Climate
Earth Science - Middle School
Earth's Climate
Multimedia Lesson
Climate and Its Causes
Presentation
Climate Zones and Biomes
Presentation
The Tropical Zone
Presentation
The Temperate Zone
Presentation
The Polar Zone
Presentation
Climate Change
Presentation
Global Warming
Presentation
Ozone depletion
Presentation
Atmosphere Overview
Presentation
Layers of the Atmosphere
Presentation
Earth's Seasons
Virtual Lab
Biomes
Interactive
Climate
Study Guide
Earth`s Climate
Quiz
Climate
Quiz
Earth`s Climate
Flash Cards
Climate
Flash Cards
Earth`s Climate
Worksheet
Climate
Worksheet
Earth`s Climate
Game
Climate
Game
Earth`s Climate
Vocabulary List
Climate
Vocabulary List
Climate and Its Causes
Flip Chart
Seasons
Flip Chart
Climate Zones and Biomes
Flip Chart
The Tropical Zone
Flip Chart
The Temperate Zone
Flip Chart
The Polar Zone
Flip Chart
Climate Change
Flip Chart
Global Warming
Flip Chart
Ozone Depletion
Flip Chart
Earth’s Climate Vocabulary Review
Flip Chart
Study Guide Climate
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CLIMATE What Is Climate? The condition of the atmosphere at a specific time in a specific place is known as the weather. Climate is the average weather of a region over an extended period of time. A number of global and local, natural and human-made factors affect climate. The Causes of Climate The two most important factors that determine the characteristics of climate are temperature and precipitation. Temperature and precipitation, in turn, are affected by a number of other factors. One key factor affecting climate is latitude. Because the Earth is a globe, the sun’s rays hit the equator more directly than they do near the poles. This means the sun’s radiation is more concentrated near the equator and the same energy is more spread out nearer the poles. A second factor is that the Earth is tilted at 23.5 degrees on its axis as it rotates around the sun. As it does, the Northern and Southern hemispheres are either pointing toward or away from the sun’s rays. Consequently, lands near the equator have smaller temperature fluctuations throughout the year. The climate is predictably warm and humid. By contrast, as one travels north and south of the equator, the lands experience more dramatic temperature swings throughout the year, including hot summers and cold winters. The poles, because they receive the most indirect radiation from the sun, are exceptionally cold throughout the year and have alternating periods of six months of sunlight and six months of darkness (hence the saying, “Land of the midnight sun.”) Climates are also affected by winds. Various regions of the Earth have winds that blow mostly from one direction. They have an important impact on the region’s climate because they influence temperature and moisture in the area. These are called prevailing winds. Prevailing winds that travel across water are more humid as they pick up water vapor. Prevailing winds that travel across broad expanses of land tend to be very dry. Geographical features, like mountains, also affect climate. There are two ways that mountains affect climate. • First, the climate at the top of the mountain is colder than at the foot of the mountain because the atmosphere is less dense and therefore cannot hold as much heat. © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at www.NewPathLearning.com.
• Second, mountains affect the distribution of precipitation (rain and snow). When moisture-laden clouds come to a mountain, they are pushed upward. The altitude of mountains causes air to rise and then cool. When it cools, rain or snow comes out of the air mass. The air mass is now dry as it descends the other side of the mountain. The dry air now absorbs moisture. The result is a desert environment. This is called the rain shadow effect. Another factor affecting climate is ocean currents. The oceans’ surface currents help distribute temperatures around the globe. Cool polar surface currents move toward the equator bringing cooler temperatures to southern regions. By contrast, warm tropical surface currents from the equator carry warmer temperatures to northern regions. Lesson Checkpoint: Name two ways that mountains affect climate. Climate Regions and Types of Climate Climate zones are geographical regions of relatively similar climate with similar temperatures and precipitation. Latitude defines these zones. The climate zones between the equator and 23.5 degrees North and South are tropical zones. The climate zones between 23.5 degrees and 66.5 degrees North and South of the equator are described as temperate zones. The climate zones between 66.5 degrees North and South and the poles are the polar zones. Temperature and precipitation are highest at the equator and both gradually decrease toward the poles. © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at www.NewPathLearning.com.
