depth study climate change Flashcards

1
Q

climate change definition?

A

a long-term change in the statistical distribution of weather patterns over periods of time that range fo=rom decades to millions of years

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2
Q

weather vs climate?

A

Weather – short term, specific to a location at a particular time (daily, temp, rain, wind)

Climate – long term average weather conditions in a region (temp, precipitation)

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3
Q

areas of high rainfall?

5 points

A
  • regions of rising moist air and low pressure
  • low latitude near the equator (tropics, near sun)
  • Mid-latitude regions experience moderate-high levels of rainfall, created by cold fronts or low pressure (higher rainfall in winter)
  • Coastal areas experience higher rainfall than inland (closer to water)
  • Regions on windward slopes of mountains, increasing altitudes cause water vapor and winds
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4
Q

areas of low rainfall?

5 points

A
  • Regions with high pressure, reduces condensation resulting in clear skies
  • Subtropic regions
  • Polar regions due to lack of evaporation and moisture (heat depict)
  • Inland areas due to distance from bodies of water
  • Leeward slopes of mountains (facing ocean side)
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5
Q

areas of high temperature?

4 points

A
  • Areas closer to equator (warmer, direct insolation)
  • Hottest places on earth are in subtropical climate zones of high pressure, no cloud cover, high insolation
  • Most comfortable climates in mid-latitude zones
  • Areas of low albedo (reflection of surface) absorb more insolation (higher temp)
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6
Q

areas of low temperature?

5 points

A
  • Areas closer to the poles
  • Heat deficit zones, receive less insolation due to the angle of the earth
  • Regions beyond 37 degrees N and S
  • Areas of high albedo
  • Areas of high altitude (in atmosphere)
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7
Q

heatbudget definition/key element?

2 points

A

-The balance of incoming and outgoing heat on earth
- Once the insolation has been absorbed, it is eventually re-radiated back into the atmosphere

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8
Q

greenhouse gas definition?

2 points

A

The process by which greenhouse gasses trap a proportion of the outgoing longwave radiation from the earth
- this leads to the warming of the atmosphere

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9
Q

how does the heat budget influence the earths climate?

2 points

A

-Any alteration to the balance of incoming/outgoing radiation has significant impacts for the earth’s climate
-heat budged dictates planets overall temp

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10
Q

how does greenhouse gasses influence the earths climate?

1 point

A

-gasses are essential to retain heat, and keep the planet warm enough to sustain life.

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11
Q

hydrological cycle definition/key element?

2 points

A

The continuous movement of water in the earth’s spheres, in the form of solid, liquid and gas.
-driven by solar energy, which powers process of evaporation + transpiration

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12
Q

how does hydrological cycle influence earths climate?

3 points

A

-processes + regulates elements of weather (rainfall)
-undisturbed cycle creates long term climatic patterns
-alteration would amplify processes, impacting the earth’s climate by changing precipitation patterns, disrupting ecosystems and intensifying extreme weather patterns.

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13
Q

hydrological cycle diagram features?

evaporation… dont just list

4 points

A

-evaporation: water changing from liquid to gas, due to insolation. Mostly in oceans
-condensation: water changing from gas to liquid. Occurs in atmosphere
-precipitation: occurs when rain, snow, hail, falls from sky. When the atmosphere cannot hold the weight. Depends on temp (falls as liquid or solid)
- transpiration: plants release water vapor into atmosphere through leaves.

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14
Q

heat budget diagram features?

incoming insolation

3 points

A

-47% gets through to earth’s surface
-30% reflected into space
-23% absorbed by atmospheric gasses

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15
Q

heat bugdet diagram features

outgoing insolation

3 points

A

-24% latent heat
-10% directly into space from earth’s surface
-6% longwave is absorbed by greenhouse gasses

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16
Q

solar variation overview?

natural cause

2 dot points

A
  • Refers to the changes in the sun’s energy output
  • These variations occur due to changes in solar activity, such as sunspots, solar flares and shifts in solar radiation
17
Q

solar variation cause climate

natural cause

4 dot points

A
  • The solar cycle is an 11-year cycle. Sunspots are huge magnetic storms that occur on the sun’s surface
  • During a storm, extra radiant energy is released and is sent to the earth, affecting the amount of insolation received.
  • More sunspots indicate higher solar activity, increasing energy output
  • Less solar activity leads to minor cooling effects
18
Q

volcanic eruption overview?

