Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and...

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Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean interactions ENSO

Transcript of Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and...

Page 1: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Earth Systems and Resources, 10-15% The Atmosphere

•Composition •Structure (layers) •Weather and climate•Atmospheric circulation and the Coriolis Effect•Atmosphere–ocean interactions•ENSO

Page 2: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

College Board: Air Pollution• Sources — primary and secondary • Major air pollutants• Measurement units• Smog• Acid deposition — causes and effects• Heat islands and temperature inversions • Indoor air pollution; remediation and reduction• strategies • Clean Air Act and other relevant laws

Page 3: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Troposphere – ‘Sky’• 75% of mass of atmosphere• 0 to 11 miles in altitude• 78% nitrogen, 21% oxygen

(+ H2O, CO2)

• Location of ‘weather’• Temperature decreases with

altitude (lower pressure) until the next layer is reached

Page 4: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Stratosphere

• 99% of ultraviolet radiation (especially UV-B) is absorbed by the stratosphere• Temperature increases

with altitude• Ozone

• Ozone (O3) = O2 + O2 + lightning/sunlight = O3

Page 5: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Mesosphere

• The temperature decreases with increasing altitude

Page 6: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Thermosphere• Temperature increases with

increasing altitude• Very high temperatures,

very few molecules

Page 7: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Layers of the Atmosphere

• Thermosphere – ‘top’ layer; absorbs solar radiation

• Mesosphere – middle layer; most meteors ‘melt’ here

• Stratosphere - UV absorbed by ozone

• Troposphere – ‘sky’; decreasing temperature; 78%, 21%

Page 8: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Climate: Introduction

• Weather – the condition of the atmosphere in a local area• Temperature, atmospheric pressure, cloudiness,

wind, humidity and precipitation• Climate - a larger area’s average weather conditions

over a looonnng time• Seasons • More direct sun – summer• Less direct sun - winter

Page 9: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• Warmer molecules rise, cooler molecules fill the space• The surface of the earth heats

unevenly• Land masses change

temperature faster than water

• Wind – moving air mass

http://www.youtube.com/

watch?v=klOhwR5h_Aw

Page 10: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• Caused by a pressure gradient:• Cooler air has more air pressure (air is more dense)

warmer air has less pressure (air is less dense) • Air moves from cooler, high pressure air to warmer,

low pressure• Wind – movement of air

Wind

Page 11: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Global Air Circulation

• Six giant convection cells occur at different latitudes• Heat and moisture are circulated

around but not evenly• Pattern of circulation creates

different climates (biomes)• Deserts around ___ latitude• Rains around ___ latitude• ‘Horse’ latitudes – ‘doldrums’

Page 12: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Ocean Currents: Distribute Heat and Nutrients

• Ocean currents influence climate by distributing heat from place to place and mixing and distributing nutrients.

http://www.youtube.com/watch?v=6vgvTeuoDWY&edufilter=vH8ntV7keCE-ZLl5wRMzNg

Page 13: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Breezes• Mountain breeze - cooler air sinks down causing

increased winds on the mountain.• Valley breeze – air mass is forced into a smaller area

which causes high winds to form through the valleys• Warm, moist air masses hitting cooler air on the tops of

mountains causes the moisture in the air to condense forming precipitation

• Valleys are often fertile, good places for crops

Page 14: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• Pressure – molecules pushing • Air pressure - the weight of the air/atmosphere • At sea level – 14.7 pounds per square inch• 760mm Hg (1 Barr)

• Barometer measures atmospheric pressure

Altitude Affects Temperature

Page 15: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Rain shadow effect

Page 16: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

The Coriolis Effect

• The rotation of the Earth on its axis that deflects winds to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.

http://www.youtube.com/watch?v=i2mec3vgeaI&edufilter=vH8ntV7keCE-ZLl5wRMzNg

http://www.youtube.com/watch?v=XiYs4QBWTOo&edufilter=vH8ntV7keCE-ZLl5wRMzNg

Page 17: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

ENSO• El Nino – Southern Oscillation• Disruption of the normal ocean-air interactions• Pushes down the upwelling of nutrients from the

ocean floor – less nutrient = less primary productivity

• Rain patterns change – drought in some places, heavy rain in others

• Colder winters in NE US, more Atlantic hurricanes

Page 18: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Pollutants• Produced from a source into the atmosphere• Particulates (particles), gases• Natural causes: • Volcanoes, fires, sea salt, pollen, dust, decaying

vegetation• Anthropogenic – caused by humans• Methane, various oxides, ozone, dust particles,

microorganisms, and chlorofluorocarbons (CFC’s)• Anthropogenic causes of Primary Pollutants –

factories, cars, power generation

Page 19: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Air Pollution – Primary and Secondary Pollutants

