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Weather & Climate PHYS503 Physics Colloquium March 24, 2008 Deepak Rajput Graduate Research Assistant Center for Laser Applications University of Tennessee Space Institute Tullahoma, Tennessee 37388-9700 Email: drajput@utsi.edu Web: http://www.drajput.com
Warning ,[object Object]
Outline ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object]
Building blocks of weather ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Effects of air pressure on weather ,[object Object],[object Object]
Humidity ,[object Object],[object Object],[object Object],Absolute The quantity of water in a particular volume of air (g/cm 3 ).  Relative Specific Specific humidity  is the ratio of water vapor to dry air in a particular volume. It is expressed as a ratio of kilograms of water vapor,  m w , per kilogram of mixture,  m t . i.e.,
Measuring and regulating humidity ,[object Object],[object Object],[object Object],[object Object],[object Object],Psychrometer Hygrometer
Dew Point ,[object Object],[object Object],[object Object]
Effects of humidity ,[object Object],[object Object],[object Object],[object Object],When humidity increases, the evaporation of sweat from the skin decreases, and  the body’s efforts to maintain the acceptable body temperature impairs.  If the atmosphere is as warm as or warmer than the skin during times of high  humidity, blood brought to the body surface cannot dissipate heat by conduction  to the air, and results in a condition called  hyperpyrexia .  Under such conditions, less blood goes to the active muscles, the brain and other internal organs, which results in  fatigue , and eventually leads to a condition called as  hyperthermia  or  heat stoke .
[object Object],Effects of humidity ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],Clouds
Types of Clouds – High Clouds (above 20,000 feet)
Types of Clouds – Mid Clouds (between 6000 & 20,000 feet)
Types of Clouds – Low Clouds (below 6000 feet)
Types of Clouds – Low Clouds (below 6000 feet)
Precipitation ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Precipitation Rain:  Drops of liquid water fall from the clouds when water vapor condenses around dust particles in the clouds, forming tiny droplets that eventually get too big for the cloud to hold so they fall, growing larger as they collect more water on their way down.  Snow:  Snow is ice that falls from the sky. Each snowflake is a delicately complex arrangement of ice crystals. A snowflake forms when water vapor sublimates, or turns directly from a gas into its solid form, ice.  Hail:  Hail is ice that falls from the sky, often in round shapes. Hailstones form within thunderstorm clouds when upward moving air keeps pellets of frozen water from falling. The pellets grow larger as drops of very cold water hit them and freeze. Eventually the balls of ice become so large and heavy that they fall to the ground as hailstones.  The largest documented hailstone weighted more than one and a half pounds!  Scientists estimate that it reached a speed of more than 80 mph as it fell toward Earth.  Sleet:  Sleet is like slush falling from the sky. Sleet forms when raindrops freeze into ice as they fall to the ground. They are usually smaller and wetter than hailstones.
Wind Wind is moving air and is caused by differences in air pressure within our atmosphere. Air under high pressure moves toward areas of low pressure. The greater the difference in pressure, the faster the air flows.
The Fastest Winds ,[object Object],[object Object],[object Object]
Describing winds ,[object Object],[object Object],[object Object],[object Object]
Beaufort Scale Source: http://home.comcast.net/~garyt1/wind.html
Wind Chill chart Source: http://home.comcast.net/~garyt1/wind.html
Weather Tullahoma Tampa Boston San Francisco Source: Date: March 22, 2008
Weather Moscow Sao Paulo Shanghai Dar es Salaam Source: Date: March 22, 2008
QUIZ ? ? Low Clouds
Wild Weather ,[object Object],[object Object],[object Object],[object Object],Cyclone:  An   area of low atmospheric pressure characterized by inward  spiraling winds that rotate  counter-clockwise  in the northern hemisphere  and  clockwise  in the southern hemisphere of the Earth.  It has 6 major categories: Polar cyclone, Polar low, Extratropical, Subtropical, Tropical and Mesoscale.
