1. CHAPTER 3 TEMPERATURE AND HUMIDITY EXTREMES CHAPTER 3 TEMPERATURE AND HUMIDITY EXTREMES

2.  Each day is like a tiny season! ◦ Daytime heating, nighttime cooling  Why do the high and low temperatures happen when they do?

5.  Daily temperature range near the ground is much greater than that above the ground!

7.  Latitude  Land and water distribution  Ocean currents  Elevation

10. Fig. 3.15, p. 78

11. Fig. 3.14, p. 77 Tale of three cities

12. Fig. 3.8, p. 70

14. Fig. 3.4, p. 66

15. Fig. 3.5, p. 67

16. Fig. 3.9, p. 71

17. Fig. 3.10, p. 72

18.  Even with the same average temperature, the range can differ considerably  Why might these be so different?

19.  Which curve is Juneau and which is Edmonton?  Why are they different? __________________ ________________

21.  (Note: these are kind of confusing!)  “Average temperature”: the average of the high and low temperature for the day  “Normal temperature”: a 30-year average

22.  Not once since 1952 has the high been exactly 62!  So, interpret the “normal” high with caution – what’s normal is for the temperature to be different each year!

23.  Standard deviation = 11.5  Mean +/- 2 standard deviations gives a range of about 39 to 85 – the high temperature will fall between these two values 95% of the time

24.  “Degree days”  When average temperature (average of high and low) is above 65 degrees F, people tend to use air conditioning ◦ “Cooling degree days” ◦ Each degree above 65 = one cooling degree day  When average temperature is below 65 degrees F, people tend to heat their homes/offices ◦ “Heating degree days” ◦ Each degree below 65 = one heating degree day

27.  When average temperature is above the base growing temperature for a crop

28.  Body’s Perception: Sensible temperature ◦ How we exchange heat energy with environment  Wind and cold ◦ Body, like the planet, must also have a heat/energy balance if temperature is to be maintained. ◦ Thin layer of warm molecules next to skin  Wind interferes with this, rapidly removes heat ◦ Sensible temperature for cold weather: Wind Chill

30.  Frostbite: Skin actually freezes and discolors  Cold, Damp Weather ◦ A cold rainy day often feels colder than a “dry” one because water on exposed skin conducts heat away from the body better than air does ◦ Hypothermia – body temp drops below normal  Most hypothermia occurs between freezing and 50° F, snow vs. rain, the wet really matters!  “Died of Exposure”

31. Fig. 3.18, p. 81

32.  The maximum amount of water vapor that can be in the air is a function of temperature ◦ The hotter it is, the greater amount of moisture that can be in the air  If this maximum amount of water vapor is actually in the air, the air is saturated  Usually the air near the ground is not saturated (but what might happen if it is?)  Most of the time, the amount of water vapor in the air stays about the same from day to night, even though the temperature goes up and down quite a bit

33.  Two types of humidity measures: absolute and relative  Absolute measures describe the actual amount of moisture in the air ◦ Examples: absolute humidity, dewpoint temperature, specific humidity, mixing ratio  Relative humidity compares the amount of moisture in the air with the amount needed for saturation

34.  Mass of water vapor divided by mass of air  Must add or subtract water vapor to the parcel to change the specific humidity

35.  Another absolute measure  Indicates how much you would have to cool the air to get to saturation.  The moisture needed for saturation at 60° is much less than at 80°. If the temperature is 80° and the dew point is 60°, you would have to cool the air 20° to have it be saturated

36.  Mixing Ratio – mass of water vapor over mass of dry air (how is this different from specific humidity?)  Vapor Pressure – The actual pressure only due to water vapor.  Both of these have actual values, and saturation values for the current temperature.

37.  Relative Humidity: (actual water vapor/saturation water vapor)*100 ◦ Can use either mixing ratio or vapor pressure ◦ RH can be changed two ways:  Change vapor content  Change saturation point (how?)

40. Fig. 3.20, p. 83 Dew Point (usually a better way to compare humidity) (usually a better way to compare humidity)

41. http://weather.unisys.com/surface/sfc_con_de wp.html

42.  Extreme Dew Points ◦ Record high T d in the US occur during heat waves of summer ◦ T d > 80°F rare in the US ◦ Highest T d in the US (90°F): New Orleans, LA; Melbourne, FL; Appleton, WI  Extreme Dew Points ◦ Highest T d in the world: Middle East near large bodies of extremely warm water  Red Sea: surface temperature of 98°F  Sharjah, United Arab Emirates, T d 93°F  Dhahran, Saudi Arabia, T d 95°F

43. Fig. 3.21, p. 83

44.  Body cools by emitting infrared energy and perspiration evaporation  Less evaporation causes people to feel hotter (perception, remember!)  Air with 100% relative humidity is saturated because the air is holding as much water in the vapor state that it can hold (at that temperature)  The higher the relative humidity, the less evaporation

45. Fig. 3.24, p. 87 Heat index – factors in both temperature and humidity

47. Table 3.6, p. 88

48.  On average, the deadliest weather in U.S.  Prolonged period of abnormally hot (& humid, usually) weather  Almost 50,000 died in Europe in 2003

49. Table 3.5, p. 87

50. Table 3.7, p. 89

51.  “Air was so heavy and thick because of the humidity” (Yankees getting off the plane in Houston)  Humid Air and Dry Air Do Not Weigh the Same ◦ At the same temperature and level in the atmosphere, hot, humid air is lighter (less dense) than hot, dry air  A molecule of water vapor (H 2 O) weighs appreciably less than a molecule of either nitrogen (N 2 ) or oxygen (O 2 )  Still, it indeed does feel thick and heavy, related to perception and effective temperature.

53.  Standards for a Cooperative Station thermometer: ◦ Placed in a shelter 2 m above ground ◦ Shelter must be painted white ◦ Doors must open to the north (in the N. Hemisphere) ◦ Vented sides ◦ Placed on a grassy area where possible

54. (photo from surfacestations.org)

55.  Generally good siting; station has been in same location for 100+ years Orland, California (photo from surfacestations.org)

56.  Not so good! Marysville, California (photo from surfacestations.org)

57. Now most stations have automated equipment which uses electronic means

58.  http://128.194.168.16/ http://128.194.168.16/