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Special Topics Lecture
Ch. 5 Climate and Biomes Special Topics Lecture These lectures contain copyrighted images that are provided in the teacher materials for Friedland/Relyea Environmental Science for AP Textbook. By using these lectures, you guarantee that you have legal access to these images or that you have replaced the copyrighted images with images that you have the rights to use.
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Words you should know Abiotic Biotic Food Web Anthropomorphic Climate
Latitudinal Longitudinal
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Albedo The higher the albedo of a surface, the more sun that is reflected and the less heat stored The lower the albedo of a surface, the more sun that is absorbed and the more heat stored.
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VERY IMPORTANT: What causes the seasons?
The ANGLE of the sun’s rays. Direct sunlight = summer Direct = more sunlight in a smaller area more heat stored Indirect sunlight = winter Indirect = sunlight spread over larger area less heat stored
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Coriolis Effect The spinning of the earth creates
Different wind speeds at different latitudes (faster at equator, slower at poles) clockwise winds in the northern hemisphere counter clockwise winds in the southern hemisphere This movement is called the Coriolis Effect. Watch: N. hemisphere - CLOCKWISE S. hemisphere - COUNTER - CLOCKWISE
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Coriolis and Convection cells
Without the Coriolis Effect, air would travel in two large cells. The warm air at the equator would rise and move toward the poles. As it moved to the poles, it would cool and sink, then move back to the equator along land, warming as it moved. DOES NOT ACTUALLY HAPPEN With the Coriolis Effect, air still travels from the equator toward the poles, but due to the wind patterns, the 2 cells are broken into 6 global cells. Warm air rises in each cell and cools as it travels through the atmosphere, then sinks and warms as it travels across the land.
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Climate Changes with Latitude
Starting at the equator and moving to the poles it generally: gets colder and drier There are exceptions particularly for rainfall!
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Biomes – observe latitude similarities
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Climate Changes with Elevation/Altitude
As you go up in elevation: Less soil and less nutrients less plants Less oxygen lower air pressure thinner atmosphere less organisms Temperatures decreases More UV rays – limits plant growth
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Ocean Currents Transport nutrients and heat all over the globe
Driven mostly by: Wind/Coriolis Temperature gradients (colder water sinks) THERMO Salinity gradients (saltier water sinks) HALINE See other factors in HW Also called the Ocean Conveyor belt
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Upwelling Occur when ocean currents pull water from the deep ocean up to the surface Upwellings pull cold, nutrient rich water up to the surface Good for fishing: increases NPP as nutrients are often a limiting factor
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Gyres Direction driven by the Coriolis Effect and the continents
5 gyres that spin clockwise in the N. hemisphere and counter clockwise in the S. hemisphere Redistribute heat and nutrients Upwellings occur along the west coasts of continents
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Ocean Currents There are two types of Ocean Currents:
1. Surface Currents / Surface Circulation These waters make up about 10% of all the water in the ocean. These waters are the upper 400 meters of the ocean. Driven mostly by wind 2. Deep Water Currents These waters make up the other 90% of the ocean move around the ocean basins by density and gravity. The density difference is a function of different temperatures and salinity These deep waters sink into the deep ocean basins at high latitudes where the temperatures are cold enough to cause the density to increase.
