midterm 2 Flashcards

1
Q

Why does Earth have seasons?

A
  • b/c its axis is tilted as it moves around the sun.
  • earth rotates 24 hours
  • earth takes 365 days revolution around the sun.
    maintain angle of tilt 23.5
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2
Q

When is Earth closest to the Sun in its present orbit? How does this “close pass” position affect the amount of radiation received on Earth?

A

earth is (closest) to sun on (perihelion) on January 3.

This is more radiation. The distance of 147 million kilometer from the earth.

as it moves fastest during perigee the solar day would be largest. Whereas the solar day the solar day wold be smallest during apogee( aphelion = is away on July, 4 ) because the earth moves much slower at this position.

when earth is in aphelion it receives less radiation from sun and temperature would be the lowest.

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3
Q

Earth’s tilt is slowly decreasing today. As it does so, are the Polar Regions receiving more or less solar radiation in summer? In winter? How can these changes in the seasonal amount of solar radiation affect climate?

A

earth tilt decreases, the poles would be away from sun during (summer). less radiation in the summer.

during the (winter), the poles will be directly towards the sun. they would receive more solar radiation.

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4
Q

How is axial precession different from precession of the ellipse?

A

Axial precession is the wobbling motion of the earth caused by the gravitational pull of sun and moon causing slight bulge in the diameter of the earth at the equator. 23.5

precession of the eclipse( precession is slower) is the entire elliptical shape of earth orbit tends to rotate. It is slower in space.

*the combined motions of these precessions leads to the occurrence of equinoxes( twice a year, march, & September same length day&night). and solstices (revolution around sun .

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5
Q

What is the precession of the equinoxes?

A

movement of solstices around Earth’s elliptical orbit over cycles of 23,000 and 19,000 years

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6
Q

How does eccentricity combine with precession to control a key aspect of the amount of insolation Earth receives?

A

both combine would result variations of distance between earth and the sun by the seasons with the cycle of 23,000 years. solar radiation is more on perihelion and less on aphelion.

the high eccentricity would result in large contrast in the distance between the earth and sun low eccentricity would result in low contrasts.

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7
Q

During each Earth’s annual revolution around the Sun:

A

Earth maintains a constant angle of tilt.

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8
Q

The main role of eccentricity in long-term changes in solar radiation is to

A

magnify or suppress contrasts in Earth-Sun distance during the precessional cycles

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9
Q

What is TRUE about the level of summer insolation in the Northern Hemisphere TODAY?

A

It is well below the long-term average.

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10
Q

When Earth’s tilt is close to its smallest value,

A

there is the lowest summer insolation in the Northern Hemisphere.

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11
Q

When is Earth farthest away from the Sun in its present orbit?

A

during the Northern Hemisphere’s summer

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12
Q

The tilt of Earth’s axis TODAY is:

A

slowly decreasing

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13
Q

If Earth’s axis had no tilt:

A

the direct solar rays would always strike at the equator.

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14
Q

Monsoons are stronger

A

where there are large landmasses adjacent to oceans.

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15
Q

Where is the most powerful monsoonal circulation TODAY?

A

South Asia

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16
Q

Which of the following has the greatest effect on ice sheet growth or melting?

A

accumulation of snow in the winter

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17
Q

How does bedrock respond to a heavy ice load?

A

Bedrock responds with immediate fast sinking which later slows down.

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18
Q

How thick must an ice sheet be to depress the underlying bedrock by 1 kilometer?

A

3 kilometers

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19
Q

How does ice retain a record of past atmospheric gas composition?

A

in air bubbles trapped within glacial ice

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20
Q

Which isotopic transfer occurs during glaciations?

A

C12-enriched organic matter is transferred from land to the ocean

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21
Q

How did changes to ocean waters during the glaciation affect the level of atmospheric CO2?

A

Cooling of the surface and deep ocean increased the solubility of CO2 and reduced atmospheric CO2.

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22
Q

Where is most natural methane CH4 produced?

A

in swamps and bogs

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23
Q

Which of the following carbon reservoirs GAINED carbon biomass during the Last Glacial Maximum?

A

deep ocean

24
Q

What are examples of today’s monsoon areas around the world?