• Primary air pollutants – produced directly into the atmosphere

• Secondary air pollutants – produced when primary air pollutants react

Page 20: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Primary Pollutants

CO CO2Secondary Pollutants

SO2 NO NO2

Most hydrocarbons SO3

Most suspended particles HNO3

H2O2 O3 PANs

Most NO3– and SO4

2– salts

Sources Natural Stationary

Mobile

H3SO4

Page 21: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Major Pollutants

• Carbon oxides (CO, CO2)

• Nitrogen oxides (NO, NO2, HNO3)

• Sulfur oxide (SO2, H2SO4)

• SPM (Suspended Particulate Matter)• Ozone • VOCs – (Volatile Organic Compounds)• Radon

Page 22: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Major Pollutants• Carbon oxides: • Carbon monoxide (CO) is a highly toxic gas that

formed from incomplete combustion of carbon-containing materials (cars)

• 93% of carbon dioxide (CO2) in the troposphere occurs naturally as a result of the carbon cycle.

• 7% of CO2 in the troposphere is anthropogenic (burning fossil fuels; coal, oil)

• It is not regulated as a pollutant under the U.S. Clean Air Act

Page 23: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Major Pollutants• Nitrogen oxides and nitric acid: • Nitrogen oxide (NO) forms when nitrogen and

oxygen gases react in car engines and coal-burning plants

• NO can also form from lightening, soil and legumous bacteria (nitrogen fixation)

• NO reacts with air to form NO2

• NO2 reacts with water vapor in the air to form nitric acid (HNO3), acid deposition (Secondary pollutant)

Page 24: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Major Pollutants

• Sulfur dioxide (SO2) and sulfuric acid:

• About one-third of SO2 is natural

• Anthropogenic – sulfurous coal, oil refining and smelting of sulfur ores (S+ O2 SO2)

• SO2 in the atmosphere can be converted to sulfuric acid (H2SO4) and sulfate salts (SO4

2-) creating acid deposition (secondary pollutant)

Page 25: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Major Pollutants

• Suspended particulate matter (SPM):• A variety of solid particles and liquid droplets that

remain suspended in the air.• The most harmful forms of SPM are fine particles

(PM-10, with an average diameter < 10 micrometers) and ultrafine particles (PM-2.5).

• According to the EPA, SPM is responsible for about 60,000 premature deaths a year in the U.S.

Page 26: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Major Pollutants

• Ozone (O3):• A highly reactive gas that is a major component of

photochemical smog (secondary pollutant).• It can: • Cause and aggravate respiratory illness.• Can aggravate heart disease.• Damage plants, rubber in tires, fabrics, and

paints.

Page 27: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Major Pollutants• Volatile organic compounds (VOCs):• Most are hydrocarbons emitted by the leaves of

many plants and methane.• About two thirds of global methane is anthropogenic

• Industrial solvents such as trichloroethylene (TCE), benzene, and vinyl chloride.• Long-term exposure to benzene can cause cancer, blood

disorders, and immune system damage.

Page 28: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• Radon (Rn):• A naturally occurring radioactive gas found in some

types of soil and rock.• It can seep into homes and buildings above

Page 29: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Secondary Pollutants

• Form when primary pollutants react in the atmosphere• Smog• Photochemical Smog• Acid precipitation/deposition

Page 30: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Secondary Pollutants

• Smoke + fog = Smog• Sulfur dioxide + droplets of sulfuric acid + various

particulates (smoke, ash) produced by burning coal.

• In most developed countries, industrial smog is not a problem because of good pollution controls

Page 31: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Photochemical Smog

• Mixture of air pollutants produced by the reaction of nitrogen oxides + volatile organic hydrocarbons in the sunlight.

Page 32: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Acid Deposition• Acid deposition consists of rain, snow, dust, or

gas with a pH lower than 5.6.

Page 33: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Acid Deposition

• Sulfur dioxides, nitrogen oxides, and particulates react in the atmosphere to produce acidic chemicals that can travel long distances before returning to the earth’s surface.• Tall smokestacks reduce local air pollution but

can increase regional air pollution.• Acid deposition contributes to chronic

respiratory disease and can leach toxic metals (such as lead and mercury) from soils and rocks into acidic lakes used as sources for drinking water.

Page 34: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Acid Deposition• Air pollution is one

of several interacting stresses that can damage, weaken, or kill trees and pollute surface and groundwater.

Page 35: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Factors Influencing Levels of Outdoor Air Pollution

• Outdoor air pollution can be reduced by:• settling out, precipitation, sea spray, winds, and

chemical reactions. • Outdoor air pollution can be increased by:• urban buildings (slow wind dispersal of pollutants),

mountains (promote temperature inversions), and high temperatures (promote photochemical reactions).