natural cause

2 dot points

A
  • Eruptions can influence earths climate by releasing gases and ash into the atmosphere
  • Their impact depends on the size, frequency and type of eruption
19
Q

volcanic eruptuon cause of climate?

natural cause

3 dot points

A
  • Initially dust and ash emitted into the upper atmosphere can create a short-term cooling effect
  • 2O2 reacts with water vapor to form sulphate aerosols, which prevents some of the suns rays from heating the earth
  • Greenhouse gases contribute some warming effect
20
Q

urban overview?

anthropogenic causes

one point

A
  • Activities associated with urban land use contribute to most anthropogenic greenhouse gas emissions
21
Q

urban cause of climate?

anthropogenic cause

4 dot points

A
  • Human caused Greenhouse gas emissions – urban…
  • Energy use in cities (is increasing due to rapid urbanization and population growth)
  • Urbanization and land use changes
  • Urban activities (housing, transport, energy, industrial processes)
22
Q

deforestation overview point?

anthropogenic causes

one point

A
  • Contributes to climate change by releasing stored CO2 into the atmosphere when trees are removed, and by reducing the plant’s ability to absorb CO2
23
Q

deforestation cause of climate?

anthropogenic causes

2 points

A
  • Trees absorb and store carbon. When forests are cleared or burned, this stored carbon is released back into the atmosphere as CO2
  • The less trees there are, the less ability for the planet to absorb CO2
24
Q

climate change rate overview?

1 dot point

A
  • More recent climate change is occurring at a rate much faster than in the past, mostly due to anthropogenic processes
25
climate change rate indicators? | x4
- increase carbon dioxide - increase global temp - global ice melt - sea level rise
26
evidence through geological time summary? | 3 points
- geological time scale is system of measurement used to describe events throughout earths history - Different spans of time are determined by changes in layers of environmental features - Uses proxy data to establish past climate conditions
27
ice cores as evidence? | 7 points
- A core sample removed from ice sheets or glaciers - Dating cores through layers - Bubbles trapped in ice capture gas concentrations of the atmosphere - Preserved record of historical atmospheric composition - Each passing year, show falls over ice sheets and each layer of snow has a different texture and chemistry - Each layer provides info about the climate each year - tell scientists about temperature, precipitation, atmospheric composition, volcanic activity and wind patterns
28
evidence in recent human history? | 3 points
- Evidence of changes in climate comes from observations of climate system based on direct measurements and remote sensing and other platforms. - Due to technological advancements since the 1950s, more comprehensive and diverse sets of observations are being collected - With paleoclimatic data, they provide a detailed view of the variability and long-term changes
29
atmosphere as evidence?
- Global temperature measurements in the past decade have been the hottest on record - Atmospheric concentrations of major greenhouse gasses have been increasing - Rapid CO2 increase - More frequent and intense heatwaves, causing deaths and infrastructure failures - Shifting rainfall patterns | 5 points
30
albedo surface reflectivity climate and land change | climate x4, land change x2
Climate – melting ice sheets - Ice and snow have high albedo, reflecting most sunlight - ice melts, due to rising temps, darker ocean is exposed - Darker surfaces absorb more heat - Deforestation contributes to warm temperature, which melts ice sheets Land change – deforestation - Forests have low albedo of (5-15), but they also absorb CO2, helping regulate - When forests are cleared, exposed soil and bare land absorb more heat
31
natural carbon sequestration climate and land change | climate x2, land change x1
Climate – raising temperature - Any changes to this process affect climate - Land cover change results in releasing of greenhouse gasses to atmosphere, further warming earth Land change – deforestation - When trees are cut, the absorbed CO2 gets released back into the atmosphere, warming the climate and rising temps.
32
natural environment present impacts | x5
- Main impact: increased melting due to rising temps - Loss of ice mass worldwide (shrinking mountain glaciers) - Loss of habitat - Contribute to rising sea levels - Reduction in albedo affect, meaning less radiation reflected, further warming
32
natural environment projected impacts | x4
- Collapse of major ice sheets - Triggering irreversible sea level rise - Loss of permafrost, releasing methane, accelerating climate change - Distribution of freshwater availability
32
anthropogenic environment projected impacts | x3
- Flooding – sea level rise (coastal cities, provoke extreme weather events) - Threatened freshwater - Warmer conditions (increasing diseases)
33
anthropogenic environment present impacts | x4
- Main impact – temperature rise - Intensified urban heat island effect - More frequent and intense heatwaves - Increased demand for air conditioning (more energy, GHG increase)