Download Global warming & its effects

Survey
yes no Was this document useful for you?
   Thank you for your participation!

* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project

Document related concepts

Marine geology of the Cape Peninsula and False Bay wikipedia , lookup

Anoxic event wikipedia , lookup

Marine debris wikipedia , lookup

Southern Ocean wikipedia , lookup

Tsunami wikipedia , lookup

Marine biology wikipedia , lookup

Ecosystem of the North Pacific Subtropical Gyre wikipedia , lookup

Abyssal plain wikipedia , lookup

Ocean acidification wikipedia , lookup

Indian Ocean wikipedia , lookup

Wind wave wikipedia , lookup

Sea wikipedia , lookup

Global Energy and Water Cycle Experiment wikipedia , lookup

Marine pollution wikipedia , lookup

Arctic Ocean wikipedia , lookup

Effects of global warming on oceans wikipedia , lookup

Marine habitats wikipedia , lookup

Ocean wikipedia , lookup

Physical oceanography wikipedia , lookup

Transcript
Global warming & its effects
 What will be the effect of global warming on glaciers
and the polar icecap?
 What will happen to ocean levels and coastal
communities in our region?
 Read p. 27 and discuss!
The last ice age!
(you think our winters are cold!)
 Last ice age began about 120 000 years ago, and ended
only 11 000 years ago!
 Almost all of Canada was covered by a glacier!
Read pp. 28-30
Solving problems using science
 Can science alone solve problems like global warming?
 Cultural views, societal views, etc. are very important
part of solving problems.
 Questions 1-5, p. 28
 Questions 1-8, p. 35
 Pause and Reflect... p.35
Chapter 2
Exploration of ocean basins
 Read p. 38-46
Ocean basins
 The surface of the ocean floor is as varied as the land.
 The five major oceans, from largest to smallest, are
 the Pacific
 the Atlantic
 the Indian
 the Southern
 the Arctic
 The low points in the oceans are called basins.
 Oceans are vital to life, as they control temperature,
create weather patterns and provide
water for water cycles.
 Basins becoming bigger – demo (p. 41)
Ocean basins (cont’d)
 The ocean basins contain mountains, valleys and
plains.
 The largest changes to the ocean basin occur through
the movement of tectonic plates, although there is also
erosion via storms, earthquakes and icebergs.
Origin of ocean water
 Oceans have filled over hundreds of millions of years.
 Scientists believe the oceans are more than 3 billion
years old.
 Water may have originally been released from volcanic
eruptions when the vapour from the eruption cooled
and condensed.
 Some believe the water came from ice comets.
Origin (cont’d)
 Pangea began to split up due to plate tectonics.
 Earth’s surface is made of large, slow-moving sections
of rock called tectonic plates.
 http://www.ucmp.berkeley.edu/geology/anim1.html
Technologies for studying ocean basins
 Read pp. 46-49
 STSE
 Define the following technologies in your notebook:
 Sonar
 Satellites
 Core sampling
 Underwater photography/videography
 Deep sea submersibles
 Diving
 Write a paragraph explaining how these technologies
have improved over time. (ex. Diving vs. Submersible
and wire line depth probe vs. Sonar)
Continental margins and others
 Abyssal plains are the pieces of oceanic crust between
a spreading mid-ocean ridge and the trench it
disappears into.
 Continental shelf is the submerged part of the
continent between the coast and the edge of the basin.
 Continental slope is the section that slopes downward
to the seafloor.
 Mid-ocean ridge is where the sea floor is still being
formed by volcanic eruptions. Two plates are being
pushed apart (magma oozes out from the core and
hardens) and a mountain change forms!
Draw a profile diagram include:
continental shelf
continental slope
abyssal plain
mid-ocean ridge
 Read Science Watch p. 52
 Do questions 1-11, p. 53.
Ocean Currents
 Read pp. 54-61
Ocean Currents
 There are more than 20 major currents which move
large amounts of water predictably around the oceans.
 Currents move large quantities of water, minerals, solar
energy, oxygen and carbon dioxide, plankton and fish.
 Currents are caused and driven by water
density and salt content, the wind, the
spin of Earth, coastlines and the moon.
 Largest current is the Antarctic
Circumpolar Current in the
Southern Ocean, at 24 000 km long
 Ocean currents are either
 Surface currents (0 - 200 m)
 Deep water currents (200 m and deeper)
What makes surface currents move?
 Wind
 As air warms from solar energy, it rises, and cooler air rushes to replace
it. This creates wind.
 As the wind passes along the surface of the water, it bumps the water
molecules and moves them along in the same direction.
 Spin of the Earth
 Earth spins from West to East (counter clockwise)
 The Coriolis effect deflects winds and currents to
the right/East in the Northern hemisphere
(opposite in the Southern hemisphere)
http://video.google.ca/videosearch?q=the%20physics%20of%20weather&h
l=en&rlz=1T4GWYE_enCA242CA242&um=1&ie=UTF-8&sa=N&tab=wv#
 Shape of continents
 Currents move through the oceans and around
the continents like rocks in a stream.
What makes deep currents move?
 Water temperature
 Like air, warm water rises, and cool water falls
 Density current = cool, dense water moving on an ocean floor.
 Three layers of water dependent on temperature:



