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Test your basic knowledge |
Global Warming
Start Test
Study First
Subjects
:
literacy
,
science
Instructions:
Answer 50 questions in 15 minutes.
If you are not ready to take this test, you can
study here
.
Match each statement with the correct term.
Don't refresh. All questions and answers are randomly picked and ordered every time you load a test.
This is a study tool. The 3 wrong answers for each question are randomly chosen from answers to other questions. So, you might find at times the answers obvious, but you will see it re-enforces your understanding as you take the test each time.
1. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Sea-Ice Albedo
Atmospheric Composition
Methane
More rain means no drought
2. Just remember the general direction of the circulation - Rising northern pacific. You start in between Greenland and Europe (youngest water) - Oldest water is in the Pacific Ocean - Salty water> fresh water - Cold Water > Warm Water
Atmospheric Structure
Thermohaline Circulation
Monthly maximums and minimums
Discontinuous
3. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Nitrous Oxide (N2O)
Questions to think about
Layers of Earth
Thermohaline Circulation
4. Over the past century what has happened to the Earth's temperature?
GHG
Permafrost
Dynamic thinning
Some regions of the Earth have warmed faster than other regions.
5. Much of the Arctic is overlain by snow and sea ice (land ice and sea ice) - It makes warming a much bigger deal in the Arctic
Why ice-albedo feedback is a big deal in the Arctic
Ice in the Arctic
IPCC
Antarctica
6. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Atmospheric Structure
Hydrological Drought
Shortwave Length
Thermokarst Lake
7. Volcanic eruptions - Sunspots - Wobbly Earth
Severe coastal erosion
The Ozone Hole
Black Carbon
Natural Causes of Warming
8. Less frequent and weaker
Methane
Severe coastal erosion
Carbon Dioxide
Inversion Layer Summer
9. 10 : 1 - grounding ; surface
Ice Cap
.75OC/km-1
Grounding v Surface Melting
Amount of light actually reaching the Earth
10. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Ice shelf
20%
% of Greenhouse Gases
Thermokarst Lake
11. Is best viewed as a combination of...- Natural Variability - Associated with atmospheric circulation patterns - Growing Radiative Forcing - Associated with rising concentrations of atmospheric greenhouse gases - Strongly suggests a human influence.
Thermokarst
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Melt
Ice loss
12. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
What happens with the Ozone Hole
Precipitation and High Latitudes
Mass Balance
Ocean-Ice-Atmosphere Interaction
13. O Climate change in the Arctic is occurring now - Changes have been huge already
In the Arctic where the air is cooler
Today melting ice
Thermohaline Circulatoin
Grounding Lines
14. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Grounding Lines
Mass Change
Warming; cooling
Heat Source and Pressure
15. A dome shaped cover of perennial ice and snow.
Ice Cap
Sea ice melt does not change sea level
reduction in sea-ice
Deep tropics between 15O N and 15 O S are quite
16. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Open talik
Thermokarst
Severe coastal erosion
Warming; cooling
17. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Antarctica
Methane
Where rise in OC is greatest
Inversion Layer Winter
18. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Absolute thresholds
Ice-Albedo
Reduction in sea-ice extent
75-OC
19. Refers to the irregular warming in the Sea Surface Temperatures (SST) from the coasts of Peru and Ecuador to the equatorial central Pacific - the Southern Oscillation
Sea Ice
50%
El Nino
Frozen Soil
20. Surface Mass Balance is of the order of _____ melting is ____ times more.
70%
30%
1 m/yr; 10x
Why Water Vapor is not a climate forcing
21. Arctic troposphere is thinner (8-10 km) than the tropics...The depth of the atmospheric layer is much shallower in the Arctic - It takes less energy to warm the Arctic rather than the Tropics - Same as heating an apartment vs. a house
Carbon Dioxide
Why Water Vapor is not a climate forcing
summer
Thinner atmosphere
22. Summer increase in cloud cover - Winter decrease in cloud cover.
23. In ________- inversion layer is more common in the Arctic
Heat Source and Pressure
Monthly maximums and minimums
Longwave Radiation
winter
24. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Black Carbon
Ocean water
Thermohaline Circulation
Albedos of Snow and Ice
25. Where does the ozone protect us?
Snow and snow covered ice absorb
In the stratosphere.