Climates are usually described not only by their average temperature and precipitation, but also by the flora and fauna that particular climate supports. The term biome refers to a large geographical region, the climate found there and the plants and animals that live in that region. Many of the world’s different biomes are described below. The biome characterized by low precipitation (0 to 25 cm/yr), soil poor in organic matter and average temperatures between 60 and 120 degrees F is the tropical desert. A similar biome is the temperate desert. Temperate deserts and tropical deserts are very similar in regard to plant and animal life, annual precipitation and soil quality. They differ in average temperatures. Temperate deserts can be much cooler, as low as 30 degrees F. The biome characterized by annual precipitation of 100 cm/yr, average temperatures of 80 to 90 degrees F, tall grasses and scattered trees, and animals like gazelles, lions and elephants is the tropical savanna. The prairies of North America have the most fertile soil of all of the biomes. Average annual precipitation is about 60 cm/year. Temperatures vary widely from very hot summers to very cold winters (upwards of 100 degrees F in the summer and 20 below zero F in the winter.) The land supports large grazing animals like bison. This biome is called the temperate grassland. © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at www.NewPathLearning.com.
The biomes known as the tundra and taiga belong to the polar zone. The tundra is marked by low temperatures and very short growing seasons. Tree growth here is limited. Instead, small shrubs and small plants like grasses, lichens and mosses are abundant. The Arctic tundra is the large region indicated in this map near the North Pole. Alpine tundra is found high in mountainous regions. Just south of the tundra is the biome called the taiga. It is marked by coniferous forests, acidic soil, and relatively low annual precipitation of about 50 cm/yr. Moose, elk, wolves and bears roam this biome. The boundary between the tundra and the taiga where tree growth ends is called the tree line. A temperate forest is a biome marked by very rich soil, thick woods of maple, cherry and oak trees. It is inhabited by birds, squirrels, owls and other woodland creatures. As the name indicates, this biome is found in temperate regions where temperatures and precipitation allow rich deciduous forest growth. Lesson Checkpoint: Describe one biome. © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at www.NewPathLearning.com.
What causes climate change? Climate change is both a natural phenomenon as well as one created by human activity. Geologic evidence has shown that there have been a number of glacial and interglacial periods. During glacial periods, dramatic decreases in global temperatures have allowed the advance of massive ice sheets from the North Pole well down the North American continent. During interglacial periods, global warming melted the glaciers causing the leading edge of the glaciers to retreat back to more northern regions. Glacial and interglacial periods are episodes that occur within ice ages. There are a number of theories explaining the cause or causes of ice ages. The Milankovitch Theory says that changes in the Earth’s orbit around the sun and changes of the tilt of the Earth on its axis combine to cause periods of glaciation and other periods of warming. (This theory was proposed by the Yugoslavian scientist Milutin Milankovitch.) Another theory proposes that the ice ages occurred because a single landmass called Pangaea was positioned near the South Pole where large sheets of ice moved over the land. When Pangaea broke apart, the landmasses moved closer to the equator, which ended the glaciation. This could explain glaciation in the southern continents, but not those in the northern continents. It is also possible that periods of unusually high volcanic activity put so much ash into the atmosphere that significant amounts of the sun’s radiation was blocked out, causing dramatic drops in global temperatures and, therefore, causing periods of glaciation. These are all theories. Studies continue and more theories will most likely be developed as our knowledge of Earth history increases. It is always possible, if not probable, that a combination of these factors each had a role to play in the ice ages. The ice ages indicate that the Earth has experienced periods of global cooling and global warming. Global Warming Theories Many scientists believe that we are now in another period of global warming. This time, however, human activity may be a cause in this trend. Energy from the sun comes to the Earth as electromagnetic radiation. This energy causes materials to heat up. The heat created at the Earth’s surface is held near the surface by a natural phenomenon called the Greenhouse Effect. We tend to think of the greenhouse effect as a phenomenon caused by the emission of massive amounts of greenhouse gases created by burning © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at www.NewPathLearning.com.
fossil fuels. The greenhouse effect, however, is the natural process by which gases hold heat near the Earth’s surface. Without this effect, Earth would not be habitable because it would be too cold. However, the concern is that the creation of massive amounts of greenhouse gases from the burning of fossil fuels could be enhancing this natural phenomenon and causing more dramatic global warming than otherwise would occur. There are a number of factors influencing global warming. Gases like carbon dioxide from burning fossil fuels (oil, natural gas and coal) accumulate in the atmosphere. This is compounded by massive deforestation which removes trees and plants that consume carbon dioxide in the process of photosynthesis. Greenhouse gases are also produced by volcanoes, decomposing plant material (like swamp gases), and other natural sources. Global warming will lead to a number of environmental changes which in turn will dramatically affect climates and biomes all over the world. Some of the evidence that is presently cited as proof of a global warming trend includes the melting polar ice caps, changes in regional weather patterns, and increased regional and global temperatures. Such changes could affect crop growth, lead to expanding desert climates in some regions and increased flooding in other regions. It is expected that the melting polar ice caps will raise the average sea levels globally and flood coastal lands. Lesson Checkpoint: What is the Greenhouse Effect? Ozone and Ozone Depletion The Earth is protected from harmful ultraviolet radiation from the sun by a layer of ozone in the atmosphere. Ozone is a molecule of three oxygen atoms. When ozone forms near the Earth’s surface it is considered pollution and hazardous to human health. But when it forms in the stratosphere, it filters out harmful ultraviolet radiation from the sun. Exposure to ultraviolet radiation is known to be a cause of skin cancer and may also be linked to damage to the eyes. In the 1970’s scientists determined that a type of chemical called chlorofluorocarbons (CFC’s) was destroying the ozone layer and literally leaving a hole in it. Environmental laws were enacted that eliminated production and use of chlorofluorocarbons. Lesson Checkpoint: How does the ozone layer help humans? © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at www.NewPathLearning.com.
