SlideShare ist ein Scribd-Unternehmen logo
1 von 34
Global Warming

An iceberg melts in Kulusuk, Greenland, near the Arctic Circle.
•Global warming is a rise in
global temperatures that
could result from the
increased absorption
of radiation due to higher
levels of
greenhouse gases.
•50% of all radiation that reaches the Earth is
absorbed. The remaining 50% is reflected back
out to space.
•The greenhouse effect is
the natural heating of
Earth’s surface caused by
the retention of heat by
certain atmospheric gases
called greenhouse gases.
•Scientists theorize that any
increase in the amount of
greenhouse gases, particular
carbon dioxide (CO2), would
result in the increased
absorption
of radiation.
1. Greenhouse
Effect is
responsible for
the Earth’s
warm and
livable climate.
2. Greenhouse
gases include:
a.Water vapor
b.Methane
c.Carbon
dioxide
d.Ozone
e.Nitrous oxide
3. The sun
sends
radiation.
4. Some of
The Atmosphere reflects
the energy.
the sun’sheat is
reflected by
the
atmosphere.
4. Atmosphere:
5) On Earth:
Energy that passes
through, are
absorbed by the
ground, water, gases,
and plants.
•A portion of the solar
radiation that reaches
the Earth’s surface
such as ice, snow, and
ocean are reflected.
6. Radiation
trigger the
greenhouse
Radiation trigger the
gases togases to
move.
greenhouse
move.aAs a result,the
As result, the
atmosphere is heated.
atmosphere is
heated.
Consequences of Global Warming:
•

Unless we act now, your children will inherit a hotter world, dirtier
air and water, more severe floods and droughts, and more wildfires.

I.

CLIMATE
PATTERN
CHANGES
ecosystem shifts and species die-off

a. warmer
temperatures
b. drought and
wildfire
c. more intense
rainstorms
Greater evaporation as a result of global warming
could increase the risk of wildfires.
II. HEALTH
EFFECTS
a. deadly heat
waves and the
spread of
disease

Greater evaporation as a result of global
warming
could increase the risk of wildfires.

More frequent and more intensive heat waves could
result in more heat-related deaths. Photo: Gary Braasch,
Chicago, July 1995. See the
World View of Global Warming website for more Gary
Braasch photos illustrating the consequences of the
changing climate.
III.

WARMING WATER
a. more powerful hurricanes
b. melting glaciers
c. sea-level rise

The satellite photo at far left shows the Larson B ice shelf on Jan. 31, 2002. Ice appears as solid
white. Moving to the right, in photos taken Feb. 17 and Feb. 23, the ice begins to disintegrate. In the
photos at far right, taken Mar. 5 and Mar 7, note water (blue) where solid ice had been, and that a
portion of the shelf is drifting away. Photos: National Aeronautics and Space Administration
Ancient ice shelf breaks free
A giant ice shelf the size of 11,000 football fields has snapped free from Canada's
Arctic, scientists said. The mass of ice broke clear 16 months ago from the coast
of Ellesmere Island.
•Credit
•Jacques Descloitres, MODIS Rapid Response Team, NASA/GSFC

The Arctic’s largest ice shelf is breaking up. The Ward
Hunt Ice Shelf is a remnant of the compacted snow and
ancient sea ice that extended along the northern shores
of Ellesmere Island in Northern Canada until the early
IV. ECOSYSTEM
DISRUPTION
a. ecosystem shifts and
species die-off.
Warmer temperatures may cause some
ecosystems, including alpine meadows
in the Rocky Mountains, to disappear.

For more Environmental Facts:
Natural Resources Defense Council
This file photo provided by
Mary Sage shows a polar
bear watching a whaling
crew off shore near Barrow,
Alaska, Monday, May 22,
2006. Polar bears are in
deep trouble because of
global warming and other
factors and deserve federal
protection under the
Endangered Species Act,
the Bush administration is
proposing Wednesday, Dec.
27, 2006. (AP
Photo/Courtesy of Mary
Sage, Joseph Napaaqtuq
Sage)
Polar Bears are dying at alarming rates due to Global Warming.
Blue Man Group – Earth to America (Global Warming) 1:49 min
How Do Ice Cores of Glaciers Tell Us about Past Climates?

