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SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between the poles and the equator. SC.912.E.7.3: Differentiate and describe the various interactions among Earth systems, including: atmosphere, hydrosphere, cryosphere, geosphere, and biosphere. SC.912.E.7.4: Summarize the conditions that contribute to the climate of a geographic area, including the relationships to lakes and oceans.
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SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Jan 14, 2016

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Mercy Underwood
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Page 1: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of

energy between the poles and the equator.

SC.912.E.7.3: Differentiate and describe the various interactions among Earth systems,

including: atmosphere, hydrosphere, cryosphere, geosphere, and biosphere.

SC.912.E.7.4: Summarize the conditions that contribute to the climate of a geographic area, including the relationships to lakes and oceans.

Page 2: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

SC.912.E.7.7: Identify, analyze, and relate the internal (Earth system) and external

(astronomical) conditions that contribute to global climate change.

SC.912.E.7.6: Relate the formation of severe weather to the

various physical factors.

SC.912.E.7.5: Predict future weather conditions based on present observations and conceptual

models and recognize limitations and uncertainties of such predictions.

Page 3: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

The three-cell model divides the circulation of

each hemisphere intothree distinct cells:

the heat-driven Hadley cell that circulates air between the Tropics and subtropics,a Ferrel cell in the middle latitudes, and a polar cell.

Page 4: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.
Page 5: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Thermohaline Circulation in the Atlantic

Page 6: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Three astronomical factors influence the Climate cycles of glacial & interglacial periods:

Eccentricity -

Obliquity -

Precession –

These three factors make up the Milankovitch cycles.

Page 7: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

The eccentricity of Earth’s orbit changes cyclically with a cycle of about 100,000 years being especially prominent.

Page 8: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Obliquity refers to the tilt of Earth’s axis, which also varies cyclically

(Tilt varies between 22° and 25° off the perpendicular).

Page 9: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Precession (wobble) is the cyclical change in the orientation of Earth’s axis.

Page 10: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

These astronomical forces, or Milankovitch Cycles, coincide and reinforce one another

every 100,000 years.

Over time, natural climate change involves 90,000 years of cooling,

followed by 10,000 years of warming.

These natural cycles result in glacials/interglacials.

Page 11: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

The end of the last Ice Age was approximately 12,000 years ago.

Sea level was 120 meters lower than today.

Page 12: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

We should have “turned the corner” and entered into a gradual cooling

phase.

Page 13: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Don’t changes in solar activity cause climate change?

Yes and No!In the past, solar activity was a

major climate forcing mechanism.

Today, the rapid and abundant output of GHGsdwarfs the solar influence.

Page 14: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

The solar constant is decreasing.

Simultaneously, global temperatures have steadily increased.

Page 15: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Don’t volcanoes produce more CO2 than humans?

Volcanoes on land and under the sea release about 200 million tons of CO2 annually.

Fossil fuel CO2 emissions in 2010 tipped

the scales at 26.8 billion tons (USGS)

Page 16: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

So, the Natural Drivers:

Astronomical Factors (Milankovitch Cycles)

Solar Output

and Volcanism

Do not account for the recent rapid warming

Page 17: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Instead, Greenhouse Gases account for the warming over the past 50 years.

They result from the combustion of Fossil Fuels

(coal, oil, natural gas)

Agriculture (cows)

Deforestation

Melting Permafrost…

Page 18: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.
Page 19: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

NASA Atmospheric Infrared Sounder (AIRS) July 2008

Global Carbon Dioxide Levels

Page 20: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

DendroclimatologyTree rings provide

records of climate history.

Insight into past climates is based oninformation in geological and biological records.

What evidence do we have?

Page 21: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Palynology provides information of past vegetation, and therefore, climate.

Lake bottom sediment cores trap pollen grains

Page 22: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.
Page 23: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Oxygen Isotope Analysis

Ratio of Oxygen-18 to Oxygen-16 in calcitefrom deep sea sediment cores measuredwith a mass spectrometer reveal climate

500 million years ago.

Page 24: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Less Oxygen 18 = colder climatic periods

Page 25: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

CO2 has risen every year since measurements began

Page 26: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

According to the Environmental Protection Agency,greenhouse gases from fossil fuel combustion are responsible

for most of the warming of the last 50 years.

Page 27: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Earth’s mean surface temperaturehas increased about 1.5ºF since 1900

NOAA’s State of the Climate Report NASA’s Surface Temperature Analysis

NASA reports that most of the warminghas occurred over the past 30 years.

Page 28: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.
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Page 30: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

2005 and 2010 tied as the hottest years on record.

2001 to 2010 is the hottest decade on record.

1991 to 2000 is the second hottest decade on record.

2012 was the hottest year on record in the U.S.

Page 31: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Climate models predict that mean Earth temperature could increase from 2.5 ºF to 10.5ºF above 1990 levels by 2100.

“Global temperatures are dangerously close to the highest ever estimated to

have occurred in the past million years” (NASA)

Page 32: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

Since 1950, the Arctic has lost

50% of its extent

Page 33: SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.

The first report of the IPCC was published 1990, then 1995,2001, & the FAR (AR4) in 2007

Climate Change 2007:

The Physical Science Basis

Climate Change 2007:

Impacts, Adaptation

and Vulnerability

Climate Change 2007: Mitigation of Climate

Change

Climate Change 2007:

Synthesis Report