Greenhouse Effect: Earth’s Blanket What is a greenhouse? Wikipedia | GNU Smithsonian Greenhouse Effect Process by which thermal radiation from a planetary surface is absorbed by atmospheric greenhouse gases, and is re-radiated in all directions What gets in and what is blocked? © 2011 The Pennsylvania State University Albedo Reflecting power of a surface Ratio of reflected radiation from the surface to incident radiation upon it No units 0.3 is the global average albedo Why are urban areas warmer than rural areas? Surface Albedo Fresh Asphalt 0.04 Worn Asphalt 0.12 Conifer forest (Summer) 0.08 - 0.15 Deciduous trees 0.15 - 0.18 Bare soil 0.17 Green grass 0.25 Desert sand 0.4 New concrete 0.55 Ocean ice 0.5 - 0.7 Fresh snow 0.80 - 0.90 Earth’s Energy Budget NOAA|NWS Greenhouse Gas (GHG) Gas in an atmosphere that absorbs and emits radiation within the thermal infrared range GHG’s in Earth’s atmosphere in order of abundance NASA Water Vapor (H2O) Carbon Dioxide (CO2) Methane (CH4) Nitrous Oxide (N2O) Ozone (O3) GHG Concentration Depends on rates of emission and rates of removal If emissions increase with time, atmospheric concentration will increase with time, regardless of the atmospheric lifespan of the gas Water Vapor - H2O Natural Source •Evaporation of water •Sublimation of ice •Plant and animal respiration Anthropogenic source •Evaporation and transpiration losses from watering lawns Lifespan •9 days in the atmosphere Location •Troposphere Does it do us any good? •Supports life •Triggers convection currents •Leads to cloud formation Carbon Dioxide - CO2 Natural Source •Animal and plant respiration •Ocean-atmosphere exchange •Photosynthesis (sink) Anthropogenic source •Fossil fuel combustion •Deforestation (lack of sink) Lifespan •More than half is removed within a century •A small fraction (20%) can remain in the atmosphere for many millenia Location •Troposphere Does it do us any good? •Photosynthesis Methane - CH4 Natural Source •Wetlands •Termites Anthropogenic source •Raising ruminant animals (cattle) •Energy production from coal and natural gas •Rice agriculture •Biomass burning Lifespan •12 years •Removed by chemical processes in the atmosphere Location •Troposphere •Stratosphere Does it do us any good? •Helps regulate temperature Nitrous Oxide - N2O Natural Source •Oceans •Chemical oxidation of ammonia in the atmosphere •Soils Anthropogenic source •Transformation of fertilizer nitrogen into N2O and its subsequent emission from agricultural soils •Biomass burning •Raising cattle Lifespan •110 years •Destroyed in the stratosphere by solar radiation Location •Troposphere •Stratosphere Does it do us any good? •Helps regulate temperature Ozone - O3 Natural Source •Formed when O2 molecule photodissociates after absorbing an IR photon •Free O molecule bonds with O2 to form O3 Anthropogenic source •Chlorofluorocarbons (CFC’s) contain molecules which can destroy ozone in the stratosphere •Tropospheric ozone formed from reactions with carbon monixide, methane, and other volitile organic compounds •Tropospheric ozone is found in smog Lifespan •Tropospheric ozone (a few days) •Stratosphere – long lived due to the oxygen-ozone cycle Location •Stratosphere (Ozone Layer) •Troposphere (harmful) •Mesosphere Does it do us any good? •Stratospheric ozone protects us from 97-99% of the sun’s UV radiation Some GHG Concentration Trends NOAA | accessed via Wikipedia What if … there were no GHG’s? Would Earth be very hot or very cold? … WHY? VS. Would the air be very dry or very wet? Hint: What is the most abundant GHG? Goldilocks Principle Earth … Just Right Venus … Too Hot Mars .. Too Cold Extremely dense Almost no atmosphere Perfect atmosphere to atmosphere High concentration of CO2 High surface temperature of 464˚C Low concentration of sustain life Correct concentration of GHG’s Temperature range of 10˚C to 20˚C NASA | Image processing by R. Nunes CO2 Wide temperature range of -135˚C to 30˚C NASA | accessed via Wikipedia NASA | accessed via Wikipedia NASA | accessed via Wikipedia Global Warming? Why do we use the term “Global Warming”? 2000–2009 was the warmest decade on record worldwide