WEATHER AND CLIMATE Chapter 2 UNDERSTANDING WEATHER Section

  • Slides: 31
Download presentation
WEATHER AND CLIMATE Chapter 2 UNDERSTANDING WEATHER

WEATHER AND CLIMATE Chapter 2 UNDERSTANDING WEATHER

Section 1 A Water in the Air

Section 1 A Water in the Air

the condition of the atmosphere at a particular time and place weather

the condition of the atmosphere at a particular time and place weather

the continuous movement of water from water sources into the air, onto land, into

the continuous movement of water from water sources into the air, onto land, into and over ground, and back to the water sources water cycle

the change of state from a liquid to a vapor evaporation

the change of state from a liquid to a vapor evaporation

the process by which plants release water vapor into the air through their leaves

the process by which plants release water vapor into the air through their leaves transpiration

the change of state from a gas to a liquid condensation

the change of state from a gas to a liquid condensation

solid or liquid water that falls from the air to the Earth precipitation

solid or liquid water that falls from the air to the Earth precipitation

Cold Weather Precipitation

Cold Weather Precipitation

water, usually from precipitation, that flows across land collects in rivers, streams, and eventually

water, usually from precipitation, that flows across land collects in rivers, streams, and eventually the ocean runoff

the amount of water vapor or moisture in the air humidity

the amount of water vapor or moisture in the air humidity

As water evaporates, the humidity of the air _____. increases

As water evaporates, the humidity of the air _____. increases

Humidity can cause a _____ day. bad hair

Humidity can cause a _____ day. bad hair

As temperature decreases, the air’s ability to hold moisture _____. decreases

As temperature decreases, the air’s ability to hold moisture _____. decreases

Warmer air can hold _______ more water vapor than cooler air.

Warmer air can hold _______ more water vapor than cooler air.

the amount of moisture the air contains compared with the maximum amount it can

the amount of moisture the air contains compared with the maximum amount it can hold at a particular temperature relative humidity Actual Amount Compared to Maximum Amount Relative Humidity of 5/10 =50%

Calculate Relative Humidity: • The air actually holds 8 grams of water vapor at

Calculate Relative Humidity: • The air actually holds 8 grams of water vapor at a temperature that could hold 32 grams of water vapor 25% • The air could hold 50 grams of water vapor but actually holds 40 80% Hint: Divide the amount in the air by the amount it can hold. Then multiply by 100.

instrument used to measure wind speed anemometer

instrument used to measure wind speed anemometer

an instrument used to measure relative humidity psychrometer

an instrument used to measure relative humidity psychrometer

Using the following slide, determine the relative humidity when: • the dry-bulb reading is

Using the following slide, determine the relative humidity when: • the dry-bulb reading is 16˚C with a wet-bulb difference of 7

Relative Humidity (in Percentage) Difference Between Wet-Bulb Reading and Dry-Bulb Reading ˚C 1 2

Relative Humidity (in Percentage) Difference Between Wet-Bulb Reading and Dry-Bulb Reading ˚C 1 2 3 4 5 6 7 8 0 81 64 46 29 13 2 84 68 52 37 22 7 4 85 71 57 43 29 16 6 86 73 60 48 35 24 11 8 87 75 63 51 40 29 19 8 10 88 77 66 55 44 34 24 15 12 89 78 68 58 48 39 29 21 14 90 79 70 60 51 42 34 26 16 90 81 71 63 54 46 38 30 18 91 82 73 65 57 49 41 34 20 91 83 74 66 59 51 44 37

Using the following slide, determine the relative humidity when: • the dry-bulb reading is

Using the following slide, determine the relative humidity when: • the dry-bulb reading is 4˚C and the wet-bulb reading is 10˚C. HINT: 1 st Find the difference! 10 – 4 = 6

Relative Humidity (in Percentage) Difference Between Wet-Bulb Reading and Dry-Bulb Reading ˚C 1 2

Relative Humidity (in Percentage) Difference Between Wet-Bulb Reading and Dry-Bulb Reading ˚C 1 2 3 4 5 6 7 8 0 81 64 46 29 13 2 84 68 52 37 22 7 4 85 71 57 43 29 16 6 86 73 60 48 35 24 11 8 87 75 63 51 40 29 19 8 10 88 77 66 55 44 34 24 15 12 89 78 68 58 48 39 29 21 14 90 79 70 60 51 42 34 26 16 90 81 71 63 54 46 38 30 18 91 82 73 65 57 49 41 34 20 91 83 74 66 59 51 44 37

When air holds all the water it can hold at a given temperature, it

When air holds all the water it can hold at a given temperature, it is said to be _____. saturated

Saturated air has a relative humidity of ____%. 100

Saturated air has a relative humidity of ____%. 100

If the amount of water vapor in the air stays the same, the relative

If the amount of water vapor in the air stays the same, the relative humidity _____ decreases as the temperature rises.

Before condensation can occur, the air must be saturated and cooled. ____

Before condensation can occur, the air must be saturated and cooled. ____

the temperature to which air must cool to be completely saturated dew point

the temperature to which air must cool to be completely saturated dew point

Before it can condense, water vapor must have a _______ surface on which it

Before it can condense, water vapor must have a _______ surface on which it can condense.

Fun and Games • Bill Nye the Science Guy on “The Water Cycle” •

Fun and Games • Bill Nye the Science Guy on “The Water Cycle” • Part 1 • Part 2 • Part 3 • Magic School Bus “Wet All Over” • Water Cycle Animation

Fun and Games • Brain POP Video, Activities, and Quiz on Humidity User Name:

Fun and Games • Brain POP Video, Activities, and Quiz on Humidity User Name: tabernaclesd_2 Password: brainpop • Water Cycle • Vocabulary Games