•Research scientists collect and study glacial ice cores.
•Data from these ice cores provide one of the most
complete records of past climate conditions. Of greatest
interest are the deep cores obtained by drilling programs in
Summit, Greenland and Vostok, Antarctica.
•The Vostok ice core provides the longest continuous
record of Antarctic climatic history.
•Analysis of the core has been completed to a depth of
3350 meters, representing approximately 440,000
years of climate history.
Vostok ice core drilling site, Antarctica
Ice cores
reveal the
story of Earth's
climate in
reverse order.
The uppermost
layers of the
core tell the
most recent
history, with
increasingly
deeper layers
providing a
record of
progressively
older periods
(Law of
Superposition).
Scientists can determine the amount of carbon dioxide
that was in the air during different time periods by
analyzing gas bubbles trapped in ice cores. Carbon
dioxide is a greenhouse gas that plays a major role in the
atmosphere’s energy balance.
Scientists can reconstruct a record of temperatures that
occurred in the past by analyzing the ratio of oxygen isotopes
trapped within air bubbles in the ice (O16 & O18).
The graph below shows how the temperature has changed over
the past 165,000 years. The graph shows temperature
anomalies—variations in the temperature above or below
Vostok’s present day average temperature of -56ºC.

High

LOW
Temperature and carbon dioxide data are plotted together
on this graph. This makes it easier to compare the two
variables and how they may be related.
Recent Changes in Atmospheric Carbon Dioxide
Scientists have been precisely measuring the amount of
carbon dioxide in the atmosphere since 1958. The results
of these studies are plotted on the graph below. The
yearly average CO2 level is represented by the smooth
black line, and seasonal changes appear as small peaks
and dips.
Ice core research projects are working to extend the record of
global climate further back in time and over more of Earth’s
surface.
To learn about their most recent discoveries, visit the links
provided:

Explore these links for more information about ice core
projects and climate research:
Graph of Vostok ice core data extending back for 400,000 years
Greenland Ice Sheet Project 2
North Greenland Ice Core Project
Taylor Dome Ice Core Project
European Project for Ice Coring in Antarctica (EPICA)
World Data Center for Paleoclimatology
Collection of photographs about polar ice core research
National Ice Core Laboratory

Weitere ähnliche Inhalte

Was ist angesagt?

Chapter 3 section 1 powerpoint
Chapter 3 section 1 powerpointChapter 3 section 1 powerpoint
Chapter 3 section 1 powerpointJason Hauck
 
Unit 5 b ch 13 s1 climate & climate change
Unit 5 b ch 13 s1  climate & climate changeUnit 5 b ch 13 s1  climate & climate change
Unit 5 b ch 13 s1 climate & climate changewja10255
 
Distribution of Temperature and its Impact on Marine Organism
Distribution of Temperature and its Impact on Marine OrganismDistribution of Temperature and its Impact on Marine Organism
Distribution of Temperature and its Impact on Marine OrganismGayatri R. Kachh
 
Unit 5 b ch 13 s3 global warming
Unit 5 b ch 13 s3  global warmingUnit 5 b ch 13 s3  global warming
Unit 5 b ch 13 s3 global warmingwja10255
 
GLOBAL FREEZING/GLOBAL COOLING.
GLOBAL FREEZING/GLOBAL COOLING.GLOBAL FREEZING/GLOBAL COOLING.
GLOBAL FREEZING/GLOBAL COOLING.Shaiza Awan
 
Global Cooling - Don Easterbrook
Global Cooling - Don EasterbrookGlobal Cooling - Don Easterbrook
Global Cooling - Don EasterbrookPaul Murphy
 
Ocean atmosphere interactions
Ocean atmosphere interactionsOcean atmosphere interactions
Ocean atmosphere interactionsJanine Samelo
 
