cP cT mT mT
Local wind ,[object Object]
This creates density difference.
Draw the diagrams in your notes.,[object Object]
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__________ sink equator
rise low 	Air would then warm atthe equator and_____________(due to ___________ density) and flow back to the_____________ poles
	this would create two great _________ cells over the Earth convection
	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  Hemisphere Intended Actual due To coriolis (rotation)
Left in the  Southern  Hemisphere Intended Actual due To coriolis (rotation)
Left     And to the __________ in theSouthernHemisphere
 two convection cells tobreak into ________convection cells 6
Planetary Wind and Moisture Belts in the Troposphere Dry NE Wet 60°N SW                 Dry                                    30°N Horse latitudes NE Doldrums                Wet                                         0° SE                Dry                                 30°S Horse latitudes N NW Wet 60°S W E SE Dry S

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Here are the steps to convert the barometric pressure code to millibars:1. If the first digit is 5 or greater, add 1000.2. Place a decimal point before the last two digits. So for 887:1. The first digit (8) is not 5 or greater, so do not add 1000.2. Place a decimal point before the last two digits.887 = 988.7 millibars

  • 2. Weather is… THE SHORT TERM CONDITION OF THE ATMOSPHERE
  • 3.
  • 5.
  • 6. 4. Humidity:Moisture content of the atmosphere
  • 7. In what layer of our atmosphere does our weather occur? Troposphere
  • 8.
  • 9.
  • 10. What is our atmosphere made of?
  • 11. Argon 0.93 % Carbon Dioxide 0.03 % Water vapor 0.0 to 4.0 % 0.01 % Neon Helium Methane Krypton Hydrogen Ozone Xenon Oxygen 21% Nitrogen 78% Other 1%
  • 12. See Front Cover of your ESRT!!!
  • 13.
  • 14.
  • 15.
  • 16.
  • 17.
  • 18.
  • 19. Each time a molecule hits the thermometer bulb energy is transferred and the temperature rises
  • 20.
  • 21.
  • 23. WHICH SAMPLE HAS MORE KINETIC ENERGY? Motion COLD HOT
  • 24. WHICH SAMPLE HAS MORE KINETIC ENERGY? Motion HOT COLD Energy transferred
  • 31. HOT COLD Hot air rises because of increased kinetic energy
  • 32.
  • 34.
  • 35. Each notch Is worth 2 degrees Each notch is worth 1 degree 95 190 85 355 170 Each notch is worth 1 degree 345 150 335
  • 36. ALL YOU NEED TO DO IS READ ACROSS AND USE A STRAIGHT EDGE ICE BOILING WATER 1. FARENHEIT 2. CELSIUS 3. KELVIN 32 212 0 100 273 373
  • 37. 158 70 CELSIUS = FARENHEIT = KELVIN 343
  • 38. 82 180 FARENHEIT = CELSIUS = KELVIN 355
  • 39. ABSOLUTE ZERO (ZERO DEGREESKELVIN) Lowest possible temperature NO KINETIC ENERGY THE MOLECULES ARE NOT MOVING
  • 41. REVIEW QUESTONS: WHICH SKIIER HAS THE GREATEST KINETIC ENERGY? A B D C
  • 42. WHICH SKIIER HAS THE GREATEST POTENTIAL ENERGY? A B D C
  • 43. DURING ENERGY CHANGES, IF ONE BODYIS LOSING ENERGY, THE OTHER IS _______ ENERGY: Gaining THE WAVE LOSES ENERGY: THE SAND GAINS ENERGY
  • 44. DURING ENERGY CHANGES, IF ONE BODYIS LOSING ENERGY THE OTHER IS GAINING ENERGY: THE WAVE LOSES ENERGY: THE SAND GAINS ENERGY
  • 45. DURING ENERGY CHANGES THE TOTAL ENERGY REMAINS THE SAME ENERGY ALWAYS FLOWS FROM HIGH TO LOW (source to sink)
  • 46. THE ENERGY WILL FLOW FROM: THE FLAME TO THE FINGER
  • 47. ENERGY WILL FLOW FROM ICE THE FINGER TO THE ICE
  • 48. THE LIQUID LOSES ENERGY AS THE ICE GAINS ENERGY
  • 49. WHEN WILL THE EXCHANGE OF ENERGY STOP? WHEN EQUILIBRIUM IS REACHED THE LIQUID AND THE ICE REACH THE SAME TEMPERATURE
  • 50. The Affects of Air Temperature
  • 51. Imagine two open containers of air: One is filled with hot air and the other is filled with cold air HOT COLD
  • 52. Which container has more kinetic energy? HOT COLD
  • 53. Which container has higher air pressure? HOT COLD
  • 54. Which container has greater density? HOT COLD
  • 55. Air molecule Water molecule Which container can hold more water? COLD HOT
  • 56. Air molecule Water molecule HOT COLD
  • 57.
