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Test your basic knowledge |
Global Warming
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Subjects
:
literacy
,
science
Instructions:
Answer 50 questions in 15 minutes.
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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. Heat is provided by outside sources that flow down the continental slope to reach the deepest part of the glacier. High pressure decreases the melting point and favors melting.
La Nia
Thermohaline Circulatoin
Dynamic thinning
Active Layer
2. 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.
Thinner atmosphere
Thermohaline Circulation Effect
Mass Budget
Ice loss
3. Taliks are found under lakes because of the ability of water to store and vertically transfer heat energy - Vertical extent of the taliks found under lakes is related to the depth and volume of the overlying water body.
Talik
Ice Sheets
How talik forms under lakes
Types of Albedo
4. Is not an externally imposed perturbation to the climate system.
GHG
Active Layer
Discontinuous Permafrosrt
Why Water Vapor is not a climate forcing
5. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
In the troposphere that we live in.
Sublimation
doubles
Melt
6. Really measures volume.
Altimetry
reduction in sea-ice
Change in vegetation generates a further feedback
Hydrological Drought
7. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Is precipitation around the world increasing?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Sea ice melt does not change sea level
Mass Change
8. Fresh snow and snow-covered sea ice may have an albedo higher than 80% - even when melting in the summer. Sea ice has a higher albedo and can absorb as little as 10% of the solar energy. On average - sea ice albedo is around 85%
Ice Discharge
Positive feedbacks both found in...
In the troposphere that we live in.
Albedos of Snow and Ice
9. O The amount of energy moving in the form of photons or other elementary particles at a certain distance from the source per unit of area per second. Area/second
Mass Budget
Sea Ice
Thermohaline Circulatoin
Radiative Flux
10. Some parts of the planet are dry because of their location: most of the deserts are around 30 N and 30 S - where sinking air predominates
How the cryosphere is affected by climate change
Dry
Surface Mass Balance
Why the Arctic climate is special
11. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Atmospheric Composition?
Ozone Hole
.75OC/km-1
Greenhouse Gases
12. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
45%
Heat wave
Natural Causes of Warming
13. Number of days that exceed a given temperature
Absolute thresholds
Hydrological Drought
Ice Cap
Ice absorbs
14. The buoyant force is equal to the weight of the displaced water.
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15. Melting Point decreases
Radiative Forcing
.75OC/km-1
Surface Mass Balance
How the cryosphere is affected by climate change
16. CO2 - CH4 - O3 - H2O - N2O - CFCs
All Greenhouse gases
What effects the density
Surface Mass Balance
Antarctica
17. 85%
Sea-Ice Albedo
Ice Discharge
Permafrost Degradation
Thermohaline Circulation
18. Ocean retains ____ CO2
Ice shelf
25%
Depth v Surface
Sea Ice
19. Rainy on yearly average. In these regions - rising air predominates.
Threshold departures
Deep tropics between 15O N and 15 O S are quite
Hydrological Drought
.7O Celsius over the past century.
20. Measures input and output.
Grounding v Surface Melting
Ice Sheets
Mass Budget
Heat wave
21. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
Antarctica
air can warm dramatically
Atmospheric Circulation
22. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Percentile departures
.7O Celsius over the past century.
Atmospheric Composition
Dynamic thinning
23. 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
Ocean water
Thickness of the active layer and the permafrost depend on this
Some regions of the Earth have warmed faster than other regions.
24. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
More rain means no drought
La Nia
Global warming and hot nights?
Positive feedbacks both found in...
25. Reduction of snow and ice cover - Changes in atmospheric circulation.
Some regions of the Earth have warmed faster than other regions.
Cause of break of inversion layers or decrease in frequency
Albedos of Snow and Ice
Hydrological Drought
26. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Threshold departures
Change in vegetation generates a further feedback
Indirect heat wave effect
How a closed talik forms
27. x7 smaller - 7m total sea level equivalent.
What effects the density
Greenland
.75OC/km-1
45%
28. 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
Thermohaline Circulation Effect
doubles
45%
Longwave Radiation
29. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
The Ozone Hole
Indirect heat wave effect
Inversion Layer (feedback)
Greenhouse Gases
30. Greenhouse gases are a ___ portion of the atmosphere
Very small portion
Amount of light actually reaching the Earth
Longwave Radiation
Thermokarst
31. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Black Carbon
GHG
50%
32. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
summer
Time Variable Gravity
Stronger
Ocean-Ice-Atmosphere Interaction
33. Grace - Tells us how much mass change we have - M - This is the measure of gravity (gives us the mass) - Directly measure mass change - Poor resolution
Discontinuous Permafrosrt
Mass Change
Thermokarst Lake
El Nio is in the coasts of...
34. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Where rise in OC is greatest
Active Layer
Severe coastal erosion
30%
35. Amount of light absorbed by atmosphere
20%
Ice Sheets
How a closed talik forms
Thermohaline Circulation
36. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
Closed talik
Altimetry Pros
Increases - decreases
Deep tropics between 15O N and 15 O S are quite
37. Surface Mass Balance is of the order of _____ melting is ____ times more.
IN the last 2 decades what we've seen
Ice in the Arctic
reduction in sea-ice
1 m/yr; 10x
38. Changes over time in the highest and lowest single temperature observed during a given month of the year.
% of Greenhouse Gases
Accumulation
More rain means no drought
Monthly maximums and minimums
39. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Mass Budget
Shortwave Length
Atmospheric Structure
Contributions to CO2 from different activities
40. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
.7O Celsius over the past century.
Absolute thresholds
Thermokarst Lake
75-OC
41. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Affect Floods and Droughts
Methane
Hydrological Drought
doubles
42. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
Altimetry
Snow and snow covered ice absorb
Surface Mass Balance
43. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Sublimation
Importance of ice sheets
Thermohaline Circulation
Ice Motion
44. Atmosphere retains ____ CO2
45%
Ice/snow
Ocean water
Sublimation
45. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Ozone
Greenland
How to define a heatwave
Affect Floods and Droughts
46. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
US and precipitation
Reduction in sea-ice extent
Surface Mass Balance
Altimetry Cons
47. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Where rise in OC is greatest
The Ozone Hole
Air pollution
doubles
48. 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
Effect of Deforestation on CO-2
Changes in Arctic sea-ice Extent
Air pollution
49. The high pressure decreases the melting point and favors melting - Melt water being less dense rises along the water column along the ice shelf bottom and may either escape the cavity or refreeze at some intermediate depth. Melting point decreases:
Thermohaline Circulation
Heat Source and Pressure
Layers of Earth
Thermokarst Lake
50. Wet gets _____ - dry gets ____ - Wet - 50ON (sub polar) Canada - N Europe - Russia - Tropical area- monsoon (rainforest) - Drier - Subtropics - Australia - S. Africa - Mediterranean - Caribbean - Mexico - SW US
Major distinction between Kyoto Protocol and Convention
Wetter; drier
Nitrous Oxide (N2O)
Layers of Earth
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