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Chapter 5 Ecosystems and the Physical Environment

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Matter moves between ecosystems, biotic & abiotic environments, and organisms. Unlike energy ... Exosphere (500km and up) Outermost layer ... – PowerPoint PPT presentation

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Title: Chapter 5 Ecosystems and the Physical Environment


1
Chapter 5Ecosystems and the Physical Environment
2
Overview of Chapter 5
  • Biogeochemical Cycles
  • Solar Radiation
  • The Atmosphere
  • The Global Ocean
  • Weather and Climate
  • Internal Planetary Processes

3
Biogeochemical Cycles
  • Matter moves between ecosystems, biotic abiotic
    environments, and organisms
  • Unlike energy
  • Biogeochemical cycling involves
  • Biological, geologic and chemical interactions
  • Five major cycles
  • Carbon, Nitrogen, Phosphorus, Sulfur and Water
    (hydrologic)

4
The Carbon Cycle
5
The Nitrogen Cycle
6
The Phosphorus Cycle
7
The Sulfur Cycle
8
The Water (Hydrologic) Cycle
9
Solar Radiation
  • Sun provides energy for life, powers
    biogeochemical cycles, and determines climate
  • 69 of incoming solar radiation is absorbed by
    atmosphere and earth
  • Remainder is reflected
  • Albedo
  • The reflectance of solar energy off earths
    surface
  • Dark colors low albedo
  • Forests and ocean
  • Light colors high albedo
  • Ice caps

10
Temperature Changes with Latitude
  • Solar energy does not hit earth uniformly
  • Due to earths spherical shape and tilt

Equator (a) High concentration Little Reflection
High Temperature
Closer to Poles (c) Low concentration Higher
Reflection Low Temperature
From (a) to (c)
In diagram below
11
Temperature Changes with Season
  • Seasons determined by earths tilt (23.5)
  • Causes each hemisphere to tilt toward the sun for
    half the year
  • Northern Hemisphere tilts towards the sun from
    March 21- September 22 (warm season)

12
The Atmosphere
  • Invisible layer of gases that envelopes earth
  • Content
  • 21 Oxygen
  • 78 Nitrogen
  • 1 Argon, Carbon dioxide, Neon and Helium
  • Density decreases with distance from earth
  • Shields earth from high energy radiation

13
Atmospheric Layers
  • Troposphere (0-10km)
  • Where weather occurs
  • Temperature decreases with altitude
  • Stratosphere (10-45km)
  • Temperature increases with altitude- very stable
  • Ozone layer absorbs UV
  • Mesosphere (45-80km)
  • Temperature decreases with altitude

14
Atmospheric Layers
  • Thermosphere (80-500km)
  • Gases in thin air absorb x-rays and short-wave UV
    radiation very hot
  • Source of aurora
  • Exosphere (500km and up)
  • Outermost layer
  • Atmosphere continues to thin until converges with
    interplanetary space

15
Atmospheric Circulation
  • Near Equator
  • Warm air rises, cools and splits to flow towards
    the poles
  • 30NS sinks back to surface
  • Air moves along surface back towards equator
  • This occurs at higher latitudes as well
  • Moves heat from equator to the poles

16
Surface Winds
High
  • Large winds due in part to pressures caused by
    global circulation of air
  • Left side of diagram
  • Winds blow from high to low pressure
  • Right side of diagram

Low
High
Low
High
Low
High
17
Coriolis Effect
  • Earths rotation influences direction of wind
  • Earth rotates from East to West
  • Deflects wind from straight-line path
  • Coriolis Effect
  • Influence of the earths rotation on movement of
    air and fluids
  • Turns them Right in the Northern Hemisphere
  • Turns them Left in the Southern Hemisphere

18
Coriolis Effect
  • Visualize it as a Merry-Go-Round (see below)

19
Global Ocean Circulation
  • Prevailing winds produce ocean currents and
    generate gyres
  • Example the North Atlantic Ocean
  • Trade winds blow west
  • Westerlies blow east
  • Creates a clockwise gyre in the North Atlantic
  • Circular pattern influenced by coriolis effect

20
Global Ocean Circulation
Westerlies
Trade winds
21
Position of Landmasses
Large landmasses in the Northern Hemisphere help
to dictate ocean currents and flow
Very little land in the Southern Hemisphere
22
Vertical Mixing of Ocean
23
Ocean Interaction with Atmosphere- ENSO
  • El Niño-Southern Oscillation (ENSO)
  • Def periodic large scale warming of surface
    waters of tropical eastern Pacific Ocean
  • Alters ocean and atmospheric circulation patterns
  • Normal conditions- westward blowing tradewinds
    keep warmest water in western Pacific
  • ENSO conditions- trade winds weaken and warm
    water expands eastward to South America
  • Big effect on fishing industry off South America

24
ENSO Climate Patterns
25
Weather and Climate
  • Weather
  • The conditions in the atmosphere at a given place
    and time
  • Temperature, precipitation, cloudiness, etc.
  • Climate
  • The average weather conditions that occur in a
    place over a period of years
  • 2 most important factors temperature and
    precipitation
  • Earth as many climates

26
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27
Rain Shadows
  • Mountains force humid air to rise
  • Air cools with altitude, clouds form and
    precipitation occurs (windward side)
  • Dry air mass moves down opposite leeward side of
    mountain

28
Tornadoes
  • Powerful funnel of air associated with a severe
    thunderstorm
  • Formation
  • Mass of cool dry air collides with warm humid air
  • Produces a strong updraft of spinning air under a
    cloud
  • Spinning funnel becomes tornado when it descends
    from cloud
  • Wind velocity up to 300mph
  • Width ranges from 1m to 3.2km

29
Tropical Cyclone
  • Giant rotating tropical storms
  • Wind gt119km per hour
  • Formation
  • Strong winds pick up moisture over warm surface
    waters
  • Starts to spin due to Earths
  • rotation
  • Spin causes upward spiral
  • of clouds
  • Damaging on land
  • High winds
  • Storm surges

30
Internal Planetary Processes
  • Layers of the earth
  • Lithosphere
  • Outermost rigid rock layer composed of plates
  • Asthenosphere
  • Lower mantle comprised of hot soft rock
  • Plate Tectonics- study of the processes by which
    the lithospheric plates move over the
    asthenosphere
  • Plate Boundary- where 2 plates meet
  • Common site of earthquakes and volcanoes

31
Plates and Plate Boundaries
32
Types of Plate Boundaries
  • Convergent Plate Boundary-2 plates move together
    (may get subduction)
  • Divergent Plate Boundary-2 plates move apart

33
Types of Plate Boundaries
  • Transform Plate Boundary- 2 plates move
    horizontally in opposite, parallel directions

34
Earthquakes
  • Caused by the release of accumulated energy as
    rocks in the lithosphere suddenly shift or break
  • Occur along faults
  • Energy released as seismic wave
  • Focus- the site where the earthquake originates
    below the surface
  • Epicenter- located on the earths surface,
    directly above the focus
  • Richter scale and the moment magnitude scales are
    used to measure the magnitude

35
Tsunami
  • Giant undersea wave caused by an earthquake,
    volcanic eruption or landslide
  • Travel gt 450mph
  • Tsunami wave may be 1m deep in ocean
  • Becomes 30.5m high on shore
  • Magnitude 9.3 earthquake in Indian Ocean
  • Triggered tsunami that killed over 230,000 people
    in South Asia and Africa

36
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