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Meteorology ,[object Object]
Components of Weather What do you need to know today? ,[object Object],2. Many different atmospheric processes affect New York State.
A.  Earth’s Energy ,[object Object],[object Object],Indirect Rays Direct Rays
Solar Electromagnetic Spectrum The solar  electromagnetic spectrum  includes visible light, as well as X-rays, ultraviolet rays and infrared rays.
Factors Affecting Insolation –  Duration  (TIME –How Long) ,[object Object],[object Object]
Causes of Weather ,[object Object]
A.  Weather/Atmospheric Variables ,[object Object],[object Object],[object Object],[object Object]
Weather Instruments ,[object Object]
Weather Instruments ,[object Object],[object Object]
Weather Instruments ,[object Object],[object Object]
Weather Instruments ,[object Object],[object Object]
B.  Atmosphere =  The envelope of air (mixture of gases) that surrounds Earth. ,[object Object],[object Object],[object Object],[object Object],[object Object]
B.  Atmosphere ,[object Object],[object Object],[object Object]
Bill Nye The Science Guy  ,[object Object],[object Object],[object Object]
B.  Atmosphere 1.  Composition vs. Altitude ,[object Object]
B.  Atmosphere 2.  Atmosphere and Solar Energy
B.  Atmosphere 2.  Atmosphere and Solar Energy ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
C. Temperature and Heat
C. Temperature and Heat  1.  Heat Transfer  ,[object Object],[object Object],[object Object]
C. Temperature and Heat  1.  Heat Transfer ,[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object]
2.  Measuring Temperature ,[object Object],[object Object],[object Object],[object Object]
Isotherms on Synoptic Weather Map Why do the isotherms seem to run E – W across the map?
3.  Factors that Effect the Amount/Rate of Heating ,[object Object]
3.  Factors that Effect the Amount/Rate of Heating ,[object Object],[object Object]
3.  Factors that Effect the Amount/Rate of Heating ,[object Object],[object Object],[object Object],[object Object]
3.  Factors that Effect the Amount/Rate of Heating ,[object Object],[object Object],[object Object]
A surface which is smooth will reflect more than it will absorb
D.  MOISTURE 1.  Changes in State ,[object Object],[object Object],[object Object]
D.  MOISTURE 1.  Changes in State ,[object Object],[object Object],[object Object]
D.  MOISTURE 1.  Changes in State ,[object Object],[object Object],[object Object],[object Object],[object Object]
D.  MOISTURE 1.  Changes in State ,[object Object]
D.  MOISTURE 1.  Changes in State ,[object Object],[object Object],[object Object]
Use your review book – page 118 and the ESRT to complete your worksheet
D.  MOISTURE 2.  Moisture in the Atmosphere ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
D.  MOISTURE 2.  Moisture in the Atmosphere ,[object Object],[object Object]
D.  MOISTURE 2.  Moisture in the Atmosphere ,[object Object]
D.  MOISTURE 2.  Moisture in the Atmosphere ,[object Object],[object Object]
Factors Affecting the Rate of Evaporation ,[object Object],[object Object],[object Object]
Factors Affecting the Rate of Evaporation ,[object Object],[object Object]
Factors Affecting the Rate of Evaporation ,[object Object],[object Object],[object Object]
2.  Dew Point  Temperature ,[object Object],[object Object]
2.  Dew Point Temperature ,[object Object]
2.  Dew Point Temperature ,[object Object],[object Object]
3.  Relative Humidity ,[object Object],[object Object],[object Object],[object Object],[object Object]
3. Relative Humidity ,[object Object],[object Object]
3. Relative Humidity ,[object Object],[object Object],[object Object]
3. Relative Humidity ,[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],Using the ESRT to determine Dew Point & Relative Humidity Handy Dandy Earth Science Reference Tables Page  12
The “Dry Bulb” ,[object Object],[object Object],[object Object],20 °C
The “Wet Bulb” ,[object Object],[object Object],12 °C Wet Booty
A Dry Day… ,[object Object],[object Object],20 °C Difference between wet bulb & dry bulb is 12  °C. 8 °C 20 °C 14 °C 12 °C
A Humid Day… ,[object Object],[object Object],14 °C 20 °C Difference between wet bulb & dry bulb is 6  °C.
Page 12 of your Handy Dandy Earth Science Reference Tables ,[object Object],[object Object],[object Object]
Dry-bulb temperature is your air temperature. 20  °C
14  °C
4  °C
Subtract (the difference) between the dry bulb and wet bulb
14 °C 20 °C 20-14=6
16 °C 18 °C 18-16=2
8 °C 20 °C 20-8=12 Put it all together Relative Humidity = 11%
10 °C 14 °C 14-10=4 Relative Humidity = 60%
10 °C 14 °C 14-10=4 Dew Point = 6°C The Dew Point Chart works the same way
Try These. 57% 17  °C 86% 4  °C 57% 4  °C Now do the worksheet for homework on the next page of your notes 8 °C 12 °C 5 °C 6 °C 20 °C 26°C DPT R Humidity Wet Bulb Dry Bulb
 