Little ice age
Little ice ageLittle ice age
Little ice agelukebudi
 
Earth's Climate
Earth's ClimateEarth's Climate
Earth's ClimateOhMiss
 
4.1 -- BIO
4.1 -- BIO4.1 -- BIO
4.1 -- BIOheyylo
 
Abruptclimatechange 7229
Abruptclimatechange 7229Abruptclimatechange 7229
Abruptclimatechange 7229www.thiiink.com
 
L1 Extent Of Ice
L1 Extent Of IceL1 Extent Of Ice
L1 Extent Of Icetudorgeog
 
Climate change part 1
Climate change part 1Climate change part 1
Climate change part 1Ed Stermer
 
Global climate watch
Global climate watchGlobal climate watch
Global climate watchEdwin Clerval
 
Temperature and its vertical distribution in ocean water
Temperature and its vertical distribution in ocean water Temperature and its vertical distribution in ocean water
Temperature and its vertical distribution in ocean water Tanuj Joshi
 
Biology 4 1
Biology 4 1Biology 4 1
Biology 4 1Tamara
 

Was ist angesagt? (20)

Chapter 3 section 1 powerpoint
Chapter 3 section 1 powerpointChapter 3 section 1 powerpoint
Chapter 3 section 1 powerpoint
 
Theglobalwarming
TheglobalwarmingTheglobalwarming
Theglobalwarming
 
Unit 5 b ch 13 s1 climate & climate change
Unit 5 b ch 13 s1  climate & climate changeUnit 5 b ch 13 s1  climate & climate change
Unit 5 b ch 13 s1 climate & climate change
 
Distribution of Temperature and its Impact on Marine Organism
Distribution of Temperature and its Impact on Marine OrganismDistribution of Temperature and its Impact on Marine Organism
Distribution of Temperature and its Impact on Marine Organism
 
Unit 5 b ch 13 s3 global warming
Unit 5 b ch 13 s3  global warmingUnit 5 b ch 13 s3  global warming
Unit 5 b ch 13 s3 global warming
 
Cafe sci
Cafe sciCafe sci
Cafe sci
 
GLOBAL FREEZING/GLOBAL COOLING.
GLOBAL FREEZING/GLOBAL COOLING.GLOBAL FREEZING/GLOBAL COOLING.
GLOBAL FREEZING/GLOBAL COOLING.
 
The global warming
The global warmingThe global warming
The global warming
 
Global Cooling - Don Easterbrook
Global Cooling - Don EasterbrookGlobal Cooling - Don Easterbrook
Global Cooling - Don Easterbrook
 
Ocean atmosphere interactions
Ocean atmosphere interactionsOcean atmosphere interactions
Ocean atmosphere interactions
 
Global warming
Global warmingGlobal warming
Global warming
 
Little ice age
Little ice ageLittle ice age
Little ice age
 
Earth's Climate
Earth's ClimateEarth's Climate
Earth's Climate
 
4.1 -- BIO
4.1 -- BIO4.1 -- BIO
4.1 -- BIO
 
Abruptclimatechange 7229
Abruptclimatechange 7229Abruptclimatechange 7229
Abruptclimatechange 7229
 
L1 Extent Of Ice
L1 Extent Of IceL1 Extent Of Ice
L1 Extent Of Ice
 
Climate change part 1
Climate change part 1Climate change part 1
Climate change part 1
 
Global climate watch
Global climate watchGlobal climate watch
Global climate watch
 
Temperature and its vertical distribution in ocean water
Temperature and its vertical distribution in ocean water Temperature and its vertical distribution in ocean water
Temperature and its vertical distribution in ocean water
 
Biology 4 1
Biology 4 1Biology 4 1
Biology 4 1
 

Ähnlich wie Global Warming

Smc Newsletter February 06
Smc Newsletter February 06Smc Newsletter February 06
Smc Newsletter February 06Larry Telles
 