Surface: 0 - 200 m, warmest
Thermocline: 200 m - 1 km, rapidly cools
Deep water: 1 km and deeper, just above freezing
 Water salinity
 Adding fresh water decreases salinity
 Evaporation and freezing increases salinity
 Densest ocean waters at the poles
 Upwelling occurs when nutrient-rich
cold water finally moves up to the surface
 Convection current demo... P. 36 Curriculum Guide
 Questions 1-10, p. 63
Ocean Waves
 Read pp. 64-66
Ocean Waves
 Most waves are created by wind.
 In open ocean, waves are called swells.
 Swells “break” in shallow water, called breakers.
 The largest waves are tsunamis, caused by undersea
earthquakes, landslides or volcanic eruptions.
 Tsunami - From The Discovery Channel-B (12-26-04)
◦ http://video.google.com/videoplay?docid=-
4333412395835151021&vt=lf&hl=en
 Newfoundland Tsunami and photos
 http://www.collectionscanada.gc.ca/sos/002028-1100e.html
Breakers
 As a wave approaches the shore, its wavelength
decreases and its height increases.
Class project!
 Newfoundland Tsunami
 Make a poster about the 1929 Newfoundland Tsunami
 Include:






Date
Location (map)
Cause
Death toll
Destruction
Pictures
Tides
 Read p.69-71
Tides
 Hopewell Rocks – Bay of Fundy Tides
◦ http://video.google.ca/videoplay?docid=3956711618129258915&ei=-1W5SNTFH4yawH96NnYDA&q=fundy+tides&vt=lf
 Tides are caused by gravities of Earth and the Moon.
 High tides occur where the Moon is
closest to Earth (and opposite side)
 Low tides occur at 90º to the high tides.
 Tidal range (difference between
high and low) averages 2 m in NL.
 The Sun’s gravity, when lined up
properly, can produce extreme tides.
 These are called spring tides
 When the Sun, Moon and Earth are not lined up,
the tides are called neap tides.
 Questions 1-4, p.71
Shoreline interactions
 Read pp. 66-69
Interactions at shorelines
 Waves erode coastal areas based on the force of the waves, and
the composition of the shoreline.
 Headlands made up of harder rock, and erode less, but absorb
most wave force.
 Bays occur between headlands, are generally calm.
 http://maps.google.ca/maps?sourceid=navclient&ie=UTF8&rlz=1T4GWYE_enCA242CA242&q=Goose%20bay&um=1&sa=
N&tab=wl
 Sea stacks are extra-hard
rock left behind from eroded
headlands.
Reminder from Grade 7...
 Weathering – breakdown of rocks into smaller
particles
 Erosion – the movement of those weathered particles
 Deposition – when eroded material is left behin
Shorelines
 Waves have the power to erode shorelines and deposit
sediments on the shore.
 Tides work together with waves and determine the
range of shoreline that can be affected by wave action.
 The interaction with shorelines depend on:
 Shape of the shoreline
 Slope of the shoreline (shallow means deposition of
sediments, steep means erosion)
 Type of rock material (sandstone erodes faster than
shale)
 Wave energy
Limestone
Class Activity
 6 groups (4/5 per group)
 You are to research the processes of erosion and
deposition that result from wave action and water flow
on one of the following: beaches, shoal, sand bars, sea
caves, sea stacks, sea arches
 Present your findings on a poster. Be sure to include
pictures and NL location!
Prevention/reduction of wave
action along shorelines
 Breakwaters
http://maps.google.ca/maps?sourceid=navclient&ie=U
TF8&rlz=1T4GWYE_enCA242CA242&q=foxtrap%20mari
na&um=1&sa=N&tab=wl
 Jetties/wharves
 Vegetation
 Questions 1-5, p.69
 Read Wild, Weird, Wonderful, p. 76 (The Spout!)
 http://video.google.ca/videosearch?sourceid=navclient&
ie=UTF8&rlz=1T4GWYE_enCA242CA242&q=the%20spout%20e
ast%20coast%20trail&um=1&sa=N&tab=wv#
 Questions 1-13, p. 77
 Foldable for review! p. 39
 http://video.google.ca/videoplay?docid=669595010475
6107303&ei=pv7fSJrxFoT0gGSy4yiCw&q=the+spout+east+coast+trail&vt=lf
 List 10 points/key terms in your notebook shown in the
video that we have discussed this chapter.
 Quiz!
 Test!