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Climate and Terrestrial Biodiversity

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Presentation on theme: "Climate and Terrestrial Biodiversity"— Presentation transcript:

1 Climate and Terrestrial Biodiversity
Chapter 7

2 7.1

3 The Earth Has Many Different Climates
Weather – local area’s short-term temperature, precipitation, humidity, wind speed, cloud cover, etc. Measured over hours or days

4 The Earth Has Many Different Climates
Climate – area’s general pattern of atmospheric or weather conditions Measured over long periods of time

5 The Earth Has Many Different Climates
Climate - varies over different parts of the earth Uneven heating of the earth’s surface by the sun Rotation of the earth on its axis Properties of air, water, and land

6 Earth’s Atmosphere Tropics – air is warm Equator – 30o N/S

7 Polar regions – air is cold
Earth’s Atmosphere Polar regions – air is cold 60o - 90o N/S

8 Convection Currents Up-and-down movement of air due to temperature differences

9 Convection Currents Rule: Hot air rises and cold air sinks. Equator
Hot air rises and heads toward the poles

10 Convection Currents Rule: Hot air rises and cold air sinks. Poles
Cold air rushes in to fill the space at the equator

11 Figure 6.5

12 Wind Horizontal movement of air

13 Convection Currents + Earth’s Rotation
Equator

14 Coriolis Effect Earth rotates and causes circulating air to be deflected Causes things thrown in straight line to move to the right or left (depends on hemisphere) If the Earth did not rotate and remained stationary, the atmosphere would circulate between the poles (high pressure areas) and the equator (a low pressure area) in a simple back-and-forth pattern. But because the Earth rotates, circulating air is deflected. Instead of circulating in a straight pattern, the air deflects toward the right in the Northern Hemisphere and toward the left in the Southern Hemisphere, resulting in curved paths. This deflection is called the Coriolis effect. It is named after the French mathematician Gaspard Gustave de Coriolis ( ), who studied the transfer of energy in rotating systems like waterwheels. (Ross, 1995). Continue to 2 3 4  (top) 

15 Imagine a merry-go-round…

16 Suppose you (represented by the dark blue circle) and a friend (represented by light blue circle) are on a merry go round. You gently toss a ball towards your friend The ball doesn’t actually get there!

17 Coriolis Effect Summary
Causes moving objects on Earth to follow curved paths Northern Hemisphere – follows a path to the right of its intended target Southern Hemisphere – follows a path to the left of its intended target Acts on all moving objects

18 Your Turn! Deflected Activity Global Wind Patterns

19 Prevailing Winds Major wind patterns on the Earth Direction caused by:
Convection currents Earth’s rotation from west to east Air pressure

20 Global Air Circulation

21 Wind Belts Doldrums Between 5 degrees North and 5 degrees South latitude Winds are calm

22 Wind Belts Trade Winds Historically: Used by ships traveling between Europe and the Americas 5o-30o North and South of the Equator

23 Trade Winds Northern Hemisphere
Warm air around the equator rises and flows north toward the pole Earth’s rotation deflects air toward the right

24 Trade Winds Southern Hemisphere Similar pattern
Winds blow from the southeast toward the northwest Descend near 30 degrees South latitude

25 Wind Belts Westerly Winds
Remaining air (air that does not descend at 30 degrees North or South latitude) continues toward the poles

26 Wind Belts Polar Easterlies
Cool air sinks and moves towards the equator Air is deflected by Earth’s rotation

27

28 Winds Drive Surface Ocean Currents!
Global winds drag on the water’s surface Cause water to move and build up in the direction that the wind is blowing

29 Natural Capital: Generalized Map of the Earth’s Current Climate Zones

30 Your Turn! Coastal Upwelling

31 Climate and Biomes

32 Biotic and Abiotic Factors
Biological (living) influences on an organism within an ecosystem Predators Prey Abiotic Factors Physical (non-living) factors that shape ecosystems Temperature Precipitation Humidity

33 What is a biome? Terrestrial community that covers a large area and is characterized by certain soil and climate conditions Particular assemblages of plants and animals.

34 Biomes Variations in plants and animals help different species survive under different conditions in different biomes. Tolerance - ability to survive and reproduce under conditions that differ from their optimal conditions

35 The Major Biomes 60°N 30°N 0° Equator 30°S 60°S Temperate grassland
Tropical rain forest Temperate grassland This map shows the locations of the world’s major biomes. Other parts of Earth’s surface are classified as mountains or ice caps. Each biome has a characteristic climate and community of organisms. Temperate forest Northwestern coniferous forest Tropical dry forest Desert Temperate woodland and shrubland Boreal forest (Taiga) Tropical savanna Tundra Mountains and ice caps

36 Biomes Large terrestrial regions characterized by similar climate, soil, plants, and animals Location irrelevant

37 Biomes Not uniform; consist of a mosaic of patches with different biological communities

38 Generalized Effects of Elevation and Latitude on Climate and Biomes

39 Natural Capital: Average Precipitation and Average Temperature as Limiting Factors

40 Your Turn! Biome Jigsaw Biome Bags

41 Global Air Circulation, Ocean Currents, and Biomes

42 Energy Transfer by Convection in the Atmosphere
Heat is absorbed and released more slowly by water than by land Moderate weather and climate of nearby lands

43 Biomes and Climate The climate of a region is an important factor in determining which organisms can survive there. Temperature and precipitation can vary over small distances. Microclimate - the climate in a small area that differs from the climate around it

44 The Earth’s Surface Features Affect Local Climates
Cities Microclimates More haze and smog Higher temperatures Lower wind speeds Causes Bricks, asphalt, and concrete absorb and hold heat Buildings block wind flow

45 The Earth’s Surface Features Affect Local Climates
Mountains Rain shadow effect: moist air blowing inland is forced upward; cools and expands Loses most of its moisture as rain or snow on the windward slope Air dries and warms over leeward side; increases ability to hold moisture and dries ecosystem

46 Climate Terms Tropical – warm; receives direct or nearly direct sunlight year round Desert - dry Temperate – moderate

47 Climate Graphs of Three Types of Deserts

48 Climate Graphs of Tropical, Temperate, and Cold Grasslands

49 Chaparral Vegetation in Utah, U.S.

50 Climate Graphs of Tropical, Temperate, and Cold Forests

51 Stratification of Specialized Plant and Animal Niches in a Tropical Rain Forest

52 Major Human Impacts on Terrestrial Ecosystems

53 Tundra

54 Taiga See Clip

55 Tropical Rain Forest

56 Temperate Forest

57 Temperate Grassland

58 Desert

59 Chaparral


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