Quaternary Environment Flashcards

1
Q

What are the 3 types of sea level change?

A

Steric
Eustatic
Isostatic

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2
Q

Describe Steric effect on sea level

A

Changes in sea level due to temperature, salinity and the dependence of density on temperature and salinity

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3
Q

Describe the Eustatic effect of sea level

A

Global changes in sea level

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4
Q

Describe Isostatic effect on sea level

A

Local changes in sea level due to the rising or sinking of land masses

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5
Q

What are 3 types of evidence of climate change?

A

Lithological evidence
Biological evidence
Geomorphological evidence

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6
Q

Explain Lithological evidence

A

Evidence found in rocks and sediments

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7
Q

Explain biological evidence

A

Evidence from fossils, such as diatoms, plant macrofossils, and foraminifera.
Also Pollen stratigraphy

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8
Q

Explain Geomorphological evidence

A

Evidence from landforms, such as glacial landforms

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9
Q

What are Milankovitch cycles?

A

Cyclical changes in Earth’s Orbital and rotational parameters

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10
Q

Eccentricity

A

Changes in the shape of Earth’s orbit around the sun

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11
Q

Obliquity

A

Changes in the tilt of Earth’s axis of rotation

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12
Q

Precession

A

Wobble in Earth’s rotational axis

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13
Q

How do orbital and rotational changes influence earth’s climate?

A

They affect the amount and distribution of incoming solar radiation (insolation), which in turn influences Earth’s climate and the growth and retreat of ice sheets

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14
Q

INSOLATION

A

INcident SOlar radiATION

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15
Q

How do Milankovitch cycles affect ice sheet dynamics?

A

Warmer summers due to higher insolation, leads to increased ice melt, while cooler summers allow ice to survive year-round, contributing to ice sheet growth

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16
Q

What are ocean climate change indicators?

A

1 - Sea Surface Temperature
2 - Ocean Heat Content
3 - Ocean pH
4 - Dissolved Oxygen Concentration
5 - Artic Sea Ice Extent, Thickness, and Volume
6 - Sea Level
7 - Strength of the AMOC

17
Q

Sea Surface Temperature (SST)

A

The temperature of the ocean’s surface

18
Q

Ocean Heat Content (OHC)

A

The amount of heat stored in the ocean

19
Q

Ocean pH

A

The acidity of the ocean

which is increasing due to the absorption of CO2 from the atmosphere.

20
Q

Dissolved Oxygen Concentration

A

The amount of oxygen dissolved in seawater

21
Q

Arctic Sea Ice Extent, Thickness, and Volume

A

The extent, thickness, and volume of sea ice in the Arctic are declining rapidly, which has significant implications for the regional climate, ecosystems, and human communities

22
Q

Sea Level

A

Global sea level is rising due to the melting of glaciers and ice sheets, as well as the thermal expansion of seawater as it warms

23
Q

Strength of the AMOC (Atlantic Meridional Overturning Circulation):

A

This major ocean current system, which plays a critical role in regulating global climate, is showing signs of weakening, which could have profound effects on regional and global climate patterns

24
Q

What are the two main methods for dating climate records?

A

Radiocarbon dating and Cosmogenic nuclide dating

25
Q

Radiocarbon dating

A

Based on the decay of the radioactive isotope carbon-14, this method is used to date organic materials up to around 60,000 years old

26
Q

Cosmogenic nuclide dating

A

This method utilises the accumulation of radioactive isotopes produced by cosmic rays in surface materials to determine the time of exposure, allowing dating of landforms and other geological features