A

They consist of those in South Asia, Southeast Asia, parts of West Africa which are very weak. The only monsoon systems in the Southern Hemisphere are the Amazon Valley and NE Australia.

25
Q

What controls the size of ice sheets?

A
  • Through accumulation in which they initially as snow at mean annual temps below 10°C
  • melting begins at mean summer temps above 0°C (= mean annual temps above -10°C).
  • Ablation can accelerate rapidly if temperatures warm
26
Q

What is The Milankovitch Theory?

A
  • summer insolation controls ice sheet growth
  • ice sheet growth in the Northern Hemisphere which occurs during times when summer insolation is reduced
  • amount of summer insolation arriving at the top of atmosphere at 65°N can vary by +/-12% around the long-term mean value
27
Q

In perfect ice sheet growth conditions, when does Low summer insolation occur?

A

When the earth’s orbital tilt is small which becomes more highly eccentric, when the northern summer solstice occurs once the earth is farthest from the sun, reverse situation results in ice sheet melting, and tilt is ~23.5° and decreasing

28
Q

A 3-million-year δO18 record is based on what?

A

Benthic foraminifera and ice core rafting debris in a sediment core from the Northern Atlantic is the evidence that the regime of 41,000-year cycles (change in obliquity) persisted in the Northern Hemisphere from ~2,75 to 0.9 MYA

29
Q

According to the evidence of the Interglacial period near 130K years, which coral reefs does the next abrupt deglaciation (termination) between 17K and 10K years ago come from?

A

Bermuda: no major uplifts or sinking of the crust
Fossil coral reef lies: 6 m (18 ft) above modern sea level
Dated at 125,000 years old (U/Th method)

30
Q

What is the main reason why the time interval between 130K and 120K was only over the last 150K years?

A

It was when the amount of ice on Earth was even smaller than today (i.e. sea level was higher which allowed the coral reefs to function)

31
Q

Is the Milankovitch Theory a Full Answer?

A

It explains the ice volumes at 41K and 23K-year cycles. It also explains the time lag behind summer insolation maxima. However, it does not explain the dominance of 41K-year cycle over 23K-year cycle over the interval of 2 million years in the Northern Hemisphere. It also fails to explain the emergence of a 100K-year oscillation in the last 0.9 million years

32
Q

What are examples of Orbital-Scale CO2 Changes?

A
  • 800,000-year record from Dome C in Antarctica
  • Large-scale 100,000-year cycles similar to the ice volume cycles which are determined by the marine O18/O16 isotope analysis
  • variations of CO2 between ~200 ppm during glaciations and ~300 ppm in the interglacials.
33
Q

Prior to 350 MYA, why is the 41,000-year cycle considered to be more obvious?

A

It is because the climate changes in the Arctic regions are more influenced by the tilt.

34
Q

What happened In the last 150,000 years?

A

There was phasing of the GHG relative to ice volume at the orbital period, forcing of the ice sheets at the 23K-year period (CH4), and finally an ice-driven feedback at the 41K-year period (CO2).

35
Q

What was the first proposed explanation of how the 41K-year cycle dominate until 0.9 mil years ago if the strongest insolation forcing is at 23K-year cycle?

A

It talked about when when Earth is closest to the Sun (at perihelion) it moves faster in the orbit, how it reduces the length of the summer season, along with the extra insolation at the 23K-year cycles is cancelled out by the shortening of the warmest season.

36
Q

What was the second proposed explanation of how the 41K-year cycle dominate until 0.9 mil years ago if the strongest insolation forcing is at 23K-year cycle?

A

It explained the result of the 23K-year precession insolation changes, when northern ice sheets were growing Antarctic ice was shrinking and how the globally averaged 23K-year signal was cancelled by a 23K-year response of the Antarctic with opposite timing.

37
Q

The second mystery of the ice ages: why did fluctuations start centering near a period over 100K years after 0.9 million years ago?

A

It mentioned the slow cooling and rapid warming at the 100K-year cycles and correlation between reconstructed SSTs in the North Atlantic and vegetation in Europe.

38
Q

In what ways did ice sheets make the glacial world a “dirtier” place?

A

Glaciers are prolific producers of debris.

39
Q

How do scientists use the composition of pollen in lake sediments to determine the climate change?

A

Grasses and herbs are more common in areas where rainfall is low. Tree pollen is more common in high rainfall areas.