  • 58. hot air has less pressure
  • 59. hot air can hold more water
  • 60. hot air is less dense
  • 61.
  • 63.
  • 65. A barometer measures pressure in inches of mercury or millibars see reference table page 13
  • 66. Standard pressure is 1013.2 millibars or 29.92 inches of mercury
  • 67. Each notch is worth 1.0 Each notch is worth 0.01 1039.0 30.65 1038.0 1037.0
  • 68. Convert 1040.0 millibars to inches of mercury
  • 69. 30.71
  • 71. Water vapor is very _________ compared to dry air: light (Nitrogen is heavier than hydrogen and oxygen)
  • 72. SO: When water vapor is added to dry air the air pressure ___________ decreases
  • 73. Because the air is lighter Decreases in air that is full of water vapor Pressure
  • 75.
  • 80.
  • 81. equilibrium The Earth is always trying to achieve_______________
  • 82. high Energy is constantly being re-distributedflowing from _______to _______ low
  • 83. How can we decreasepressure without changing our elevation? Increase temperature Increase humidity
  • 84. Warmer and Wet Low pressure High pressure Cooler and Dry
  • 85. Latitude…. Earth Poles low Temp: pressure: density: humidity: high high low EQUATOR high temp: pressure: density: humidity: low low high
  • 86. WIND:
  • 87. Come from Winds are described by the direction they ___________
  • 88.
  • 90. WINDS BLOW FROM HIGH TO LOW
  • 91. FASTESTWINDSOCCURWHERE THE ISOBARS ARE_________________ Close together
  • 92.
  • 93. N 30.0 29.8 W S FASTEST SPEED 29.6 NE WIND E
  • 94. 29.6 29.8 SW WIND 30.0 N W E FASTEST SPEED S
  • 95. 29.8 FASTEST SPEED L 29.6 30.0 N W E Winds blow Toward The center S
  • 96. 4. Humidity and CLOUD FORMATION
  • 97. The Formation of Clouds A. Define cloud:large group of H2O droplets suspended in air B. Steps involved in cloud formation: warm moist air rises expands cools condenses
  • 98. 1. Describe the mass of air that would lead to cloud formation in terms of temperature, humidity, density Warm Moist Low density
  • 99. 2. The air will risebecause of low density 3. Describe what the air does as it rises: expands cools condenses
  • 100. 4. Clouds will form if this rising moist air a. cools to the dew point temp. b. has condensation nuclei available. (dust, pollutants etc..)
  • 101. 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)
  • 106. D. Effects of aMountain Range: OrographicEffect (adiabatic cooling)
  • 107. Condenses Dry air cools Sinks expands Wind compresses warms Moist air rises mountain
  • 108. 1. The side of the mountain with the moist prevailing winds is called the _____________ Summary: Windward side moist air rises expands cools condenses Wind
  • 109. 2. The air descends to the otherside of the mountain which is called the ______________________ Summary: Leeward side dry air sinks compresses warms Wind
  • 110. D. Precipitation A. Describe what causes precipitation: Precipitation forms around Dust particles (pollutants) droplets combine (coalesce)become heavy and fall
  • 111. B. Explain why precipitation cleans the atmosphere: as precipitation forms around dust/pollutants…they are removed from theatmosphere as precipitation falls
  • 112. 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
  • 113. E. Complete the chart below: Warm moist Rise Expand Decrease Decrease Cool Sink Compress Increase Increase
  • 114. Dew Point and Relative Humidity!
  • 115. Dew Point Temperature The temperature at which the air is holding the ____________ amount of water. The air is _____________ Maximum saturated
  • 116. 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 decrease percentage Stay the same,
  • 117. The dew point and relative humidity are determined by using an instrument called a _______________________ sling psychrometer
  • 118. The psychrometer has two thermometers, a dry bulb and a wet bulb. The psychrometer is whirled in the air so that evaporation will occur.
  • 119. The lower the moisture content of the air, the ________ evaporation will occur from the wet bulb and the wet bulb temperature will be _________ more lowered
  • 120. Use your ESRT to fill in the chart…The answer the questions
  • 121. Do Now: Read the “Structure of the atmosphere notes” and answer questions 1 through 6 using your reference tables.
  • 122. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C Wind speed 25 knots Wind direction SW
  • 123. Synoptic Weather Maps Atmospheric variables are collected from thousands of weather stations around the world four times each day.
  • 124. 1. Station Model Provides a summary of the current atmospheric conditions in an area.
  • 125.
  • 126. Additional symbols used on weather maps and station models
  • 127.
  • 128. The shaded portion of the circle represents the % cloud.
  • 129. The line represents the direction the wind is coming from.
  • 130. 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.