Sci 10 Lesson 1 May 4 - Natural Causes of Climate Change
Sci 10 Lesson 1 May 4  -  Natural Causes of Climate ChangeSci 10 Lesson 1 May 4  -  Natural Causes of Climate Change
Sci 10 Lesson 1 May 4 - Natural Causes of Climate Changemsoonscience
 
5. What Is The Evidence For Global Warming Nsr
5. What Is The Evidence For Global Warming   Nsr5. What Is The Evidence For Global Warming   Nsr
5. What Is The Evidence For Global Warming Nsrtudorgeog
 
Climate: Climatic Change - Evidence, Cycles and The Future
Climate: Climatic Change - Evidence, Cycles and The FutureClimate: Climatic Change - Evidence, Cycles and The Future
Climate: Climatic Change - Evidence, Cycles and The Futuregeomillie
 
5_6062343142848333965.doc
5_6062343142848333965.doc5_6062343142848333965.doc
5_6062343142848333965.docLakshayRao7
 
PLEISTOCENE GLACIATION[2].pptx
PLEISTOCENE GLACIATION[2].pptxPLEISTOCENE GLACIATION[2].pptx
PLEISTOCENE GLACIATION[2].pptxImposter7
 
Climate change co2 or crop irrigation
Climate change  co2 or crop irrigationClimate change  co2 or crop irrigation
Climate change co2 or crop irrigationKeith_Shotbolt
 
Ice ages
Ice agesIce ages
Ice agesgeovino
 
The causes of climate change
The causes of climate changeThe causes of climate change
The causes of climate changeWill Williams
 
HPU NCS2200 Climate change part 1
HPU NCS2200 Climate change part 1HPU NCS2200 Climate change part 1
HPU NCS2200 Climate change part 1cooperk2
 
Antarctic climate history and global climate changes
Antarctic climate history and global climate changesAntarctic climate history and global climate changes
Antarctic climate history and global climate changesPontus Lurcock
 
1.  Find 2 scientific articles (with opposing viewpoints) which ad.docx
1.  Find 2 scientific articles (with opposing viewpoints) which ad.docx1.  Find 2 scientific articles (with opposing viewpoints) which ad.docx
1.  Find 2 scientific articles (with opposing viewpoints) which ad.docxchristiandean12115
 
Climate Change: What we really Know?
Climate Change: What we really Know?Climate Change: What we really Know?
Climate Change: What we really Know?Arfar M. Razi
 
Tp climate change-101-2
Tp climate change-101-2Tp climate change-101-2
Tp climate change-101-2TMN-COT
 

Ähnlich wie Global Warming (20)

Hansen
HansenHansen
Hansen
 
Smc Newsletter February 06
Smc Newsletter February 06Smc Newsletter February 06
Smc Newsletter February 06
 
Sci 10 Lesson 1 May 4 - Natural Causes of Climate Change
Sci 10 Lesson 1 May 4  -  Natural Causes of Climate ChangeSci 10 Lesson 1 May 4  -  Natural Causes of Climate Change
Sci 10 Lesson 1 May 4 - Natural Causes of Climate Change
 
5. What Is The Evidence For Global Warming Nsr
5. What Is The Evidence For Global Warming   Nsr5. What Is The Evidence For Global Warming   Nsr
5. What Is The Evidence For Global Warming Nsr
 
Climate: Climatic Change - Evidence, Cycles and The Future
Climate: Climatic Change - Evidence, Cycles and The FutureClimate: Climatic Change - Evidence, Cycles and The Future
Climate: Climatic Change - Evidence, Cycles and The Future
 
5_6062343142848333965.doc
5_6062343142848333965.doc5_6062343142848333965.doc
5_6062343142848333965.doc
 
PLEISTOCENE GLACIATION[2].pptx
PLEISTOCENE GLACIATION[2].pptxPLEISTOCENE GLACIATION[2].pptx
PLEISTOCENE GLACIATION[2].pptx
 
Climate change co2 or crop irrigation
Climate change  co2 or crop irrigationClimate change  co2 or crop irrigation
Climate change co2 or crop irrigation
 
