causality L2 PQ

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28 Terms

1
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1. Early scientific work in the 19th century demonstrated that Earth’s atmosphere traps heat. Which scientists correctly match their contribution?
b) John ____ – experimentally identified ___ and ___ ____-absorbing gases

tyndall, CO2 H20 heat

2
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2. What did Eunice Foote contribute to early climate science?
b) Demonstrated that water ___ and ___ absorb __

vapour CO2 heat

3
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3. Svante Arrhenius is significant because he:
b) ____ temperature increases from ___ rises

quantitifed CO2

4
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4. What is the relationship between CO₂ and temperature over the last 800,000 years?
***c) ____ changed first; ____ followed as a feedback

temperature, CO2

5
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5. Why do scientists reject solar forcing as the cause of current warming?
b) Solar energy has remained constant or slightly ___ while Earth warmed

declined

6
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6. The Keeling Curve is significant because it:
c) Records direct atmospheric CO₂ ___ since 1958

increases

7
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7. Which natural processes have historically triggered glacial and interglacial cycles?
b) Milankovitch cycles:
__ x3

eccentricity obliquity precession

8
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8. Which statement about the Holocene is correct?
c) It provided ___ climate conditions that enabled __

stable agriculture

9
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9. Which of the following are positive feedbacks that amplify warming?
b) Melting ice → lower albedo → more absorption
c) Permafrost thaw releasing ____
e) More water ___ in a warming atmosphere

methane, vapour

10
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10. The chemical fingerprint of rising CO₂ shows that most new CO₂ in the atmosphere comes from:

fossil fuels

11
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11. Evidence for human-driven warming:

a) Rising fossil-fuel CO₂ ____ signature
b) ____ Curve showing rapid CO₂ rise
c) Ice ____ records showing CO₂ and temperature move ___
e) Global scientific assessments (____)

isotopic, keeling, core, together, IPCC

12
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12. Climate “tipping points” refer to:
c) ____ after which changes become ___

thresholds, irreversible

13
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<p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>13. Hothouse Earth conditions refer to:</span></strong><span><br> c) Global temperature rises ___°C above modern levels</span></span></p>

13. Hothouse Earth conditions refer to:
c) Global temperature rises ___°C above modern levels

3-4

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<p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>1. Briefly explain the major contributions of Fourier, Tyndall, Eunice Foote, and Arrhenius to early climate science.</span></strong></span></p><ul><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>____:</span></strong><span> Proposed that Earth’s ____ traps heat → early idea of ____ effect.</span></span></p></li><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Tyndall:</span></strong><span> Experimentally identified CO₂ and H₂O as major heat-absorbing gases.</span></span></p></li><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Foote:</span></strong><span> Demonstrated that CO₂ and water vapor warm when exposed to sunlight; early evidence of greenhouse gases.</span></span></p></li></ul><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Arrhenius:</span></strong><span> Quantified warming expected from increased CO₂ and linked fossil fuel combustion to rising global temperatures.</span></span></p>

1. Briefly explain the major contributions of Fourier, Tyndall, Eunice Foote, and Arrhenius to early climate science.

  • ____: Proposed that Earth’s ____ traps heat → early idea of ____ effect.

  • Tyndall: Experimentally identified CO₂ and H₂O as major heat-absorbing gases.

  • Foote: Demonstrated that CO₂ and water vapor warm when exposed to sunlight; early evidence of greenhouse gases.

Arrhenius: Quantified warming expected from increased CO₂ and linked fossil fuel combustion to rising global temperatures.

fourier, atmosphere, greenhouse

15
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1. Briefly explain the major contributions of Fourier, Tyndall, Eunice Foote, and Arrhenius to early climate science.

  • Fourier: Proposed that Earth’s atmosphere traps heat → early idea of greenhouse effect.

  • ___: Experimentally identified ___ and ____as major ___-absorbing ___

  • Foote: Demonstrated that CO₂ and water vapor warm when exposed to sunlight; early evidence of greenhouse gases.

