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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. 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.
Ice Shelf
Strong
Nitrous Oxide (N2O)
Antarctica
2. Frozen +2 years - Few centimeters to 1500 m
Ice absorbs
75-OC
Permafrost
Effect of Deforestation on CO-2
3. Melting Point decreases
Sea Ice Extent is Changing in Antarctica as well
Air pollution
Some parts of the planet are dry because of their location
.75OC/km-1
4. Cooler water and drought conditions.
Dynamic thinning
Changes in Arctic sea-ice Extent
Is precipitation around the world increasing?
La Nia
5. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Where rise in OC is greatest
Reduction in sea-ice extent
Rainy
Meteorological Drought
6. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Grounding Lines
Change in vegetation generates a further feedback
Ice Sheets
7. Total absorbed solar radiation
70%
Inversion Layer Summer
Ice-Albedo
Antarctica
8. Summer increase in cloud cover - Winter decrease in cloud cover.
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9. 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.
Thermohaline Circulation
Contributions to CO2 from different activities
Importance of ice sheets
Changes in Arctic sea-ice Extent
10. 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
Normal condition for air
Albedo
30%
11. Antarctica - stratosphere - Sep-Oct
Ozone Hole
Greenhouse Gases
Global warming and hot nights?
Meteorological Drought
12. 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.
Altimetry Cons
Methane
How talik forms under lakes
Once every 4 years.
13. Greenhouse gases are mixed in the ____
Reduction in sea-ice extent
Negative Ice-Albedo Feedback
Ozone
Troposphere
14. Permafrost- A frozen soil
Frozen Soil
Altimetry Cons
What effects the density
30%
15. 1.4 USA - 57 m total sea level equivalent
Some parts of the planet are dry because of their location
How to define a heatwave
Albedos of Snow and Ice
Antarctica
16. Where does the ozone protect us?
In the stratosphere.
Meteorological Drought
air can warm dramatically
7%
17. What can cause a change in the Earth's climate balance?
Dynamic thinning
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
reduction in sea-ice
Warm
18. O Climate change in the Arctic is occurring now - Changes have been huge already
Contributions to CO2 from different activities
Today melting ice
Shortwave Length
20%
19. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Atlantic Thermohaline Circulation
El Nio is in the coasts of...
Ice Cap
Deep tropics between 15O N and 15 O S are quite
20. Rainy on yearly average. In these regions - rising air predominates.
50%
Atmospheric Circulation
Deep tropics between 15O N and 15 O S are quite
Permafrost
21. Volcanic eruptions - Sunspots - Wobbly Earth
Through talik
Shortwave Length
Sunspots
Natural Causes of Warming
22. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Surface Mass Balance
Sea ice melt does not change sea level
All Greenhouse gases
Thermokarst Lake
23. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Sea ice melt does not change sea level
Increases - decreases
Discontinuous
Frozen Soil
24. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Hydrological Drought
Agricultural Drought
Atlantic Thermohaline Circulation
Grounding Lines
25. 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.
Ice loss
Nitrous Oxide (N2O)
Stronger
Atmospheric Composition
26. Warming- positive feedback - Cooling- negative feedback.
Very small portion
Accumulation
All Greenhouse gases
Ice-Albedo
27. Precipitation intensity will rise ___ for every 1 OC of warming.
7%
Ice in the Arctic
Ocean water
Positive
28. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
20%
Strong
Greenhouse Gases
The cryosphere
29. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Some parts of the planet are dry because of their location
Threshold departures
What effects the density
Discontinuous Permafrosrt
30. Industrial product - 300 ppb (parts per billion)
Atmospheric Circulation
How to define a heatwave
Sublimation
Nitrous Oxide (N2O)
31. ~15% of incident solar energy (albedo 85)
Ocean-Ice-Atmosphere Interaction
Some parts of the planet are dry because of their location
Snow and snow covered ice absorb
Atmospheric Structure
32. he increase of ozone concentration in the atmosphere helps ____ our planet
reduction in sea-ice
Ice in the Arctic
La Nia
Warm
33. Extent 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.
Ocean water
reduction in sea-ice
Ice-Ocean Interactions
Mass Change
34. 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.
Energy Budget
Ice-Ocean Interactions
winter
In the Arctic where the air is cooler
35. LW - SW - 55% absorbed by surface
25%
Energy Budget
Altimetry
75-OC
36. 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%
El Nino
Ice/snow
Surface Mass Balance
Albedos of Snow and Ice
37. The past climate...for this reason - both keep good records of climate change.
Talik
Meteorological Drought
Thickness of the active layer and the permafrost depend on this
winter
38. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
How a closed talik forms
Normal condition for air
Sunspots
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
39. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
Indirect heat wave effect
The Ozone Hole
Ice Shelf
Where rise in OC is greatest
40. A thick - floating slab of freshwater ice extending from coast to coast.
Threshold departures
Ice shelf
Earth's tilt
20%
41. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Altimetry (height)
Greenhouse Gases
Arctic Atmosphere
42. Holds unique and key information - Are highly interconnected - Respond and drive climate change - Are the largest freshwater reservoirs of the planet - Ice cores tell us that in climate records - nothing is regular and ice sheet plays major role.
Climate Change in the Arctic
El Nino
Thermokarst
Ice Sheets
43. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Negative Ice-Albedo Feedback
Thermohaline Circulation Effect
Active Layer
Greenhouse Gases
44. How often does El Nio occur?
Once every 4 years.
Dynamic thinning
Atmospheric Composition?
US and precipitation
45. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Ice-Ocean Interactions
Radiative Flux
Grounding Lines
How to define a heatwave
46. 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:
.7O Celsius over the past century.
Permafrost Degradation
Thermohaline Circulation Effect
Thermohaline Circulation
47. Really measures volume.
Altimetry
Thermokarst Lake
El Nio is in the coasts of...
Atmospheric Composition?
48. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Methane
Ocean water
Positive
Stratospheric Ozone Depletion
49. Like weighing oneself on the scale.
Monthly maximums and minimums
Time Variable Gravity
Average radiative flux reaching the atmosphere
Questions to think about
50. 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
Greenland
Ice Shelf
doubles