HUMAN IMPACT on the BIOSPHERE Chapter 6-4 Charting a course for the Future
Foothill High School Science Department Human Impact Charting a Course for the Future.
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Transcript of Foothill High School Science Department Human Impact Charting a Course for the Future.
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Human ImpactHuman Impact
Charting a Course
for the Future
Charting a Course
for the Future
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Charting A CourseCharting A Course
Key ConceptKey Concept::As We Enter The 21As We Enter The 21stst Century, Many Century, Many
Biologists Are Concerned About The Biologists Are Concerned About The Biological Effects Of Global Change Biological Effects Of Global Change To:To:
1.1. ResourcesResources2.2. AirAir3.3. WaterWater4.4. BiodiversityBiodiversity
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Oxygen GasOxygen Gas
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Ozone MoleculeOzone Molecule
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Ozone DepletionOzone Depletion
• Ozone layerOzone layer–20/50 km above earth 20/50 km above earth (12 – 31 miles) (12 – 31 miles)
–Oxygen = OOxygen = O22
–Ozone = OOzone = O33
• Ozone at ground level is a pollutantOzone at ground level is a pollutant• In the upper atmosphere it is In the upper atmosphere it is VERYVERY
importantimportant
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Ozone LayerOzone Layer
• Absorbs Ultraviolet Radiation (UV)Absorbs Ultraviolet Radiation (UV)
• UV Radiation Can Cause:UV Radiation Can Cause:– SunburnSunburn– CancerCancer– Eye DamageEye Damage– CataractsCataracts– Decreased Resistance To DiseaseDecreased Resistance To Disease– Destruction of Plants & phytoplanktonDestruction of Plants & phytoplankton
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
OzoneOzone
The Universal Sunscreen
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Ozone Hole
-South Pole
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Ozone DepletionOzone Depletion
• Discovered in 1970’s over Antarctica Discovered in 1970’s over Antarctica
• Hole is growing largerHole is growing larger
• Now occurring over the ArcticNow occurring over the Arctic
• 1995 1995 – grew large enough to expose U.S.grew large enough to expose U.S.
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Ozone Hole Caused ByOzone Hole Caused By
CFC’sCFC’sChlorofluorocarbonsChlorofluorocarbons
CFC’s act as a catalystCFC’s act as a catalyst
CFC’s have a long half-lifeCFC’s have a long half-life
2O2O33 + CFC’s 3O + CFC’s 3O22
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Where Do CFC’s Originate?Where Do CFC’s Originate?
• CFC’s found inCFC’s found in–aerosol cansaerosol cans
–coolants used incoolants used in• refrigeratorsrefrigerators
• freezersfreezers
• automobile air conditioning automobile air conditioning
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Montreal ProtocolMontreal Protocol
19871987
46 Nations46 Nations
Agreed to end use of CFC’s Agreed to end use of CFC’s by 2000by 2000
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Change In Atmospheric ChlorineChange In Atmospheric Chlorine
0
2
4
6
8
10
12
14
1950 1970 1990 2000 2010 2030 2050 2070 2090
Pa
rts
pe
r B
illi
on
Historical NoRestrictions Montreal All Nations
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Global WarmingGlobal Warming
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Global WarmingGlobal Warming
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Global WarmingGlobal Warming
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Global WarmingGlobal Warming
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Climate ChangeClimate Change
• Any Climate Change will have profound Any Climate Change will have profound effects on the Biosphere.effects on the Biosphere.
• Over past 120 years average global Over past 120 years average global temperature has increased 0.5 degrees temperature has increased 0.5 degrees Celsius (0.9 degrees F)Celsius (0.9 degrees F)
• Rise between 1980-2000 fastest in over Rise between 1980-2000 fastest in over 100 years.100 years.
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Foothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science DepartmentFoothill High School Science Department
Climate ChangeClimate Change
• Ice caps are Ice caps are meltingmelting
• Arctic Sea Ice Arctic Sea Ice may be gone in may be gone in 50 years50 years
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Why is it happening?Why is it happening?
• CO2 Methane (Greenhouse Gases)CO2 Methane (Greenhouse Gases)
• Burning Fossil Fuels, ForestsBurning Fossil Fuels, Forests
• Project Increase of 1 – 2 degrees Project Increase of 1 – 2 degrees Celsius by 2050 Celsius by 2050
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Global Warming EffectsGlobal Warming Effects
• Polar Ice MeltPolar Ice Melt
• Rising Sea LevelsRising Sea Levels
• Increase in number & severity of Increase in number & severity of stormsstorms
• North American droughtsNorth American droughts
• Shifts in plant & animal species Shifts in plant & animal species distributiondistribution
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Ways to Help the BiosphereWays to Help the Biosphere
• Decrease energy consumptionDecrease energy consumption– Insulate HomesInsulate Homes– Energy Efficient AppliancesEnergy Efficient Appliances– High Mileage CarsHigh Mileage Cars– High Efficiency Energy ProductionHigh Efficiency Energy Production
• Alternate Fuel SourcesAlternate Fuel Sources– Fuel CellsFuel Cells– WindWind