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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. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
How a closed talik forms
Climate Change in the Arctic
Surface Mass Balance
Altimetry
2. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Average radiative flux reaching the atmosphere
Grounding Lines
Ice shelf
Threshold departures
3. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Inversion Layer Summer
Ice loss
Open talik
Closed talik
4. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
summer
Stratospheric Ozone Depletion
Reduction in sea-ice extent
Ozone
5. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Precipitation and High Latitudes
Active Layer
doubles
Shortwave Length
6. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Greenhouse Gases
Ocean water
Discontinuous Permafrosrt
Albedo
7. Warming- positive feedback - Cooling- negative feedback.
Stronger
Very small portion
Discontinuous Permafrosrt
Ice-Albedo
8. 10 : 1 - grounding ; surface
Ice Motion
Surface Mass Balance
Grounding v Surface Melting
Cause of break of inversion layers or decrease in frequency
9. Cooler water and drought conditions.
7%
La Nia
How to define a heatwave
Precipitation and High Latitudes
10. LW - SW - 55% absorbed by surface
Greenland
Atmospheric Circulation
Energy Budget
Rainy
11. Reduction of snow and ice cover - Changes in atmospheric circulation.
Affect Floods and Droughts
Sublimation
Ice Shelf
Cause of break of inversion layers or decrease in frequency
12. The Earth emits this.
7%
Longwave Radiation
Thermohaline Circulatoin
Nitrous Oxide (N2O)
13. Set up in 1988 by WMO and UNEP.
Today melting ice
Indirect heat wave effect
IPCC
Layers of Earth
14. 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%
Negative
Energy Budget
Albedos of Snow and Ice
Cause of break of inversion layers or decrease in frequency
15. 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
Open talik
Mass Change
Ice Cap
Altimetry Cons
16. Frozen +2 years - Few centimeters to 1500 m
Time Variable Gravity
Dry
Why the Arctic climate is special
Permafrost
17. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Warming; cooling
Percentile departures
Sea Ice Extent is Changing in Antarctica as well
45%
18. 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.
Permafrost Degradation
Thermokarst
In the Arctic where the air is cooler
Normal condition for air
19. ~10% of incident solar energy (albedo 90)
Some parts of the planet are dry because of their location
Ice absorbs
All Greenhouse gases
Arctic Atmosphere
20. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
Altimetry
Monthly maximums and minimums
20%
21. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Affect Floods and Droughts
Why ice-albedo feedback is a big deal in the Arctic
Sublimation
Sunspots
22. High cloud has a _____ effect and cool cloud has a ____ effect
Warming; cooling
Stratospheric Ozone Depletion
Closed talik
30%
23. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Ocean-Ice-Atmosphere Interaction
Snow and snow covered ice absorb
Arctic Atmosphere
Ice absorbs
24. 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.
Changes in Arctic sea-ice Extent
Ice loss
Earth's tilt
Percentile departures
25. A dome shaped cover of perennial ice and snow.
Changes in Arctic sea-ice Extent
70%
Ice Cap
Wetter; drier
26. Greenhouse gases are mixed in the ____
Troposphere
Surface Mass Balance
Ocean-Ice-Atmosphere Interaction
winter
27. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Permafrost Degradation
The cryosphere
Effect of Deforestation on CO-2
La Nia
28. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
Snow and snow covered ice absorb
Importance of ice sheets
Ocean water
29. Permafrost- A frozen soil
Negative
Frozen Soil
Ice Sheets
Time Variable Gravity
30. Total absorbed solar radiation
Ice Sheets
Indirect heat wave effect
70%
Negative
31. In average: +1% in respect to 100 years ago.
Rainy
Types of Albedo
Is precipitation around the world increasing?
Thermohaline Circulation
32. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Ice Sheets
Heat wave
Average radiative flux reaching the atmosphere
The Ozone Hole
33. Clouds 40~90% - Vegetation 10~15%
Types of Albedo
70%
Inversion Layer Winter
Closed talik
34. 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
Altimetry Cons
Dynamic thinning
The Ozone Hole
35. 240 w/m squared
Heat wave
.7O Celsius over the past century.
Amount of light actually reaching the Earth
Major distinction between Kyoto Protocol and Convention
36. Less frequent and weaker
More rain means no drought
Radiative Flux
Inversion Layer Summer
Depth v Surface
37. CO2 GHG forcing - H2O - dominant/major GHG
Major distinction between Kyoto Protocol and Convention
Average radiative flux reaching the atmosphere
GHG
Is precipitation around the world increasing?
38. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Rainy
Ocean water
Average radiative flux reaching the atmosphere
Carbon Dioxide
39. Laser radar - H V - Long time series - high accuracy - Density
Change in vegetation generates a further feedback
Surface Mass Balance
Altimetry (height)
Ocean water
40. Rainy on yearly average. In these regions - rising air predominates.
Deep tropics between 15O N and 15 O S are quite
Ozone Hole
More rain means no drought
In the troposphere that we live in.
41. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Warm
Reduction in sea-ice extent
Energy Budget
Air pollution
42. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Normal condition for air
Inversion Layer Winter
Positive feedbacks both found in...
Mass Change
43. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Open talik
Grounding Lines
Ice-Ocean Interactions
Wetter; drier
44. Amount of light absorbed by surface
Normal condition for air
50%
Shortwave Length
Cloud Feedbacks
45. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Permafrost
Ice/snow
Layers of Earth
Grounding Lines
46. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Inversion Layer Winter
Sea ice melt does not change sea level
IPCC
El Nino
47. 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.
Ice Sheets
Ozone Hole
Heat Source and Pressure
Ice-Ocean Interactions
48. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
reduction in sea-ice
Cause of break of inversion layers or decrease in frequency
Atmospheric Structure
Ice Cap
49. How often does El Nio occur?
El Nio is in the coasts of...
Change in vegetation generates a further feedback
Once every 4 years.
Discontinuous
50. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Heat Source and Pressure
Grounding Lines
Shortwave Length