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Terrestrial Biodiversity . AP Environmental Science. Climate and Life on Land. Different climates lead to different communities of organisms, especially vegetation. Biomes – large terrestrial (land) regions characterized by similar climate, soil, plants, and animals.
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Terrestrial Biodiversity AP Environmental Science
Climate and Life on Land • Different climates lead to different communities of organisms, especially vegetation. • Biomes – large terrestrial (land) regions characterized by similar climate, soil, plants, and animals. • Each biome contains many ecosystems whose communities have adapted to differences in climate, soil, and other environmental factors.
Weather or Climate? • Weather: physical conditions of the lower atmosphere that occur over hours or days. • Temperature • Precipitation • Humidity • Cloud coverage • Etc. • Climate: long term differences in temperature and precipitation • 3 decades (30 years) to 1000s of years • This distinction is important when discussing climate change/global warming. Long term data should be used. Climate matters because it determines where humans and other species can survive.
Different Climates on Earth • Tropical – areas near the equator, receives the most intense sunlight • Polar – areas near the poles, receives the least intense sunlight • Temperate - between tropical and poles • Climate varies in different parts of Earth because of an uneven distribution of heat and precipitation around the world by air and ocean currents.
Factors That Determine How Air Circulates • Uneven heating of the Earth’s surface by the sun • Air is heated more at the equator where the sun strikes directly, strikes the poles at an angle and covers a larger area. • Tropical = hot • Polar = cold • Temperate = hot and cold seasons • More solar radiation = more evaporation = more condensation = more precipitation
Factors That Determine How Air Circulates • Rotation of Earth on its axis. • Spins faster at the equator than the poles • Hot air collects, rises and moves north & south to cooler areas • Cells- huge areas distinguished by direction of air movement • Prevailing Winds – different directions of air movement • Blow continuously, distribute heat & moisture around Earth, drive ocean currents
Factors That Determine How Air Circulates • Properties of air, water, & land • Sun evaporates water transfer of heat from oceans to atmosphere creation of convection cells vertical circulation of air, heat, moisture
Ocean Currents • Mass movement of surface water in the oceans • Created by heat from the sun and changes in water density • Warm currents are shallow and less salty • Cold currents are deeper and salty • Driven by prevailing winds and Earth’s rotation • Interrupted by continents
Air, Water, & Climate • Air circulation patterns, prevailing winds, the configuration of continents, and ocean currents form 6 giant cells (3 above/3 below the equator) • These lead to the uneven distribution of heat & moisture, resulting in varying climates, and biomes • Deserts, grasslands, forests, etc.
Earth’s Surface & Microclimates • Climate near Large Bodies of Water • Water absorbs /releases heat slower than land • Oceans/Lakes moderate weather & climate of nearby land by absorbing solar radiation • Climates of Cities • Bricks, concrete, asphalt absorb & hold heat • Building block wind flow • Vehicles & heating/cooling systems release large amounts of heat & pollutants • All these cause more haze/smog increase temperatures decrease in wind speeds
Earth’s Surface & Microclimates • Climate near Mountains • Mountains interrupt the flow of prevailing winds/storms forcing them upwards • Upward = cooling moisture condenses/falls on the windward slope • Dry air passes over mountain and flows down the leeward slope & warms • Rain shadow effect formation of deserts (Death Valley)
Greenhouse Gases Keep Us Warm • Greenhouse gases: water, carbon dioxide, nitrous oxides, methane present in the lower atmosphere. • Natural Greenhouse effect: natural warming effect of the troposphere. • Allows life to be sustained on Earth • Human acts are increasing the amount of greenhouse gases in the atmosphere by: • Burning fossil fuels • Clearing forests (deforestation) • Growing crops/raising cattle
Fronts • Front: a boundary between two air masses with different temperatures and densities. • Warm Front • Warm air advances on cool air warm air is less dense at slide atop the cool air forms condensation (clouds) clouds thicken & descend precipitation • Causes cloudy skies and drizzle • Cold Front • Cold air advances on warm air cold air is more dense and wedges below the warm air produces tall thunderbolt clouds • Causes high winds and thunderstorms but leaves clear skies and cooler temps
Jet Streams • Jet streams: rapidly flowing air current (strong winds) that move east to west in a wavy pattern. • Located at the top of the troposphere • Strong influence on weather patterns
Atmospheric Pressure • Atmospheric Pressure- caused by the collision of high speed molecules in the air • Mostly oxygen & nitrogen • Greater at the Earth’s surface because they are squeezed under the air above them • High – air mass with high pressure • Cool dense air that slowly descends becoming warmer • Causes clear skies and fair weather • Low – air mass with low pressure • Warm air with low density rises and cools condensation clouds form precipitation • Causes cloudy, stormy weather
Other Weather Terms • Dew point – temperature at which condensation takes place • Condensation nuclei – particles of dust, smoke, sea salts, or volcanic ash that serve as surfaces for rain to form on • Upwelling – upward movement of ocean water, mixes the upper levels and lower levels of sea water • Upper levels – warm, phytoplankton • Lower levels – nutrient rich
ENSO • El Nino – Southern Oscillation (ENSO) – the weakening or reversal of the tropical trade winds that normally blow east to west (Pacific Ocean) • Causes drought in Australia, S. East Asia & storms in W. United States • Can be tracked • La Nina – reverse of ENSO, normal conditions • More Atlantic hurricanes, colder winter in Canada and NE United States, rains SE Asia
Extreme Weather • Tornadoes – over land • Form when large, dry cold front runs into a mass of warm, humid air • Tropical Cyclones – over ocean • Hurricanes (Atlantic), Typhoons (Pacific) • Form when low pressure cells grow over warm tropical waters
The most important factors in a biome are temperature and precipitation. • Biomes tend to converge around latitude lines on the globe.