Clouds How Do Clouds Form?
Clouds ,[object Object]
Clouds ,[object Object]
Components of Weather E.  Air Pressure What is pressure? The  weight of a column of air  – this creates air pressure HIGH LOW High pressure is cold air sinking (More Dense) Low pressure is warm air rising (Less dense)
E.  Air pressure
E.  Air Pressure ,[object Object],[object Object],[object Object]
2.  Changes in Atmospheric Pressure ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
2.  Changes in Atmospheric Pressure ,[object Object],[object Object]
2.  Changes in Atmospheric Pressure ,[object Object],[object Object]
3.  Mapping An Air Pressure Field ,[object Object],[object Object]
3.  Mapping An Air Pressure Field ,[object Object],[object Object]
3.  Mapping An Air Pressure Field ,[object Object],[object Object],[object Object],[object Object]
Your map should look like this!
High and Low Pressure
Components of Weather High Pressure System:   Anticyclone
Anticyclones ,[object Object],[object Object]
Components of Weather Low Pressure System:   Depression or Cyclone
Or……Cyclones ,[object Object],[object Object]
Wind ,[object Object],[object Object]
How is Wind Formed? Sun heats ground Ground heats air Air rises and cools in the atmosphere As air cools it can no longer rise Cold air sinks WIND moves between high and low pressure LOW HIGH
A.  What Makes the Wind Blow? ,[object Object],[object Object],[object Object],[object Object],[object Object]
Sea Breeze/Land Breeze
B.  Wind Direction and Speed Winds are named  for the direction  that they come   FROM
Wind Direction and Speed ,[object Object]
2.  Wind is represented by this symbol at a  weather station : ,[object Object],[object Object],[object Object],[object Object],feather
Westerly Wind
North Westerly  Wind
Now You Try It 15kts 45kts 25kts 20kts 30kts 40kts 35kts
B.  Wind Speed and Direction ,[object Object],[object Object],[object Object]
[object Object]
Coriolis Effect ,[object Object]
Map View
Profile View Buffalo Boston Buffalo Chicago
Global Winds ,[object Object],[object Object]
Global Winds ,[object Object],[object Object]
Components of Weather F.  Air Masses What is an Air Mass? An  air mass  is a large body of air in the troposphere moving in a particular direction, with the same  temperature ,  pressure  and  humidity  throughout.
Components of Weather Air Masses Affecting the U.S.
1.  Source Region =  Place on Earth where an air mass forms ,[object Object],[object Object],[object Object],[object Object]
Types of Air Masses ,[object Object],[object Object],[object Object],It’s right here in ESRT Pg 13
4.  Fronts –  the interface between 2 different air masses ,[object Object],[object Object],[object Object],[object Object],[object Object],ESRT pg 13 – What it looks like on a weather map!
  Warm Front  Cold Front  Occluded Front Stationary Front:  Warm and Cold air meet head on and neither gives way. Low pressure usually “track” along a stationary front bringing heavy, steady precipitation Thunderstorms, lightning, tornadoes Brings intense change – brief periods of stormy weather (severe) Covers wide area Wind changes “ bullies” the warm air UP quickly Lots of Clouds as air rises up precipitation Air is dense and hugs the ground Showers for long period Cold air meets warm air and mixes Cold Air –moves fast Warm air
The Stages of Front Formation
Station Models IT’S in the ESRT!
Weather Map Symbols IT’S in the ESRT!
Hurricanes ,[object Object],[object Object],[object Object]
 
