Presentation on theme: "Things to Ponder Why are polar bears often used to illustrate climate change? What is the atmosphere? What are the primary layers of the atmosphere?"— Presentation transcript:
1Things to PonderWhy are polar bears often used to illustrate climate change?What is the atmosphere?What are the primary layers of the atmosphere?
2The Atmosphere, Climate and Global Warming Chapter 23The Atmosphere, Climate and Global Warming
3Climate Change Central Questions & Key Concepts What is the atmosphere?What is the difference between weather & climate?How does the Earth’s climate fluctuate?What factors affect climate?What are the possible effects of global warming?What can humans do about potential climate change?Ozone depletion and global warming are two very different things.
4The Atmosphere The thin layer of gases that envelops the Earth Chemical reactionsAtmospheric circulation produces weather and climates
5The Atmosphereby weightthickestlayerweatherVery little water
6Processes That Remove Materials from the Atmosphere Sedimentation:Particles that are heavier than air settle out as a result of gravity.Ex: Coal /volcanic particles will settle out over timeRain out:Precipitation will physically and chemically flush materials from the atmosphere.Ex: CO2 + H2O H2CO3 carbon dioxide is removedOxidation:Where oxygen is chemically combined with other substances.Ex: atmospheric sulfur dioxide oxidizes to form sulfur trioxide which produces sulfuric acidPhotodissociation:Solar radiation can break down bonds in this chemical process. For example ozone may break down due to this process from O3 to O2.
7Vocabulary Used to Characterize Air Pressure:force per unit areaAtmospheric pressure:is the weight of overlying atmosphere per unit areaQuestion: Does the atmospheric pressure increase as altitude increases or does it decrease?Temperature:a measure of thermal energy, ie the kinetic energy of the motion of atoms in a substance.Question: as temperature increases does kinetic energy increase or decrease?Water vapor:The amount of water vapor present in a particular place depends on several things including air temperature, air pressure and available water vapor (from various processes – remember the water cycle?)
8Weather vs. Climate NOT THE SAME THING!! Weather is what conditions of the atmosphere are over a short period of time, (hours, days, weeks)Climate:climate is how the atmosphere "behaves" over relatively long periods of time (seasons, decades)that “behavior” includes the representative or characteristic atmospheric conditions for a region on EarthMicroclimateThe climate of a very small local area
9Short Term Climate Variation In addition to long-term climate change, there are shorter term climate variations.This so-called climate variability can be represented by periodic or intermittent changes related to El Niño, La Niña, volcanic eruptions, or other changes in the Earth system.
10El Niño/Southern Oscillation (ENSO) Natural. Occurs every 5-10 years. Last monthsA disruption in the natural weather circulationThe trade winds that usually blow warm surface water towards the western edge of Australia and Indonesia, and nutrient rich cold water (good for fish) towards the west coast of South America weaken or change direction totally.Causes small changes in ocean temperature that in turn cause very large changes in global weather patterns.Events believed to have been caused by El Nino:drought conditions in Indonensia, Africa and Australia. Flooding in South America as well as 1993 Mississippi and 1995 California floods,So what is La NiñaNormalEl Niño
11Major Climatic ChangeMajor climatic changes have occurred during the past 2 million yearsAppearances and retreats of glaciersDuring the past 100 years, the mean global annual temperature has increased by .5 degrees Celsius
12The Greenhouse Effect Greenhouse Effect Greenhouse Gasses The process of trapping heat in the atmosphereNATURAL!Without it the world would be too cold to support life!Water vapor (85% of greenhouse warming), water particles (12%) and several other gases warm the Earth’s atmosphere because they absorb and emit radiationGreenhouse GassesGasses that have a greenhouse effectWater vaporAnthropogenic sources: carbon dioxide, methane, nitrous oxide, CFCs (page _____)
13The Natural Greenhouse Effect Albedo: known as surface reflectivity of sun’s radiation
14Changes in the Earth’s Temperature During the Past Million Years The mean average temperature of the Earth has swung up and down by several degrees Celsius over the past million years due to variations in the Earth’s orbit around the sun.Interglacial periods – Times of relatively ice free periods, whereas times of low temperature reflect glacial events.Global climate can also change in shorter times – ex: continental glaciation ended 12,500 years ago with rapid warming – only lasting a few decades.
1520th Century RiseThe first 5 years of the 20th century were some of the warmest in the 142 years since temperatures have been recorded and in the last 1,000 years according to geologic data (see pages ____________ for how this data is collected).Warming since the mid 70s has been approximately 3X as fast as the previous 100 yearsThe 10 warmest years have all occurred since 1990 and the five warmest since 1997The warmest year on record was 2005, with 1998 second, and 2002 and 2003 tied for second. (2005 data)In the US 2003 was cooler and wetter than average in the eastern US, warmer and drier in the western part. New Mexico had its warmest year on record.In Europe in 2003 summer heat waves occurred with the warmest seasonal temperatures ever recorded in several countries. 15,000 people died in Paris.Warm conditions with drought contributed to severe wildfires in Australia, the United States and Canada.A year or two of high temperatures is NOT by itself an indication of global warming, however, the persistent trend of increasing temperatures over three decades is compelling evidence that global warming is real.