Arrhenius: Quantified warming expected from increased CO₂ and linked fossil fuel combustion to rising global temperatures.

tyndall CO2 H20 heat gases

16
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1. Briefly explain the major contributions of Fourier, Tyndall, Eunice Foote, and Arrhenius to early climate science.

  • Fourier: Proposed that Earth’s atmosphere traps heat → early idea of greenhouse effect.

  • Tyndall: Experimentally identified CO₂ and H₂O as major heat-absorbing gases.

  • ___: Demonstrated that ____ and water ____ warm when exposed to ____; early evidence of ____

Arrhenius: Quantified warming expected from increased CO₂ and linked fossil fuel combustion to rising global temperatures.

foote, CO2, vapour, sunlight, greenhouse gases

17
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1. Briefly explain the major contributions of Fourier, Tyndall, Eunice Foote, and Arrhenius to early climate science.

  • Fourier: Proposed that Earth’s atmosphere traps heat → early idea of greenhouse effect.

  • Tyndall: Experimentally identified CO₂ and H₂O as major heat-absorbing gases.

  • Foote: Demonstrated that CO₂ and water vapor warm when exposed to sunlight; early evidence of greenhouse gases.

_____: ____ warming expected from ____ CO₂ and linked fossil fuel ___ to rising global ___.

arrhenius, quantified, increased, combustion, temperatures

18
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<p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>2. Identify and briefly explain the three Milankovitch orbital variations.</span></strong></span></p><ul><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>____:</span></strong><span> 100,000-year cycle; Earth’s orbit changes from ___ </span></span><span data-name="left_right_arrow" data-type="emoji">↔</span><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><span> ____, altering solar ____.</span></span></p></li><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Obliquity:</span></strong><span> 41,000-year cycle; tilt of Earth’s axis shifts between ~21.5° and 24.5°, changing seasonal contrast.</span></span></p></li></ul><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Precession:</span></strong><span> 26,000-year cycle; wobble of Earth’s axis changes timing of seasons relative to orbit.</span></span></p>

2. Identify and briefly explain the three Milankovitch orbital variations.

  • ____: 100,000-year cycle; Earth’s orbit changes from ___ ____, altering solar ____.

  • Obliquity: 41,000-year cycle; tilt of Earth’s axis shifts between ~21.5° and 24.5°, changing seasonal contrast.

Precession: 26,000-year cycle; wobble of Earth’s axis changes timing of seasons relative to orbit.

19
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<p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>2. Identify and briefly explain the three Milankovitch orbital variations.</span></strong></span></p><ul><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Eccentricity:</span></strong><span> 100,000-year cycle; Earth’s orbit changes from circular </span></span><span data-name="left_right_arrow" data-type="emoji">↔</span><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><span> elliptical, altering solar distance.</span></span></p></li><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>____:</span></strong><span> 41,000-year cycle; ___ of Earth’s ____ shifts between ~____° and ____°, changing ____ contrast.</span></span></p></li></ul><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Precession:</span></strong><span> 26,000-year cycle; wobble of Earth’s axis changes timing of seasons relative to orbit.</span></span></p>

2. Identify and briefly explain the three Milankovitch orbital variations.

  • Eccentricity: 100,000-year cycle; Earth’s orbit changes from circular elliptical, altering solar distance.

  • ____: 41,000-year cycle; ___ of Earth’s ____ shifts between ~____° and ____°, changing ____ contrast.

