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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. Total absorbed solar radiation
Negative Ice-Albedo Feedback
Talik
70%
Contributions to CO2 from different activities
2. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Discontinuous
How the cryosphere is affected by climate change
Ice-Ocean Interactions
Infrared radiation
3. Greenhouse gases are mixed in the ____
Cause of break of inversion layers or decrease in frequency
Altimetry Cons
Inversion Layer Winter
Troposphere
4. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Air pollution
Active Layer
Natural Causes of Warming
El Nino
5. Forms in a mosaic of favoured locations.
Altimetry Cons
Archimedes' Principle
Discontinuous Permafrosrt
El Nino
6. ~10% of incident solar energy (albedo 90)
doubles
Ice absorbs
Black Carbon
Is precipitation around the world increasing?
7. Over the Northern Hemisphere than the tropics.
Infrared radiation
7%
30%
Where rise in OC is greatest
8. Surface Mass Balance is of the order of _____ melting is ____ times more.
Ice Motion
Climate Change in the Arctic
Permafrost
1 m/yr; 10x
9. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
How talik forms under lakes
Average radiative flux reaching the atmosphere
winter
Layers of Earth
10. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Altimetry Cons
El Nio is in the coasts of...
Atmospheric Composition?
Radiative Forcing
11. South polar vortex - Temperatures drop below 80O Celsius in the lower stratosphere - At these temperatures the chemicals in the stratosphere freeze and form Polar Stratospheric Clouds (PSCS) - These increase the concentration of CFCs in turn destroyi
Ice Motion
The cryosphere
What happens with the Ozone Hole
Radiative Flux
12. 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.
Thinner atmosphere
50%
Altimetry Cons
What effects the density
13. More common
Inversion Layer Winter
Active Layer
Increases - decreases
Snow and snow covered ice absorb
14. Number of days when temperatures climb above average by a fixed amount.
Absolute thresholds
Heat wave
Active Layer
Threshold departures
15. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Thermokarst
Depth v Surface
La Nia
16. 85%
Ice-Ocean Interactions
Altimetry Pros
Sea-Ice Albedo
Energy Budget
17. The past climate...for this reason - both keep good records of climate change.
Normal condition for air
La Nia
Thickness of the active layer and the permafrost depend on this
Ice Discharge
18. The order of 1 m/year. Melting is ten times more.
Surface Mass Balance
Precipitation and High Latitudes
Change in vegetation generates a further feedback
Agricultural Drought
19. The air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
In the Arctic where the air is cooler
The cryosphere
Longwave Radiation
Thinner atmosphere
20. Descending Air dry - Convection cells are wet.
Greenhouse Gases
Where rise in OC is greatest
Permafrost
Atmospheric Circulation
21. Less frequent and weaker
La Nia
Altimetry (height)
Radiative Forcing
Inversion Layer Summer
22. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice Motion
Warm
Snow and snow covered ice absorb
23. ~15% of incident solar energy (albedo 85)
More rain means no drought
Contributions to CO2 from different activities
Snow and snow covered ice absorb
Accumulation
24. Warming- positive feedback - Cooling- negative feedback.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
20%
1 m/yr; 10x
Ice-Albedo
25. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Ice absorbs
30%
Calving
In the stratosphere.
26. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Discontinuous
Sea Ice Extent is Changing in Antarctica as well
Calving
Major distinction between Kyoto Protocol and Convention
27. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Ozone Hole
Questions to think about
Monthly maximums and minimums
Energy Budget
28. Greenhouse gases are a ___ portion of the atmosphere
Layers of Earth
Very small portion
Major distinction between Kyoto Protocol and Convention
How a closed talik forms
29. 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
Ozone
.75OC/km-1
Hydrological Drought
Why ice-albedo feedback is a big deal in the Arctic
30. Antarctica - stratosphere - Sep-Oct
Through talik
Ozone Hole
Carbon Dioxide
Ocean water
31. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Major distinction between Kyoto Protocol and Convention
Where rise in OC is greatest
Layers of Earth
Thinner atmosphere
32. Rainy on yearly average. In these regions - rising air predominates.
Once every 4 years.
doubles
Major distinction between Kyoto Protocol and Convention
Deep tropics between 15O N and 15 O S are quite
33. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
.7O Celsius over the past century.
Arctic Atmosphere
Ice Discharge
Percentile departures
34. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Negative
Why ice-albedo feedback is a big deal in the Arctic
Thermokarst Lake
35. 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
Grounding Lines
Talik
Radiative Flux
Sublimation
36. A dome shaped cover of perennial ice and snow.
.75OC/km-1
How a closed talik forms
Warm
Ice Cap
37. 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.
Stronger
Permafrost Degradation
Arctic Atmosphere
La Nia
38. 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.
Discontinuous
Major distinction between Kyoto Protocol and Convention
Meteorological Drought
Thermokarst
39. Where do greenhouse gases warm up the Earth?
The cryosphere
In the troposphere that we live in.
Meteorological Drought
Altimetry Pros
40. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Altimetry
Thermokarst Lake
Surface Mass Balance
Atmospheric Composition
41. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
The Ozone Hole
Ice Motion
Ocean water
Heat wave
42. The buoyant force is equal to the weight of the displaced water.
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43. Precipitation intensity will rise ___ for every 1 OC of warming.
Thermohaline Circulation Effect
Carbon Dioxide
Thermohaline Circulation
7%
44. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
How we measure Mass Balance
Radiative Forcing
How talik forms under lakes
In the troposphere that we live in.
45. 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
Once every 4 years.
Dry
Natural Causes of Warming
46. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Layers of Earth
Arctic Atmosphere
Thermokarst
US and precipitation
47. Over the past century what has happened to the Earth's temperature?
Some regions of the Earth have warmed faster than other regions.
45%
How we measure Mass Balance
Importance of ice sheets
48. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
Arctic Atmosphere
Average radiative flux reaching the atmosphere
Types of Albedo
49. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
US and precipitation
Layers of Earth
How a closed talik forms
Thickness of the active layer and the permafrost depend on this
50. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Depth v Surface
Ice Sheets
The Ozone Hole
How a closed talik forms