1. Chapter 4 Weather

2. Solar Radiation Temperature Changes with Latitude Like equator Like at poles

3. Seasonal Changes Temperature Changes with Season

4. The Atmosphere Nitrogen 78% Oxygen 21% CO 2.038% Carbon dioxide Argon Water vapor Pollutants Helium Etc. 1%

5. The Atmosphere O2O2 O3O3 O.S. Jet Black Bird

6. Atmospheric Circulation Circulation spawned by heating / cooling Prevailing winds: Generated by pressure differences and Coriolis effect

7. Trade Winds

8. Horse Latitudes 30 degrees north (Horse latitudes) & 30 degrees south (Horse Latitudes) & Equator (Doldrums)

9. Coriolis Effect Southern Hemisphere

10. Coriolis Effect

11. Size of deflection is directly related to both the speed at which the air is moving and its latitude. The Coriolis force is zero right at the equator. The Coriolis force only acts on large objects like air masses moving considerable distances. Small objects, for example ships at sea, are too small to experience significant deflections. Gaspard de Coriolis (1792-1843)

12. El Niño/Southern Oscillation (ENSO) Chicken and Egg scenario – ocean temperatures or trade winds? This decreases during El Niño Increases during La Niña http://esminfo.prenhall.com/ science/geoanimations/ani mations/26_NinoNina.html

13. Enso Neutral Conditions

14. El Niño/Southern Oscillation (ENSO) – enso only refers to el nino 1.Heavier rainfall over coastal equatorial South America 2.Drought in Western Pacific (Indonesia & Australia) 3.Increased transmission of disease – mosquitoes and stagnant water – Les or More water and heat 4.Migration of fish species (North or South – Inshore or Out) 5.Death of seals and sea birds due to changing fisheries 6.Heavier rains in the southwestern deserts of United States 7.Fewer hurricanes in the Atlantic 8.Changes in disease due to shifts in temperature and moisture 2010-2011 Australia has record flooding? La Nina or El Nino Weak or Strong

15. El Nino La Nina

16. Tornados

18. Tornado formation: http://www.youtube.com/watch?v=7KDz6dGQ5RE http://www.youtube.com/watch?v=7KDz6dGQ5RE Tornado Formation: http://www.youtube.com/watch?v=MjjwPQRVbWk http://www.youtube.com/watch?v=MjjwPQRVbWk Tornado Formation http://www.youtube.com/watch?v=7bHSS1ImFQI http://www.youtube.com/watch?v=7bHSS1ImFQI

19. The Global Ocean Patterns of Circulation in the Ocean Influenced by: 1. Coriolis Effect 2. Winds 3. Land Masses 4. Water Density

20. The Global Ocean Patterns of Circulation in the Ocean

21. The Global Ocean Vertical Mixing of Ocean Water

22. 1.Anatomy of a Hurricanehttp://www.youtube.com/watch?v=HJydFJORWf4&feature=r elatedhttp://www.youtube.com/watch?v=HJydFJORWf4&feature=r elated 2.Hurricane Formation: http://www.youtube.com/watch?v=SNEG4YKElgY http://www.youtube.com/watch?v=SNEG4YKElgY

23. 2005 Hurricane tracks

24. Hurricanes Severe weather events: Tropical cyclones Atlantic Ocean = hurricanes Pacific Ocean = typhoons Indian Ocean = cyclones Category One Hurricane: Winds 74-95 mph Category Two Hurricane: Winds 96-110 mph - Storm surge generally 6-8 feet above normal Category Three Hurricane: Winds 111-130 mph - Some structural damage to small residences Category Four Hurricane: Winds 131-155 mph - Complete destruction of mobile homes Category Five Hurricane: Winds greater than 155 mph - Storm surge generally greater than 18 ft above normal and framed homes destroyed

25. Hurricanes 1.Hurricanes are powered by the energy released during condensation 2. Hurricanes are steered by prevailing wind patterns and wind sheer will destroy a hurricane. 3. What are positive and what are negative feed-back-loops for hurricanes 4. When winds reach 74mph a tropical storm becomes a hurricane 5. Why is the eye clear? Air coming in from the eye wall is coming inward towards the center from all directions. This convergence causes the air to sink in the eye. This sinking creates a warmer environment and the clouds evaporate leaving a clear area in the center.

