biomes
Chapter 39: Biomes
List of Biomes
Tundra
Taiga
Desert
Chaparral
Grassland
Tropical Savanna
Tropical Rainforest
Temperate Deciduous Forest
Temperate Evergreen Forest
Mountain Zones
Polar Ice
Learning Objectives (Chapter 39, Sections 39.1 – 39.3)
Explain the major climate patterns found on the planet.
Identify the geographical location of terrestrial biomes.
Describe the main characteristics of the terrestrial biomes, including:
Tropical rainforests
Temperate forests
Taiga
Tundra
Tropical savanna
Temperate grassland
Desert
Mediterranean shrubland
Polar ice
Definition of Biomes
A biome is defined as a major type of ecosystem that is characterized by a specific climate and species composition.
Reference: Section 39.1, Figure 37.1
Climate vs. Weather
Weather: The conditions of the atmosphere over a short period of time.
Climate: How the atmosphere behaves over a long period of time and space.
Characteristics:
Can change within minutes or hours (weather).
Average regional weather pattern observed over decades (climate).
Example of Weather vs. Climate
Average temperatures throughout the year (30-year normal average):
Demonstrated via a temperature graph showing seasonal variability for January through December.
Characteristics of Climate
Important characteristics used to define climate include temperature and rainfall.
Example:
Spring: cool and rainy
Summer: hot and humid
Primary Producers in Biomes
Primary producers include organisms like plants and phytoplankton, which produce the food that sustains other organisms in the biome.
Reference: Section 39.1, Figure 39.1
Abiotic Factors Influencing Species Composition
Abiotic factors that significantly impact ecosystems include:
Light
Moisture
Temperature
Nutrient availability
Oxygen availability
Salinity
Fire
Important to understand how these factors affect primary producers, subsequently impacting the entire food web.
Ecosystem Diversity
Variations in climate result in different ecosystems across the Earth.
Reference: MODIS Oceans Group, NASA Goddard Space Flight Center, Section 39.2, Figure 39.3
Influence of Seasonality on Climate
The tilt of the Earth causes different seasons, which are opposite in the two hemispheres.
Near the equator, the sun's position explains long days and warm temperatures year-round.
Conversely, poles experience short days and colder temperatures year-round.
Reference: Section 39.2, Figure 39.2
Air Circulation Patterns
Air circulation influences climate by determining moisture levels in various regions.
Warm water evaporates near the equator, rises, forms clouds, and precipitates over tropical areas.
Dry air descends around 30 degrees latitude, leading to desert formation.
Reference: Section 39.2, Figure 39.4
Midlatitudes vs. Polar Latitudes
Near 60 degrees latitude: Warm air rises, releasing precipitation over midlatitudes (temperate biomes).
Cold, dry air remains over polar biomes.
Reference: Section 39.2, Figure 39.4
Impact of Ocean Currents on Climate
Ocean currents, both warm and cool, significantly impact coastal climates.
Example: Cold water currents along the west coast of North America vs. warmer currents on the east coast.
Reference: Section 39.2, Figure 39.5
Effect of Mountains on Climate
Mountains influence surrounding climates in two key ways:
Higher elevations are cooler, impacting temperature.
Mountains block winds, causing one side to be wet and the opposite side (rain shadow) to be dry.
Reference: Section 39.2, Figure 39.6
Characteristics of Terrestrial Biomes
Terrestrial biomes possess distinctive communities.
Temperature and moisture are crucial in determining the dominant plant species.
Vegetation influences the biodiversity of organisms within each biome.
Reference: Section 39.3, Figure 39.8
Descriptions of Major Terrestrial Biomes
Tropical Rainforest
Characterized as warm and wet with the highest species diversity of all terrestrial biomes.
Current threats include global deforestation, affecting water and carbon cycles.
Reference: Section 39.3, Figures 39.8, 39.9
Temperate Forests
Features warm summers, cool winters, and consistent rainfall.
Common flora: deciduous trees that shed leaves in autumn and coniferous evergreens.
Geographical range: large areas between 30 and 60 degrees North latitude.
Reference: Section 39.3
Taiga (Boreal Forest)
Environment is cold with relatively dry conditions.
Characterized by long, harsh winters lasting over six months, resulting in a short growing season.
Limited moisture in winter months as water may be frozen.
Flora mainly consists of evergreen trees, with only a few species of mammals and birds staying year-round.
Reference: Section 39.3, Figures 39.8, 39.11
Tundra
Defined by very cold temperatures and minimal moisture.
Animals possess thick fur due to extreme cold.
Features a frozen layer (permafrost) beneath the topsoil that restricts vegetation to small plant species.
Reference: Section 39.3, Figures 39.8, 39.11
Polar Ice
A biome characterized by extreme cold, dryness, and winds throughout the year.
Features distinct differences between the Arctic and Antarctic regions.
Arctic: a thin ice layer covering the Arctic Ocean.
Antarctic: a substantial landmass covered by thick ice.
Both polar regions exhibit interactions with water, possessing characteristics of both terrestrial and aquatic biomes.
Phytoplankton serve as the primary producers in this biome.
Reference: Section 39.3, Figure 39.17
Tropical Savanna
Describes a warm environment with distinct wet and dry seasons.
Characterized by sparse trees and shrubs, with a dominance of perennial grasses and drought-resistant flora (palms, acacias).
Commonly inhabited by herds of grazing animals which play a significant role in this ecosystem.
Fire plays a crucial role in maintaining savanna health by promoting the growth of fire-adapted flora, preventing overgrowth, and aiding nutrient cycling.
Reference: Section 39.3, Figures 39.8, 39.12
Temperate Grassland
Exhibits a moderately moist climate characterized by hot summers and cold winters.
Vegetative landscape predominantly features wind-pollinated grasses, with minimal tree presence.
Large herbivorous grazers are common within these ecosystems.
Reference: Section 39.3, Figures 39.8, 39.13
Desert
Both cold and hot deserts share a common trait of being arid, receiving less than 20 ext{ cm} of precipitation annually.
Typically located at 30^{ ext{°}} North and South latitudes or in rain shadows of high mountains.
Soil types are low in organic content.
Flora adapted to water storage, with a prevalence of nocturnal animals.
Reference: Section 39.3, Figures 39.8, 39.14
Examples of desert flora and fauna:
Fennec fox
Desert beetle
Lappet-faced vulture
Cacti
Various shrubs and grasses
Mediterranean Shrubland (Chaparral)
Characterized by hot, dry summers and cool, moist winters, making it prone to fire during the summer months due to low humidity.
Vegetation is comprised of fire-resistant, drought-tolerant plants.
Common fauna includes jack rabbits, mule deer, and coyotes.
Reference: Section 39.3, Figures 39.8, 39.15