20So what is “Global Warming” A natural or human induced increase in the average global temperature of the atmosphere near the earth’s surface4 factorsAmount of sunlight Earth receivesAmount of sunlight Earth reflectsRetention of heat by atmosphereEvaporation and condensation of water vaporNegative and Positive feedback cycles affect the atmosphereIncrease in emission of greenhouse gassesSolar Forcing, Natural Cycles, Aerosols (global dimming), Volcanic Eruptions, El Nino
21Projecting Future Changes in Earth’s Climate Climate modelsApparent influence of human activitiesCould be natural changes
23Evidence for Global Warming http://climate.nasa.gov/evidence/ Sea level riseGlobal sea level rose about 17 centimeters (6.7 inches) in the last century. The rate in the last decade, however, is nearly double that of the last century.Global temperature riseAll three major global surface temperature reconstructions show that Earth has warmed since The 2000s had a solar output decline but still warmed.Warming oceansThe oceans have absorbed much of this increased heat, with the top 700 meters (about 2,300 feet) of ocean showing warming of degrees Fahrenheit since 1969.Shrinking ice sheetsThe Greenland and Antarctic ice sheets have decreased in mass. Data from NASA's Gravity Recovery and Climate Experiment show Greenland lost 150 to 250 cubic kilometers (36 to 60 cubic miles) of ice per year between 2002 and 2006, while Antarctica lost about 152 cubic kilometers (36 cubic miles) of ice between 2002 and 2005.
24Evidence for Global Warming http://climate.nasa.gov/evidence/ Declining Arctic sea iceBoth the extent and thickness of Arctic sea ice has declined rapidly over the last several decadesGlacial retreatGlaciers are retreating almost everywhere around the world - including in the Alps, Himalayas, Andes, Rockies, Alaska and AfricaExtreme eventsThe number of record high temperature events in the United States has been increasing, while the number of record low temperature events has been decreasing, since The U.S. has also witnessed increasing numbers of intense rainfall events.Ocean acidificationSince the beginning of the Industrial Revolution, the acidity of surface ocean waters has increased by about 30 percent. This increase is the result of humans emitting more carbon dioxide into the atmosphere and hence more being absorbed into the oceans. The amount of carbon dioxide absorbed by the upper layer of the oceans is increasing by about 2 billion tons per year.
28Negative Feedback Cycles Associated with the Greenhouse Effect Warming stimulates algae growth.Algae absorbs CO2.Warming stimulates plant growth.Plants absorb CO2.Polar regions receive more precipitation from warmer air carrying more moistureIncreased snow and ice could cause the solar energy to be reflected causing coolingIncreases in water evaporation from the ocean and the land could increase clouds.The clouds reflect the sunlight and cool the surface.
29Positive Feedback Cycles Associated with the Greenhouse Effect Increased evaporationAdded water vapor in the air that does not condense will cause additional warming.Melting permafrost at high latitudesReleases methane, as a by product of decomposition of organic materials in the melted permafrost layer, which would cause additional warming. Releasing old carbon locked in the soil..Reduction in the amount of snow packReplaced by darker vegetation/soil could increase absorption of solar energy further warming the Earth’s surface.Increased use of air conditioning in warmer climatesIncreased use of fossil fuels could increase release of CO2.
30Old Carbon vs. New Carbon Old carbon can be defined as carbon that is trapped and not currently part of our current carbon cycle.In fossil fuels – released through burning.In Arctic Soils – being released as temperatures increase.New carbon is carbon that is part of the current carbon cycle. It has recently entered the soil through vegetation.Biofuels release CO2 but it is NEW carbon
31Factors Affecting Changes in Earth’s Average Temperature Changes in solar outputChanges in Earth’s albedoModerating effect of oceansClouds and water vaporAir pollution
32Climate Change and Human Activities Increased use/burning of fossil fuelsAdds ~ 5.5 gigatons per year to the atmosphere. The carbon combines with oxygen to produce CO2DeforestationAdds ~ 1.6 gigatons per year to the atmosphere. Burning of the trees releases carbon stored in the wood that combines with oxygen to produce CO2Not to mention the fact that the trees are no longer taking IN CO2!
33Effects of Global Warming Changes in climatic patternsMelting icecaps & glaciersRise in sea levelCoral reef bleachingChanges in biosphere
35Solutions: Dealing with the Threat of Climate Change Options:Do nothingDo more researchAct now to reduce risksPrecautionary Principle
36Removing CO2 From the Atmosphere TreeplantationCoalpower plantTanker deliversCO2 from plantto rigOil rigCrop fieldSwitchgrassfieldSpent oil reservoir isused for CO2 depositCO2 is pumpeddown to reservoirthrough abandoned oil fieldAbandonedoil fieldCO2 ispumped downfrom rig forDeep oceandisposal= CO2 deposit= CO2 pumping
37Reducing Greenhouse Gas Emissions European Climate Exchange: Carbon TradingA nation will agree to cap its emissionsCorporations are issued emission permits that allow X amount of emissions. These can be traded.Rio Earth Summit (1992)Rio de Jeneiro, Brazil: Blueprint for reduction of CO2 emissions. USA disagreed said it was too costly.Kyoto Treaty (1997)Legally binding emission limits discussed.166 nations signed. USA refused to sign, though eventually agreed to cut emissions 7% below 1990 levels. Recommended levels were 60-80%.
38Reducing Greenhouse Gas Emissions Continued… G-8 meeting (2008)New U.N. treaty to be discussed in Copenhagen in Leaders including USA agreed to consider and adopt reductions of greenhouse gas emission of at least 50%.Facts:United States has 5% of the world’s population, yet emits 25% of the atmospheric CO2.California by ITSELF is 12th in the world for CO2 emissions. CA, however, passed legislation in 2006 to reduce emissions by 25% by 2020.
39There are links between them. For next time: What are those links? The ozone hole is a completely different phenomenon to global warming!There are links between them.For next time: What are those links?