Climate Midterm Questions

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37 Terms

1
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What is the climatically relevant energy source for a rocky planet?

The Sun (solar radiation)

2
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Does heat flux from the Earth’s interior modulate the Earth’s climate? If not, why?

No, it’s too small compared to solar input to significantly affect climate

3
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What kind of heat transfer mechanisms exist? Which is relevant for heat gain from the sun and heat loss from the earth to space?

Conduction, convection, and radiation; Since Earth sits in the hard vacuum of the

outer space, Earth’s heat gain from the Sun

and heat loss from the Earth to the space occur

only via electromagnetic radiation.

4
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What determines the amount and strength of radiative heat flux from a planetary body? (Stars, Planets)

Temperature, emissivity, and surface area (Stefan-Boltzmann Law)

5
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What describes Stefan-Boltzmann and Wien’s Displacement laws?

Stefan-Boltzmann relates energy flux to temperature; Wien’s Law states he wavelength of the maximum intensity of blackbody radiation is inversely proportional to the temperature.

6
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Does the incoming irradiance strongly interact with the atmospheric greenhouse gases?

The vibration wavelength (frequency) range of most greenhouse gasses in Earth’s atmosphere is ~ 4 to which is much larger than that of the Sun . In order a greenhouse gas to interact with radiation, both the latter and former need have a comparable wavelength ranges.

7
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Why is atmospheric CO2 a strong greenhouse gas for a planet with a surface temperature around 280–310 K?

he deviation between the predicted and measured values of flux amount and spectral distribution of outgoing thermal radiation (at 284 K) is significantly large. This means that the outgoing thermal radiation interacts strongly with the atmospheric gases

8
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Over a broad range of values, how is the relationship between atmospheric CO2 and outgoing longwave radiation?

Inversely related; higher CO2 decreases outgoing longwave radiation

9
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What is the relationship between the mass, age, surface temperature, and luminosity of a star?

Larger and younger stars are hotter and more luminous

10
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Is the Sun strong enough to facilitate liquid water on Earth?

No, not alone; greenhouse gases make conditions warm enough for liquid water

11
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How does the evolution of atmospheric O2 influence greenhouse gas presence?

The absence of atmospheric O2 during the early part of Earth’s history, might have allowed a sustained presence of potent greenhouse gases such as NH3 and CO. The addition of these greenhouse gases would substantially increase Earth’s surface temperature, enabling the presence of liquid water. present atmospheric level

12
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What makes the Cryogenian glaciation unique?

Global-scale (“Snowball Earth”) glaciation covering nearly all latitudes

13
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What are the names, timing, and duration of the two Cryogenian glaciations?

Sturtian (~717–660 Ma) and Marinoan (~650–635 Ma)

14
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What is the nature and sequence of Cryogenian glacial deposits?

Diamictites, deglacial (IRD), followed by cap dolostone (cd) layers

15
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What caused and ended the Cryogenian glaciation?

cause: Warm and Wet climate, land masses centered around equator, presence of newly formed large igneous provinces (ILP)

end: Cold climate, wide-spread ice cover, reduced chemical weathering leading to increase of CO2

16
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What are climatic consequences of post-Pangaea tectonics?


an increase ocean ridge and hot spot activity, volcanism, led to unbalanced atmospheric CO2 concentration, which were unbalanced by CO2 removal from chemical weathering.

17
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What happens with a strongly enhanced seafloor spreading rate?

Increased volcanic CO2, warmer climate, higher sea level, and lower deep-water oxygen

18
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How does a weak pole-to-tropic temperature gradient affect deep water formation?

It weakens thermohaline circulation and reduces oxygenation

19
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How does an extremely warm climate affect O2 in seawater?

Warm water holds less dissolved oxygen

20
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Is there a link between sea level rise, warm climate, and black shale?

Yes; high sea level and anoxia promote black shale deposition

21
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What was the driving force of the PETM?

Rapid release of greenhouse gases, likely methane

22
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How does the PETM compare with Mid-Cretaceous warming?

PETM was shorter and faster; Mid-Cretaceous was longer and tectonically driven

23
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Why is the carbon isotope ratio of carbonate indicative of PETM greenhouse gas?

Because methane and organic carbon have low δ13C values

24
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What is methane hydrate?

A crystalline solid of methane and water molecules

25
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How and where is methane hydrate formed?

Under low temperature and high pressure in marine sediments and permafrost

26
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Which parameters control methane hydrate stability?

Temperature, pressure, and methane concentration

27
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What happened around 2.7 and 30–34 Ma ago?

Onset of Northern Hemisphere glaciation and Antarctic glaciation due to tectonic and CO2 changes

28
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What are three factors that enhance chemical silicate weathering?

Temperature, precipitation, and vegetation

29
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What enhanced chemical weathering and global cooling over last 10–15 Ma?

Uplift of mountain ranges increasing erosion and weathering rates; carbonate weathering affects short-term CO2 balance

30
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Why is silicate weathering more effective at removing CO2 than carbonate?

It converts CO2 into stable carbonates permanently stored in rocks

31
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Did enhanced silicate weathering contribute to bipolar glaciation ~2.7 Ma?

Yes, by reducing atmospheric CO2 levels

32
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What are the three main orbital parameter changes?

Eccentricity, obliquity, and precession

33
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What causes cyclic variations in Earth-Sun configuration?

Gravitational interactions with other planets

34
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Which Earth-Sun changes affect high vs. low latitudes more?

Obliquity affects high latitudes; precession affects low latitudes

35
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Which physical law describes season length and intensity?

Kepler’s Second Law (equal areas in equal times)

36
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What is the key statement of Kepler’s 2nd Law?

Planets sweep equal areas in equal times; orbital speed varies

37
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How are season length and heat intensity related?

Shorter seasons are more intense when Earth moves faster in its orbit