Ice ages
Ice agesIce ages
Ice ages
 
ENV 101 Ch16 lecture ppt_a
ENV 101 Ch16 lecture ppt_aENV 101 Ch16 lecture ppt_a
ENV 101 Ch16 lecture ppt_a
 
The causes of climate change
The causes of climate changeThe causes of climate change
The causes of climate change
 
FinalDraft
FinalDraftFinalDraft
FinalDraft
 
HPU NCS2200 Climate change part 1
HPU NCS2200 Climate change part 1HPU NCS2200 Climate change part 1
HPU NCS2200 Climate change part 1
 
Antarctic climate history and global climate changes
Antarctic climate history and global climate changesAntarctic climate history and global climate changes
Antarctic climate history and global climate changes
 
Ice ages
Ice agesIce ages
Ice ages
 
Climppf1
Climppf1Climppf1
Climppf1
 
Chemtrails
ChemtrailsChemtrails
Chemtrails
 
1.  Find 2 scientific articles (with opposing viewpoints) which ad.docx
1.  Find 2 scientific articles (with opposing viewpoints) which ad.docx1.  Find 2 scientific articles (with opposing viewpoints) which ad.docx
1.  Find 2 scientific articles (with opposing viewpoints) which ad.docx
 
Climate Change: What we really Know?
Climate Change: What we really Know?Climate Change: What we really Know?
Climate Change: What we really Know?
 
Tp climate change-101-2
Tp climate change-101-2Tp climate change-101-2
Tp climate change-101-2
 

Mehr von Bantay's Earth Science!

Severe Weather - Lightning, Tornadoes, & Hurricanes
Severe Weather -  Lightning, Tornadoes, & HurricanesSevere Weather -  Lightning, Tornadoes, & Hurricanes
Severe Weather - Lightning, Tornadoes, & HurricanesBantay's Earth Science!
 
Earth - Sun - Moon Relationships: Annual Motions/Seasons
Earth - Sun - Moon Relationships: Annual Motions/SeasonsEarth - Sun - Moon Relationships: Annual Motions/Seasons
Earth - Sun - Moon Relationships: Annual Motions/SeasonsBantay's Earth Science!
 
Solar System Formation/Sun/Comets/Meteors
Solar System Formation/Sun/Comets/MeteorsSolar System Formation/Sun/Comets/Meteors
Solar System Formation/Sun/Comets/MeteorsBantay's Earth Science!
 
Planetary Motion & Historical People in Astronomy
Planetary Motion & Historical People in AstronomyPlanetary Motion & Historical People in Astronomy
Planetary Motion & Historical People in AstronomyBantay's Earth Science!
 
Types of maps, long, lat, satellites, time zones
Types of maps, long, lat, satellites, time zonesTypes of maps, long, lat, satellites, time zones
Types of maps, long, lat, satellites, time zonesBantay's Earth Science!
 

Mehr von Bantay's Earth Science! (20)

Severe Weather - Lightning, Tornadoes, & Hurricanes
Severe Weather -  Lightning, Tornadoes, & HurricanesSevere Weather -  Lightning, Tornadoes, & Hurricanes
Severe Weather - Lightning, Tornadoes, & Hurricanes
 
Station Models
Station ModelsStation Models
Station Models
 
Cloud Development & Classification
Cloud Development & ClassificationCloud Development & Classification
Cloud Development & Classification
 
Air Masses, Global Winds, and Fronts
Air Masses, Global Winds, and FrontsAir Masses, Global Winds, and Fronts
Air Masses, Global Winds, and Fronts
 
Air Pressure and Moisture
Air Pressure and Moisture Air Pressure and Moisture
Air Pressure and Moisture
 
Intro to Meteorology: Our Atmosphere
Intro to Meteorology: Our AtmosphereIntro to Meteorology: Our Atmosphere
Intro to Meteorology: Our Atmosphere
 
Earth - Sun - Moon Relationships: Annual Motions/Seasons
Earth - Sun - Moon Relationships: Annual Motions/SeasonsEarth - Sun - Moon Relationships: Annual Motions/Seasons
Earth - Sun - Moon Relationships: Annual Motions/Seasons
 
