Presentation is loading. Please wait.

Presentation is loading. Please wait.

Weather ©Mark Place, 2009-2010 www.LearnEarthScience.com.

Similar presentations


Presentation on theme: "Weather ©Mark Place, 2009-2010 www.LearnEarthScience.com."— Presentation transcript:

1 Weather ©Mark Place,

2 weather basics The Sun The uneven heating of the Earth’s Surface.
Where does the energy for weather originate? The Sun The uneven heating of the Earth’s Surface.

3 In the US, the general direction that weather systems move is toward
weather basics In the US, the general direction that weather systems move is toward the northeast ESRT page 14

4 dewpoint are measured in
Station Models Please go to page 13 of the ESRTs Temperature and dewpoint are measured in degrees _______ F

5 .. Cloud Cover Temperature 76 138 Wind Direction & Speed -30\
Current Weather 55 Dewpoint Barometric Trend Barometric Pressure

6 Add a 9 or 10 in front to fit on the scale
Barometric Pressure 138 Add a decimal between the last two digits 13.8 Add a 9 or 10 in front to fit on the scale (ranges from to ) 1013.8 Less than 500: ADD A 10 Greater than 500: ADD A 9

7 Evaporation Rates Relative Humidity Temperature Surface Area

8 as temperature increases, the rate of evaporation
Evaporation Rates Direct Relationship as temperature increases, the rate of evaporation increases Relative Humidity Temperature Surface Area

9 as surface area increases, the rate of evaporation
Evaporation Rates Direct Relationship as surface area increases, the rate of evaporation increases Relative Humidity Temperature Surface Area

10 as the air becomes more saturated, the rate of evaporation
Evaporation Rates Indirect Relationship as the air becomes more saturated, the rate of evaporation decreases Relative Humidity Temperature Surface Area

11 What natural process cleans the atmosphere? precipitation Rain Snow Hail

12 Cloud Formation

13 Cools to the dewpoint Expands Warm Air Rises

14 Clouds are likely to form when:
The air is saturated and rising The temperature is at the dewpoint Condensation nuclei are available

15

16 As air temperature increases Warm air holds more water.
the air can hold more water Warm air holds more water.

17 lower due to evaporation
Sling Psychrometer Dry bulb measures air temperature Wet bulb temp is lower due to evaporation

18 Using the charts on page 12 of the ESRTs, calculate the relative
humidity and dew point using the following information. Dry Bulb Wet Bulb Difference Dew Point Relative Humidity (%) 14 10 4 20 5 30 19 18 56

19

20

21 Using the charts on page 12 of the ESRTs, calculate the relative
humidity and dew point using the following information. Dry Bulb Wet Bulb Difference Dew Point Relative Humidity (%) 14 10 4 20 5 30 19 18 56 6 60 15 12 58 23 7 55 13 5 9

22 Relative Humidity vs Air Temperature Indirect Relationship as temp increases RH decreases

23 As dew point increases, the amount of moisture in the air

24 dewpoint get closer together, the probability of precipitation
As temperature and dewpoint get closer together, the probability of precipitation INCREASES

25 probability of precipitation?
Which has the greatest probability of precipitation?

26 Pressure and Wind ©Mark Place,

27 What instrument is used to measure:
wind speed air pressure anemometer barometer [ORIGIN from Greek anemos ‘wind’] [ORIGIN from Greek baros ‘weight’]

28 AIR PRESSURE

29 How are winds named? The direction from which they come

30 What causes wind? differences in pressure

31 WIND

32 Which pressure gradient would result in greater wind velocity?

33

34 measurements using the chart
Convert the following measurements using the chart on page 13 of the ESRTs. 29.73 997 30.18 994

35 Wind blows from areas of
to areas of high pressure low pressure

36 Draw the relationship between air pressure and air density.

37 This is because the air is Therefore, clouds CANNOT form.
In a high pressure area, air will (rise, sink) because the air is (less, more) dense. This is because the air is (cold, warm) and (rises, sinks). Therefore, clouds CANNOT form.

38 This is because the air is
In a low pressure area, air will (rise, sink) because the air is (less, more) dense. This is because the air is (cold, warm) and (rises, sinks). Therefore, clouds are LIKELY to form.

39 Correctly draw the direction of wind flow
around both a high and a low pressure area in the NORTHERN HEMISPHERE.

40 counterclockwise wind direction
low pressure high pressure warm or cold air air rising or sinking clouds or no clouds clockwise or counterclockwise wind direction winds toward or away from the center warm cold rising sinking clouds no clouds counter clockwise clockwise toward away

41 Correctly label on each diagram where the
On the diagrams below, label which one represents a land breeze and which represents a sea breeze. Correctly label on each diagram where the high and low pressure areas would be found.