Table Of Contents: Earth’s Climate
1. Climate and Its Causes
2.1. What Is Climate?
The weather is the condition of the atmosphere at a specific time and place. The climate is the average weather of a region over an extended period of time. If you travel around the world, you will find many different climates.
2.2. Causes of Climate
Temperature and precipitation are the most important factors that impact climate. Temperature is influenced by latitude, altitude, large bodies of water, and ocean currents. Precipitation is influenced by winds and mountains.
2.3. Latitude Affects Temperature
The latitude of a region affects temperature. The sun’s radiation is most concentrated at the equator, resulting in warm temperatures. In polar regions, temperatures are much colder because the same amount of energy is spread across a larger amount of land.
2.4. Altitude Affects Temperature
Regions that are located at higher altitudes experience cooler temperatures. The air on top of a mountain is much cooler than the air at the base of a mountain because air temperature gets colder as you move to higher elevations in the troposphere.
2.5. Oceans and Lakes Affect Temperature
Oceans and large lakes influence the climate. Water heats and cools more slowly than land, helping moderate the temperature of nearby land. The California coast has mild temperatures due to warm air blowing from the Pacific Ocean.
2.6. Ocean Currents Affect Temperature
The ocean has surface currents that help distribute temperatures around the globe. Polar currents carry cool water toward the equator, and tropical currents carry warm water away from the equator. For example, the Gulf Stream creates warm air temperatures around southern Iceland and significantly impacts the climate of this region.
2.7. Prevailing Wind Affects Moisture
Prevailing winds blow primarily in one direction and influence the moisture in a region. Winds that travel across water are humid because they carry water vapor. Winds that travel across broad regions of land tend to be dry.
2.8. Mountains Affect Precipitation
Mountains play a role in the climate. Moisture-laden clouds that run into mountains are pushed upward. As the clouds cool, rain or snow occurs. When the clouds move down the other side of the mountains, the dry air creates a desert climate. This effect is called a rain shadow.
2.9. Seasons and the Earth’s Tilt
Seasonal weather occurs because the Earth is tilted on its axis as it rotates around the sun. Throughout the year, the Northern and Southern hemispheres will be either pointing toward or away from the sun. Land near the equator has year-round warm and humid climates, while regions further from the equator experience more dramatic temperature changes.
2. Pause and Interact
3.1. Review
Use the whiteboard tools to complete the activity.
3. Climate Zones and Biomes
4.1. Climate Zones
Climate zones are geographic regions with relatively similar temperature and precipitation. The Earth has three major climate zones—tropical, temperate and polar.
4.2. Biomes
The areas within a climate zone can be further divided into biomes. A biome is a large geographic region that is characterized by a particular climate and the organisms that live in this region.
4. The Tropical Zone
5.1. Tropical Zone
The tropical zone extends from the equator to 23.5 degrees in latitude, north and south. Temperatures are typically hot in this zone. The three biomes found in this region include rain forests, savannahs and deserts.
5.2. Tropical Rain Forest
Tropical rain forests have high rainfall and high temperatures throughout the year. Although rain forests are lush, the soil is nutrient-poor because frequent rains wash away the topsoil. More plant and animal species are found here than in any other biome.
5.3. Tropical Savannah and Desert
A tropical savannah is a hot grassland that has a wet and dry season. A savannah covers a large region across central Africa. Tropical deserts are hot and dry. Many desert animals and plants have adapted to live in this extreme environment. The soil is nutrient-poor in both of these biomes.
5. The Temperate Zone
6.1. Temperate Zone
The temperate zone is located between 23.5 and 66.5 degrees latitude, north and south. Although the biomes in the temperate zone experience four distinct seasons, they have a wide variety of temperatures and precipitation. The four biomes include the forest, grassland, chaparral and desert.
