The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow .

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Chapter 43, Problem 4SA

Summary Introduction

Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

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Answer 2

Question

Chapter 43, Problem 4SA

Summary Introduction

Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

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Answer 3

Question

Chapter 43, Problem 4SA

Summary Introduction

Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

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Answer 4

Question

Chapter 43, Problem 4SA

Summary Introduction

Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

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Answer 5

Chapter 43, Problem 4SA

Summary Introduction

Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

Answer 6

Chapter 43, Problem 4SA

Summary Introduction

Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

Answer 7

Chapter 43, Problem 4SA

Summary Introduction

Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

Answer 8

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Answer 11

Ch. 43 - Prob. 1SA Ch. 43 - Which latitude will have the most hours of...Ch. 43 - Prob. 3SA Ch. 43 - Prob. 4SA Ch. 43 - Prob. 5SA Ch. 43 - ____________ have a deep layer of humus-rich...Ch. 43 - Prob. 7SA Ch. 43 - Prob. 8SA Ch. 43 - Prob. 9SA Ch. 43 - Prob. 10SA

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow .

Solution Summary: The author explains that the correct answer is option a. Warm air with high moisture content arises from the ocean and when it encounters mountain ranges, it rises higher to cross them.

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Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

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Chapter 43 Solutions

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow .

Solution Summary: The author explains that the correct answer is option a. Warm air with high moisture content arises from the ocean and when it encounters mountain ranges, it rises higher to cross them.

Concept explainers

Videos

Introduction: The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.

Want to see the full answer?

Chapter 43 Solutions

Introduction:

The cooling and condensing of warm, moist air when it rises higher near the mountain peaks, resulting in rainfall on one side (windward side) and scanty or nil rainfall on the other side (leeward side) of the mountain, which is called a rain shadow.