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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. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
El Nio is in the coasts of...
Severe coastal erosion
Atmospheric Composition
The Ozone Hole
2. Over the past century what has happened to the Earth's temperature?
What happens with the Ozone Hole
Black Carbon
Change in vegetation generates a further feedback
Some regions of the Earth have warmed faster than other regions.
3. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Positive
Thermohaline Circulation
Thermokarst
Albedo
4. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Atmospheric Structure
How a closed talik forms
Time Variable Gravity
Ice in the Arctic
5. Clouds 40~90% - Vegetation 10~15%
Precipitation and High Latitudes
Types of Albedo
Grounding Lines
Ocean water
6. he increase of ozone concentration in the atmosphere helps ____ our planet
Stratospheric Ozone Depletion
Warm
Permafrost
Sea ice melt does not change sea level
7. 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
Thermokarst
Through talik
Dry
How talik forms under lakes
8. 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
Why Water Vapor is not a climate forcing
Thermohaline Circulation
In the troposphere that we live in.
Ice loss
9. 85%
More rain means no drought
Sea-Ice Albedo
Heat wave
Antarctica
10. ~10% of incident solar energy (albedo 90)
Sea Ice Extent is Changing in Antarctica as well
Sea Ice
Ice absorbs
Warming; cooling
11. Where do greenhouse gases warm up the Earth?
In the troposphere that we live in.
Discontinuous
30%
Today melting ice
12. 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
How talik forms under lakes
Reduction in sea-ice extent
Wetter; drier
13. Descending Air dry - Convection cells are wet.
The Ozone Hole
Methane
Why the Arctic climate is special
Atmospheric Circulation
14. 1.4 USA - 57 m total sea level equivalent
Black Carbon
Heat wave
Antarctica
Today melting ice
15. 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
Through talik
Reduction in sea-ice extent
45%
Thermokarst Lake
16. O Climate change in the Arctic is occurring now - Changes have been huge already
Ozone Hole
Change in vegetation generates a further feedback
Thermohaline Circulatoin
Today melting ice
17. Greenhouse gases are mixed in the ____
Sea-Ice Albedo
Monthly maximums and minimums
Troposphere
Thickness of the active layer and the permafrost depend on this
18. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Why the Arctic climate is special
Ozone Hole
Precipitation and High Latitudes
Severe coastal erosion
19. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Sea Ice
Ozone Hole
doubles
Change in vegetation generates a further feedback
20. In ________- inversion layer is more common in the Arctic
Sunspots
Calving
Sea-Ice Albedo
winter
21. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
winter
Altimetry Pros
How a closed talik forms
The cryosphere
22. Arctic warms faster than other parts of the globe in response to a given increase in greenhouse gasses - More direct route to warming - In the Arctic a greater fraction of any increase in radiation absorbed by the surface goes directly into warming t
Mass Balance
doubles
Why the Arctic climate is special
Global warming and hot nights?
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.
Effect of Deforestation on CO-2
Ocean water
Is precipitation around the world increasing?
Major distinction between Kyoto Protocol and Convention
24. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Rainy
.7O Celsius over the past century.
Surface Mass Balance
Ice/snow
25. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Monthly maximums and minimums
Severe coastal erosion
Altimetry Cons
Radiative Flux
26. 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
Thinner atmosphere
Negative
Effect of Deforestation on CO-2
Thermohaline Circulation
27. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Grounding Lines
Closed talik
Albedos of Snow and Ice
28. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Strong
Mass Balance
Talik
Ozone Hole
29. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Ice/snow
Hydrological Drought
Air pollution
Today melting ice
30. The buoyant force is equal to the weight of the displaced water.
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31. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
% of Greenhouse Gases
Thermokarst Lake
Ocean water
Atmospheric Circulation
32. CO2 GHG forcing - H2O - dominant/major GHG
Reduction in sea-ice extent
Infrared radiation
GHG
Ice Shelf
33. 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:
Methane
Thermohaline Circulation
Indirect heat wave effect
Threshold departures
34. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Sea Ice
summer
Negative
How the cryosphere is affected by climate change
35. Surface Mass Balance is of the order of _____ melting is ____ times more.
Altimetry Pros
1 m/yr; 10x
30%
Mass Balance
36. High vs low
Cloud Feedbacks
Talik
Time Variable Gravity
How a closed talik forms
37. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Heat Source and Pressure
Rainy
Hydrological Drought
In the troposphere that we live in.
38. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
summer
Nitrous Oxide (N2O)
Negative Ice-Albedo Feedback
39. x7 smaller - 7m total sea level equivalent.
Altimetry
Inversion Layer Winter
Thermokarst
Greenland
40. Where does the ozone protect us?
1 m/yr; 10x
In the stratosphere.
Permafrost Degradation
Sunspots
41. Grounding line is the last portion of a glacier grounded to bedrock - after this line there are ice shelves - Glaciers contribute to sea level rise after passing the grounding line - Maximum thinning at grounding line.
Surface Mass Balance
Absolute thresholds
Ice Shelf
Troposphere
42. 10 : 1 - grounding ; surface
Grounding v Surface Melting
The Ozone Hole
Sea Ice
Negative Ice-Albedo Feedback
43. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ozone
Inversion Layer Summer
Grounding v Surface Melting
Reduction in sea-ice extent
44. Warming- positive feedback - Cooling- negative feedback.
Altimetry (height)
Increases - decreases
GHG
Ice-Albedo
45. Really measures volume.
Thermohaline Circulation Effect
Altimetry
Greenhouse Gases
Nitrous Oxide (N2O)
46. Summer increase in cloud cover - Winter decrease in cloud cover.
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47. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
GHG
Active Layer
Thermohaline Circulatoin
Talik
48. 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.
Thermohaline Circulatoin
Rainy
Depth v Surface
Infrared radiation
49. Forms in a mosaic of favoured locations.
Warming; cooling
Arctic Atmosphere
US and precipitation
Discontinuous Permafrosrt
50. A naturally or artificially caused decrease in the thickness and/or areal extent of permafrost - It is caused by the deepening fo the active layer and the thawing of the adjacent permafrost.
El Nio is in the coasts of...
Heat Source and Pressure
Permafrost Degradation
Thickness of the active layer and the permafrost depend on this