Paleoclimate Flashcards

1
Q

What is paleoclimate?

A

it is the study of earth’s climate and helps us understand what influences this kind of climate variation

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2
Q

What are some methods used to study past climate?

A
  • ice cores
  • dendrochronology
  • eras
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3
Q

What are the drivers of glacial-interglacial cycles?

A
  • orbital variations
  • volcanic activity
  • solar variability
  • greenhouse gas concentration
  • plate tectonics and continental drift
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4
Q

How does analyzing ice cores help reconstruct the past climate?

A

drilling into ice and looking at the gasses trapped in the bubbles in the ice reveals the greenhouse gas levels overtime

ex: radioactive isotopes show clues

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5
Q

What is dendrochronology? How does it help reconstruct the past climate?

A

it is the study of tree rings

by looking at the size of the tree rings, it gives us an idea of the environment during that year

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6
Q

How do the sizes of tree rings give us information on the past environment?

A
  • Wide rings - favorable conditions
  • Narrow rings - stressful conditions
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7
Q

What were the different paleoclimate periods?

A
  • mesozoic era
  • cenozoic era
  • quarternary period
  • paleocene-eocene thermal maximum
  • last galcial maximum
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8
Q

What was the mesozoic era?

A
  • 252 - 66 million years ago
  • was a time of warm and stable climate; no ice caps; high CO2 levels
  • Supported tropical and subtropical ecosystems
  • Dinosaurs and large vegetations
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9
Q

What was the cenozoic era?

A
  • 66 million years ago - present
  • gradual cooling trend
  • new ecosystems (grasslands); rise of mammals, birds, and flowering plants
  • foundation for today’s glacial-interglacial cycles and climate variability
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10
Q

What was the quarternary period?

A
  • 2.6 millions years ago - present
  • Cycles of glaciation and interglacial warming, driven by orbital changes
  • Evolution and migration of early humans; varied ecosystems
  • Demonstrates natural climate cycles; helps distinguish human-driven changes from natural climate variations
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11
Q

What was the paleocene- eocene thermal maximum?

A
  • 56 million years ago
  • abrupt warming of 5-8ºC over 200,000 years because of a large greenhouse gas release
  • species migrations, adaptations; ocean acidification
  • reveals consequences of rapid warming and greenhouse gas releases on ecosystems
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12
Q

What was the last glacial maximum?

A
  • ~20,000 years ago
  • peak of the last ice age
  • sea levels were lower
  • Ice-adapted ecosystems
  • benchmark for understanding glacial cycles and potential future cooling scenarios
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13
Q

How does orbital variation impact the climate?

A
  • movement of earth in space affects climate change
  • Eccentricity, obliquity, and precession alter Earth’s distance and orientation to the Sun
  • impact the amount and distribution of sunlight that the earth receives
  • higher obliquity -> warmer summers and cold winters
  • Drives glacial-interglacial cycles over tens of thousands of years
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14
Q

What is the Milankovitch Cycle?

A

Milankovitch cycles are periodic changes in the orbital characteristics of a planet that control how much sunlight it receives, thus affecting its climate and habitability over hundreds of thousands of years.

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15
Q

How do volcanic eruptions impact the climate?

A
  • impacts sunlight and solar radiation
  • Eruptions release aerosols (cooling effect) and greenhouse gases like CO₂ (warming effect)
  • Causes short-term cooling and can contribute to long-term warming with CO₂ buildup
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16
Q

How does the solar variability impact the climate?

A
  • Changes in solar radiation due to sunspot cycles and periods like the Maunder Minimum
  • Leads to temperature fluctuations over decades and centuries
17
Q

What does sunspot activity tell us about the climate?

A
  • higher activity - warmer
  • lower activity - cooler
18
Q

How do the greenhouse gas concentrations impact the climate?

A
  • CO₂ and methane levels vary naturally due to volcanic activity, biological processes, and oceans
  • Affects the greenhouse effect, influencing global temperatures over time
19
Q

How do plate tectonics and continental drift impact the climate?

A
  • Continental movement alters ocean currents, wind patterns, and heat distribution
  • Shapes long-term climate by modifying ocean circulation and atmospheric conditions
20
Q

What were the consequences of the Ice Age?

A
  • Lower CO2 levels can allow ice sheets to expand
  • positioning of continents can impact how the ice caps retreat
  • Contributed to the deposition of rich soils
  • Caused valleys and other changes in the landscape
  • Affected biodiversity
21
Q

What is an anthropocene?

A

period of time during which human activities have impacted the environment enough to constitute a distinct geological change

22
Q

Why is the anthropocene important?

A
  • increase in global temperature
  • rapid biodiversity loss
  • increased fragmentation
23
Q

What is the debate with the topic of the anthropocene?

A

Geologists say we’re not in an anthropocene epoch and that to be considered an epoch we must have a unique marker on the geological record but some say that the epoch started in 1950s around the time of the industrialization

24
Q

What is hyper-novelty?

A

A phenomenon where rapid pace of technological, social, and environmental changes outstrips the human species’ ability to adapt

25
Q

What is the problem with hyper-novelty?

A
  • Creates a mismatch between our evolved instincts and the demand of our contemporary life
  • Create risks in modern agriculture and social stability
  • The speed in which the world is changing is faster than our evolutionary adaptation