lecture 17: weather and climate Flashcards

1
Q

global atmospheric circulation

A

polar cell: rising warm moist air, low pressure
farrel cell: descending cool, dry air, high pressure
hadley cell: rising warm moist air, low pressure

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2
Q

weather vs climate

A

weather: meteorological condition at a given location and time, short term and localized
climate: meteroological condition that prevails in a region, long term and regional “statistics of weather” averaged over time

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3
Q

3 causes of natural climate variations (1: plate tectonics)

A

continents near poles increases snow accumulation and glacier formaiton which increases albedo and reflects solar energy back to space
- ocean current brings warm water and increased precipitation to high lattitudes (ocean conveyer belt)

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4
Q

3 causes of natural climate variations (2: solar irridance)

A

amount of solar energy received per unit on Earth
depends on:
1. total solar irridance produced at sun
2. orientation and distance of earth with respect to sun
- changes occur due to solar cycle

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5
Q

sun spots (solar irridance)

A

storms on the surface of sun which mark 11 year peaks in solar output

  • during periods, sun heats earth more
  • sun and climate going in opposite directions (total irridance over last 400 years increased but last 50 years decrease)
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6
Q

milankovitch cycles (solar irridance)

A

variations in earths astronomical movements (orbital Eccentricity, axial Tilt, and axial Precession) that influence solar irradiance on time scales of 1,000s to 100,000s of years
- explain large scale warming or cooling trends on geological time scales

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7
Q
  1. orbital eccentricity
A

changes in the earths orbit between nearly circular and more eliptical, averaging 100,000 years
- today cycle is nearly circular

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8
Q
  1. axial tilt (obliquity)
A

changes in earths axial tilt b/w 21.5-24.5
cycle of 41,000 years
greater tilt = greater extremes which results in decreased glaciation and warmer temperatures
tilt today is 23.5 which is large seasonal variations

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9
Q
  1. axial precession (wobble)
A

changes in earths wobble around its tilt axis
- from pointing at polaris (North star) to star vega
timespan of 19,000-23,000 years
today earth is closest to sun during northern hemisphere winter

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10
Q

3 causes of natural climate variations (3: greenhouse gases)

A

climate is kept stable by natural emissions of greenhouse gases in atmosphere, feedback system keeps Earth at average of +15 degrees rather than -18 degrees

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11
Q

what 4 things modulate atmospheric CO2

A
  1. weathering of silicate rocks
  2. volcanism
  3. biology (marine organisms of CaCO3 shells
  4. burial and subduction of carbon rich sediments
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12
Q

how do we measure CO2 concentrations

A

air bubbles trapped in ice cores

- variations from 180-300ppm over 400,000 years

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13
Q

anthropogenic sources of greenhouse gases

A

CO2- burning of fossil fuels and forests
CH4- decomposition of vegetation in absence of O2
N2O- chemical fertilizers and automotive combustion
O3- automotive/industrial gases (smog)
CFC- coolants and solvents (now banned)

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14
Q

current rate of warming

A

0.7 degrees in 100 years
natural global warming occurs at most 1,000 years/C
10x faster and accelerating
models predict earth will warm between 2-6 degrees in the next century (20x faster)

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15
Q

sea level rise

A

90% of heat absorbed by oceans which increases volume (thermal expansion) melting ice adds water to oceans
suggest 0.3-1.2m (30-120cm) by the end of century

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16
Q

climate change impact: northern canada

A
  • northwestern passage opened up for commercial maritime traffic
  • potential for more arctic natural resource development
  • melting permafrost weakens and undermines infrastructure
  • wildlife adapted to cold climate shift northward by 150km for every degree of warming
17
Q

climate change impact: british columbia

A
  • pacific waters too warm for sockeye salmon
  • increased likelihood of more wildfires and longer fire seasons
  • increased winter precipitation raises risk for spring snowmelt flooding
  • higher winter precipitation also increases the risk for landslide and avalanches in mountanoious regions
18
Q

climate change impact: atlantic canada

A
  • rising sea levels and greater storm activity will generate more powerful storm surges
  • increased flooding, coastal erosion and property damage
  • little chance for cod and salmon recovery, possibility for new invader species to take over
19
Q

climate change impact: ontario and quebec

A
  • reduced water levels in the great lakes and St Lawrence river affects shipping and hydroelectric power generation
  • reduced risk from snowmelt and ice jam flooding but higher of flash flooding
  • longer and more severe heat waves
  • potential for worse air pollution in the form of smog, airborne dust and ground level ozone
20
Q

climate change impact: prarie provinces

A
  • longer growing season (longer frost-free period)
  • reduced soil moisture and irrigation waters
  • shrinking wetlands
  • increased in drought frequency and severity
  • crops more at risk to pests and disease
21
Q

climate change and hurricanes

A

rising ocean heat content provides more energy for tropical storms
- number of storms is increasing

22
Q

climate change and storm surges

A

sea level rise will also increase coastal vulnerability to storm surges

23
Q

climate change and wildfires

A

increase wildfire events

24
Q

climate change and earthquakes

A

Parvie fault scarp in sweden: Mw earthquake due to isostatic rebound
- melting of glacial ice