Intro to Climate System

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67 Terms

1
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What are the two main types of climate change discussed in Earth's history?

Tectonic-Scale Climate Change and Orbital-Scale Climate Change.

2
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What characterizes the current climate period in Earth's history?

We are currently in an ice-house period.

3
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What must a molecule do to be considered IR active?

It must undergo a change in dipole upon vibration.

4
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What is the positive feedback mechanism involving albedo?

Climate cooling leads to increased snow/ice, which raises reflectivity, resulting in less solar radiation absorbed and further cooling.

5
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How does increased water vapor contribute to climate warming?

Increased atmospheric water vapor traps more solar radiation, leading to further warming.

6
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Why is water vapor not considered climate forcing?

It is a product of increased temperatures rather than an output from human activities.

7
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What role does vegetation play in precipitation feedback mechanisms?

Increased precipitation leads to forest growth, which increases water transpiration and further precipitation.

8
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What are some examples of climate archives?

Pollen, lake levels, ocean cores, tree rings, corals, and ice cores.

9
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What information can ice cores provide about past climates?

They contain air bubbles of CO2 and CH4, snow layer thickness, and dust that indicates wind direction and strength.

10
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What is the Gaia Hypothesis?

It suggests that Earth acts as a self-regulating organism that maintains conditions suitable for life.

11
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What is the Faint Young Sun Paradox?

The paradox that the early Earth should have been frozen due to a dimmer sun, yet evidence shows it was warm enough for liquid water.

12
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What is the proposed solution to the Faint Young Sun Paradox?

The Earth's Thermostat, which involves cycling greenhouse gases between reservoirs to maintain temperature.

13
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How does chemical weathering contribute to Earth's temperature regulation?

Increased weathering removes CO2 from the atmosphere, reducing warming as temperatures rise.

14
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What is the Snowball Earth theory?

The theory that the Earth was once nearly entirely covered in ice during extreme ice-house periods.

15
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What evidence supports the Snowball Earth theory?

Evidence of glaciation in various continents around 850-550 Ma, suggesting they were near the equator at that time.

16
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What is the Polar Position Hypothesis?

It states that ice sheets will only form on continents that are near the poles due to lower solar intensity.

17
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What was the climate condition during the time of Pangaea?

Pangaea was a hothouse period with no evidence of ice sheets and was warmer and drier than today.

18
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What are biotic proxies in climate studies?

They are changes in plants and animals, such as pollen or microfossils, used to infer past climate conditions.

19
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How do isotopes inform about past climates?

Isotopes can indicate temperatures, precipitation, and nutrient levels based on their ratios in various materials.

20
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What are speleothems?

Cave mineral deposits that record groundwater composition over thousands of years.

21
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What role do tree rings play in climate studies?

The width of tree rings indicates the amount of cellulose deposited, reflecting past precipitation and temperature conditions.

22
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What is the significance of ocean sediments in climate research?

They provide information about past temperatures and pH levels based on isotopes and alkenones present.

23
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What evidence suggests that Pangaea had high CO2 levels?

Evidence of palm-like vegetation at 40° latitudes indicates CO2 levels of 1650 ppm.

24
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What is the BLAG Hypothesis?

Proposed by Berner, Lasaga, and Garrels, it suggests that plate tectonics influence CO2 changes through increased seafloor spreading and magma release.

25
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What is the Uplift Weathering hypothesis?

It posits that continental collisions increase uplift, forming mountains that enhance weathering and CO2 removal, leading to global cooling.

26
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What two factors determine the occurrence of icehouse periods?

1) Presence of polar continents for ice sheet formation. 2) Tectonic movement affecting atmospheric CO2 levels.

27
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What characterized the hot house world around 100 Ma?

There was no ice, even in Antarctica, and coral reefs extended to 40° from the equator.

28
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How do ocean systems affect temperature distribution?

Oceans transport warmer and cooler water effectively, influencing global climate.

29
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What is the relationship between salinity and density in seawater?

Cold water is denser than warm water, and salt water is denser than fresh water.

30
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What drives thermohaline circulation?

Differences in seawater density due to temperature and salinity.

31
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What is the overturning time in ocean circulation?

The time it takes for a water molecule to complete a full loop of the globe.

32
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What is the Ocean Heat Transport Hypothesis?

It suggests that warm, salty water can sink and spread warmth globally, contributing to hothouse conditions.

33
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What is palaeoceanography?

The study of Earth's ocean history, focusing on past circulation, chemistry, biology, and sedimentation.

