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Energy Balance and Global Temperature

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Page 1: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Energy Balance and Global Temperature

Page 2: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Global Temperature Controls

• Latitude• Altitude• Cloud cover• Direction of Prevailing Winds• Ocean Currents• Principal of Continentality

– Differential heating of land and water

Page 3: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Radiation and Temperature

Daily temperature cycle– Radiation: Most? Least? - Temp:

Most? Least?

Annual temperature cycle– Radiation: Most? Least? - Temp:

Most? Least?

Page 4: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Radiation and Temperature

Daily temperature cycle– Radiation: Most? Least? - Temp:

Most? Least?

Annual temperature cycle– Radiation: Most? Least? - Temp:

Most? Least?Conclusion: heat transfer takes time,

so temperature lags behind radiation.

Page 5: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Heat Transfer

Atmosphere and oceans transfer heat from the tropics to the poles.

Page 6: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Global Energy Balance

NO. Why not?

Page 7: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

REVIEW:Methods of Heat

Transfer• Radiation (no medium, no mass transfer)• Conduction (sensible heat - solids)• Convection (sensible heat - fluids)

• Latent heat (not sensible, H2O changes of state)

Page 8: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Principle of Continentality

The further a location is from an ocean, the more dramatic its annual and daily changes in temperature.

Thus, the hottest and coldest areas of the earth are found in continental interiors, while marine locations are generally very mild.

Page 9: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Annual Temperature Ranges

Page 10: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

The Earth’s Radiation

• Global climate stable? Energy in (sun) = energy out (earth)

• Earth – lower temperature (15ºC) than sun (6000ºC) – terrestrial radiation is longwave (max. at 10

microns)– the atmosphere is a GOOD absorber and

emitter of longwave (LW) radiation

Page 11: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

The Greenhouse Effect

Page 12: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

The Greenhouse Effect• Keeps Earth’s average temperature 35ºC warmer (15ºC now, -20 ºC otherwise)

• Human role? ‘A heated debate’

Venus 480ºC thick carbon dioxide

Mars -62 ºC little carbon dioxide

Page 13: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

The Global Warming HypothesisHuman-induced rise in CO2 levels is theorized to lead to unnatural warming of atmosphere.

• Likely effects: – Increased storminess– Rising sea level – Loss of arable land (some areas hotter, others cooler)– Extinction of thousands of species– Loss of nearly all coral reef

• Possible effects even include climate “flip-flop” wherein dangerous rapid cooling sets in!

Page 14: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

b

Page 15: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Global Surface Temperature Increase

1860-1997

Page 16: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Critics note that historic temperatures were higher.

Page 17: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Critics note that historic temperatures were higher.

Page 18: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Critics note that historic temperatures were higher.

The Pleistocene is the geologic epoch that covers the period from 10,000 to 2 million years ago. The Pleistocene was marked by a series of glacial and interglacial periods.

Page 19: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Historic correlation between C02 and

temperature

Page 20: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Changes in Solar Radiation

• 21,000 year cycle: perihelion shifts throughout the year

• 41,000 year cycle: +/- 1.5° change in Earth's tilt

• 100,000 year cycle: Orbital eccentricity of the elliptical orbit of the Earth

The most recent ice age lasted 100, 000 years. We are currently in an interglacial period (Holocene).

Milankovitch Cycles explain much (60%+) of the changes:

Page 21: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

So is Global Warming Happening? How much?

GLOBAL average temperatures will likely rise by 2.2-10°F (1.4-5.8°C) by the year 2100, according to the most authoritative report yet produced by the UN Intergovernmental Panel on Climate Change (IPCC). These are massive increases over the .5C rise seen over the last 100 years.

Source: UN IPCC, 2001

Page 22: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

So is sea level rise happening? How much?

GLOBAL average sea levels will likely rise by .5 - .9 meters (1.5 – 2.7 feet) by the year 2100, according to the most authoritative report yet produced by the UN Intergovernmental Panel on Climate Change (IPCC). When added to storm surges and high tides, these small changes may have large effects.

Source: UN IPCC, 2001

Page 23: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

So is Global Warming Happening? How much?

"Climate change will bring warm, wet weather, which will encourage plants to grow, followed by long periods of drought, during which they will burn. We can already see this in Florida," - Meinrat Andreae, Max Planck Institute

for Chemistry, August 2001.

"One person flying in an airplane for one hour is responsible for the same greenhouse gas emissions as a typical Bangladeshi in a whole year," - Beatrice Schell, European federation for Transport and Environment, November 2001.

Page 24: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

So is Global Warming Happening?

“…a wide range of careful studies shows that the changes in global temperature observed during the 20th century, including some patterns of change, were likely to have been significantly greater than those resulting from natural variability alone. The world's best climate scientists agree that the balance of evidence suggests that there is a discernible influence on global temperature. This conclusion is steadily being strengthened.” (Engineers for Social Responsibility, 2002)

• “”We must act to ensure continued economic growth for our citizens and for citizens throughout the world," - George W Bush, June 2001, Explaining his opposition to the 1997 Kyoto Protocol, a document that calls for only 5% reduction of greenhouse gases. IPCC says 60% reduction needed to stabilize levels.

Page 25: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Key Points - Temperature

• Global temp. controls• Global energy balance• Heat transfer• Greenhouse effect

Bondi Beach, Sydney Australia, Study Abroad - 01/2001

Franz Joseph Glacier, New Zealand Study Abroad - 01/2001

Page 26: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Predicted temperature changes: Hadley Centre model

Source: UKMO Hadley Center [http://www.met-office.gov.uk/research/hadleycentre/]

Page 27: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Predicted precipitation changes: Hadley Center model

Source: UKMO Hadley Center [http://www.met-office.gov.uk/research/hadleycentre/]

Page 28: Energy Balance and Global Temperature. Global Temperature Controls Latitude Altitude Cloud cover Direction of Prevailing Winds Ocean Currents Principal

Ecosystem change

• Very difficult to model!

• Response depends on CO2 fertilization, temperature, Precipitation, evapotranspiration, competition,...