How do we know? Understanding the Evidence€¦ · Web viewHow do we know? Understanding the...

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Name: __________________________________________________________________________ Is Man-made CO 2 Warming the Planet? As you watch the debate, think about the evidence each side brings up, how are they talking, what side seems more credible, why? (https://www.youtube.com/watch? v=gWT-EWKIR3M ) How do we know? Understanding the Evidence Proxy data is data that paleoclimatologists gather from natural recorders of climate changes, e.g., tree rings, ice cores, fossil pollen, ocean sediments, coral and historical data. By analyzing records taken from these and other proxy sources, scientists can extend our understanding of climate far beyond the 140 year instrumental record. For Bill Nye Against bill Nye

Transcript of How do we know? Understanding the Evidence€¦ · Web viewHow do we know? Understanding the...

Page 1: How do we know? Understanding the Evidence€¦ · Web viewHow do we know? Understanding the Evidence Understanding the Evidence Proxy data is data that paleoclimatologists gather

Name: __________________________________________________________________________

Is Man-made CO2 Warming the Planet?

As you watch the debate, think about the evidence each side brings up, how are they talking, what side seems more credible, why? (https://www.youtube.com/watch?v=gWT-EWKIR3M)

How do we know? Understanding the EvidenceProxy data is data that paleoclimatologists gather from natural recorders of climate changes, e.g., tree rings, ice cores, fossil pollen, ocean sediments, coral and historical data. By analyzing records taken from these and other proxy sources, scientists can extend our understanding of climate far beyond the 140 year instrumental record.

For Bill Nye Against bill Nye

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Name: __________________________________________________________________________

1. So maybe yesterday the graph was too recent. So lets look at the last 800,000 years. Is there a relationship between temperature and CO2 according to the ice core data?

2. Can we confirm that more CO2 means a higher global temperature? Or do we need more?

History

Earth is believed to have formed about 5 billion years ago. In the first 500 million years a dense atmosphere emerged from the vapor and gases that were expelled during degassing of the planet's interior. These gases may have consisted of hydrogen (H2), water vapor, methane (CH4) , and carbon oxides. Prior to 3.5 billion years ago the atmosphere probably consisted of carbon dioxide (CO2), carbon monoxide (CO), water (H2O), nitrogen (N2), and hydrogen.

The hydrosphere was formed 4 billion years ago from the condensation of water vapor, resulting in oceans of water in which sedimentation occured.

The most important feature of the ancient environment was the absence of free oxygen. Evidence of such an anaerobic reducing atmosphere is hidden in early rock formations that contain many elements, such as iron and uranium, in their reduced states. Elements in this state are not found in the rocks of mid-Precambrian and younger ages, less than 3 billion years old.

One billion years ago, early aquatic organisms called blue-green algae began using energy from the Sun to split molecules of H2O and CO2 and recombine them into organic compounds and molecular oxygen (O2). This solar energy conversion process is known as photosynthesis. Some of the photosynthetically created oxygen combined with organic carbon to recreate CO2 molecules. The remaining oxygen accumulated in the atmosphere, touching off a massive ecological disaster with respect to early existing anaerobic organisms. As oxygen in the atmosphere increased, CO2 decreased.

High in the atmosphere, some oxygen (O2) molecules absorbed energy from the Sun's ultraviolet (UV) rays and split to form single oxygen atoms. These atoms combining with remaining oxygen (O2) to form ozone (O3) molecules, which are very effective at absorbing UV rays. The thin layer of ozone that surrounds Earth acts as a shield, protecting the planet from irradiation by UV light.

The amount of ozone required to shield Earth from biologically lethal UV radiation, wavelengths from 200 to 300 nanometers (nm), is believed to have been in existence 600 million years ago. At this time, the oxygen level was approximately 10% of its present atmospheric concentration. Prior to this period, life was restricted to the ocean. The presence of ozone enabled organisms to develop and live on the land. Ozone played a significant role in the evolution of life on Earth, and allows life as we presently know it to exist.

gSo what have we seen happening?

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What trends have we seen influencing climate history?The causes of climate change are complex. There are several major factors that can affect the climate system, including:

Changes in solar output (sunspots) Changes in Earth's orbit (M. Cycles) Changes in atmospheric content of greenhouse

gases (CO2, Methane, Water Vapor)Milankovitch CyclesIt is important to consider scale when interpreting climate change through time.

Long term- Hundreds of millions of years; Medium term- One million years; Short term- ~160,000 years; Modern period- Hundreds of years

When we have more oxygen (O2), the planet is _____________________________.o Producers:

When we have more carbon dioxide (CO2), the planet is _______________________.o Producers:

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How has the sun changed over time?

Why do we have seasons (not climate!)?

Big Debate: Is man-made CO2 warming the planet? Explain.

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What coming next? What determines an areas climate?

*** Teacher Notes The Milankovitch Theory states that variations in Earth's orbit causes climate to change through time. According to this theory, changes in the shape of Earth's orbit around the sun (eccentricity), variations in Earth's axis tilt (obliquity), and the tendency for Earth to 'wobble' with respect to the direction of its rotational axis (precession) affect climate. This wobble can lead to fluctuations in the amount and distribution of incoming solar radiation, resulting in dramatic changes in climate over long time scales. Wobble may cause ice ages.