42 Sea Breeze (daytime) H L
On the diagrams below, label which one represents a land breeze and which represents a sea breeze. Correctly label on each diagram where the high and low pressure areas would be found. Sea Breeze (daytime) H L

43 Land Breeze (night time) L H
On the diagrams below, label which one represents a land breeze and which represents a sea breeze. Correctly label on each diagram where the high and low pressure areas would be found. Land Breeze (night time) L H

44 What’s the relationship
between wind and waves? direct (the stronger the wind, the bigger the waves)

45 45°N 45°S 75°N 20°N Using the chart on page 14, state the prevailing
wind direction for each latitude below: 45°N 45°S 75°N 20°N

46

47 45°N 45°S 75°N 20°N southwest northwest northeast northeast
Using the chart on page 14, state the prevailing wind direction for each latitude below: 45°N 45°S 75°N 20°N southwest northwest northeast northeast

48 Is air rising or sinking
at the equator?

49 Is air rising or sinking
at 30°N?

50 ©Mark Place, Air Masses

51 AIR MASS What's the definition? A large body of air with similar characteristics throughout

52 Air masses are classified based on their
and amount of temperature moisture

53 Air masses get their characteristics based on
where they form

54 continental dry maritime moist Tropical warm Polar cold Arctic
The abbreviations used to classify air masses use the following letters: c, m, T, P, and A. For each letter, describe its property: Word Means c m T P A continental dry maritime moist Tropical warm Polar cold Arctic very cold

55 What would their characteristics be?
mT cP warm and moist cold and dry

56 High or Low Pressure? mT cP H L

57

58

59 What type of air mass would form over each area? Please label. cA mP mP cP cT mT mT mT

60 World Air Mass Source Regions

61

62

63 cP air mass dry, cool air High Pressure Area mT air mass warm, moist air Low Pressure Center

64 Fronts ©Mark Place,

65 a boundary (interface)
FRONTS a boundary (interface) between air masses

66 The Rule: triangles and bumps always point in the direction the front is moving

67 a cold front moving south
an occluded front a stationary front with cold air on the south side a warm front moving north a stationary front with warm air on the south side

68 cP cP Warm front Cold front mT Warm Cold Cold

69

70 Cold Fronts Animation #1

71

72

73

74 Warm Fronts Animation #1

75

76

77

78

79 Using the Words below, complete the paragraph.
COLD FRONTS: Using the Words below, complete the paragraph. 15 degrees, cold, cold, colder, colder, cooler, clouds, drier, hail, rain, thunderstorms, tornadoes, towering clouds form, warm, warmer Passage of a cold front: Cold fronts occur when a air mass replaces a air mass.  In a cold front the air follows the warm air, and, because air is denser, pushes air out of its way, forcing the warm air to rise. The lifting warm air mass becomes , and start to form. Precipitation at cold fronts are usually heavier although less extensive (50-70 km) and less prolonged. The reason for this is that the uplift of warm air there is stronger due to the undercutting of cold air, so , and , , and can occur. The air behind a cold front is noticeably and than the air ahead of it. When the cold front passes through, temperatures can drop more than within the first hour.

80 WARM FRONTS: Using the Words below, complete the paragraph air, cirrus clouds, cold, colder air mass, in front of them, lifts up, move slowly, settling over the cold front, warm, warmer, warmer and more humid Warm fronts: Warm fronts occur, when a air mass approaches a The warmer air and over the colder air. fronts are usually more gentle than fronts, , gently and moving it out of the way. Precipitation at warm fronts are usually less heavy although more extensive ( km), than at the cold fronts. The behind a warm front is warmer and more moist than the air ahead of it. Warm fronts bring more steady, lighter rain or snow ………………………, which can last from a few hours to several days. When a warm front passes through, the air becomes noticeably than it was before. The first signs of the warm front are the , followed by the cirrostratus, altostratus, nimbocumulus and stratocumulus types of clouds.

81 Hurricanes Lightning Tornadoes
©Mark Place,

82 HURRICANES

83

84

85

86

87

88

89

90 Footage

91

92

93 LIGHTNING

94

95

96

97 Tornado Safety

98

99

100

101

102


Download ppt "Weather ©Mark Place, 2009-2010 www.LearnEarthScience.com."

Similar presentations


Ads by Google