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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. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Active Layer
Altimetry Pros
The cryosphere
2. 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
Troposphere
Ocean-Ice-Atmosphere Interaction
Heat Source and Pressure
Why ice-albedo feedback is a big deal in the Arctic
3. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Sea ice melt does not change sea level
doubles
Meteorological Drought
Grounding Lines
4. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Dry
The Ozone Hole
Frozen Soil
Methane
5. 240 w/m squared
Ice shelf
How to define a heatwave
Amount of light actually reaching the Earth
70%
6. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Dry
Archimedes' Principle
Ozone Hole
Discontinuous
7. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stronger
Methane
Closed talik
reduction in sea-ice
8. 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
Ice Shelf
Accumulation
Ice Motion
Permafrost
9. Melting Point decreases
Archimedes' Principle
Altimetry (height)
.75OC/km-1
Through talik
10. 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.
Sea ice melt does not change sea level
Dynamic thinning
Ice Shelf
Albedos of Snow and Ice
11. 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
Dynamic thinning
Heat wave
Stratospheric Ozone Depletion
12. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Increases - decreases
reduction in sea-ice
Normal condition for air
13. The Earth emits this.
Stronger
Once every 4 years.
Longwave Radiation
30%
14. Water vapor means more water up in the clouds and less in the ground!
Ocean water
Positive
More rain means no drought
Warm
15. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Types of Albedo
How to define a heatwave
All Greenhouse gases
Greenhouse Gases
16. 85%
Ice Motion
US and precipitation
Strong
Sea-Ice Albedo
17. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Negative
Sublimation
Active Layer
Time Variable Gravity
18. Forms in a mosaic of favoured locations.
75-OC
Discontinuous Permafrosrt
Archimedes' Principle
El Nio is in the coasts of...
19. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Meteorological Drought
Sea Ice
Altimetry Cons
Discontinuous Permafrosrt
20. CO2 - CH4 - O3 - H2O - N2O - CFCs
Dynamic thinning
Altimetry Cons
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
All Greenhouse gases
21. Radiation absorbed by atmospheric greenhouse gases?
45%
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Thinner atmosphere
Today melting ice
22. Over the Northern Hemisphere than the tropics.
Contributions to CO2 from different activities
Where rise in OC is greatest
Inversion Layer Summer
Ice Sheets
23. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Discontinuous
Average radiative flux reaching the atmosphere
How talik forms under lakes
1 m/yr; 10x
24. O Unfrozen soil that stays within the permafrost.
Monthly maximums and minimums
Active Layer
Talik
Mass Budget
25. High cloud has a _____ effect and cool cloud has a ____ effect
Altimetry Cons
Ice Sheets
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Warming; cooling
26. 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
Cause of break of inversion layers or decrease in frequency
GHG
Through talik
27. Unfrozen ground that is found within a mass of permafrost
Closed talik
Rainy
Thermokarst
Some parts of the planet are dry because of their location
28. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
Thermokarst
Time Variable Gravity
Ozone
29. Warming- positive feedback - Cooling- negative feedback.
Stratospheric Ozone Depletion
Albedo
Permafrost
Ice-Albedo
30. 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.
Inversion Layer Summer
Ocean-Ice-Atmosphere Interaction
Ice Sheets
Major distinction between Kyoto Protocol and Convention
31. Like weighing oneself on the scale.
Time Variable Gravity
Mass Balance
Grounding Lines
Black Carbon
32. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
25%
Dry
Grounding Lines
Reduction in sea-ice extent
33. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
IN the last 2 decades what we've seen
Atmospheric Composition?
Warming; cooling
Stronger
34. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Methane
Wetter; drier
Global warming and hot nights?
Cloud Feedbacks
35. ~15% of incident solar energy (albedo 85)
Meteorological Drought
Snow and snow covered ice absorb
Ice Sheets
Ice Cap
36. 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:
Shortwave Length
Threshold departures
Accumulation
Thermohaline Circulation
37. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
30%
Warming; cooling
Sublimation
Mass Budget
38. Measures input and output.
Mass Budget
Ice Sheets
Very small portion
Infrared radiation
39. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
1 m/yr; 10x
20%
Thermohaline Circulation Effect
75-OC
40. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
summer
Accumulation
Albedo
Melt
41. Where does the ozone protect us?
In the stratosphere.
Negative
Questions to think about
Ozone Hole
42. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
Surface Mass Balance
Mass Budget
1 m/yr; 10x
43. 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
Dynamic thinning
Radiative Flux
What effects the density
Average radiative flux reaching the atmosphere
44. Longwave radiation - any radiation with a long wave will heat up quickly.
Sea ice melt does not change sea level
Heat wave
Infrared radiation
Increases - decreases
45. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Discontinuous Permafrosrt
What happens with the Ozone Hole
Threshold departures
Heat Source and Pressure
46. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Ocean water
Open talik
% of Greenhouse Gases
Ice-Albedo
47. 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
doubles
Wetter; drier
Ice/snow
Absolute thresholds
48. Really measures volume.
Absolute thresholds
Major distinction between Kyoto Protocol and Convention
Altimetry
The cryosphere
49. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Global warming and hot nights?
Arctic Atmosphere
Changes in Arctic sea-ice Extent
Positive
50. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Natural Causes of Warming
Thermohaline Circulatoin
air can warm dramatically
Albedo