M2L3 - Climate Cont. Flashcards

1
Q

Written or Oral histories

A
  • Either direct or indirect
  • Nautical journals recording weather conditions
  • Timing of harvest dates
  • Oral history of lived experiences
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2
Q

Corals

A
  • Use calcium carbonate to build their skeletons
  • Complex relationship between temp, light, nutrients
  • Growth impacted by pH, salinity
  • Also trap oxygen and other elements (can tell us about past environment)
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3
Q

Pollen

A
  • Often deposited in sediment records
  • Unique shapes to different species of plants
  • Can inform what was growing at a certain location
  • Used in conjunction with sediment dating
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4
Q

Ice cores

A
  • Have snow and ice accumulated across millennia
  • Contain dust, air bubbles, isotope signature
  • Capture a signal at time of deposition
  • Can provide information on many climate variables and volcanic activity
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5
Q

Tree ring analysis

A
  • Dendrochronology
  • Can provide climate and environmental parameters
  • Width of ring represents growth
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6
Q

Lake and ocean sediments

A
  • Deposited at different rates, depending on the environment
  • Can include pollen, diatoms, other biological records
  • Thickness of layers can give info on hydrology and land use
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7
Q

Earth’s eccentricity

A
  • Orbit isn’t perfectly circular
  • Eccentricity is a measure of the departure from a perfect circle
  • Cycle occurs over ~100k years
  • Currently at most circular
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8
Q

Obliquity

A
  • Measure of change in axis of rotation
  • Larger the tilt, the more extreme the seasons are
  • 41k year cycle
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9
Q

Axial precession

A
  • How close we are to the sun in summer
  • 23k year cycle
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10
Q

Earth’s climate record

A
  • Lack of data from before 500 million years ago
  • Temporal resolution of data gets worse as you go back in time
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11
Q

Pleistocene climate

A

Rhythmic patterns

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12
Q

Holocene climate

A

Stability

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13
Q

Milankovitch cycles

A
  • Series of variations in the Earth’s orbit around the sun that cause climate change
  • Still ongoing, may explain small amounts of change
  • Can’t explain the rapid rate of change seen since industrialisation
  • Currently in interglacial period, should be cooling not warming
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14
Q

Cretaceous alberta

A
  • 144 to 66 million years ago
  • Death and decomposition of plant and marine life
  • Bacteria broke down light oil resulting in Bitumen
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15
Q

Where did meteor that killed dinosaurs land

A

Chicxulub crater, mexico

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16
Q

How did meteor kill dinosaurs

A
  • Resulted in large amount of sediment and dust mobilising
  • Dust blocked solar radiation (sun), changing the climate
  • Change in environment
  • Rapid change of environment means loss of species (mass extinction)
17
Q

Paleocene-Eocene thermal maximum (PETM)

A
  • Occurred approximately 56 million years ago
  • Period of rapid warming (5-8ºC over 200k years)
  • Large amounts of volcanic activity
  • Dramatic change in species and sediments around the world
  • Acidification of oceans
18
Q

Ice ages

A
  • Period when glaciers are present (opposed to greenhouse periods when no glaciers present)
  • Long and cold periods of alternating glacial and interglacial periods
  • At least 5 ice ages in history
19
Q

Interglacial

A

Period between ice ages

20
Q

Current ice age period

A

Interglacial period within the Quaternary Ice age

21
Q

The last glaciation

A
  • Ice sheets over 3km thick sculpted much of canada
  • Sea level 120m lower (continental shelves exposed)
  • Land bridge to Asia
22
Q

End of the last glaciation

A
  • Ice sheets retreat producing lots of water
  • Glacial lakes form then drain
  • Water drains to the oceans
  • Sea level rises to current levels
23
Q

Electromagnetic radiation types (from long to short wavelength)

A
  • Radio
  • Microwaves
  • Infrared
  • Visible light
  • UV
  • X-rays
  • Gamma rays
24
Q

Incoming solar radiation

A
  • 29% reflected
  • 48% absorbed at the surface
  • 23% absorbed by the atmosphere
25
Q

Planck’s law

A
  • Power flux = P/a = σT^4
  • σ = Stefan Boltzmann constant
  • T = Temperature
  • P = Power
  • a = Area
26
Q

Stefan Boltzmann constant

A

5.67 x 10-8 (W/m2K4)

27
Q

EMR emissions

A
  • Everything with a temperature emits EMR
  • Wavelength is function of temperature of emitting body
  • Solar EMR (solar radiation) is emitted across spectra (visible wavelengths, infrared, UV)
  • Terrestrial EMR is predominantly infrared
28
Q

Greenhouse effect

A
  • Atmosphere acts as a blanket on Earth
  • By trapping radiation ‘inside’ (atmosphere, or garden greenhouse), warms up the environment.
  • Atmosphere is dominated by Nitrogen
29
Q

Greenhouse gasses

A
  • Atmosphere is transparent to visible EMR
  • GreenHouse Gases (GHGs) absorb UV and Infrared EMR warming the atmosphere
30
Q

Clouds and EMR

A

Clouds block all EMR because they are made of liquid or solid water

31
Q

Main two greenhouse gasses

A
  • Carbon dioxide and methane
  • Part of complex system
32
Q

Carbon reservoirs

A
  • Atmosphere
  • Oceans
  • Living things
  • Once living things (fossils, methane hydrates, permafrost)
  • Rocks
33
Q

Rock weathering

A

Carbonic acid dissolves rocks

34
Q

Carbonate precipitation

A

Coral and crustacean growth