Page 36: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Temperature Inversions• Cool, cloudy weather in a valley surrounded by

mountains can trap air pollutants (left).• Areas with sunny climate, light winds, mountains

on three sides and an ocean on the other (right) are susceptible to inversions. (L.A., Birmingham)

Page 37: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Reducing Outdoor Air Pollution

• Coal-fired, electric-generating plants:• Electrostatic precipitator: are used to attract

negatively charged particles in a smokestack into a collector

• Wet scrubber: fine mists of water vapor trap particulates and convert them to a sludge that is collected and disposed of usually in a landfill.

Page 38: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Using the Marketplace to Reduce Air Pollution

• The Clean Air Act established ‘Cap and Trade’ to help reduce SO2 emissions

• Enables the 110 most polluting power plants to buy and sell SO2 pollution rights

• Incentive to build ‘green’ technologies to reduce pollutants

• Between 1990-2002, emissions were reduced

Page 39: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Reducing Outdoor Air Pollution

• Prevent and control air pollution from motor vehicles• Clean Air Act - a new car in the U.S. emits 75% less

pollution than pre-1970 cars.• Increased motor vehicle use in developing countries;

many have no pollution control devices and burn leaded gasoline (lead emissions high)

Page 40: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

The Natural Greenhouse Effect• Greenhouse gases - keeps earth warm

• Water vapor• Carbon dioxide• Methane• Nitrous oxide

• Fluctuations in gases, plus changes in solar output cause the fluctuations in temperature over the past 400,000 years

• Temperatures have remained fairly stable but began to rise during the last century

Page 41: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

How Do We Know What Temperatures Were in the Past?

• Scientists analyze tiny air bubbles trapped in ice cores learn about past:• troposphere composition. • temperature trends.• greenhouse gas concentrations.• solar, snowfall, and forest fire activity.

Page 42: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Global Warming• Considerable scientific evidence and climate models

indicate that large inputs of greenhouse gases from anthropogenic activities into the troposphere can enhance the natural greenhouse effect and change the earth’s climate in your lifetime.

• In 2005, an ice core showed that CO2 levels in the troposphere are the highest they have been in 650,000 years.

http://www.youtube.com/watch?v=oJAbATJCugs&edufilter=vH8ntV7keCE-ZLl5wRMzNg

http://www.youtube.com/watch?v=rweblFwt-BM&edufilter=vH8ntV7keCE-ZLl5wRMzNg

Page 43: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• Increase in average concentration of three greenhouse gases between 1860 and 2004

• Mostly due to: • Burning fossil fuels• Deforestation• Agriculture

Page 44: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• Evidence of Global Warming:• The 20th century was the hottest century in the past 1000

years• Since 1900, the earth’s average tropospheric temperature has

risen 0.6 C°.• Over the past 50 years, Arctic temperatures have risen almost

twice as fast as those in the rest of the world.• Glaciers and floating sea ice are melting and shrinking at

increasing rates.• Warmer temperatures in Alaska, Russia, and the Arctic are

melting permafrost releasing more CO2 and CH4 into the troposphere.

• During the last century, the world’s sea level rose by 10-20 cm, mostly due to runoff from melting and land-based ice and the expansion of ocean water as temperatures rise.

Page 45: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Factors Affecting Temperature

• Some factors can amplify (positive feedback) and some can slow (negative feedback) projected global warming

• Oceans may remove heat and CO2

• Warmer temperatures create more clouds that could warm or cool the troposphere

Page 46: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• 70% of the solar radiation that falls on Earth is absorbed and runs the water cycle, drives winds and ocean currents, powers photosynthesis, and warms the planet.

Solar Radiation - Absorption

Page 47: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Rising Sea Levels

• During this century rising seas levels are projected to flood low-lying urban areas, coastal estuaries, wetlands, coral reefs, and barrier islands and beaches.

Page 48: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Changing Ocean Currents• May cause both excessive warming and severe cooling• A warmer troposphere may decrease the ability of the

ocean to remove and store CO2 by decreasing the nutrient supply for phytoplankton and increasing the acidity of ocean water.

• Global warming will lead to prolonged heat waves and droughts in some areas and prolonged heavy rains and increased flooding in other areas

Page 49: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Effects of Global Warming

• Agricultural productivity may increase in some areas and decrease in others

• Rising sea levels could reduce crop and fish production by flooding areas coastal areas

• Increase deaths from:• Heat and disruption of food supply.• Spread of tropical diseases to temperate regions.• Increase the number of environmental refugees.

Page 50: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• Climate change is a difficult problem to deal with because:• The problem is global.• The effects will last a long time.• Many actions that might reduce the threat are

controversial because they can impact economies and lifestyles.