40
Q

How different was the climate in the western US during the LGM and why?

A

Today it is dryer. Southward displacement of the jetstream used to bring increased rain and cloud cover.

41
Q

What is the best method of measuring the melting rate of ice sheets over the last 17K years?

A

Studying tropical coral reefs far from the polar ice sheets(sea level rising

42
Q

Does the timing of ice sheet melting support the Milankovitch theory that orbital insolation controls the size of ice sheets? Explain why yes or no.

A

Radiocarbon dating shows the retreat of the large ice sheet in North America, and the timing of these retreats agrees with the Milankovitch theory

43
Q

What is the Younger Dryas and what are the reason(s) for this phenomenon?

A

A period of a sudden big drop in temperature during the middle of the last deglaciation in the North Atlantic region

44
Q

Is there evidence that solar changes drive millennial oscillations of climate?

A

Weaker magnetic field→ weaker solar shielding–> more bombardment by cosmic particles–> faster production of 14C

45
Q

What are the cyclical changes in Earth’s eccentric orbit (eccentricity)?

A

The orbit is an ellipse, not a circle and the motion of the earth results in seasonal shifts between long summer days and short winter days. There is a 2.1 million year cycle but its amplitude is very weak

46
Q

What are the cyclical changes in the Earth’s wobble (precession)?

A

It is caused due to the gravitational pull by the Sun and the Moon on the equatorial bulge which causes rotation of up to 26 miles.

47
Q

How is the Earth’s wobble motion determined?

A

By the direction of the axis leaning

48
Q

In what sense are ice sheets both a climatic response and a source of climatic forcing?

A

Ice sheets respond to summer isolation forcing, which changes their size. Ice sheets forcing results from changes in size.

49
Q

Name an ice-driven response and explain its origin.

A

Effects on North-Atlantic ocean temp. is correlated with ice sheet size.

50
Q

How could the northern hemisphere ice sheets

affect climate in the Southern Hemisphere?

A

Ice sheet over North America has a large influence on nearby ocean temps. The colder temps over the ice sheet, combined with a clockwise flow of winds around the central ice dome, sends very cold winds blowing southeastward over the western North Atlantic Ocean.

51
Q

What evidence suggests that orbital-scale
changes in northern hemisphere ice volume drive
changes in atmospheric CO2, rather than the
opposite?

A

Ultimately, both are driven by changes in Earth’s orbit,
Strong correlation suggests two signals are linked.
Insolation → ice sheets → CO2 levels → positive feedback to ice sheet changes

52
Q

What is the major uncertainty about the total volume of ice sheets at the glacial maximum?

A

Major uncertainty is how far the glaciers reached. in most places they were shown to be extending farther than at any point in history. doubt over whether or not ice sheets reached the ocean, some argued north ice sheets weren’t as far as they had been previously because they were starved for moisture, main reason for uncertainty was because of a lack of C14 dating evidence. Second debate was over extent of glacial marine ice sheets that formed on shallow continental shelves with bases below sea level. Thickness and height of ice sheets also debated

53
Q

Describe how proglacial lakes travel slowly across the landscape behind melting ice sheets.

A

Big lake in front of ice sheet = lake occupies bedrock depression. Ice sheet decrease lake from melting ice; idea that the big lake retreats w/ ice melting -> melting.

54
Q

What do orbital trends imply about future changes in monsoons and northern ice sheets?

A

More ice, fewer monsoons as decrease in temperature.

55
Q

How do the processes that control δ18O changes measured in ice sheets differ from those measured in ocean cores?

A
  • Ice cores: δ18O signals reflect several influences: Temperature of snowfall, *Source of moisture, Transport paths, Season of precipitation
  • Ocean cores: δ18O signals reflect two influences: Temperature of seawater and Ice volume in continents
  • Relationship: As marine δ18O becomes more positive, δ18O in ice cores becomes more negative.
56
Q

What other regions show millennial oscillations like those in the North Atlantic and Greenland?

A

N.H. Mid-latitude Europe, Asia, USA, N.H. Tropics, Equatorial Atlantic, South American Andes, New Zealand, Antarctic

57
Q

Are millennial oscillations true cycles?

A

No, the case for cyclic behavior is very weak, fluctuations are random and unpredictable