The EAR 111 Practice Final assesses understanding of climate change, feedback mechanisms, sources of atmospheric CO2, and historical climate trends. It is designed for learners to evaluate key processes in Earth's climate system and interpret geologic data.
Positive and warmer
Positive and cooler
Negative and warmer
Negative and cooler
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Surface ocean
Soil
Vegetation
Mantle
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Iv, i, ii, iii
I, iv, ii, iii
I, iii, ii, iv
Iv, ii, i ,iii
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Steadily dropping
Steadily rising
Constant
Fluctuating
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Precession
Tilt
Eccentricity
Solstice
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0-.1
.7-1.2
1.5-2
Earlier than 2.5
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Produced; taken up
Decomposed; taken up
Produced; released
Decomposed; released
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Atlantic Indian Pacific
Indian Pacific Atlantic
Pacific Atlantic Indian
Pacific Indian Atlantic
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Soil
Ocean
Riverbeds
Wetland
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Most recent strong glaciation
Most recent strong deglaciation
Longest glaciation
Longest deglaciation
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20
40
60
100
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Much higher than
Much lower than
Similar to
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Higher; Atlantic
Higher; Indian
Lower; Arctic
Lower; Pacific
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Cordilleran
Laurentide
Greenland
Scandinavian
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Warmer and dryer
Warmer and wetter
Colder and dryer
Colder and wetter
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CLIMAP data could be wrong
CLIMAP data might not be sufficient
Temperature fluctuation is bigger in tropics
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Ice
Lake sediments
Moraine
Seawater
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3k
5k
10k
16k
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Ice-sheet response can pre-date insolation
Ice-sheet was bigger before 10ka
Ocean volume was smaller before 10ka
Melting was not controlled by insolation
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C14 dated sea level curve
U-Th dated sea level curve
13C of Coral
13C of Forams
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Heavier 018
Lighter 018
Heavier C13
Lighter C13
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Younger Dryas
Little Ice Age
Medieval warm period
LGM
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Thermal bipolar seesaw
Insolation oscillation
Ice-sheet melting oscillation
Greenhouse gas oscillation
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Savanna; C3 to C4
Sahara; C3 to C4
Savanna; C13 to C14
Sahara; C13 to C14
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Monsoon
Agriculture
Ice sheet
Younger Dryas
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Strong monsoon
Weak monsoon
Extreme cooling
Extreme warming
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Freezing
Drought
Earthquake
Riots
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Heat
Water
Sunlight
Nutrient
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At high latitude S. hemisphere
Near the tropics
At high latitude N. hemisphere
At mid-latitude N. hemisphere
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Precise age control
Widely available
Easy to sample
Length of record
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Unusual air circulation pattern
Less rainfall in eastern Pacific
Warming of surface water
Weakened upwelling in eastern pacific
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1500-1600
1600-1700
1700-1800
1800-1900
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Melting of mountain glaciers and sea-ice
Frequent El Nino
Frequent draught and stronger tropicals
Stopping of thermohaline circulation
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D13C and d18O
Radioactivity and d18O
D18O
D13C and radioactivity
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Human
Nature
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Vinegar
Fossil fuel burning
Industrial waste water
Acid rain
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2
5
8
10
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Carbonic acid
Bicarbonate ion
Carbonate ion
Calcium carbonate
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Increase;decrease
Decrease ; decrease
Decrease; increase
Increase; increase
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Easier, harder
Harder, harder
Harder, easier
Easier, easier
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Paleocene-Eocene Thermal Maximum
LIttle Ice Age
Younger Dryas
Extinction of dinosaur
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Very high
Very low
Low
Highly variable
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N Atlantic
S Atlantic
S Pacific
N Pacific
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Oxidation of organic matter
Dissolution of co2
Dissolution of CaCO3
Photosynthesis
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Oxidation of organic matter
Poor ventilation
Dissolution of co2
Photosynthesis
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Atmospheric co2
Ventilation
Temperature
Oxygen utilization
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Nutrient
Co2
Toxic chemicals
Heavy metal
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Limestone
Organic rich shale
Organic lean shale
Granite
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