Radiative Forcing
Agricultural Drought
26. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Stronger
How talik forms under lakes
Sea Ice
Why Water Vapor is not a climate forcing
27. What can cause a change in the Earth's climate balance?
Cloud Feedbacks
Carbon Dioxide
Thermokarst Lake
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
28. 240 w/m squared
Warming; cooling
Change in vegetation generates a further feedback
Amount of light actually reaching the Earth
Wetter; drier
29. Forms in a mosaic of favoured locations.
Discontinuous Permafrosrt
Climate Change in the Arctic
Amount of light actually reaching the Earth
Change in vegetation generates a further feedback
30. Climate models suggest once the sea ice cover is thinned sufficiently - a strong kick from natural variability could initiate a rapid slide towards ice-free conditions in the summer.
Heat Source and Pressure
Permafrost Degradation
Changes in Arctic sea-ice Extent
Very small portion
31. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Methane
Antarctica
Radiative Flux
Effect of Deforestation on CO-2
32. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Ice Motion
Atlantic Thermohaline Circulation
Depth v Surface
Monthly maximums and minimums
33. The buoyant force is equal to the weight of the displaced water.
34. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Ice shelf
Affect Floods and Droughts
Mass Balance
Hydrological Drought
35. Greenhouse gases are mixed in the ____
Rainy
In the Arctic where the air is cooler
Permafrost
Troposphere
36. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Cause of break of inversion layers or decrease in frequency
What happens with the Ozone Hole
Thermokarst Lake
Global warming and hot nights?
37. A mass of land ice - continental or sub-continental in extent - and thick enough to cover most of the underlying bedrock topography - If you have a warm ocean - it will melt the ice sheet. Its shape is mainly determined by the dynamics of its outward
30%
Through talik
Global warming and hot nights?
Ice Sheets
38. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
Positive feedbacks both found in...
Hydrological Drought
Ice Shelf
doubles
39. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Albedo
Ice in the Arctic
Grounding Lines
Very small portion
40. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
El Nio is in the coasts of...
7%
Stratospheric Ozone Depletion
Albedo
41. Cooler water and drought conditions.
Greenhouse Gases
In the stratosphere.
La Nia
Affect Floods and Droughts
42. Is not an externally imposed perturbation to the climate system.
Meteorological Drought
Why Water Vapor is not a climate forcing
Permafrost Degradation
Is precipitation around the world increasing?
43. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Heat wave
Atmospheric Composition?
Average radiative flux reaching the atmosphere
Ocean water
44. Reduction of Summer Sea- will increase the warming because less energy will be reflected back to the atmosphere by the ice and more will be absorbed by the ocean - Snow and snow covered ice absorb 15% of incident solar energy - Ice absorbs 10% of inc
Types of Albedo
Why Water Vapor is not a climate forcing
Some parts of the planet are dry because of their location
Reduction in sea-ice extent
45. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Thermohaline Circulation
Some regions of the Earth have warmed faster than other regions.
Agricultural Drought
How a closed talik forms
46. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Negative
Methane
Severe coastal erosion
Contributions to CO2 from different activities
47. The past climate...for this reason - both keep good records of climate change.
Melt
Warm
Cloud Feedbacks
Thickness of the active layer and the permafrost depend on this
48. Industrial product - 300 ppb (parts per billion)
30%
Nitrous Oxide (N2O)
Dry
Inversion Layer (feedback)
49. The major distinction between the Protocol and the Convention is that while the Convention encouraged industrialized countries to stabilize GHG emissions - the Protocol commits them to do so.
Major distinction between Kyoto Protocol and Convention
Negative
Thinner atmosphere
All Greenhouse gases
50. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Meteorological Drought
Radiative Forcing
% of Greenhouse Gases
Types of Albedo