Lecture 12 Big Problems. Global Warming The E-M Spectrum.

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Transcript of Lecture 12 Big Problems. Global Warming The E-M Spectrum.

Lecture 12

Big Problems

Global Warming

The E-M Spectrum

Fate of Solar Radiation Fate of Solar Radiation Reaching the EarthReaching the Earth

reflectionreflectioncloudsclouds

snow and icesnow and ice

the earth’s surfacethe earth’s surface

atmospheric dustatmospheric dust

reflectionreflectioncloudsclouds

snow and icesnow and ice

the earth’s surfacethe earth’s surface

atmospheric dustatmospheric dust

Fate of Solar Radiation Fate of Solar Radiation Reaching the EarthReaching the Earth

absorptionabsorptionatmosphereatmosphere

oceansoceans

landland

plant photosynthesisplant photosynthesis

absorptionabsorptionatmosphereatmosphere

oceansoceans

landland

plant photosynthesisplant photosynthesis

Fate of Solar Radiation Fate of Solar Radiation Reaching the EarthReaching the Earth

radiationradiationradiationradiation

The Greenhouse Effect

Greenhouse GasesGreenhouse Gases

Carbon DioxideMethane

Nitrous OxideWater Vapor

Ozone

                                                                                                          

                                               Thousands of Years Before Present

Tem

per

atu

re C

han

ge

(oF

)

Atm

osp

her

ic C

O2

(pp

m)

Year

Temperature

Carbon Dioxide

Tem

per

atu

re C

han

ge

(oF

)

Atm

osp

her

ic C

O2

(pp

m)

Atmospheric CO2 & Surface Temperature TrendsAtmospheric CO2 & Surface Temperature Trends

Sea level rise

Increased plant primary productivity

Shifts in the distribution of plants and animals

Water contamination and outbreaks of water-borne diseases

Increased storm severity

Potential melting or enlargement of polar ice caps

Changes to patterns of rainfall

More severe droughts or increased precipitation

changes to ocean circulation patterns

Predicted changes with increased greenhouse warming

Ice Age 18,000 years ago

Sea Level Changes due to Ice Ages and Ice Cap Melting

                                                                                                                    

                                     

Year

Ch

ang

es in

Mea

n S

ea L

evel

Mean Sea Level RiseMean Sea Level Rise

                                                                                                                   

                                      

Summer Arctic Sea Ice Decline Comparison between 1979 & 2005Summer Arctic Sea Ice Decline Comparison between 1979 & 2005

Early Fall Arctic Sea Ice ExtentEarly Fall Arctic Sea Ice ExtentS

ea Ic

e E

xten

t (m

illio

n k

m2 )

Year

    

                 

Greenland Seasonal Surface Melting

Surface melting

Permafrost

Permafrost

                 

                                   

Permafrost melting

Permafrost melting

Permafrost melting

Drunken forest

Year

North Atlantic Tropical Storms10-year running average

North Atlantic Tropical Storms10-year running average

Nam

ed T

rop

ical

Sto

rms

1 Meter Sea Level Rise Waikiki1 Meter Sea Level Rise Waikiki

http://www.soest.hawaii.edu/HMRG/FloodingOahu/index.phphttp://www.soest.hawaii.edu/coasts/sealevel/waikiki.html

Sea Level Rise

• Destroys coastal habitat (e.g. salt marshes, mangroves)

• Destroys human property• Increases pollution• Decreases freshwater supply

Effect on Marine Life• Phytoplankton bloom due to light and

temperature cues• Changes will impact food web• Hypoxia may result

Effect on Fisheries

• Migrations are in response to temperature• May impact fisheries

Effect on Corals• Coral bleaching • Leads to loss of habitat and food for reef-

dependent species

CurrentsOceanic conveyor belt may change ocean currents • Currents carry plankton• Bring food and oxygen• Distribute eggs and larvae• Remove wastes and pollutants

Salinity• Animals have a narrow range of tolerance• Glacial melting inputs lots of freshwater

Acidity• CO2 makes water acidic• Corals and other calcium carbonate species

can’t make skeleton• Impact on plankton development impacts food

web

Temperature• Higher temperature results in less O2

- Results in hypoxia• Ice melting leaves no resting/hunting areas for

polar bears• Antarctic Krill impacts food web

Larsen B Ice Shelf

• 220 m thick• Lost 5700 km2

(2x Rhode Island)