Moon's Properties and Characteristics
Moon's Properties and CharacteristicsMoon's Properties and Characteristics
Moon's Properties and Characteristics
 
Solar System Formation/Sun/Comets/Meteors
Solar System Formation/Sun/Comets/MeteorsSolar System Formation/Sun/Comets/Meteors
Solar System Formation/Sun/Comets/Meteors
 
Solar System
Solar SystemSolar System
Solar System
 
Planetary Motion & Historical People in Astronomy
Planetary Motion & Historical People in AstronomyPlanetary Motion & Historical People in Astronomy
Planetary Motion & Historical People in Astronomy
 
Galaxies
GalaxiesGalaxies
Galaxies
 
Stars - Basic Properties/H- R Diagram
Stars - Basic Properties/H- R DiagramStars - Basic Properties/H- R Diagram
Stars - Basic Properties/H- R Diagram
 
Stars - Stellar Evolution
Stars - Stellar EvolutionStars - Stellar Evolution
Stars - Stellar Evolution
 
Notes - Radiation Electromagnetic
Notes - Radiation ElectromagneticNotes - Radiation Electromagnetic
Notes - Radiation Electromagnetic
 
Intro to Astronomy
Intro to AstronomyIntro to Astronomy
Intro to Astronomy
 
Topographic Maps Notes
Topographic Maps NotesTopographic Maps Notes
Topographic Maps Notes
 
Types of maps, long, lat, satellites, time zones
Types of maps, long, lat, satellites, time zonesTypes of maps, long, lat, satellites, time zones
Types of maps, long, lat, satellites, time zones
 
5_Density Lab Overview
5_Density Lab Overview5_Density Lab Overview
5_Density Lab Overview
 
4_Lab Safety
4_Lab Safety4_Lab Safety
4_Lab Safety
 

Kürzlich hochgeladen

A Critique of the Proposed National Education Policy Reform
A Critique of the Proposed National Education Policy ReformA Critique of the Proposed National Education Policy Reform
A Critique of the Proposed National Education Policy ReformChameera Dedduwage
 
Interactive Powerpoint_How to Master effective communication
Interactive Powerpoint_How to Master effective communicationInteractive Powerpoint_How to Master effective communication
Interactive Powerpoint_How to Master effective communicationnomboosow
 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactdawncurless
 
Disha NEET Physics Guide for classes 11 and 12.pdf
Disha NEET Physics Guide for classes 11 and 12.pdfDisha NEET Physics Guide for classes 11 and 12.pdf
Disha NEET Physics Guide for classes 11 and 12.pdfchloefrazer622
 
microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introductionMaksud Ahmed
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphThiyagu K
 
Student login on Anyboli platform.helpin
Student login on Anyboli platform.helpinStudent login on Anyboli platform.helpin
Student login on Anyboli platform.helpinRaunakKeshri1
 
Introduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsIntroduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsTechSoup
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxiammrhaywood
 
Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104misteraugie
 
The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13Steve Thomason
 
Paris 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityParis 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityGeoBlogs
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeThiyagu K
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Disha Kariya
 
Separation of Lanthanides/ Lanthanides and Actinides
Separation of Lanthanides/ Lanthanides and ActinidesSeparation of Lanthanides/ Lanthanides and Actinides
Separation of Lanthanides/ Lanthanides and ActinidesFatimaKhan178732
 
Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17Celine George
 
CARE OF CHILD IN INCUBATOR..........pptx
CARE OF CHILD IN INCUBATOR..........pptxCARE OF CHILD IN INCUBATOR..........pptx
CARE OF CHILD IN INCUBATOR..........pptxGaneshChakor2
 

Kürzlich hochgeladen (20)

A Critique of the Proposed National Education Policy Reform
A Critique of the Proposed National Education Policy ReformA Critique of the Proposed National Education Policy Reform
A Critique of the Proposed National Education Policy Reform
 
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptxINDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
 