Wild Weather ,[object Object],[object Object],[object Object],[object Object]
Hurricane Catarina: March 24 – 28, 2004 | Speed: 100 mph Region: Southeastern Brazil
Wild Weather ,[object Object],[object Object],[object Object],[object Object]
Climate ,[object Object],[object Object],[object Object],[object Object]
Climate ,[object Object],[object Object]
[object Object],[object Object],[object Object],Climate
[object Object],[object Object],[object Object],Climate: Complicating Factors
[object Object],[object Object],[object Object],[object Object],[object Object],Climate: Complicating Factors
[object Object],[object Object],Climate IPCC: Intergovernmental Panel on Climate Change
[object Object],Effects of global climate change
[object Object],Effects of global climate change
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Effects of global climate change
Prevention ,[object Object],[object Object]
Ten Things  We  Can Do to Fight Global Warming   ,[object Object],[object Object],[object Object],Source: http://uspirg.org/uspirg.asp?id2=7629&id3=USPIRG&id4=USPIRGFS&
Ten Things  We  Can Do to Fight Global Warming   ,[object Object],[object Object],[object Object],Source: http://uspirg.org/uspirg.asp?id2=7629&id3=USPIRG&id4=USPIRGFS&
Ten Things  We  Can Do to Fight Global Warming   ,[object Object],[object Object],[object Object],Source: http://uspirg.org/uspirg.asp?id2=7629&id3=USPIRG&id4=USPIRGFS&
Ten Things  We  Can Do to Fight Global Warming   ,[object Object],US PIRG: United States Public Interest Research Groups Source: http://uspirg.org/uspirg.asp?id2=7629&id3=USPIRG&id4=USPIRGFS&
[object Object],[object Object]
[object Object]

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Weather and Climate

  • 1. Weather & Climate PHYS503 Physics Colloquium March 24, 2008 Deepak Rajput Graduate Research Assistant Center for Laser Applications University of Tennessee Space Institute Tullahoma, Tennessee 37388-9700 Email: drajput@utsi.edu Web: http://www.drajput.com
  • 2.
  • 3.
  • 4.
  • 5.
  • 6.
  • 7.
  • 8.
  • 9.
  • 10.
  • 11.
  • 12.
  • 13. Types of Clouds – High Clouds (above 20,000 feet)
  • 14. Types of Clouds – Mid Clouds (between 6000 & 20,000 feet)
  • 15. Types of Clouds – Low Clouds (below 6000 feet)
  • 16. Types of Clouds – Low Clouds (below 6000 feet)
  • 17.
  • 18. Precipitation Rain: Drops of liquid water fall from the clouds when water vapor condenses around dust particles in the clouds, forming tiny droplets that eventually get too big for the cloud to hold so they fall, growing larger as they collect more water on their way down. Snow: Snow is ice that falls from the sky. Each snowflake is a delicately complex arrangement of ice crystals. A snowflake forms when water vapor sublimates, or turns directly from a gas into its solid form, ice. Hail: Hail is ice that falls from the sky, often in round shapes. Hailstones form within thunderstorm clouds when upward moving air keeps pellets of frozen water from falling. The pellets grow larger as drops of very cold water hit them and freeze. Eventually the balls of ice become so large and heavy that they fall to the ground as hailstones. The largest documented hailstone weighted more than one and a half pounds! Scientists estimate that it reached a speed of more than 80 mph as it fell toward Earth. Sleet: Sleet is like slush falling from the sky. Sleet forms when raindrops freeze into ice as they fall to the ground. They are usually smaller and wetter than hailstones.
  • 19. Wind Wind is moving air and is caused by differences in air pressure within our atmosphere. Air under high pressure moves toward areas of low pressure. The greater the difference in pressure, the faster the air flows.
  • 20.
  • 21.
  • 22. Beaufort Scale Source: http://home.comcast.net/~garyt1/wind.html
  • 23. Wind Chill chart Source: http://home.comcast.net/~garyt1/wind.html
  • 24. Weather Tullahoma Tampa Boston San Francisco Source: Date: March 22, 2008
  • 25. Weather Moscow Sao Paulo Shanghai Dar es Salaam Source: Date: March 22, 2008
  • 26. QUIZ ? ? Low Clouds
  • 27.
  • 28.
  • 29. Hurricane Catarina: March 24 – 28, 2004 | Speed: 100 mph Region: Southeastern Brazil
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