• The problem is a long-term political issue.• The harmful and beneficial impacts of climate

change are not spread evenly.

Page 51: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

• Two ways to deal with global warming:• Mitigation - reduce greenhouse gas emissions

• Use less fossil fuels• Replace coal with natural gas• Shift to clean, renewable resources (solar, wind)• Scrubbers, precipitators, catalytic converters

• Adaptation - devise strategies to reduce effects of emissions• Plant, replant trees • Give energy technologies to developing nations• Limit urban sprawl

Page 52: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Pollution Control Devices

• Emission Control Devices – filter particles• Scrubbers – use water to filter particles and gases• Catalytic Converters – on cars; finish burning wastes

to decrease carbon monoxide levels

Page 53: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

The Kyoto Protocol – Treaty on Global Warming• Started January, 2005• 189 countries signed• Global companies (BP, IBM, Toyota) have plans to

reduce emissions• Requires 38 participating developed countries to cut

their emissions of CO2, CH4, and N2O by 2012• Developing countries were excluded• U.S. did not sign because developing countries

(China, India and Brazil) were excluded• California and Maine participate

• Kyoto will have little effect without US, China and India

Page 54: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Ozone Depletion

• Ozone layer in the stratosphere keeps about 95% of the sun’s harmful UV radiation from reaching the earth’s surface

• UV damages: DNA, phytoplankton, skin cancer• Chlorofluorocarbon (CFCs) destroys ozone • Halogens (chlorine, bromine, iodine) from: fire extinguishers,

propellants, solvents

• Montreal Protocol - 1988, banned production of CFCs

http://www.youtube.com/watch?v=bZWrSr7c09k&edufilter=vH8ntV7keCE-ZLl5wRMzNg

http://www.youtube.com/watch?v=lD6xnAVvPbQ&edufilter=vH8ntV7keCE-ZLl5wRMzNg

Page 55: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Indoor Air Pollution• Usually is a greater threat to health than outdoor air

pollution (?)• Four most dangerous indoor air pollutants in developed

countries are:• Tobacco smoke• Formaldehyde• Radioactive radon-222 gas.• Very small fine and ultrafine particles.

Page 56: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Chloroform

Benzo-a-pyrene

Styrene

Radon-222

Methylene Chloride

Tobacco Smoke

Carbon Monoxide

Asbestos

Nitrogen Oxides

1, 1, 1-Trichloroethane

Particulates

FormaldehydeTetrachloroethylene

Para-dichlorobenzene

Page 57: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Air Pollution Kills

• Each year, air pollution prematurely kills about 3 million people, mostly from indoor air pollution in developing countries.• In the U.S., estimated annual deaths from indoor

and outdoor air pollution range from 150,000 to 350,000.

• According to the EPA, each year more than 125,000 Americans get cancer from breathing diesel fumes.

Page 58: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Clean Air Act(s)• 1963 • 1970, 1977 and 1990 - amended• Involves EPA• Sets standards for acceptable levels of sulfur oxides,

nitrogen oxides, ozone, carbon monoxide, hydrocarbons, lead, et.al

• Provides pollution credits for industries that utilize pollution-control devices (Cap and Trade)

• It established NAAQS and AQI

Page 59: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

National Ambient Air Quality Standards (NAAQS)

• Sets acceptable concentrations for 6 “criteria” pollutants that:• Threaten public health/the environment over broad

areas (non-point)• Are emitted in large quantities

• CO, Pb, NOx, Ozone, Particulates and SO2

Page 60: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Air Quality Index (AQI)

• Measures levels of 5 criteria pollutants• Forecast of daily air pollution levels• Purpose to educate and protect public- focuses on

health effects• Categories: green= good, yellow= moderate, orange=

unhealthy for sensitive groups, red= unhealthy, purple= very unhealthy

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National Emissions Standards for Hazardous Air Pollutants• Regulates emissions (from point sources)• For specific substances (air toxics w/ known or

suspected serious health effects (mutagens, carcinogens, neurotoxins)

• Tend to be local, from point sources• Ammonia, chlorine, asbestos, arsenic, mercury,

benzene

Page 62: Earth Systems and Resources, 10-15% The Atmosphere Composition Structure (layers) Weather and climate Atmospheric circulation and the Coriolis Effect Atmosphere–ocean.

Laws and Regulations:• Kyoto Protocols – reduce greenhouse gas emissions• Global; US – no

• Montreal Protocols – ban production of CFC’s to prevent loss of ozone • Global; US – yes

• Clean Air Act(s) – reduce air pollutants• US - EPA• NAAQS – sets standards for amount of pollutants that can

be emitted • AQI – measures and forecasts major pollutants