34
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How can sediment accumulation rates be explained?

Sediment sinks faster due to aggregation, allowing rates of 100-200 m per day.

35
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What do Mg/Ca/O isotopes in CaCO3 skeletons indicate?

They provide information about past sea surface temperatures (SST) and ice levels.

36
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What is isotopic fractionation?

The difference in energy required to bind heavier vs. lighter isotopes, affecting their distribution.

37
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How are isotope abundances measured?

Using an Isotope Ratio Mass Spectrometer (IRMS), reported relative to a standard as δ.

38
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What is the Kinetic Isotope Effect (KIE)?

The influence of isotopes on the kinetics of a reaction, where lighter isotopes diffuse faster.

39
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What is the Equilibrium Isotope Effect (EIE)?

The impact of isotopes on the position of equilibrium, affecting bond strengths in reactants and products.

40
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What happens to oxygen isotopes during warmer periods?

Lighter 16O evaporates more, leading to higher 18O concentrations in oceans.

41
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What is Henry's Law in relation to oceanic CO2?

It relates the solubility of gases in seawater to the partial pressure of the gas.

42
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Why isn't the ocean acidic despite dissolved CO2?

Chemical weathering introduces weak acids that buffer against pH decreases.

43
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What role do bicarbonate ions play in ocean acidity?

They act as a buffer, helping to maintain ocean pH levels despite CO2 presence.

44
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What is the primary component of dissolved CO2 at pH = 8?

HCO3- makes up around 80% of the total dissolved CO2.

45
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What temperature increase occurred around 55 Ma during the PETM?

A temperature increase of around 6 °C.

46
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What evidence indicates the PETM temperature increase?

A decrease in abundance of 13C and Ca in foraminifera, with an increase in Mg.

47
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How do foraminifera adjust their skeleton composition at higher temperatures?

They use more Mg and less Ca to make their skeletons.

48
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What trend is observed in boron isotopes in sediments at lower pH?

11B decreases at lower pH, indicating higher CO2 levels.

49
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What does the relative abundance of B isotopes in marine carbonates indicate?

It can be used as a proxy for the partial pressure of CO2.

50
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What are GDGTs and how are they related to temperature?

GDGTs are indicators of temperature; their cyclopentane rings relate to sea surface temperature.

51
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What geological event around 30 Ma affected Antarctica's climate?

The opening of Drake's Passage isolated Antarctica with a ring of cold water.

52
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What significant geological change occurred around 3.5 Ma?

South America moved towards North America, closing the gateway between the Pacific and Atlantic.

53
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What are Milankovitch cycles?

Processes that cause changes in solar forcing, leading to glacial and interglacial periods.

54
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What is the significance of summer temperatures in ice sheet build-up?

Summer temperatures are more important than winter temperatures for ice sheet formation.

55
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How can glacial and interglacial periods be inferred?

From oxygen isotopes, with even numbers indicating glacial periods and odd numbers indicating interglacial periods.

56
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What role do cave deposits play in climate history?

Cave deposits, like stalagmites, can provide records of past climate conditions.

57
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What is the process of amino acid geochronology?

It measures the ratio of L to D forms of amino acids to determine the age of organic materials.

58
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What happens to CO2 during glacial periods?

Some CO2 dissolves in oceans, is taken up by phytoplankton, and a larger proportion dissolves into global deep water.

59
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What triggers the shutdown of thermohaline circulation?

An increase in fresh water in the North Atlantic prevents salty water from sinking.

60
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What was the Younger Dryas?

A period around 12.8 to 11.5 ka marked by a prolonged shutdown of thermohaline circulation.

61
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How do long-lived species like arctica islandica provide climate data?

They grow shells with rings that indicate long-term temperature changes.

62
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What is the relationship between stomata size and CO2 levels?

Smaller stomata indicate higher atmospheric CO2 concentrations.

63
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What is ocean acidification?

The process where increased CO2 leads to lower ocean pH and affects marine life.

64
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What happens to carbonate ions as atmospheric CO2 increases?

The proportion of CO3^2- decreases, leading to ocean acidification.

65
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What is the stoichiometric solubility product (KSP) for calcium carbonate?

KSP = [Ca2+][CO3^2-], indicating the saturation state of seawater with CaCO3.

66
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What does it mean if Ω < 1 in seawater?

It indicates that CaCO3 will dissolve, as the seawater is undersaturated.

67
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What is the impact of increased atmospheric CO2 on ocean chemistry?

It leads to decreased pH, increased HCO3-, and decreased CO3^2-.