Interactive Powerpoint_How to Master effective communication
Interactive Powerpoint_How to Master effective communicationInteractive Powerpoint_How to Master effective communication
Interactive Powerpoint_How to Master effective communication
 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impact
 
Disha NEET Physics Guide for classes 11 and 12.pdf
Disha NEET Physics Guide for classes 11 and 12.pdfDisha NEET Physics Guide for classes 11 and 12.pdf
Disha NEET Physics Guide for classes 11 and 12.pdf
 
Advance Mobile Application Development class 07
Advance Mobile Application Development class 07Advance Mobile Application Development class 07
Advance Mobile Application Development class 07
 
microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introduction
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot Graph
 
Student login on Anyboli platform.helpin
Student login on Anyboli platform.helpinStudent login on Anyboli platform.helpin
Student login on Anyboli platform.helpin
 
Introduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The BasicsIntroduction to Nonprofit Accounting: The Basics
Introduction to Nonprofit Accounting: The Basics
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
 
Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104
 
The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13
 
Paris 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activityParis 2024 Olympic Geographies - an activity
Paris 2024 Olympic Geographies - an activity
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and Mode
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..
 
Separation of Lanthanides/ Lanthanides and Actinides
Separation of Lanthanides/ Lanthanides and ActinidesSeparation of Lanthanides/ Lanthanides and Actinides
Separation of Lanthanides/ Lanthanides and Actinides
 
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
 
Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17
 
CARE OF CHILD IN INCUBATOR..........pptx
CARE OF CHILD IN INCUBATOR..........pptxCARE OF CHILD IN INCUBATOR..........pptx
CARE OF CHILD IN INCUBATOR..........pptx
 