6.2. Temperate Forest and Grassland
Temperate forest biomes have plenty of rain and are known for their evergreen and deciduous trees. The soil is fertile due to the dropping and decaying of leaves every year. Temperate grasslands have little rainfall, and very few trees grow in these biomes. This biome has the most fertile soil, and many crops are grown in these areas.
6.3. Temperate Chaparral and Desert
Temperate chaparral regions are cool and wet in the winter and hot and dry in the summer. Primarily short evergreen shrubs grow in the chaparral’s rocky, nutrient-poor soil. The temperate desert has a year-round dry climate and the soil is nutrient-poor. This type of desert biome is hot during the day and cool overnight.
6. The Polar Zone
7.1. Polar Zone
The polar zone extends beyond 66.5 degrees latitude, both north and south. It is the zone with the coldest year-round climate. The tundra and taiga are the two biomes found in this zone.
7.2. Tundra
The tundra has very short growing seasons, with almost 24 hours of light during the summer and 24 hours of dark during the winter. The very top layer of soil will thaw, but remain muddy. All the soil below this is frozen, and is known as permafrost.
7.3. Taiga
The taiga is located south of the tundra, and is characterized by its coniferous forests. The soil is acidic, and few plants grow on the forest floor. The boundary between the tundra and taiga is called the tree line.
7. Pause and Interact
8.1. Review
Use the whiteboard tools to complete the activity.
8.2. Biomes
Follow the onscreen instructions.
8. Climate Change
9.1. Ice Ages
Scientists use geologic evidence to study how the Earth’s climate has changed over time. The Earth has experienced several ice ages, which are periods of cooling that last thousands of years.
9.2. Glacial and Interglacial Periods
The most recent ice age occurred about two million years ago. Throughout an ice age there are episodes called glacial and interglacial periods. Glacial periods experience global cooling and massive ice sheets develop and move south. Interglacial periods experience global warming and the edges of glaciers melt and retreat.
9.3. What Caused the Ice Ages?
Theories that attempt to explain the occurrence of ice ages include the Earth’s changing motion, continental movement due to plate tectonics, volcanic ash in the atmosphere, and the impact of an asteroid hitting the Earth’s surface. A combination of these theories may have influenced climate change over geologic time.
9. Global Warming
10.1. The Earth is Getting Warmer
The Earth is currently in an interglacial period of warming. Many scientists believe that human activity is playing a role in global climate change. An increase in the greenhouse effect could be contributing to warmer temperatures.
10.2. Greenhouse Effect
A natural phenomenon called the greenhouse effect heats the Earth’s surface. This effect occurs when energy from the sun reaches the Earth as electromagnetic radiation and causes material to heat up. Atmospheric gases absorb and re-radiate this heat, keeping it close to the Earth’s surface.
10.3. Increased Atmospheric Carbon Dioxide
The burning of fossil fuels and massive deforestation are both human activities that are contributing to an increase in atmospheric carbon dioxide levels. Increases in carbon dioxide and greenhouse gases enhance the greenhouse effect.
10.4. The Impact of Global Warming
Global warming leads to environmental changes that impact worldwide climates and biomes. Changing regional weather patterns, increasing global temperatures, and melting polar ice caps are evidence of a current global warming trend. These changes may affect crop growth, flooding, desert formation, and a rise in sea level.
10. Ozone depletion
11.1. A Thinning Ozone Layer
The ozone layer in the stratosphere protects the Earth from harmful ultraviolet radiation. In the 1970s scientists noticed a thinning layer of ozone over Antarctica. Human-produced chemicals called chlorofluorocarbons (CFCs) were the primary cause of this ozone depletion.
11.2. Ozone Layer Recovery
Through an international effort, the production and use of CFCs has decreased, but the ozone layer may not recover for many years. This is just one example of how humans and pollution can have a significant effect on the Earth’s atmosphere.
11. Vocabulary Review
12.1. Vocabulary Matching Review
The Earth is currently in an interglacial period of warming. Many scientists believe that human activity is playing a role in global climate change. An increase in the greenhouse effect could be contributing to warmer temperatures.
12. Virtual Investigation
13.1. Earth's Seasons
Seasonal weather varies at different locations on Earth and impacts the climate of a region. Seasons are caused by the tilt of the Earth's axis as it revolves around the Sun. In this virtual investigation you will explore the sunlight's yearly patterns at different locations on Earth. Study the sunlight's patterns and analyze the data about each location to learn more about the relationship of seasons, the Earth's tilt, and the Earth's yearly orbit around the Sun.
13. Assessment
14.1. Earth's Climate
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