Weather and Climate are closely related, yet distinct concepts that play a significant role in our daily lives and the environment.
Weather: Describes the current physically conditions of the atmosphere (temp, moisture, pressure, wind)
Climate: description of long-term pattern of weather in a particular area
Both affect and are affected by human activities, and are the main determinants of the establishments of biomes and ecosystems.
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Atmospheric Development and composition
Earliest atmosphere believe to be composed of H gas and He, which is mostly diffused into space over billions of years
Volcanic emissions added C, N, O, S and other trace elements into current composition
The evolutionary development of photosynthetic producers added O2.
Current atmospheric composition is primarily N2 gas, O2 gas, H2O vapor, aerosols, particulates.
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The ZONES of our layered atmosphere
Troposphere
Exist from the surface up to 18 km (tropopause), fairly uniform chemical composition, variable temperature dropping with increased altitude.
Stratosphere
Extends from the tropopause (temperature gradient) up to 50 km, fairly stable temperature, 1000x lower moisture, 1000x greater ozone, earth's protective layer.
Mesosphere
Low temperature zone up to 80 km (ionosphere)
Thermosphere
High temperature zone, diminishing zone
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Weather Generation
The sun's insolation supplies the necessary heat and light energy
The incoming solar radiation is either absorbed or reflected depending on the location albedo
Greenhouse gasses such as carbon dioxide and methane efficiently trap the heat energy close to the surface creating the “Greenhouse Effect”, making earth life possible!
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The Role of Water in Weather Generation
Convection currents: created by vertical density gradient of different temperature air masses carry with the large amounts of water vapor created by evaporation, this transfer of latent energy creates cyclical pressure gradients
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Weather Patterns (circulation of weather)
The sun's energy is unevenly distributed due to the angle at which it strikes the earth's spherical shape, and the tilt of the planet.
convection currents are influenced by the earth's rotation, and the frictional drag close to the surface
Coriolis Effect: spiraling wind patterns created by the convection currents that are influenced by the earth's rotation
*Prevailing winds are named for the direction in which they originate.
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Jet Streams
Undulating hurricane force winds at the top of the troposphere
Affects weather pattern
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Conflicting weather (storms)
Front: The boundary between 2 air masses of different temperatures and density.
Cold Front: occurs when a cooler moving air mass displaces warmer air
Warm Front: occurs when a warmer moving air mass slides up and over a cooler air mass
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Storms
Hurricanes: large cyclonic ocean storms with heavy rain and winds exceeding 74 mph
Tornados: strong swirling winds and uplifts created when a strong cold front pushes under a warm moist air mass over land
Monsoons: A seasonal reversal of wing patterns caused by the different heating and cooling rates of ocean and continents creating prolonged heavy rains
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Natural Climate Variability
Milankovitch Cycles: are periodic shifts in the earth's orbits and axis tilt
Along with solar fluctuations, and galactic and geologic events, may explain major historical weather patterns. (ex. Ice ages, el nino, la nina)
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Anthropogenic Climate Change
Best evidence suggests recent human activity is increasing the “Greenhouse effect”, thus influencing global climate change.
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What are the effects, why should you care?
More extreme weather
Droughts, floods, heat waves, hurricanes, sea level rise
Loss/shift of habitat types
Increased economic and human costs
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Solutions (KYOTO Protocol)
Implementing emissions trading
Technology sharing with less developed countries
Modify behaviors (reduce deforestation, carbon capture, renewable energies)
Helping poorer countries respond to climate change
Air Pollution
Air Pollution: Foul, unclean, or dirty air
Can be naturally occurring (volcanoes, dust storms, sea spray, decomposition) or anthropogenic in origin, but concentration of airborne contamination in inhabited areas is almost entirely human caused
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Categories of Pollutants
Primary pollutants: Released directly from the source in a harmful form
Secondary Pollutants: Modified to a hazardous form after release
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Conventional (criteria) pollutants: Contribute the largest volume of air-quality degradation, identified by E.P.A (clean air act 1970)
Sulfur Oxide
SO2, SO3
Primarily generated by coal combustion and smelting
Acid Deposition: sulfuric acid precipitation, carried by prevailing winds, alter the pH of land and water
Economic
Nitrogen Oxides
Nitric Oxide (NO)
Eye and lung irritant, cellular harm
(HNO3) nitric acid deposition
Carbon Oxides and Hydrocarbons
Carbon Dioxide (CO2) and Carbon Monoxide (CO), primarily from fossil fuel combustion, and cement production
Methane (CH4) from decomposition and livestock farts and burps
CO gas is highly toxic
Overload of greenhouse gases
Heavy Metals and Halogens
Toxic metals such as Lead (Pb), Mercury (HG) and others, released during fossil fuel combustion, smelting, and waste incineration
Chlorofluorocarbons (CFCs) from spray propellants and refrigerants
Highly toxic materials, lead causes brain damage
CFCs diffuse into the stratosphere and destroy the UV protective ozone layer leading to increases in skin cancer and blindness.
Particulates and Aerosols
Respiratory distress
Large-scale smog (often magnified due to inversion)
Volatile Organic Compounds (VOCs)
Naturally occurring and synthetic organic compounds
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Unconventional Pollutants
Radon Gas
Carcinogen formed from the decay of naturally occuring uranium below ground
Aesthetic Degradation (excessive noice, odor, light)
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What can we do about air pollution
Particulate Removal
Industrial filters, precipitators, and scrubbers
Reduction (sulfur oxides, nitrogen oxides)
Limit use, cleaner burning fields, fossil fuel replacements.
Hydrocarbon Control
Minimize incomplete combustion