Global Climates Flashcards

1
Q

How does Isotope fractionation work with O16 and O18?

A
  • O16 is lighter and evaporated easy, leaving ocean O18 rich
  • moved towards poles (glaciers or land)
  • precipitation has the O18 fall first from the clouds, then O16
  • O16 becomes locked in the ice OR runs back to ocean
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2
Q

Climate and Climatology is..

A

weather of over time, and the study of such

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3
Q

Genetic Climate Classification

A

-based on causative factors

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4
Q

Empirical Climate Classification

A

-based on statistical data (temperature and precipitation)

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5
Q

Applied Climate Classification

A

-created for particular climate-related problems

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6
Q

Six Basic Climate Categories

A
  • Tropical
  • Mesothermal
  • Microthermal
  • Polar
  • Highland
  • Dry
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7
Q

Polar and Highland

A
  • dry cold air
  • extreme daylength range
  • high albedo
  • low precipitation
  • ice cap and ice sheet climate , tundra climate, polar marine climate
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8
Q

Dry Climates

A
  • 15 and 30 N and S
  • dry subsiding air in high pressure systems
  • mountain rain shadows
  • continental interiors
  • above 30 (N) semiarid grasslands
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9
Q

Microthermal Climates

A
  • lowering sun angles and increase daylentgh variability causes temperature ranges
  • cool to cold
  • cP air mass in winter and convectional thunderstorms in summer
  • 21% of land surface
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10
Q

Mesothermal Climates

A
  • summers hot to warm to cool
  • shifting maritime and continental air massses
  • P from low (summer) and high (winter) systems = changing weather
  • humid subtropical: winter dry, hot summer, moist all year
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11
Q

Tropical Climates

A
  • 36% of land and ocean
  • consistent daylength, insolation, warm , maritime air masses, shifting ITCZ
  • tropical rain forest climate - constant ITCZ, warm and water surplus
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12
Q

Climate Change: Tropical Zone width, Rossby waves, ice mass, ocean heat

A
  • zone widened >2 degrees
  • Rossby waves amplified
  • ice sheets losing mass
  • ocean heat increased
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13
Q

Climate Models

A
  • mathematical
  • based on established science
  • discretization, variable spatial and temporal resolutions
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14
Q

Climate Model Data

A
  • observations

- proxy methods (paleoclimatology)

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15
Q

Climate Proxies

A

-observations providing info about past environmental coniditions

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16
Q

Types of Climate Proxies

A
  • geological
  • biotic
  • corals, speleothems
  • tree rings
17
Q

Climate Archives

A
  • lake sediments (10 y to 20 kY to 30 My)
  • ocean sediments ( up to 170 My)
  • land cores (Gy)
  • ice cores (1 y to 0.9 My)