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El Nino Southern Oscillation
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El Nino Southern Oscillation (ENSO)
El Nino – warming event in the tropical Pacific Ocean Caused by weak/no trade winds blowing WEST The upwelling along the west coast of the Americas stops Occurs in cycles every 2-7 years La Nina – cooling event in the tropical Pacific Ocean The opposite end of the spectrum as an El Nino Trade winds and upwelling is strong Both extremes cause extreme weather events globally
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ENSO effects – El Nino During an El Nino event
Warmer ocean temps in the Pacific Warmer and wetter in the western Americas from So. Cal south (Warmer and dryer in the Northwest US during winter and warmer and wetter in the summer) Suppresses hurricane activity in the Atlantic ocean Major declining in fishing populations during an El Nino Drought in the western Pacific and Australia
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ENSO effects – La Nina During a La Nina event
Pacific ocean temps are colder than normal Droughts along the west coast of the Americas (more snow in northwest US) Active hurricane season in the Atlantic More rain in the Western Pacific and Australia
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Microclimate – Rain shadow effect
Topography, water bodies and other local features create local climate conditions known as microclimate. For example mountains commonly result in high rainfall on the windward side and low rainfall in the rain shadow of the leeward side. We see this in LA: rainier on our side of the mountain – desert on the other side
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Biomes
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Terrestrial Biomes Terrestrial biomes are classified by precipitation and temperature patterns The warmest wettest biome is the tropical rainforest Coldest dry biome is the tundra The warmest dry biome is the subtropical desert The temperature and precipitation patterns determine the type of vegetation and animals which are specifically adapted to the climate.
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Forested Biomes All forested biomes receive a sufficient amount of rainfall to support trees (which require quite a bit of rain) Community of plants and animals are typically distributed in various layers: Emergent layer of branches above the canopy Canopy of full–grown trees Subcanopy of tree saplings Understory of herbaceous plants and shrubs
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Tropical Rain Forest Climate - Warm year-round, wet and humid year round Located - near equator, specifically around the ITZC NPP - High Decomposition – rapid Soil - thin, nutrient poor and acidic because decomposition rates are so rapid Limiting Factors – light, soil nutrients Biodiversity – highest on land Vegetation – a wide variety, but dominated by broadleaf evergreen trees Adaptations include: waxy leaves to keep extra water out, leaves shaped to allow water to drip off Animals – wide variety with a diverse and complex food web Adaptations include: Camouflage and specialization Major Human impact – deforestation for farming
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Tropical Seasonal Forest / Savanna
Climate - Warm year round with a rainy season and a dry season Located – south of the equator between 30-60o NPP - High Decomposition – moderate Soil – fairly fertile Limiting Factors – water, fire maintained Biodiversity – varies based on rainfall with scattered trees and tall grasses Vegetation – forests in the wetter areas, grasses in less wet areas Adaptations include: losing leaves during dry season to conserve water, fire maintained community Animals – wide variety particularly grazers and predators Adaptations include: Nocturnal hunting during dry season, migration for water, burrowing to avoid water loss, specialized hunting and defensive traits Major Human impact - deforestation for farming
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Subtropical Desert Climate - Warm and dry year round
Located – 30o above and below the equator NPP – Very low Decomposition – very slow Soil – almost non-existent Limiting Factors – water, nutrients Biodiversity – varies based on rainfall with scattered trees and tall grasses Vegetation – sparse and generally low to the ground with shrubs, cacti and succulents Adaptations include: no leaves, waxy coatings and water storage to conserve moisture, deep or very spread out roots to reach water, spines and protection from grazers Animals – wide variety particularly grazers and predators Adaptations include: Nocturnal animals, hibernation to escape heat, water conserving (dry feces, moisture absorbing skin) and avoid overheating (reflective skin, burrowing) Major Human impact – off road vehicles destroy delicate soil crust and threaten organisms
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Temperate Rain Forest Climate – moderate temperatures year-round and seasonal rainfall (foggy summers) Located – in the Northwest US/Canada, southwest Argentina and the east coast of Australia NPP – high Decomposition – slow due to cool temps Soil – nutrient poor and acidic Limiting Factors – light and soil nutrients Biodiversity – moderate Vegetation – large coniferous trees, ferns and mosses Adaptations include: climbing or hanging to access sunlight, leaf shape to allow water to fall Animals – wide variety including slugs, wolves and deer Adaptations include: camouflage to hide, migration, and hibernation Major Human impact – Logging and tree farming
