unit 8, exam 2 Flashcards

1
Q

faint young sun paradox

A

sun gets stronger with time so early Earth received about 70% of current energy, but Earth was still hot

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2
Q

sunspot cycles

A

11 years

more sunspots=more energy output. not enough to drive climate change

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3
Q

milankovitch cycles and orbital parameters

A

eccentricity
precession
obliquity

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4
Q

eccentricity

A

100,000 year cycle

changes in how extreme the elliptical orbit is. how close or far away the earth is from the sun

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5
Q

perihelion

A

point closest to the sun

right now in january

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6
Q

aphelion

A

point furthest from the sun

right now in june

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7
Q

precession

A

23,000 year cycle
changes that effect which hemisphere faces the sun during the perihelion/aphelion
-changes the contrast between summer and winter seasons
-THIS IS WHY ICE AGES ARE POSSIBLE
colder summers are what can make ice and snow and glaciers expand

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8
Q

obliquity

A

41,000 years
earths axis tilt changes from 22.1-24.5 and back over those years.
as tilt increases=winters colder, summers warmer
tilt decreases=seasons even out

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9
Q

global contributions

A

plate techtonics

volcanoes

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10
Q

plate techtonics

A

determine land mass and how radiation is absorbed by earth

10million to 100 million years

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11
Q

volcanoes

A

1-millions of year time scale
increase in greenhouse gases
some decrease because of aerosals(mt.pinatubo) (aerosal dimming)(deccan traps)

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12
Q

future trend of milankovitch cycles

A

less elliptial orbit
closer to the sun in june
lesser axis tilt
ALL POINTING OPPOSITE OF CLIMATE CHANGE

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13
Q

aerosal dimming

A

absorb energy and scatter or send it back out as shortwave radiation

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14
Q

deccan traps

A

big plateau of volcanic stuff in india. potentially the demise of the dinos. huge eruption after astroid

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15
Q

positive feedback

A
climate change increases as a reaction to initial change.
more of this in nature
ice albedo feedback
soil moisture feedback
warm earth feedback
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16
Q

negative feedback

A

reaction to initial change tries to balance things back out

warm earth-evaporation feedback

17
Q

arctic amplification

A

more heating is going on at the poles as compared to the equator

18
Q

sinks

A

components responsible for removing carbon from another component

19
Q

source

A

component responsible for adding carbon to another component

20
Q

methane hydrate

A

melting of land with methane forms thermokarst lakes which decay and release methane into atmosphere increase in GHG then warms system and melts permafrost

21
Q

human contributions of sources and sinks

A
Energy industry(GHG)
Aerosols (global dimming & cooling effect)
Land use/land change
Agriculture
22
Q

callendar effect

A

theory that global climate change can be brought about by enhancement of the earth greenhouse effect by increasing GHG concentration in the atmosphere

23
Q

keeling curve

A

daily record of observations of CO2 at manua loa used as evidence that atmopheric CO2 is rising and contributing to climate change.

  • 40% greater than industrial revolution
  • burning fossil fuels accounts for 75% of deforestation
24
Q

natural aerosals

A

volcanoes, dust, sea spray(salt), pollen, fire smoke

25
Q

anthroprogenic

A

diese soot, coal power, slash and burn smoke, ag emisisons of dust

26
Q

deforestation

A

decreases a natural sink of carbon

27
Q

urbanization

A

change in land surface use which alters absorbed solar energy changing the energy budget

28
Q

irrigation

A

infuences surface evaporation and T/rainfall downstream

29
Q

agriculture

A

modifies land use and water distribution
food has a large carbon Footprint, especially red meat
deforestation (91%) of amaozn is for animal ag