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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. 10 : 1 - grounding ; surface
Grounding v Surface Melting
In the stratosphere.
What happens with the Ozone Hole
Air pollution
2. LW - SW - 55% absorbed by surface
Thermohaline Circulatoin
Methane
winter
Energy Budget
3. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Sea-Ice Albedo
Thermokarst Lake
Mass Balance
Layers of Earth
4. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Meteorological Drought
Sea Ice Extent is Changing in Antarctica as well
% of Greenhouse Gases
Active Layer
5. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Negative Ice-Albedo Feedback
Albedos of Snow and Ice
Ice Motion
75-OC
6. 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
Radiative Flux
Reduction in sea-ice extent
Thermokarst
50%
7. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Permafrost
Sea-Ice Albedo
Open talik
Why ice-albedo feedback is a big deal in the Arctic
8. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Global warming and hot nights?
Dry
Active Layer
1 m/yr; 10x
9. 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
Atlantic Thermohaline Circulation
In the stratosphere.
Melt
Some regions of the Earth have warmed faster than other regions.
10. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
GHG
Calving
Heat wave
Average radiative flux reaching the atmosphere
11. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Inversion Layer Summer
Accumulation
Inversion Layer Winter
Ice Sheets
12. Soil at or below the freezing point of water for two or more years - Can be: Terrestrial - Subsea - Can be: Continuous: exists across a landscape as an unbroken layer. More than 90% is frozen - Discontinuous
Permafrost
1 m/yr; 10x
Thermokarst Lake
Permafrost Degradation
13. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
doubles
Monthly maximums and minimums
Atmospheric Composition?
Ozone Hole
14. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
What effects the density
Grounding Lines
Depth v Surface
Radiative Forcing
15. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Some parts of the planet are dry because of their location
Natural Causes of Warming
Change in vegetation generates a further feedback
How a closed talik forms
16. Forms in a mosaic of favoured locations.
Closed talik
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Discontinuous Permafrosrt
Stronger
17. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
What happens with the Ozone Hole
Thermokarst
Deep tropics between 15O N and 15 O S are quite
Positive feedbacks both found in...
18. Melting Point decreases
.75OC/km-1
Ocean water
Inversion Layer Summer
Greenhouse Gases
19. Longwave radiation - any radiation with a long wave will heat up quickly.
Global warming and hot nights?
Deep tropics between 15O N and 15 O S are quite
Infrared radiation
Inversion Layer Summer
20. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
The cryosphere
Why Water Vapor is not a climate forcing
Percentile departures
Active Layer
21. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Sunspots
How we measure Mass Balance
Ice Cap
Atmospheric Composition
22. High vs low
Black Carbon
Effect of Deforestation on CO-2
Troposphere
Cloud Feedbacks
23. The Earth emits this.
Severe coastal erosion
Longwave Radiation
Grounding v Surface Melting
Methane
24. Total absorbed solar radiation
70%
45%
All Greenhouse gases
Depth v Surface
25. 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.
Changes in Arctic sea-ice Extent
Ice Shelf
Positive feedbacks both found in...
Very small portion
26. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Dynamic thinning
reduction in sea-ice
Mass Change
Ice Discharge
27. 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
Active Layer
Thermohaline Circulatoin
Dry
Change in vegetation generates a further feedback
28. Greenhouse gases are a ___ portion of the atmosphere
Rainy
Depth v Surface
Very small portion
Grounding v Surface Melting
29. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Shortwave Length
Strong
Positive
Thermokarst
30. In _______ - the inversions are less frequent and weaker in the Arctic.
How to define a heatwave
summer
doubles
Grounding Lines
31. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
The Ozone Hole
Ice in the Arctic
Permafrost
Rainy
32. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Agricultural Drought
summer
Global warming and hot nights?
33. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
air can warm dramatically
Affect Floods and Droughts
Changes in Arctic sea-ice Extent
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
34. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Active Layer
Nitrous Oxide (N2O)
Dynamic thinning
Climate Change in the Arctic
35. Carbon dioxide - Methane - Ozone - Water Vapor - Few others - Most ___________________ are mixed in the troposphere (Except water vapor) - Water vapor is concentrated closer to the ground.
Ozone Hole
70%
Greenhouse Gases
El Nino
36. x7 smaller - 7m total sea level equivalent.
Normal condition for air
Greenland
Warming; cooling
Global warming and hot nights?
37. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Percentile departures
Global warming and hot nights?
.75OC/km-1
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
38. 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
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Atmospheric Circulation
Reduction in sea-ice extent
Altimetry Cons
39. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Ice Cap
Ice Motion
Ozone
Through talik
40. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
Methane
Thermohaline Circulatoin
Ocean water
41. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Antarctica
Layers of Earth
Thermokarst
Ice loss
42. Amount of light absorbed by atmosphere
20%
Dry
Antarctica
.75OC/km-1
43. 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%
How we measure Mass Balance
30%
Albedos of Snow and Ice
75-OC
44. How often does El Nio occur?
Altimetry Pros
In the Arctic where the air is cooler
Once every 4 years.
Ice Cap
45. They saw a massive thinning of the ice where it enters into the ocean - This is due to the pronounced melting of the ice once it is in contact with the ocean. Melt rates of 25 m/year near the grounding lines and more than 10 m/year on average.
20%
Sea Ice
Ice-Ocean Interactions
Surface Mass Balance
46. Frozen +2 years - Few centimeters to 1500 m
.7O Celsius over the past century.
Grounding Lines
Permafrost
How we measure Mass Balance
47. Greenhouse gases are mixed in the ____
Meteorological Drought
Average radiative flux reaching the atmosphere
Warming; cooling
Troposphere
48. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
La Nia
reduction in sea-ice
Thermokarst
Sublimation
49. Like weighing oneself on the scale.
Time Variable Gravity
Open talik
Inversion Layer Winter
Increases - decreases
50. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
7%
Reduction in sea-ice extent
Altimetry Cons
Sea Ice Extent is Changing in Antarctica as well