26. Katrina

28. Fronts What is a front?

29. Fronts

30. 1. A front is defined by temperature, relative humidity, and air pressure: 1. Temperature = the kinetic energy of a substance 2. Relative Humidity = is a function of temperature and water content 3. Air pressure = the weight of the atmosphere Warm Fronts 1. Retreating Cold fronts under advancing warm fronts are drawn out in a triangular fashion due to friction with the ground causing a triangular shape to the advancing warm front. 2. Warm fronts move towards the northeast 3. Warm fronts usually travel at about 15mph Cold Fronts 1. Cold fronts become rounded due to friction with the ground as they advance on warm fronts. 2. Cold fronts tend to move towards the east or southeast 3. Cold fronts usually advance at speeds of 20mph 4. Cold fronts may produce violent weather depending on their speed and air stability. 5. Faster moving cold fronts produce “squall Lines” Where high upper level winds stop a warm front from lifting up but whip up warm air ahead of the storm producing violent weather. Fronts

31. Pressure Systems (in the north) 1. Low Pressure systems rotate counter clockwise 2. High pressure systems rotate clockwise Jet Streams 1. Tend to follow the borders between warm and cold air 2. In the summer they are located further north and in the winter further south 3. Jet streams blow west to east in the northern and southern hemispheres 4. How are airline flights impacted by jet streams (speed and turbulence) Wind Shear 1.Is any sudden change in wind speed or direction causing, turbulence. Air Movement

32. Turbulence

33. Micro-Burst

35. Wind What is wind and what makes wind?

36. Beach Winds Hanging at the beach Day time Vs. Night time breezes

37. Sea breezes

38. Micro-Climate & Turbulence

39. Wind

40. Katabatic Winds Katabatic winds exist in many parts of the World and are winds that flow from the high elevations of mountains, plateaus, and hills down their slopes to the valleys or planes below. There are many diffent names for katabatic winds depending where they are located - Santa Anna (funneled & dry), and Chinook (dry).

41. Chinook Winds Over Rockies

42. Weather and Climate Rain shadows Insert Fig 5.19 b

43. Santa Ana Winds

45. NOR’EASTERNOR’EASTER

46. 1.A 10k foot mountain 2.Air temperature at mountains base is 60 degrees 3.Clouds form at 4k and extend to the mountain top 4.What is the temperature of the valley floor (leeward side) 5.How does humidity and temperature change from winward to leeward? Problem 2 A 14k peak with a valley temperature of 70 Cloud formation begins at 7k and ends at 10k (5.5 and 3.2 = temperature changes for every thousand feet) 1.What is the temperature at 7K? 2.What is the temperature at 10K? 3.What is the temperature at 14K? 4.What is the temperature in the leeward valley? Is there compression of the air as in refrigeration or a decompression? Adiabatic Problems

47. Adiabatic heating and cooling is a temperature change within a gas due to compression (resulting in heating) and expansion (resulting in cooling); no heat is added to, or removed from the gas. Why rising air cools and Rain Shadows 1.Decreased pressure 2. For every 1k/feet air rises it cools 5.5 farenheight due to lowering gas pressures and heats the same going down (adiabatic cooling & heating) 3. Air that rises and condenses at the same time only cools 3.2F for every 1k it rises due to the “heat of condensation” 4. Air moving up western slopes can come down warmer on the other side. Creating cool moist western slopes and warm dry eastern slopes. Adiabatic Temperature Change & Condensation

48. Lightning What do you know about lightning 1.Lightning 5 min. – http://www.youtube.com/watch?v=Q3Awp-3CxSUhttp://www.youtube.com/watch?v=Q3Awp-3CxSU 2. http://www.youtube.com/watch?v=6MUYsIjTKvkhttp://www.youtube.com/watch?v=6MUYsIjTKvk

49. Lightning Thunder and Lightning 1.Sound travels about one mile every 5 seconds So if you count to ten the storm is 2 miles away 2. Thunder rumbles because the sound from different points on the bolt reaches our ears at different times 3. Thunder, is produced by the heating (expansion) and cooling (contraction) of the air around a lightning strike. 4. Lightning forms from negative charges at the bottom of the cloud that meet with positive charges from the ground. A stepped leader from the cloud meets a streamer from the ground. Visible light moves up and charge flows down. Individual charges are drained separately causing lightening to flash and strike multiple times in one location.