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8.3 Terrestrial Biomes

Distribution of biomes based on climate (what controls temp and rainfall)

A biome is a large geographic region characterized by a distinct climate and vegetation, which in turn determines the types of animals that can live there. Biomes are classified into two broad categories: terrestrial biomes (occur on land) and aquatic biomes (include marine and freshwater).

The major terrestrial biomes on Earth are distinguished by their typical climate (the long-term pattern of temperature and precipitation in a region). Annual totals and fluctuations of precipitation and temperature variation on a daily and seasonal basis affect the kinds of vegetation and animal life that can exist in broad geographical regions. Since a biome is defined by climate rather than location, the same biome can occur in geographically distinct areas with similar climates.

Some parts of the planet, such as Antarctica, Greenland, and high mountain ranges, are covered by permanent ice and glaciers. These areas experience extreme cold and receive very little precipitation. While they support limited life, they are not typically classified as biomes due to their harsh, uninhabitable conditions.

What Controls Climate on Earth?

Climate is the most important factor in determining the types of organisms that can live in a particular biome. Several key factors work together to control Earth’s climate patterns:

Latitude

Latitude refers to how far a location is from the equator. The equator receives direct sunlight year-round, resulting in consistently warm temperatures and high solar energy. As you move toward the poles, sunlight strikes Earth at a lower angle, spreading the energy over a larger area and reducing the intensity of heat. This creates a gradient of climate zones: tropical near the equator, temperate in the mid-latitudes, and polar near the poles. These broad temperature zones are the foundation for the distribution of biomes across the globe. Figure – https://commons.wikimedia.org/wiki/File:Oblique_rays_02_Pengo.svg

Earth’s Tilt and the Seasons

Earth is tilted at an angle of about 23.5 degrees relative to its orbit around the Sun. Because Earth tilts on its axis, different parts of the planet get different amounts of sunlight throughout the year. This tilt creates the seasons. In the Northern Hemisphere, summer happens when the North Pole leans toward the Sun. Days are longer, and sunlight is more direct. In winter, the North Pole tilts away from the Sun, leading to shorter days and weaker sunlight. These seasonal shifts affect temperature and rainfall, which in turn influence plant growth and animal activity. https://www.flickr.com/photos/121935927@N06/13598174453/in/photostream/

Precipitation and Global Air Circulation Patterns

Precipitation is a key factor in determining the types of vegetation and animals that can survive in a region. Global air circulation patterns help explain why some areas are consistently wet while others are dry. Warm air rises near the equator, cools as it rises, and releases moisture—creating the wet conditions typical of tropical rainforests. Around 30° latitude, the now-dry air descends, warming and absorbing moisture from the land, which leads to the formation of deserts. These large-scale wind and pressure systems, such as the trade winds and westerlies, help distribute heat and moisture around the planet and are essential in shaping the world’s biomes. Can you find an image like this that shows how the moist air rises and pulls in the dry air (ref document)

Proximity to Water

Water has a high heat capacity, meaning it warms and cools more slowly than land. As a result, areas near oceans or large lakes tend to have milder climates with smaller temperature fluctuations. Coastal regions often receive more precipitation and experience less extreme seasonal changes than inland areas at the same latitude.

Other Influences on Climate

There are many other fators that also play a role on global climate patterns. Altitude affects temperature—higher elevations are generally cooler than lower ones. Topography, such as mountain ranges, can block air masses and create rain shadows, leading to dry conditions on one side of a mountain. Additionally, local wind patterns, cloud cover, and human activities can influence regional climates.   Can you find a figure like this but nicer to show a “rain shadow” – causes a desert on the dry side of the mountain… https://en.m.wikipedia.org/wiki/Precipitation#/media/File%3ASteigungsregen.jpg This is the version that is in my Pearson textbook for comparison:

Major Terrestrial Biomes

Content combined from 2 sources: https://uen.pressbooks.pub/biology1010revision/chapter/terrestrial-biomes/ https://opencurriculum.org/5380/terrestrial-biomes/ (used as reference for types of animals observed).

Tropical Rainforests
Savannas
Deserts
Chaparral
Temperate Grasslands
Temperate Forests
Boreal Forests
Arctic Tundra

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