Precession: 26,000-year cycle; wobble of Earth’s axis changes timing of seasons relative to orbit.

obliquity, tilt, axis 21.4, 24.5 seasonal

20
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<p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>2. Identify and briefly explain the three Milankovitch orbital variations.</span></strong></span></p><ul><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Eccentricity:</span></strong><span> 100,000-year cycle; Earth’s orbit changes from circular </span></span><span data-name="left_right_arrow" data-type="emoji">↔</span><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><span> elliptical, altering solar distance.</span></span></p></li><li><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>Obliquity:</span></strong><span> 41,000-year cycle; tilt of Earth’s axis shifts between ~21.5° and 24.5°, changing seasonal contrast.</span></span></p></li></ul><p><span style="background-color: transparent; font-family: &quot;Times New Roman&quot;, serif;"><strong><span>____:</span></strong><span> 26,000-year cycle; ____ of Earth’s ___ changes timing of ___ relative to ___.</span></span></p>

2. Identify and briefly explain the three Milankovitch orbital variations.

  • Eccentricity: 100,000-year cycle; Earth’s orbit changes from circular elliptical, altering solar distance.

  • Obliquity: 41,000-year cycle; tilt of Earth’s axis shifts between ~21.5° and 24.5°, changing seasonal contrast.

____: 26,000-year cycle; ____ of Earth’s ___ changes timing of ___ relative to ___.

precession, wobble, axis, seasons, orbit

21
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3. What is the significance of the Keeling Curve in understanding modern climate change?

  • Provides direct, continuous ____ of atmospheric ____ since 1958.

  • Shows a steady ____ trend from ~315 ppm → 425+ ppm today.

  • Annual “____” reflects ___ __ ___ in the ___******

  • Demonstrates rapid ___-driven CO₂ increase.

measurements, CO2, upward, wiggle, seasonal plant growth northern hemisphere human

22
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4. Explain why CO₂ is considered the “trigger” for modern climate change but a “feedback” in past ice age cycles.

  • Past: ___ changes ____ warming → oceans ____ CO₂ → amplified warming (feedback).

Today: Human fossil fuel combustion rapidly increases ____ directly → warming begins with ___rise (___).

orbital, triggered, released, CO2, CO2, trigger

23
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5. Identify and briefly explain three major lines of evidence supporting human-driven warming.

  • Rising fossil-fuel CO₂ isotopic ____: Atmospheric carbon shows distinct ____ from ___/oil/gas.

  • Keeling Curve: Direct measurements of rapidly increasing atmospheric CO₂.

Ice ____***: CO₂ ___ far exceed ____ range of past 800,000 years; ___ ******now leads rather than follows CO₂.

signature, fingerprints, coal, cores, levels, natural, warming

24
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6. Briefly describe three major positive climate feedbacks that amplify warming.

  • Ice–albedo feedback: ____ ice lowers reflectivity → more absorbed heat → more melting.

  • Water vapor feedback: ___ air holds more water ____, which is a ___ greenhouse gas.

___ carbon feedback: Thawing ___ release CO₂/____, increasing greenhouse warming.

melting, warmer, vapour, strong, permafrost, soils, methane

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7. What distinguishes the Anthropocene from the Holocene?

  • Holocene: ____ climate after last Ice ____; enabled ___ and human ____.

Anthropocene: ___** epoch where ____ activities dominate climate and Earth systems; characterized by rapid CO₂ rise, ____, and ecological disruption.

stable, age, agriculture, civilization, proposed, human, warming

26
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8. Briefly explain why solar forcing cannot account for modern global warming.

  • ___ measurements show solar energy has remained _____ or slightly declined.

  • Despite this, global temperatures have risen ___, indicating another driver (GHGs).

satellite, constant, sharply

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9. Identify and explain two ways human activities disrupt the natural carbon ___.

  • _____ fossil fuels: ____ long-stored carbon rapidly into the atmosphere, raising CO₂ levels.

___: Removes carbon ___, reducing CO₂ ___ by plants.

cycle, burning, releases, deforestation, sinks, absorption

28
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10. Define “tipping point” and give one example related to climate change.

  • A ____ beyond which the climate system ___ into a new ___ that is irreversible on human timescales.

  • ______ of major ice ____ → permanently higher sea ____.

threshold, goes, state, collapse, sheets, levels