Global Warming

  • 1. Global Warming An iceberg melts in Kulusuk, Greenland, near the Arctic Circle.
  • 2. •Global warming is a rise in global temperatures that could result from the increased absorption of radiation due to higher levels of greenhouse gases.
  • 3. •50% of all radiation that reaches the Earth is absorbed. The remaining 50% is reflected back out to space.
  • 4. •The greenhouse effect is the natural heating of Earth’s surface caused by the retention of heat by certain atmospheric gases called greenhouse gases. •Scientists theorize that any increase in the amount of greenhouse gases, particular carbon dioxide (CO2), would result in the increased absorption of radiation.
  • 5. 1. Greenhouse Effect is responsible for the Earth’s warm and livable climate.
  • 6. 2. Greenhouse gases include: a.Water vapor b.Methane c.Carbon dioxide d.Ozone e.Nitrous oxide
  • 8. 4. Some of The Atmosphere reflects the energy. the sun’sheat is reflected by the atmosphere. 4. Atmosphere:
  • 9. 5) On Earth: Energy that passes through, are absorbed by the ground, water, gases, and plants. •A portion of the solar radiation that reaches the Earth’s surface such as ice, snow, and ocean are reflected.
  • 10. 6. Radiation trigger the greenhouse Radiation trigger the gases togases to move. greenhouse move.aAs a result,the As result, the atmosphere is heated. atmosphere is heated.
  • 11. Consequences of Global Warming: • Unless we act now, your children will inherit a hotter world, dirtier air and water, more severe floods and droughts, and more wildfires. I. CLIMATE PATTERN CHANGES ecosystem shifts and species die-off a. warmer temperatures b. drought and wildfire c. more intense rainstorms Greater evaporation as a result of global warming could increase the risk of wildfires.
  • 12. II. HEALTH EFFECTS a. deadly heat waves and the spread of disease Greater evaporation as a result of global warming could increase the risk of wildfires. More frequent and more intensive heat waves could result in more heat-related deaths. Photo: Gary Braasch, Chicago, July 1995. See the World View of Global Warming website for more Gary Braasch photos illustrating the consequences of the changing climate.
  • 13. III. WARMING WATER a. more powerful hurricanes b. melting glaciers c. sea-level rise The satellite photo at far left shows the Larson B ice shelf on Jan. 31, 2002. Ice appears as solid white. Moving to the right, in photos taken Feb. 17 and Feb. 23, the ice begins to disintegrate. In the photos at far right, taken Mar. 5 and Mar 7, note water (blue) where solid ice had been, and that a portion of the shelf is drifting away. Photos: National Aeronautics and Space Administration
  • 14.
  • 15. Ancient ice shelf breaks free A giant ice shelf the size of 11,000 football fields has snapped free from Canada's Arctic, scientists said. The mass of ice broke clear 16 months ago from the coast of Ellesmere Island.
  • 16.
  • 17. •Credit •Jacques Descloitres, MODIS Rapid Response Team, NASA/GSFC The Arctic’s largest ice shelf is breaking up. The Ward Hunt Ice Shelf is a remnant of the compacted snow and ancient sea ice that extended along the northern shores of Ellesmere Island in Northern Canada until the early
  • 18. IV. ECOSYSTEM DISRUPTION a. ecosystem shifts and species die-off. Warmer temperatures may cause some ecosystems, including alpine meadows in the Rocky Mountains, to disappear. For more Environmental Facts: Natural Resources Defense Council
  • 19. This file photo provided by Mary Sage shows a polar bear watching a whaling crew off shore near Barrow, Alaska, Monday, May 22, 2006. Polar bears are in deep trouble because of global warming and other factors and deserve federal protection under the Endangered Species Act, the Bush administration is proposing Wednesday, Dec. 27, 2006. (AP Photo/Courtesy of Mary Sage, Joseph Napaaqtuq Sage)
  • 20.
  • 21.
  • 22.
  • 23. Polar Bears are dying at alarming rates due to Global Warming.
  • 24. Blue Man Group – Earth to America (Global Warming) 1:49 min
  • 25. How Do Ice Cores of Glaciers Tell Us about Past Climates? •Research scientists collect and study glacial ice cores. •Data from these ice cores provide one of the most complete records of past climate conditions. Of greatest interest are the deep cores obtained by drilling programs in Summit, Greenland and Vostok, Antarctica. •The Vostok ice core provides the longest continuous record of Antarctic climatic history. •Analysis of the core has been completed to a depth of 3350 meters, representing approximately 440,000 years of climate history.
  • 26. Vostok ice core drilling site, Antarctica
  • 27. Ice cores reveal the story of Earth's climate in reverse order. The uppermost layers of the core tell the most recent history, with increasingly deeper layers providing a record of progressively older periods (Law of Superposition).
  • 28. Scientists can determine the amount of carbon dioxide that was in the air during different time periods by analyzing gas bubbles trapped in ice cores. Carbon dioxide is a greenhouse gas that plays a major role in the atmosphere’s energy balance.
  • 29.
  • 30. Scientists can reconstruct a record of temperatures that occurred in the past by analyzing the ratio of oxygen isotopes trapped within air bubbles in the ice (O16 & O18). The graph below shows how the temperature has changed over the past 165,000 years. The graph shows temperature anomalies—variations in the temperature above or below Vostok’s present day average temperature of -56ºC. High LOW
  • 31. Temperature and carbon dioxide data are plotted together on this graph. This makes it easier to compare the two variables and how they may be related.
  • 32. Recent Changes in Atmospheric Carbon Dioxide Scientists have been precisely measuring the amount of carbon dioxide in the atmosphere since 1958. The results of these studies are plotted on the graph below. The yearly average CO2 level is represented by the smooth black line, and seasonal changes appear as small peaks and dips.
  • 33. Ice core research projects are working to extend the record of global climate further back in time and over more of Earth’s surface.
  • 34. To learn about their most recent discoveries, visit the links provided: Explore these links for more information about ice core projects and climate research: Graph of Vostok ice core data extending back for 400,000 years Greenland Ice Sheet Project 2 North Greenland Ice Core Project Taylor Dome Ice Core Project European Project for Ice Coring in Antarctica (EPICA) World Data Center for Paleoclimatology Collection of photographs about polar ice core research National Ice Core Laboratory