Lec 1 - Intro + Climate Data Flashcards

1
Q

What is weather?

A

short-term statistical descriptions of the state of the atmosphere at a given time/place

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2
Q

What are the parts of the E-A system?

A
  • Lithosphere
  • Biosphere
  • Hydrosphere
  • Atmosphere
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3
Q

What is climate the result of?

A

a place’s location!

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4
Q

What is climate?

A

Study of long-term averages/variability of weather conditions for place/region/globe

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5
Q

What are the two things to focus on in any climatic change?

A
  • Forcing
  • Responses
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6
Q

What climate components respond the fastest to changes?

A
  • atmosphere
  • land surface
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7
Q

What climate components respond very slowly to changes?

A
  • mountain glaciers
  • deep ocean
  • ice sheets
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8
Q

How do feedbacks alter climate changes?

A
  • amplifying them (positive feedback)
  • suppressing them (negative feedback)
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9
Q

Name 4 types of climate archives

A
  • sediments
  • ice
    -coral
    -trees
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10
Q

What is the major climate archive on Earth, and how does it form?

A

sediments
- continuous deposition at water bottom OR rainfall/runoff eroding/transporting it OR carried by wind
- physical/granular OR chemical/dissolved form

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11
Q

What is a moraine?

A

long, curving ridges made of jumbled mix of unsorted debris

  • sediment archive = jumbled, pushed around
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12
Q

What is a Loess?

A

rock(?) formation made by winds continuously bringing and dropping grains of sediment in undisturbed areas

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13
Q

What timescale are ice archives formed on?

A

Antarctica - 700ky
Greenland - 120ky
Mountain glaciers - 10ky

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14
Q

When are tree ring archives useful?

A
  • when looking at 10s-100s of years in past
  • when they grew somewhere with many seasons (growing period/dormant period)
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15
Q

How can corals act as a climate archive?

A
  • CaCO3 bands form annually
  • useful looking at 10s to 100s of years in the past
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16
Q

What is a more recently-emerged climate archive?

A

human records!

17
Q

How does radiometric dating work?

A
  • a certain portion of an element exists as an unstable/radioactive isotope
  • these parent isotopes decay at a known rate into stable isotope of another element
  • using the known half-life, we can figure out how long it’s been since the thing died
18
Q

How does radiocarbon dating work, and when is it useful?

A
  • 14C decays into 14N
  • half life is 5780yrs, so only useful in 10s of ky
19
Q

What are the two types of climate proxies?

A
  • biotic proxies
  • geological/geochemical proxies
20
Q

What are some types of biotic climate proxies?

A
  • pollen
  • plankton
  • macrofossils (historical ecology/distribution)
21
Q

Why are plankton so useful as climate proxies?

A
  • ubiquitous
  • well-defined climate preferences
  • have been around for a long time in geologic history
22
Q

What types of geological/geochemical data are useful as climate proxies?

A
  • sediment textures tell us about erosion/conditions
  • sediment types tell us where it came from (physical weathering, chemical weathering)
23
Q
A