Deserts • The evaporation is greater than the precipitation (usually less than 25 cm/year). • Covers 30% of the earth.
Types of Desert Biomes • Variations in annual temperature (red) and precipitation (blue) in tropical, temperate and cold deserts.
Grasslands • The rainfall is erratic & fires are common. It has & shrubs that are good for grazing animals.
Types of Grassland Biomes • Variations in annual temperature (red) and precipitation (blue) in tropical, temperate and cold deserts.
Savanna • The tropical & subtropical grassland. • It is warm all year long with alternating wet & dry seasons.
Chaparral • Temperate Grasslands • These are coastal areas. Winters are mild & wet, w/ summers being long, hot, & dry. • Chaparral has a moderate climate but its dense thickets of spiny shrubs are subject to periodic fires
Prairies • Temperate Grassland • The cold winters and hot dry summers have deep and fertile soil that make them ideal for growing crops and grazing cattle.
Tundra • Polar Grassland • Covers 10% of earth’s land. Most of the year, these treeless plains are bitterly cold with ice & snow. It has a 6 to 8 week summer w/ sunlight nearly 24 hours a day. • covered with ice and snow except during a brief summer.
Forests • Forests have enough precipitation to support stands of trees and are found in tropical, temperate, and polar regions.
Taiga (evergreen coniferous forest) • Just south of the tundra (northern part of N. America), it covers 11% of earth’s land. Its winters are long, dry & cold. Some places have sunlight 6 to 8 hours a day. The summers are short and mild, w/ sunlight 19 hours a day.
Taiga (evergreen coniferous forest) • High-elevation islands of biodiversity • Often have snow-covered peaks that reflect solar radiation and gradually release water to lower-elevation streams and ecosystems.
Taiga (evergreen coniferous forest) • Consist mostly of cone-bearing evergreen trees that keep their needles year-round to help the trees survive long and cold winters
Tropical Rainforest • Near the equator. It has warm temperatures, high humidity & heavy rainfall. • Tropical rain forests have heavy rainfall and a rich diversity of species. • Found near the equator. • Have year-round uniformity warm temperatures and high humidity
Temperate Rain Forests • Coastal areas support huge cone-bearing evergreen trees such as redwoods and Douglas fir in a cool moist environment
Temperate Deciduous Forest • It has moderate temperatures, long, warm summers, cold winters &lots of rain. Trees include oaks, hickory, maple, and beech. • Most of the trees survive winter by dropping their leaves, which decay and produce a nutrient-rich soil.
Forest Ecosystems • Forests = ~ 30% of Earth’s land surface • Types of Forests: • Old-growth/Primary Forests: uncut or regenerated forest that has not been seriously disturbed • Very diverse • Second-growth Forests: resulting from secondary ecological succession • Tree plantation/tree farm/commercial forest: managed forests containing one or two species of trees, all the same age • Less diversity
Natural Capital of Forests Ecological Services Economic Services Fuel wood Lumber Pulp for paper Mining Livestock grazing Recreation Jobs • Support energy flow and chemical cycling • Reduce soil erosion • Absorb/release water • Purify water/air • Influence climate • Store atmospheric carbon • Provide wildlife habitats
Threats to Forests • Clearing for agriculture, livestock grazing, timber, and urban development • Conversion of diverse forests to tree plantations • Damage from off-road vehicles • Pollution of forest streams • Forest fires • Insects • Climate change
Clear-Cutting • Selective Cutting: older trees cut singularly or in small groups • Clear-Cutting: removing all trees from an area • Advantages: higher timber yields, maximum profits, reforest with fast growing trees, good for trees needing full/moderate sunlight • Disadvantages: reduces biodiversity, destroys/fragments habitats, increases water pollution, flooding, erosion, eliminates recreational value.
Forest Fires • Surface fires: burn undergrowth and leaf litter on forest floor • Kills seedlings, small trees, mature trees and most animals escape • Helps prevent more serious fires • Free up valuable nutrients • Release seeds from cones • Control disease & insects • Crown fire: extremely hot fire that goes from treetop to treetop, burning whole trees • Destroy most vegetation/wildlife, increase soil erosion, burn human structures • Not major long term threat, promotes secondary succession • Serious short term threats- habitat loss, increased CO2 & other pollutants
Deforestation • Temporary for permanent removal of large areas of forest • Decreased soil fertility from erosion • Runoff leads to more soil in aquatic ecosystems • Premature extinction of specialized species • Loss of habitat • Regional climate change • Increase of CO2 in atmosphere • Acceleration of flooding
Destruction of Tropical Forests • Roads • Fires • Settler Farming • Cash crops • Cattle ranching • Logging • Tree plantation