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.
33
Embed
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.
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
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.
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.
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.
Thermohaline Circulation in the Atlantic
Three astronomical factors influence the Climate cycles of glacial & interglacial periods:
Eccentricity -
Obliquity -
Precession –
These three factors make up the Milankovitch cycles.
The eccentricity of Earth’s orbit changes cyclically with a cycle of about 100,000 years being especially prominent.
Obliquity refers to the tilt of Earth’s axis, which also varies cyclically
(Tilt varies between 22° and 25° off the perpendicular).
Precession (wobble) is the cyclical change in the orientation of Earth’s axis.
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.
The end of the last Ice Age was approximately 12,000 years ago.
Sea level was 120 meters lower than today.
We should have “turned the corner” and entered into a gradual cooling
phase.
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.
The solar constant is decreasing.
Simultaneously, global temperatures have steadily increased.
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)
So, the Natural Drivers:
Astronomical Factors (Milankovitch Cycles)
Solar Output
and Volcanism
Do not account for the recent rapid warming
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…
NASA Atmospheric Infrared Sounder (AIRS) July 2008
Global Carbon Dioxide Levels
DendroclimatologyTree rings provide
records of climate history.
Insight into past climates is based oninformation in geological and biological records.
What evidence do we have?
Palynology provides information of past vegetation, and therefore, climate.
Lake bottom sediment cores trap pollen grains
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.
Less Oxygen 18 = colder climatic periods
CO2 has risen every year since measurements began
According to the Environmental Protection Agency,greenhouse gases from fossil fuel combustion are responsible
for most of the warming of the last 50 years.
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.
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.
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)
Since 1950, the Arctic has lost
50% of its extent
The first report of the IPCC was published 1990, then 1995,2001, & the FAR (AR4) in 2007