• Reduction of 40%

Invasive Species• Algae smothers coral• Invasive species out-compete natives

Weather Events

More severe weather patterns• El Niño• Hurricanes • Mudslides• Forest Fires• Drought

Sea Surface Temperature

July 24, 2012 http://www.elnino.noaa.gov/

Origin and paths of tropical cyclones

• Tropical cyclones are intense low pressure storms created by:

– Warm water

– Moist air

– Coriolis effect

El Niño-Southern Oscillation (ENSO)

• El Niño = warm surface current in equatorial eastern Pacific that occurs periodically around Christmastime

• Southern Oscillation = change in atmospheric pressure over Pacific Ocean accompanying El Niño

• ENSO describes a combined oceanic-atmospheric disturbance

El Niño

• Oceanic and atmospheric phenomenon in the Pacific Ocean

• Occurs during December• 2 to 7 year cycle

Sea Surface Temperature

Atmospheric Winds

Upwelling

Normal conditions in the Pacific Ocean

El Niño conditions (ENSO warm phase)

La Niña conditions (ENSO cool phase; opposite of El

Niño)

El NiñoNon El Niño

1997

Non El Niño

El Niño

thermocline

upwelling

El Niño events over the last 62 years

82-83

65-6672-73

57-5886-87 91-92

94-95

97-98

02-0309-10

Red - Strong El NinoBlue- Strong La NinaBlack – moderate (either)

50-5155-56

64-65

70-71

73-74

75-7688-89

98-9999-00

07-08 10-11

11-12

1969 1951 1957 1950 1955 1973

1976 1963 1965 1954 1970 1975

1977 1968 1972 1956 1998 1988

2004 1986 1982 1962 2007 1999

2006 1987 1997 1964 2010

1991 1967

1994 1971

2002 1974

2009 1984

1995

2000

El Niño La Niña

Weak Mod Strong Weak Mod Strong

2011

Effects of severe El Niños

• Ozone (O3) protects life on earth from the damaging affects of ultraviolet radiation (UV)

• Natural produced by sun’s energy in stratosphere and lightening

• Ozone destroyed by CFC’s

• Studies suggest that the ozone layer hasbeen gradually “thinning” since 1975.

Human activities are depleting the atmospheric ozone

Ultraviolet Radiation

“A threat to the continuation of life”2

Humans: DNA damageCancer

Crops: Productivity decreaseOcean plants: Death?

VisibleInfrared (IR) UV

Ultraviolet Radiation

stratosphericozone layer

CFCs: refrigerationelectronics

foam packagingspray propellants

destroy

UV

‘96: CFC decrease noticed2006: stabilization?

‘96: CFC decrease noticed2006: stabilization?

Antarctic Total Ozone Trend

400

1950 1960 1950 1950 1950 1950 2010

300

200

100

0

To

tal o

zon

e (

Dob

son

uni

ts)

Ozone blocks UV

Oct. 1979

Oct. 2011

Size of the Antarctic ozone holeAverage Area: millions sq km

North AmericaNorth America

AntarcticaAntarctica

Prediction: 50 years to return to 1980 size

1979 2001

30

20

10

0

Natural Phenomena

Upperatmosphereresearch satellite

Volcanicemissions?

Sea spray?

Directevidence

Directevidence

sunspots

Why is it Important?

Early Warning

If global warming, likely more serious consequences

Nuclear Contamination

3

SEVERE

HIGH

ELEVATED

GUARDED

LOW

Ocean Dumping

total > 10 million Curiestotal > 10 million Curies

Three Mile Island (‘79) = 17 CuriesChernobyl (‘86) = 100 million CuriesFukushima (2011) = 60 million Curies

US

Other

Switzerland

GreatBritain

USSR

Arctic Ocean

Russia

Soviet Union’s Atomic Dumping Ground

Moscow

Human Population Growth

CrowdingResource depletionWater shortagesEpidemic diseasesFood supply limitations

“Population Wars”

4

World Population

0

2,000

4,000

6,000

8,000

10,000

12,000

1500 1700 1900 2100

estimates(millions)

Year

How is the trend changed?

How is the trend changed?

Can Society Respond

• Has society become skeptical

• Must we assign blame

• Is there leadership

• Can we get multinational agreements

• Can we afford it

Questions

• CFC’s contribute to:• Major gasses involved in global warming

are:• Global warming may result in these

environmental consequences:• A severe El Nino can cause _______ in

California.• Much of Russia’s nuclear waste is stored

_______.