Extreme Weather
 
 
 

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Meteorology

  • 1.
  • 2.
  • 3.
  • 4. Solar Electromagnetic Spectrum The solar electromagnetic spectrum includes visible light, as well as X-rays, ultraviolet rays and infrared rays.
  • 5.
  • 6.
  • 7.
  • 8.
  • 9.
  • 10.
  • 11.
  • 12.
  • 13.
  • 14.
  • 15.
  • 16. B. Atmosphere 2. Atmosphere and Solar Energy
  • 17.
  • 19.
  • 20.
  • 21.
  • 22.
  • 23. Isotherms on Synoptic Weather Map Why do the isotherms seem to run E – W across the map?
  • 24.
  • 25.
  • 26.
  • 27.
  • 28. A surface which is smooth will reflect more than it will absorb
  • 29.
  • 30.
  • 31.
  • 32.
  • 33.
  • 34. Use your review book – page 118 and the ESRT to complete your worksheet
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  • 55. Dry-bulb temperature is your air temperature. 20 °C
  • 57. 4 °C
  • 58. Subtract (the difference) between the dry bulb and wet bulb
  • 59. 14 °C 20 °C 20-14=6
  • 60. 16 °C 18 °C 18-16=2
  • 61. 8 °C 20 °C 20-8=12 Put it all together Relative Humidity = 11%
  • 62. 10 °C 14 °C 14-10=4 Relative Humidity = 60%
  • 63. 10 °C 14 °C 14-10=4 Dew Point = 6°C The Dew Point Chart works the same way
  • 64. Try These. 57% 17 °C 86% 4 °C 57% 4 °C Now do the worksheet for homework on the next page of your notes 8 °C 12 °C 5 °C 6 °C 20 °C 26°C DPT R Humidity Wet Bulb Dry Bulb
  • 65.  
  • 66. Clouds How Do Clouds Form?
  • 67.
  • 68.
  • 69. Components of Weather E. Air Pressure What is pressure? The weight of a column of air – this creates air pressure HIGH LOW High pressure is cold air sinking (More Dense) Low pressure is warm air rising (Less dense)
  • 70. E. Air pressure
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  • 78. Your map should look like this!
  • 79. High and Low Pressure
  • 80. Components of Weather High Pressure System: Anticyclone
  • 81.
  • 82. Components of Weather Low Pressure System: Depression or Cyclone
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  • 85. How is Wind Formed? Sun heats ground Ground heats air Air rises and cools in the atmosphere As air cools it can no longer rise Cold air sinks WIND moves between high and low pressure LOW HIGH
  • 86.
  • 88. B. Wind Direction and Speed Winds are named for the direction that they come FROM
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  • 93. Now You Try It 15kts 45kts 25kts 20kts 30kts 40kts 35kts
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  • 98. Profile View Buffalo Boston Buffalo Chicago
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  • 101. Components of Weather F. Air Masses What is an Air Mass? An air mass is a large body of air in the troposphere moving in a particular direction, with the same temperature , pressure and humidity throughout.
  • 102. Components of Weather Air Masses Affecting the U.S.
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  • 106. Warm Front Cold Front Occluded Front Stationary Front: Warm and Cold air meet head on and neither gives way. Low pressure usually “track” along a stationary front bringing heavy, steady precipitation Thunderstorms, lightning, tornadoes Brings intense change – brief periods of stormy weather (severe) Covers wide area Wind changes “ bullies” the warm air UP quickly Lots of Clouds as air rises up precipitation Air is dense and hugs the ground Showers for long period Cold air meets warm air and mixes Cold Air –moves fast Warm air
  • 107. The Stages of Front Formation
  • 108. Station Models IT’S in the ESRT!
  • 109. Weather Map Symbols IT’S in the ESRT!
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