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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
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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. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Threshold departures
Thickness of the active layer and the permafrost depend on this
Melt
Ice Motion
2. Surface Mass Balance is of the order of _____ melting is ____ times more.
How talik forms under lakes
Ice shelf
1 m/yr; 10x
Albedos of Snow and Ice
3. Over the Northern Hemisphere than the tropics.
Affect Floods and Droughts
Deep tropics between 15O N and 15 O S are quite
Talik
Where rise in OC is greatest
4. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
El Nino
Grounding Lines
Methane
5. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Average radiative flux reaching the atmosphere
Sunspots
Deep tropics between 15O N and 15 O S are quite
Dry
6. Less frequent and weaker
Ocean water
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Thermohaline Circulation Effect
Inversion Layer Summer
7. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
All Greenhouse gases
Stratospheric Ozone Depletion
Precipitation and High Latitudes
Threshold departures
8. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Inversion Layer (feedback)
Stronger
Thickness of the active layer and the permafrost depend on this
Rainy
9. Reduction of snow and ice cover - Changes in atmospheric circulation.
Inversion Layer Summer
Cause of break of inversion layers or decrease in frequency
Normal condition for air
70%
10. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Sublimation
Indirect heat wave effect
Heat wave
Calving
11. What can cause a change in the Earth's climate balance?
Through talik
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ice Sheets
Once every 4 years.
12. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Ice Motion
Albedos of Snow and Ice
Positive
Albedo
13. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Global warming and hot nights?
Ice in the Arctic
Active Layer
Permafrost
14. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
summer
Ice-Ocean Interactions
How a closed talik forms
Ocean water
15. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Methane
Contributions to CO2 from different activities
Ice Discharge
Discontinuous
16. A dome shaped cover of perennial ice and snow.
Ice Cap
Is precipitation around the world increasing?
Cause of break of inversion layers or decrease in frequency
Once every 4 years.
17. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
Why the Arctic climate is special
Questions to think about
air can warm dramatically
What happens with the Ozone Hole
18. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Effect of Deforestation on CO-2
Ocean-Ice-Atmosphere Interaction
Talik
19. Trade winds blow from East to West - Pool of warm water in the west - Meanwhile deep colder water rises up in the Eastern Pacific - The sea level is ~ 50-60 cm higher in Western Pacific (Indonesia) than in the Eastern Pacific (South America/Peru) -
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Percentile departures
Normal condition for air
Ice-Ocean Interactions
20. Cooler water and drought conditions.
Normal condition for air
Black Carbon
La Nia
Thickness of the active layer and the permafrost depend on this
21. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Importance of ice sheets
Sublimation
% of Greenhouse Gases
Ice-Ocean Interactions
22. Summer increase in cloud cover - Winter decrease in cloud cover.
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23. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Talik
In the troposphere that we live in.
Layers of Earth
Ice/snow
24. Like weighing oneself on the scale.
Time Variable Gravity
Altimetry
Shortwave Length
How talik forms under lakes
25. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Thickness of the active layer and the permafrost depend on this
Carbon Dioxide
Sea ice melt does not change sea level
Negative
26. 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
Discontinuous
IN the last 2 decades what we've seen
What happens with the Ozone Hole
Active Layer
27. A thick - floating slab of freshwater ice extending from coast to coast.
Average radiative flux reaching the atmosphere
Methane
How talik forms under lakes
Ice shelf
28. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
70%
More rain means no drought
Altimetry Cons
Ice-Ocean Interactions
29. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Global warming and hot nights?
1 m/yr; 10x
Ice shelf
Permafrost Degradation
30. O Unfrozen soil that stays within the permafrost.
How a closed talik forms
Permafrost
Mass Change
Talik
31. The order of 1 m/year. Melting is ten times more.
summer
Surface Mass Balance
Indirect heat wave effect
Sea-Ice Albedo
32. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
75-OC
Ice-Ocean Interactions
Closed talik
Hydrological Drought
33. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
Ice/snow
Thermokarst
Affect Floods and Droughts
Inversion Layer (feedback)
34. Frozen +2 years - Few centimeters to 1500 m
Permafrost
winter
Agricultural Drought
Sublimation
35. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Melt
Cause of break of inversion layers or decrease in frequency
Shortwave Length
36. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Albedo
Calving
Black Carbon
Arctic Atmosphere
37. 10 : 1 - grounding ; surface
Negative
Grounding v Surface Melting
Change in vegetation generates a further feedback
Ice Discharge
38. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
Percentile departures
Permafrost
Discontinuous Permafrosrt
39. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Severe coastal erosion
GHG
Stronger
Very small portion
40. The large-scale ocean circulation that moves water between the deep and surface ocean which effects salinity and temperature change - Supplies heat to the polar-regions.
Thermohaline Circulation Effect
45%
Negative Ice-Albedo Feedback
Why the Arctic climate is special
41. Number of days when temperatures climb above average by a fixed amount.
Threshold departures
Thermokarst Lake
Albedo
Indirect heat wave effect
42. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Thermokarst Lake
7%
The cryosphere
43. LW - SW - 55% absorbed by surface
Some parts of the planet are dry because of their location
The cryosphere
Snow and snow covered ice absorb
Energy Budget
44. Amount of light absorbed by surface
Monthly maximums and minimums
50%
Ozone Hole
US and precipitation
45. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Permafrost
Monthly maximums and minimums
Reduction in sea-ice extent
Ice shelf
46. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
IPCC
Surface Mass Balance
Dry
Where rise in OC is greatest
47. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
Deep tropics between 15O N and 15 O S are quite
Altimetry Pros
Thermokarst Lake
48. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
Negative
Climate Change in the Arctic
Positive
Through talik
49. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Ice Motion
Positive feedbacks both found in...
Through talik
Longwave Radiation
50. ~15% of incident solar energy (albedo 85)
Thermokarst Lake
Snow and snow covered ice absorb
air can warm dramatically
Closed talik
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