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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. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Warming; cooling
Thermokarst
All Greenhouse gases
50%
2. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Rainy
The cryosphere
Active Layer
Average radiative flux reaching the atmosphere
3. x7 smaller - 7m total sea level equivalent.
Amount of light actually reaching the Earth
Greenland
Ice Sheets
In the Arctic where the air is cooler
4. 1. They are the largest contributor to sea level rise 2. Can affect the thermohaline circulation (mainly in Greenland) 3. Are directly connected to climate change
Air pollution
Permafrost Degradation
Ice Cap
Importance of ice sheets
5. Precipitation intensity will rise ___ for every 1 OC of warming.
reduction in sea-ice
Is precipitation around the world increasing?
7%
summer
6. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Ice-Ocean Interactions
Some parts of the planet are dry because of their location
Grounding v Surface Melting
Air pollution
7. Over the past century what has happened to the Earth's temperature?
Ice-Ocean Interactions
Antarctica
.7O Celsius over the past century.
Some regions of the Earth have warmed faster than other regions.
8. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Active Layer
Air pollution
Altimetry (height)
Albedos of Snow and Ice
9. 85%
Sea-Ice Albedo
Grounding Lines
Dry
Surface Mass Balance
10. Clouds 40~90% - Vegetation 10~15%
In the stratosphere.
Ice Cap
Arctic Atmosphere
Types of Albedo
11. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Inversion Layer Winter
How we measure Mass Balance
Average radiative flux reaching the atmosphere
Agricultural Drought
12. Set up in 1988 by WMO and UNEP.
Heat wave
IPCC
Thermohaline Circulation Effect
Thinner atmosphere
13. 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
Permafrost
Heat Source and Pressure
Surface Mass Balance
Melt
14. 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) -
Threshold departures
Atmospheric Composition?
Deep tropics between 15O N and 15 O S are quite
Normal condition for air
15. Just remember the general direction of the circulation - Rising northern pacific. You start in between Greenland and Europe (youngest water) - Oldest water is in the Pacific Ocean - Salty water> fresh water - Cold Water > Warm Water
Ocean water
Thermohaline Circulation
In the Arctic where the air is cooler
Nitrous Oxide (N2O)
16. 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
Grounding v Surface Melting
Dynamic thinning
Ice absorbs
17. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ozone
Positive
Sublimation
Percentile departures
18. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Effect of Deforestation on CO-2
Meteorological Drought
Mass Budget
% of Greenhouse Gases
19. ~10% of incident solar energy (albedo 90)
Grounding Lines
Permafrost Degradation
Ice absorbs
30%
20. Number of days that exceed a given temperature
Absolute thresholds
Ice Motion
Heat Source and Pressure
Longwave Radiation
21. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Positive
Ice/snow
Why Water Vapor is not a climate forcing
Grounding Lines
22. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
.7O Celsius over the past century.
Ocean water
El Nino
Positive
23. A thick - floating slab of freshwater ice extending from coast to coast.
Strong
Ice shelf
Altimetry (height)
Infrared radiation
24. 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
Thinner atmosphere
Ice Cap
Why ice-albedo feedback is a big deal in the Arctic
Time Variable Gravity
25. 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.
Affect Floods and Droughts
Major distinction between Kyoto Protocol and Convention
Ice-Ocean Interactions
Stratospheric Ozone Depletion
26. Land Based Ecosystems retain ____ CO2.
Ice Shelf
30%
All Greenhouse gases
Positive feedbacks both found in...
27. CO2 GHG forcing - H2O - dominant/major GHG
Black Carbon
Ice absorbs
GHG
Changes in Arctic sea-ice Extent
28. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Major distinction between Kyoto Protocol and Convention
Greenhouse Gases
Sublimation
Mass Balance
29. 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.
Is precipitation around the world increasing?
Meteorological Drought
Ice Discharge
Ice Sheets
30. How often does El Nio occur?
Once every 4 years.
Very small portion
Why Water Vapor is not a climate forcing
Discontinuous
31. Volcanic eruptions - Sunspots - Wobbly Earth
Surface Mass Balance
Natural Causes of Warming
How we measure Mass Balance
Cloud Feedbacks
32. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
How talik forms under lakes
Accumulation
Dynamic thinning
Atmospheric Circulation
33. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Layers of Earth
More rain means no drought
Antarctica
Why Water Vapor is not a climate forcing
34. Arctic troposphere is thinner (8-10 km) than the tropics...The depth of the atmospheric layer is much shallower in the Arctic - It takes less energy to warm the Arctic rather than the Tropics - Same as heating an apartment vs. a house
Thinner atmosphere
Ice/snow
Heat wave
.75OC/km-1
35. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Black Carbon
Thickness of the active layer and the permafrost depend on this
Global warming and hot nights?
Stratospheric Ozone Depletion
36. Reduction of snow and ice cover - Changes in atmospheric circulation.
Increases - decreases
Cause of break of inversion layers or decrease in frequency
Ozone Hole
The cryosphere
37. 240 w/m squared
Altimetry (height)
Ozone
Mass Balance
Amount of light actually reaching the Earth
38. Number of days when temperatures climb above average by a fixed amount.
Sea-Ice Albedo
Threshold departures
Ocean-Ice-Atmosphere Interaction
Where rise in OC is greatest
39. What can cause a change in the Earth's climate balance?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Atmospheric Composition?
Changes in Arctic sea-ice Extent
Radiative Flux
40. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Deep tropics between 15O N and 15 O S are quite
Ocean water
Active Layer
Surface Mass Balance
41. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Severe coastal erosion
Thermohaline Circulation Effect
Effect of Deforestation on CO-2
Layers of Earth
42. 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.
Ice Shelf
Importance of ice sheets
Precipitation and High Latitudes
Very small portion
43. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Ozone Hole
More rain means no drought
Altimetry Cons
Altimetry (height)
44. 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
Negative
Cloud Feedbacks
Altimetry (height)
Dry
45. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
Dry
Indirect heat wave effect
Ice shelf
Amount of light actually reaching the Earth
46. Is best viewed as a combination of...- Natural Variability - Associated with atmospheric circulation patterns - Growing Radiative Forcing - Associated with rising concentrations of atmospheric greenhouse gases - Strongly suggests a human influence.
Ozone Hole
Permafrost Degradation
Antarctica
Ice loss
47. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Ice shelf
50%
Effect of Deforestation on CO-2
Threshold departures
48. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition?
Atmospheric Composition
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
US and precipitation
49. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
1 m/yr; 10x
Longwave Radiation
Warming; cooling
50. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Discontinuous
Ice Sheets
Infrared radiation
Layers of Earth