chapter 10 lesson 4

16
Chapter 10, Lesson 4 Water Vapor and Humidity water vapor humidity relative humidity transpiration cloud formation thermal convection meteorologist

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Page 1: Chapter 10 Lesson 4

Chapter 10,

Lesson 4

Water

Vapor and

Humidity

water vapor

humidity

relative humidity

transpiration

cloud formation

thermal

convection

meteorologist

Page 2: Chapter 10 Lesson 4

water vapor - water in its gas form is

water vapor. If you can see it, it’s

not really water vapor!

Page 3: Chapter 10 Lesson 4

humidity – the level of moisture in

the air; the amount of water

vapor in the air

Page 4: Chapter 10 Lesson 4

relative humidity – is when you

compare how much water vapor

is in the air to how much it

COULD hold

Page 5: Chapter 10 Lesson 4

dew point – point when the air is

completely saturated with

moisture and can hold no more.

Page 6: Chapter 10 Lesson 4

transpiration –watery vapor

passed through a membrane or

pores in a plant

Page 7: Chapter 10 Lesson 4

transpiration –watery vapor

passed through a membrane or

pores in a plant

Page 8: Chapter 10 Lesson 4

cloud formation – the way clouds form

Page 9: Chapter 10 Lesson 4

cloud formation – the way clouds

form

Page 10: Chapter 10 Lesson 4

cloud formation – the way clouds

form

Page 11: Chapter 10 Lesson 4

cloud formation – the way clouds

form

Page 12: Chapter 10 Lesson 4

cloud formation – the way clouds

form

Page 13: Chapter 10 Lesson 4

thermal – a rising air current

caused by heating the Earth’s

surface (radiation)

Page 14: Chapter 10 Lesson 4

thermal – heated air that rises

thermals help these birds to soar,

they help gliders soar, too. They

push air into the atmosphere, that

cools and forms clouds

Page 15: Chapter 10 Lesson 4

convection – when relatively

warm air is raised into the

atmosphere, often cooling and

forming clouds

Page 16: Chapter 10 Lesson 4

meteorologist – a scientist who

deals with the atmosphere,

including weather and climate