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Temperate Seasonal Forest (Deciduous Forest)
Climate –wet year round with 4 seasons Located – 30-60o latitude NPP – high Decomposition – rapid Soil – fertile due to decomposing leaf litter Limiting Factors – sunlight, cold winters Biodiversity – high Vegetation –mostly deciduous trees with multiple lower layers Adaptations include: trees lose leaves in winter to conserve energy, Animals –wide variety and diverse food web Adaptations include: hibernation, migration or food storage for winter, camouflage Major Human impact – Deforestation for agriculture and logging
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Woodland / Shrubland (Chaparral)
Climate – mild temperatures with a rainy and dry season Located – 30-60o latitude near bodies of water NPP –moderate Decomposition – moderate Soil – nutrient poor (rain leaches nutrients) Limiting Factors – rainfall in summer, low temps in winter, fire maintained Biodiversity – moderate Vegetation – scrub-like plants that are similar to desert plants, succulents and drought tolerant trees Adaptations include: storing water, waxy coatings, deep roots, leaves turn brown or fall off to conserve water, fire adapted Animals – variety of small animals like lizards, snakes, deer, owls, and some larger predators like mountain lions Adaptations include: nocturnal, live close to the ground, camouflage, burrowing Major Human impacts – human started fires and fire suppression activities, urbanization
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Temperate Grassland / Cold Desert
Climate – distinct seasons with a rainy and dry season Located –between 30-60o latitude NPP – low Decomposition – rapid Soil – excellent, deep and nutrient dense Limiting Factors – water in summer, cold in winter, fire maintained Biodiversity – moderate (but varies) Vegetation – mostly grasses, tall grasses in wetter areas, low grasses in drier areas Adaptations include: deep roots, fire adapted, Animals – Adaptations include: Major Human impact – agriculture
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Boreal Forest (Taiga, Coniferous Forest)
Climate –cold year round, moderate rain all year Located – around 60o latitude NPP – moderate Decomposition – low Soil – nutrient poor and acidic Limiting Factors – cold, nutrients, light, water Biodiversity – moderate Vegetation – mostly evergreen trees (conifers) Adaptations include: needles to conserve water and energy, chemicals to repel grazers, shaped to allow snow to slide off Animals – grazing animals including moose, bears, bobcats, chipmunks and squirrels Adaptations include: insulating layers of fur or feather, seasonal color changes, migration Major Human impacts – forestry, acid rain, resource exploration, climate change
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Tundra Climate – cold year round, very little rain, but wet in summer (melting) Located – near the poles NPP – low Decomposition – very slow Soil – nutrient depleted, thin and often frozen Limiting Factors – water, sunlight , cold, nutrients Biodiversity – low Vegetation – low growing plants Adaptations include: shallow roots for frozen soil, grow close together for warmth, grow underneath snow Animals – birds and mammals in summer, wolves, foxes and bears year round Adaptations include: migration and hibernation for winter, summer and winter “coats”, Major Human impacts – climate change, resource exploration (oil, gas, etc)
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Aquatic Biomes Aquatic biomes are classified by water type (fresh or salty), water depth (deep or shallow) and water flow rates (fast or slow) Organisms are specifically adapted to the conditions in each biome and would not survive elsewhere Many aquatic habitats and species are very sensitive to change Aquatic biomes provide major ecological services including water purification, storm water absorption, breeding grounds for fish and birds, as well as human enjoyment of their beauty
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Benthic Zone The bottom of aquatic ecosystems
Generally where the nutrients are Benthic organisms are specifically adapted to the conditions there Highest productivity is found where the benthic zone is shallow (sunlight and nutrients are available)
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Riparian Zone The vegetative zone that runs along the edges of the aquatic biome Highly productive ecosystems Important for filtering pollutants, moderating temperatures, absorbing runoff, conserving soil and providing habitat Managing an aquatic biome also involves managing the riparian zone
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Lakes Lakes are deep, but have slow flow rates, so they are prone to the accumulation of pollution or drops in DO The biodiversity in lakes depends on nutrient availability Too few nutrients and the lake cannot support a diverse food web Too many nutrients and the lake ages quickly and becomes clogged with algae (eutrophication)
