Global Warming - Environmental Science - Lecture Slides, Slides of Environmental Science

This lecture is from Environmental Science course. It covers very important aspects of our environment. Some points from these lecture slides are: Global Warming, Other Global Weather Changes, Global Temperature Changes, Global Precipitation Changes, Causes of Global Warming, Keeping Earth Warm, Greenhouse Effect, Spectrum of Sunlight, Greenhouse Gases, Ir Absorption Spectrum, Carbon Dioxide Concentrations, Carbon Dioxide Sinks, Nitrous Oxide and Global Warming, Aerosols and Clouds

Typology: Slides

2013/2014

Uploaded on 01/30/2014

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Global Warming

th 20

Century Climate Changes

  • Global Warming– Average Global Temp. = 24 h, all seasons, all locations
    • Increased 0.

o^ C (1.

o^ F) from 1900—

  • Not uniform: some places cooler (S. E. United States)• Largest increase is in the daily low temperature• Not a continuous change over time (largest change last 25 yr)
    • Other Global Weather Changes– Increased Average Precipitation (not uniform)– Shorter winters in N. Hemisphere (blooming/leaf loss)– Shrinking glaciers and polar ice caps– Dieing coral, rising sea level, more extreme weather
  • Global Temperature Changes 1901--
  • Global Precipitation Changes 1901--

Spectrum of Sunlight (dotted) and Earth’s Emitted light

The Greenhouse Effect

Greenhouse Gases (G.G.)

  • Definition = atmospheric gas that efficiently absorbsIR light emitted by Earth– N

, O 2 2

, Ar = main atmospheric gases = not G. G.

  • Water Vapor (H

O) is the most important G.G. 2

  • Naturally present from evaporation• Concentration is variable depending on season, geography• Absorbs around 7

m and above 18

m

  • Carbon Dioxide (CO

) next most important G.G. 2

  • Most from natural sources: decay of plant matter• About one-third comes from man’s combustion of fossil fuels• Absorbs at 4

m and 15

m strongly

The IR absorption spectrum of CO

2

The atmospheric IR absorption spectrum

Carbon Dioxide Concentrations

  • Analysis: how do we know what the CO

level is? 2

  • now = clean air sample– past = bubbles trapped in glaciers• Results– Pre-Industrial Revolution (before 1750) = 280 ppm CO

2

  • 2001: 371 ppm CO

2

  • 1.6 ppm per year increase– Seasonal Concentrations• Low in summer as plants grow and use up CO

2

  • High in winter as plants die and decay releasing CO

2

docsity.com

Anthropomorphic CO

Sources 2

  • Fossil Fuel Combustion—major source– Coal, oil, natural gas, gasoline produce CO

when burned 2

  • Propane: C

H 3 8

+ 5 O

----> 3 CO 2

+ 4 H 2

O 2

  • Has slowed down recently due to collapse of SovietBlock economies• Quicklime Production—minor source (few %)– Used in cement production– CaCO
  • Heat ----> CaO (quicklime) + CO 3

2

  • Burning Vegetation: forests, farmland (25% of CO

) 2 docsity.com

World CO

Emissions from Fossil Fuel 1950-1999 2

Annual net movement of CO

in the Atmosphere 2

Methane and Global Warming

  • Concentration doubled since 1750 (most since 1900)• CH

21 times worse than CO 4

for IR ----> Heat 2

– CO

concentration is 80 times that of CH 2

in air 4

– CH

not as important overall as CO 4

2

  • Sink = oxidation to CO

2

– CH

+ 2 O 4

----> CO 2

+ 2 H 2

O 2

  • Takes about 10 years for this to happen on average• Methane sources– Anaerobic Respiration: 2 CH

O ----> CH 2

+ CO 4

2

  • Swamps, marshes (swamp gas, marsh gas)– Ruminant animal digestion (sheep, cows)– Landfill decomposition, pipelines, coal mines, oil wells