  • 131. The number in the upper left represents the current temperature in Fahrenheit degrees.
  • 132. The symbol * represents the present weather.
  • 133. The number to the left of present weather is visibility in miles.
  • 134. The bottom left number represents the dew point in degrees Fahrenheit.
  • 135. The top right number represents the barometric pressure in short hand millibars. 196 = 1019.6 millibars.
  • 136. The middle right number represents the barometric trend. A steady 1.9mb rise in the past 3 hours.
  • 137. Bottom right is the amount of precipitation in the last 6 hoursWeather Station Models 196 28 6 * +1.9/ 27 .25
  • 138. The Barometric Pressure on a Station Map is in code… The number 9 or 10 has been omitted from the front
  • 139. Rule for converting the code into millibars: 1088.7 887= ___________ Because if the first digit is 5 or greater add _________ and place a decimal point before the last digit. A 10 in front
  • 140. Rule for converting the code into millibars: 916.5 2. 165= ___________ Because if the first digit is less than 5 add ________ and place a decimal point before the last digit. a 9 in front
  • 141. Change the following to abbreviated form: 956.4:______________ 1014.3: _____________ 564 143
  • 142. Change from abbreviated form: 964:______________ 126: _____________ 996.4 1014.3
  • 143. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C = Air pressure = 996 mb Dew point temperature = 18 °C Wind speed 25 knots Wind direction SW 68°F 68
  • 144. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb = Dew point temperature = 18 °C Wind speed 25 knots Wind direction SW 0 996 68 960
  • 145.
  • 146. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C =64 °F Wind direction SW Wind speed 25 knots 960 68
  • 147.
  • 148. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C =64 Wind direction SW Wind speed 25 knots 960 68 64
  • 149. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C Wind direction SW Wind speed 25 knots 960 68 64
  • 150.
  • 151. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C Wind direction SW Wind speed 25 knots 960 68 64
  • 152.
  • 153. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C Wind direction SW Wind speed 25 knots Add sleet 960 68 64
  • 154.
  • 155. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C Wind direction SW Wind speed 25 knots Add sleet 960 68 64
  • 156. Construct a Station Model Using the following Weather Data: Cloud cover: 50 % Air temp = 20°C Air pressure = 996 mb Dew point temperature = 18 °C Wind direction SW Wind speed 25 knots Add Rain a steady 1.9mb rise in the past 3 hours 960 68 +1.9/ 64
  • 157. Construct a Station Model Using the following Weather Data: 75% clouds winds from the N.W. wind speed 35 knots air temperature 28F, dew point temp. 20F visibility 5 miles barometric pressure 1032.5 barometric trend 1.1 falling steadily present weather is snow 325 28 5 * -1.1br />20
  • 158. 5. The Greenhouse EFFECT
  • 159. Video: The Greenhouse Effect Handout: label the diagrams
  • 161. THE GREENHOUSE EFFECT HEAT IS TRAPPED BY THE GLASS OF THE GREENHOUSE Incoming is Short wave outgoing is Longer wave Energy absorbed
  • 162. What are the Greenhouse gases? CO2 H20 VAPOR INFRARED METHANE GAS
  • 163. The Earth Receives Energy from two sources:
  • 164. SUN
  • 166. Electromagnetic All matter radiates some__________________________ Energy
  • 167. ALL The sun emits energy in _____ wavelengthsof the electromagneticspectrum
  • 168. ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 169. infrared The Earth radiates_____________ (heat)
  • 170. Each type of energy differs in its __________ wavelength 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 171. 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 172. ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 173. SHORT WAVE LENGTHS ARE: MOSTLY ABSORBED by THE OZONE GAMMA OZONE
  • 174. ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 175. SHORT WAVE LENGTHS ARE MOSTLY ABSORBED by THE OZONE IN THE STRATOSPHERE gamma, X-RAYS OZONE
  • 176. ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 177. SHORT WAVE LENGTHS ARE MOSTLY ABSORBED by THE OZONE IN THE STRATOSPHERE gamma, x-rays, UV OZONE
  • 178. ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 179. OZONE VISIBLE LIGHT : PASSES THROUGH THE ATMOSPHERE WITH THE GREATEST INTENSITY
  • 180.
  • 181. ELECTROMAGNETIC SPECTRUM: REFERENCE TABLE PAGE 14 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 182.