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Cultural Eutrophication
The slow aging process during which a lake, estuary, or bay evolves into a bog or marsh and eventually disappears Accelerated by excess nitrogen and phosphates which stimulate algal growth fertilizer runoff (N & P) detergents (P) animal waste (N & P) Results in less dissolved oxygen (DO) causing fish kills and loss of biodiversity
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Eutrophication
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Rivers Rivers carry water and nutrients over land and eventually deposit both into the ocean Rivers get shallower and more nutrient rich as the flow downstream River deltas are fertile due to the nutrients carried from upstream, but are prone to flooding Rivers can also carry pollution long distances Rivers are subject to dams and water diversion
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Coral Reefs – description
Coral reefs are created by tiny animals called polyps that secrete calcium carbonate around themselves. When they die, the empty crust is left behind forming the physical structure of the reef They grow very slowly and are easily damaged Reefs have very specific requirements: Warm, shallow, clear waters Extremely sensitive to changes in temp, salinity, pollution, turbidity, etc Any change in these conditions causes coral bleaching or the death of the coral reef This leaves the white shell behind (hence bleaching) Often caused by increased temps and/or runoff that clouds the water
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Coral Reefs – services Ecological Economic
Moderate climate by storing CO2 Natural barrier to protect coastlines from storms Provide habitat for a huge variety of organisms (1/4 of all marine species) Cycle nutrients Produce about 10% of global fish catch Important breeding groups Provide jobs and building materials Eco-tourism, research and education Fish collection (aquariums) Coral Reefs are valued at $260,000 - $1.6 million per square mile
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Wetlands Wetland – A general term applied to land areas which are seasonally or permanently waterlogged Found all over the world from poles to equator Ex: marsh, swamp, estuary, etc
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Wetland services Ecological Economic Purify water/water source
Provide important breeding grounds for fish and birds Filter and detoxify pollutants Purify water Important habitat for plants, insects, amphibians, reptiles, birds, fish, and mammals Groundwater recharge Store carbon (sea grasses especially) Purify water/water source Control erosion Important breeding ground for commercially valuable fish and timber Recreational opportunities: bird watching, hiking, photography, boating and hunting Protection against flooding and storms Water quality services - $1.6 billion per year, Flood control - $3-4 billion a year,
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Estuaries Areas where freshwater and saltwater ecosystems meet
Usually when a river or streams flows into the ocean Unique environment with a mixture of salty and fresh water (brackish water) Conditions change throughout the daily and seasonally with sunlight, tides, mix of water, etc
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Estuary services Ecological Economic
Provide important breeding grounds for fish and birds Filter and detoxify pollutants Purify water Important habitat for plants, insects, amphibians, reptiles, birds, fish, and mammals Extremely productive ecosystems Purify water/water source Important breeding ground for commercially valuable fish and shellfish Recreational opportunities: bird watching, hiking, photography, boating and hunting Protection against flooding and storms
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Mangrove Swamps Found along tropical and subtropical coasts
Trees have submerged roots which anchor sand and sediment protecting coastline Filter toxic pollutants, excess plant nutrients, sediments, and other pollutants. Reduce storm damage by absorbing waves and storing excess water produced by storms and tsunamis. Provide food, habitats and nursery sites for many aquatic species.
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Intertidal Zone Conditions change daily as the sun rises and sets and as the tide comes in and out each day Creates tide pools daily Organisms must be able to survive the harsh and changing conditions Organisms live under or attached to rocks or have shells to protect them from waves and changing water conditions
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Open Ocean Open ocean has a low NPP and is nutrient poor
Layers are determined by light availability
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Threats to Aquatic Biomes
Development leading to habitat destruction Filling in of wetlands to make them buildable Diversion of water for human uses Reduces water flow downstream Dams interrupt the water cycle flooding some areas and reducing water flow in others Channelization for flood control destroys benthic habitats Pollution and run-off including fertilizer, pesticides, heavy metals and acid mine drainage Reduces biodiversity Climate change sea level rise and ocean temp changes Coral bleaching and loss of costal biomes
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