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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. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
GHG
Contributions to CO2 from different activities
1 m/yr; 10x
Sea Ice
2. Amount of light absorbed by surface
Is precipitation around the world increasing?
Wetter; drier
50%
Sea ice melt does not change sea level
3. In ________- inversion layer is more common in the Arctic
Effect of Deforestation on CO-2
winter
Cause of break of inversion layers or decrease in frequency
20%
4. 10 : 1 - grounding ; surface
Grounding v Surface Melting
reduction in sea-ice
Active Layer
Once every 4 years.
5. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Thermohaline Circulation
Arctic Atmosphere
Negative
Altimetry Pros
6. Wet gets _____ - dry gets ____ - Wet - 50ON (sub polar) Canada - N Europe - Russia - Tropical area- monsoon (rainforest) - Drier - Subtropics - Australia - S. Africa - Mediterranean - Caribbean - Mexico - SW US
Permafrost
Wetter; drier
Ice Motion
Natural Causes of Warming
7. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Earth's tilt
air can warm dramatically
Warming; cooling
8. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Thermokarst Lake
Severe coastal erosion
Monthly maximums and minimums
Antarctica
9. In average: +1% in respect to 100 years ago.
Dry
Cloud Feedbacks
In the stratosphere.
Is precipitation around the world increasing?
10. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Thermokarst Lake
air can warm dramatically
Mass Budget
Altimetry Cons
11. 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
Antarctica
All Greenhouse gases
Reduction in sea-ice extent
Radiative Forcing
12. 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.
Change in vegetation generates a further feedback
How to define a heatwave
Ice-Ocean Interactions
El Nino
13. Cooler water and drought conditions.
Inversion Layer Winter
La Nia
More rain means no drought
Grounding v Surface Melting
14. CO2 - CH4 - O3 - H2O - N2O - CFCs
Sublimation
% of Greenhouse Gases
All Greenhouse gases
Questions to think about
15. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Nitrous Oxide (N2O)
Thickness of the active layer and the permafrost depend on this
Altimetry (height)
16. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Closed talik
Accumulation
Why Water Vapor is not a climate forcing
Some regions of the Earth have warmed faster than other regions.
17. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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18. Summer increase in cloud cover - Winter decrease in cloud cover.
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19. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
How we measure Mass Balance
La Nia
Atmospheric Composition?
All Greenhouse gases
20. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Antarctica
Why ice-albedo feedback is a big deal in the Arctic
Ice in the Arctic
Warm
21. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
How to define a heatwave
Inversion Layer Winter
Ozone
Ice absorbs
22. x7 smaller - 7m total sea level equivalent.
Accumulation
Surface Mass Balance
Ozone
Greenland
23. 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.
Radiative Forcing
Ice Shelf
Thermohaline Circulation Effect
summer
24. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Atmospheric Composition
air can warm dramatically
Grounding Lines
Precipitation and High Latitudes
25. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Greenhouse Gases
Snow and snow covered ice absorb
Thermokarst Lake
.75OC/km-1
26. Ocean retains ____ CO2
25%
Questions to think about
Thermohaline Circulation Effect
El Nio is in the coasts of...
27. 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
Affect Floods and Droughts
La Nia
Ice Sheets
28. 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.
Sea-Ice Albedo
Ocean water
25%
Inversion Layer (feedback)
29. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
.7O Celsius over the past century.
doubles
Agricultural Drought
Thermokarst
30. High vs low
Archimedes' Principle
Inversion Layer Summer
Cloud Feedbacks
Dry
31. Melting Point decreases
Severe coastal erosion
What happens with the Ozone Hole
.75OC/km-1
Heat Source and Pressure
32. A mass of land ice - continental or sub-continental in extent - and thick enough to cover most of the underlying bedrock topography - If you have a warm ocean - it will melt the ice sheet. Its shape is mainly determined by the dynamics of its outward
25%
Thermokarst
Carbon Dioxide
Ice Sheets
33. Forms in a mosaic of favoured locations.
Ice Shelf
Discontinuous Permafrosrt
Altimetry Pros
Changes in Arctic sea-ice Extent
34. A thick - floating slab of freshwater ice extending from coast to coast.
Reduction in sea-ice extent
Ice shelf
Cloud Feedbacks
La Nia
35. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Mass Balance
Archimedes' Principle
Layers of Earth
75-OC
36. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Surface Mass Balance
Depth v Surface
Types of Albedo
Dynamic thinning
37. 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:
Troposphere
Altimetry Cons
Thermohaline Circulation
70%
38. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Discontinuous
Stratospheric Ozone Depletion
Ozone Hole
Agricultural Drought
39. O Unfrozen soil that stays within the permafrost.
How talik forms under lakes
Talik
doubles
20%
40. 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.
Ice loss
What effects the density
Climate Change in the Arctic
Sea-Ice Albedo
41. Over the past century what has happened to the Earth's temperature?
Agricultural Drought
Some regions of the Earth have warmed faster than other regions.
Ice Cap
Ocean water
42. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Ice shelf
Heat Source and Pressure
Ocean water
Layers of Earth
43. The order of 1 m/year. Melting is ten times more.
Increases - decreases
Mass Change
Surface Mass Balance
How we measure Mass Balance
44. Like weighing oneself on the scale.
Some parts of the planet are dry because of their location
Positive
Calving
Time Variable Gravity
45. Really measures volume.
Altimetry
Importance of ice sheets
Precipitation and High Latitudes
Questions to think about
46. Water vapor means more water up in the clouds and less in the ground!
Thermohaline Circulation
Ice Sheets
Rainy
More rain means no drought
47. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Absolute thresholds
Ice/snow
Thermokarst
Sea ice melt does not change sea level
48. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Dynamic thinning
Stratospheric Ozone Depletion
Open talik
Earth's tilt
49. Radiation absorbed by atmospheric greenhouse gases?
Stronger
Meteorological Drought
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
winter
50. Industrial product - 300 ppb (parts per billion)
Warming; cooling
Sea Ice
Nitrous Oxide (N2O)
In the Arctic where the air is cooler