  • 183. 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 184. Sun emits all wavelengths (heat) infrared Earth re-radiates
  • 185. Interactions between Electromagnetic Energy & The Environment:
  • 186. 1. 2. 3. 4. 5. ABSORBTION - UV ABSORBED by OZONE IN STRATOSPHERE INFRARED ABSORBED BY CO2&H2O vapor methane, nitrous oxide REFLECTION SCATTERING REFRACTION TRANSMISSION - BY CLOUDS, ICE, SNOW & WATER - BY AEROSOLS, WATER DROPLETS, ICE CRYSTALS, AIR POLLUTANTS, DUST, POLLEN LIGHT IS BENT AS IT MOVES THROUGH VARIED DENSITIES WHEN ENERGY PASSES THROUGH A MEDIUM
  • 187. 1. ABSORPTION 2. REFLECTION 3.SCATTERING 4. REFRACTION 5. TRANSMISSION
  • 188. half Less than ______of the incoming solar radiationis receivedby the Earth’s surface
  • 189. Surface properties of the Earth and Absorption of Energy:
  • 190. Reflection vs. Absorption & Radiation Color: Texture: Light (white) reflects dark (black) absorbs Rough surface absorbs smooth surface reflects
  • 191. ELECTROMAGNETIC SPECTRUM: LAB 10-10 10-8 10-6 10-4 10-2 10 0 10 2 10 4 gamma X ray Microwaves Ultra violet Infrared Radio waves Increasingwavelength Decreasingwavelength visible Violet Blue Green Yellow Orange Red
  • 192. 6. How does too Much contribute to Global warming? CO2 CO2 H20 VAPOR INFRARED METHANE GAS CO2 absorbs infrared
  • 193.
  • 195. A. Air Mass: large amount of air with the same temperature and humidity
  • 196. B. List the characteristics that an air mass picks up from its place of origin: 1. 2. temperature humidity
  • 197. C. Types of Air Masses: Describe the Air Mass Origin Symbol c Over Land Dry - Heavier Continental m Over Water Moist - Lighter Maritime Low Latitudes T Warm - Less Dense Tropical High Latitudes P Cool - More Dense Polar Very High Latitudes A Arctic Cold - Very Dense
  • 198. Name and Description Describe the Air Mass Symbol ContinentalTropical cT Dry and Warm mT Moist and Warm MaritimeTropical Continental Polar cP Dry and Cool Maritime Polar mP Moist and Cool Continental Arctic cA Dry and Very Cold
  • 199. E. Types of Air Masses: cP mP mP cP cT mT mT
  • 200.
  • 201.
  • 202. This creates density difference.
  • 203.
  • 204. Planetary wind Pattern If The Earth Didn’t Rotate
  • 205. Cold air would_______ at the poles and flow along the surface of the Earth toward the__________ sink equator
  • 206. rise low Air would then warm atthe equator and_____________(due to ___________ density) and flow back to the_____________ poles
  • 207. this would create two great _________ cells over the Earth convection
  • 208. II. Earth’s Rotation Effect On Wind Patterns: convection
  • 209. Coriolis (Rotation) right ___________________ effect causesthe winds to deflect to the __________ in theNorthern Hemisphere
  • 210. Right in the Northern Hemisphere Intended Actual due To coriolis (rotation)
  • 211. Left in the Southern Hemisphere Intended Actual due To coriolis (rotation)
  • 212. Left And to the __________ in theSouthernHemisphere
  • 213. two convection cells tobreak into ________convection cells 6
  • 214. Planetary Wind and Moisture Belts in the Troposphere Dry NE Wet 60°N SW Dry 30°N Horse latitudes NE Doldrums Wet 0° SE Dry 30°S Horse latitudes N NW Wet 60°S W E SE Dry S
  • 215.
  • 216. Use your ReferenceTables Page 14 to describe the wind for the following latitudes:1. 42ºN _______2. 23º½N _______3. 23º½ S _______4. 70º N _____ SW NE SE NE
  • 217. 5. Which planetary wind belt is New York State Located? Dry NE SW Wet 60°N SW Dry 30°N NE Wet 0° SE Dry 30°S N NW Wet 60°S W E SE Dry S
  • 218. 6. Complete the following:The Coriolis Effect causes winds to curve to the __________________ in the N. Hemisphere right
  • 219. To Summarize: In high pressure winds blow In low pressure winds blow In or Out In or Out Clockwise or clockwise counterclockwise or counter clockwise L H
  • 220. The arrows show the wind direction: Is this a High or low pressure system? Does it carry moist or dry air? L moist
  • 222. 29.6 29.8 30.0 N Is this a high or low Pressure system? W E S
  • 223. 29.60 29.80 30.00 N W E What is the pressure at the inner isobar on This map? S
  • 224. 29.6 H 29.8 30.0 N Is this a high or low Pressure system? W E S High
  • 225. 29.60 H 29.80 30.00 N W E What is the pressure at the inner isobar on This map? S 30.20
  • 226. Which direction do winds curve in theNorthern Hemisphere? right Why?
  • 228. Is this clockwise or counter clockwise?
  • 229. The arrows show the wind direction: Is this a High or Low pressure system? H
  • 230. Does this carry moist Or dry air? H Dry
  • 231. What planetary windbelt do we live in? SW