Chapter 8 Flashcards

(32 cards)

1
Q

Weather vs Climate

A

weather is short term and local
climate is long term and regional

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2
Q

early climate classification

A

frigid, temperate, torrid

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3
Q

koppen climate system

A

based on annual and monthly average temp and precipitation

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4
Q

Tropical

A

almost entirely confined to the equator and tropics of Capricorn and cancer

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5
Q

dry

A

potential evaporation exceeds precipitation

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6
Q

mid latitude

A

summers are hot and coldest month has an average temp of -3 C

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7
Q

severe midlatitude

A

winters have at least occasional snow cover with the mean temp going below -3 C; summers are mild

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8
Q

polar

A

all months have mean temps below 10 C

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9
Q

Tropical Humid Climates

A

tropical latitudes, winterless climates, little temp change, high humidity; precipitation influenced by ITCZ

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10
Q

Dry Climates

A

30% of land area worldwide; lack of moisture or uplift; typically in subtropics; marine deserts

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11
Q

mild midlatitude climates

A

transition between warmer tropical climates and colder severe climates; hot summers, mild winters, high variable precipitation amounts

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12
Q

severe midlatitude climates

A

northern hemisphere; continentality: far from oceans; long, cold winter and short summer

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13
Q

polar climates

A

receive little insolation; no average temp over 50; extremely dry but NOT arid

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14
Q

Highland climate

A

variable; altitude is more significant than latitude; high diurnal temp variations due to dry, thin air

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15
Q

humid continental climate

A

climate of the US; dominated by westerlies and associated with frequent weather changes; warm summer, cold winter; low precipitation but high at coastal; winter precipitation associated with cyclones, summer with convection

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16
Q

boundary conditions

A

external factors that Earth’s climate responds to

17
Q

forcing agents

A

external factors driving climate change

18
Q

reasons why climate change happens

A
  1. solar output fluctuations: sunspot activity related to solar output
  2. continents shift positions: this changes patterns of temp, winds, ocean currents, and albedo
  3. Milankovitch cycle: changes total solar energy arriving at top of atmosphere and distribution of this energy around the globe
  4. changes in oceans: absorb energy, store energy, transfer energy
  5. atmospheric changes: volcanoes release aerosols (cool atmosphere) and CO2 (warms the atmosphere)
19
Q

feedback mechanisms

A

one factor affects another
positive: feedback magnifies further change in a variable
negative: feedback acts to inhibit further change

20
Q

pleistocene ice age

A
  • rapid climate change (colder)
  • CO2 was low, sea levels low
  • caused ice sheets
21
Q

Holocene Epoch

A
  • changing orbital parameters
  • rapid warming: melting of the laurentide ice sheet
  • initiated younger dryas event: rapid cooling
22
Q

medieval climate anomaly

A

the north atlantic region was unreasonably warm

23
Q

little ice age

A

followed the medieval climate anomaly; north atlantic was unreasonably cold

24
Q

hockey curve

A

medieval climate anomaly and LIA pictured

25
Permafrost melting
high albedo reflects as much as 90% of suns energy (positive feedback bc increases melting)
26
effects of climate change
more wildfires, longer growing season, water vapor in air increases, more intense rainfall, increased flooding - more hurricanes: increase in intensity
27
what does hurricane frequency depend on?
el nino (decreases frequency) and atlantic multidecadal oscillation (increases frequency)
28
isotopes that affect climate change
oxygen 16 and 18 O18 requires more energy to evaporate and condenses faster
29
Ice cores to determine past climates
- ice cores determine oxygen ratios - used to obtain temperature data from isotope ratios, provide info on past chem of atmosphere, and past volcanoes
30
oceanic sediment deposits to determine past climates
- cores include the bones and shells of plankton and other animals - CaCO3 important for determining past climate
31
biological methods to determine past climate
fossils: leaf fossils (serrated edge means cooler climate) plant fossils: used to estimate CO2 concentration - fewer stoma= high CO2 fossil pollen: widely dispersed; shows record of past vegetation
32
remnant landforms to determine past climate
the movement of water, the slow-moving of ice sheets expanding across the surface, wave action across coastlines, wind, and floating icebergs carrying debris