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Test your basic knowledge |
Global Warming
Start Test
Study First
Subjects
:
literacy
,
science
Instructions:
Answer 50 questions in 15 minutes.
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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. Ice sheets have a very ____ Albedo
Strong
Ice Motion
How we measure Mass Balance
Dynamic thinning
2. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Nitrous Oxide (N2O)
doubles
Monthly maximums and minimums
Depth v Surface
3. Over the Northern Hemisphere than the tropics.
Positive feedbacks both found in...
More rain means no drought
Where rise in OC is greatest
Air pollution
4. Measures input and output.
Very small portion
Albedo
Effect of Deforestation on CO-2
Mass Budget
5. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
30%
Dry
Ice-Albedo
6. 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
What happens with the Ozone Hole
25%
In the stratosphere.
Snow and snow covered ice absorb
7. Precipitation intensity will rise ___ for every 1 OC of warming.
Wetter; drier
Ozone
7%
Rainy
8. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Stronger
Active Layer
Why the Arctic climate is special
Earth's tilt
9. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Permafrost
More rain means no drought
20%
10. 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
Cloud Feedbacks
Grounding Lines
Melt
Ice Discharge
11. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Surface Mass Balance
Ice in the Arctic
Atmospheric Composition?
Mass Change
12. US is responsible for ___ of the total CO2
Absolute thresholds
Mass Budget
30%
.7O Celsius over the past century.
13. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Ice/snow
Discontinuous Permafrosrt
Hydrological Drought
Antarctica
14. Cooler water and drought conditions.
70%
La Nia
Indirect heat wave effect
Ice/snow
15. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
Radiative Forcing
GHG
Thermokarst
16. Antarctica - stratosphere - Sep-Oct
.7O Celsius over the past century.
50%
Ozone Hole
La Nia
17. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Ocean water
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Indirect heat wave effect
The cryosphere
18. 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.
Surface Mass Balance
La Nia
Ice Sheets
Ozone
19. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
Why ice-albedo feedback is a big deal in the Arctic
Closed talik
Antarctica
20. CO2 GHG forcing - H2O - dominant/major GHG
Sea-Ice Albedo
GHG
Albedo
Thermokarst
21. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Warming; cooling
Inversion Layer (feedback)
Sea ice melt does not change sea level
Sunspots
22. 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.
Ice/snow
Thermohaline Circulation Effect
Major distinction between Kyoto Protocol and Convention
Ice-Albedo
23. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stronger
Effect of Deforestation on CO-2
Thickness of the active layer and the permafrost depend on this
In the troposphere that we live in.
24. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Surface Mass Balance
How a closed talik forms
Major distinction between Kyoto Protocol and Convention
Why Water Vapor is not a climate forcing
25. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Dynamic thinning
Open talik
Some parts of the planet are dry because of their location
Sea Ice Extent is Changing in Antarctica as well
26. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Thermokarst
More rain means no drought
Active Layer
What happens with the Ozone Hole
27. Descending Air dry - Convection cells are wet.
20%
Atmospheric Circulation
7%
Sunspots
28. Warming- positive feedback - Cooling- negative feedback.
How to define a heatwave
Permafrost
Ice-Albedo
Ice Cap
29. 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
Ice Sheets
Mass Change
Hydrological Drought
Reduction in sea-ice extent
30. 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
Discontinuous Permafrosrt
Earth's tilt
Why ice-albedo feedback is a big deal in the Arctic
Arctic Atmosphere
31. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Grounding v Surface Melting
Permafrost Degradation
Contributions to CO2 from different activities
Layers of Earth
32. Laser radar - H V - Long time series - high accuracy - Density
% of Greenhouse Gases
Altimetry (height)
Sea-Ice Albedo
Stronger
33. In average: +1% in respect to 100 years ago.
Monthly maximums and minimums
Radiative Forcing
Is precipitation around the world increasing?
reduction in sea-ice
34. Water vapor means more water up in the clouds and less in the ground!
How we measure Mass Balance
Black Carbon
Warm
More rain means no drought
35. 10 : 1 - grounding ; surface
Thickness of the active layer and the permafrost depend on this
Grounding v Surface Melting
Thinner atmosphere
Thermohaline Circulation
36. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Methane
Precipitation and High Latitudes
Layers of Earth
Increases - decreases
37. Less frequent and weaker
Why Water Vapor is not a climate forcing
Grounding Lines
US and precipitation
Inversion Layer Summer
38. Longwave radiation - any radiation with a long wave will heat up quickly.
Ice Sheets
Infrared radiation
Calving
Why ice-albedo feedback is a big deal in the Arctic
39. Amount of light absorbed by surface
50%
Thermokarst Lake
Global warming and hot nights?
Sea Ice Extent is Changing in Antarctica as well
40. 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
doubles
Talik
Inversion Layer (feedback)
Warm
41. 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.
Sea Ice
Once every 4 years.
Climate Change in the Arctic
Surface Mass Balance
42. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
70%
Ocean water
Time Variable Gravity
43. Grace - Tells us how much mass change we have - M - This is the measure of gravity (gives us the mass) - Directly measure mass change - Poor resolution
Percentile departures
La Nia
Mass Change
El Nino
44. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Infrared radiation
US and precipitation
Dynamic thinning
Archimedes' Principle
45. What can cause a change in the Earth's climate balance?
Depth v Surface
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Contributions to CO2 from different activities
50%
46. Over the past century what has happened to the Earth's temperature?
Dynamic thinning
Some regions of the Earth have warmed faster than other regions.
Frozen Soil
Monthly maximums and minimums
47. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
45%
Warm
The Ozone Hole
75-OC
48. High vs low
Cloud Feedbacks
Greenland
Earth's tilt
US and precipitation
49. Where do greenhouse gases warm up the Earth?
IPCC
In the troposphere that we live in.
Strong
Mass Change
50. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Through talik
Ice in the Arctic
Agricultural Drought
Calving
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