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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. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ice-Ocean Interactions
Carbon Dioxide
Meteorological Drought
2. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Talik
Altimetry (height)
Inversion Layer Winter
Ocean water
3. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Meteorological Drought
US and precipitation
Ice Cap
How talik forms under lakes
4. Greenhouse gases are a ___ portion of the atmosphere
Sea-Ice Albedo
Very small portion
25%
70%
5. In _______ - the inversions are less frequent and weaker in the Arctic.
Troposphere
Contributions to CO2 from different activities
More rain means no drought
summer
6. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Amount of light actually reaching the Earth
Ice loss
Altimetry Cons
El Nio is in the coasts of...
7. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Absolute thresholds
Effect of Deforestation on CO-2
Ice loss
Heat wave
8. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Air pollution
Global warming and hot nights?
Natural Causes of Warming
Atmospheric Composition?
9. 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
Heat wave
Inversion Layer Winter
Methane
doubles
10. Occurs when there is not enough water available for a particular crop to grow at a particular time.Typically seen after!meteorological drought (when rainfall decreases) but before a hydrological drought
45%
Shortwave Length
Changes in Arctic sea-ice Extent
Agricultural Drought
11. 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
Monthly maximums and minimums
How to define a heatwave
Ice in the Arctic
12. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
air can warm dramatically
How to define a heatwave
% of Greenhouse Gases
Thermokarst
13. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Ozone
Grounding Lines
Sunspots
Reduction in sea-ice extent
14. ~15% of incident solar energy (albedo 85)
Natural Causes of Warming
Snow and snow covered ice absorb
Ozone
Active Layer
15. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Hydrological Drought
Permafrost
45%
Ice Motion
16. 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
Greenland
Reduction in sea-ice extent
Today melting ice
Albedos of Snow and Ice
17. Volcanic eruptions - Sunspots - Wobbly Earth
Thermokarst
Mass Balance
Sea Ice
Natural Causes of Warming
18. O Unfrozen soil that stays within the permafrost.
Reduction in sea-ice extent
Talik
Very small portion
Altimetry (height)
19. Arctic warms faster than other parts of the globe in response to a given increase in greenhouse gasses - More direct route to warming - In the Arctic a greater fraction of any increase in radiation absorbed by the surface goes directly into warming t
Why the Arctic climate is special
La Nia
Major distinction between Kyoto Protocol and Convention
Thermohaline Circulation
20. 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%
Ozone
Sublimation
Negative
21. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Grounding Lines
Air pollution
Some parts of the planet are dry because of their location
Atmospheric Structure
22. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
How to define a heatwave
Thermohaline Circulation
Sunspots
Ozone Hole
23. The air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
Sea Ice
In the Arctic where the air is cooler
Why ice-albedo feedback is a big deal in the Arctic
Wetter; drier
24. Frozen +2 years - Few centimeters to 1500 m
Sea ice melt does not change sea level
Permafrost
In the Arctic where the air is cooler
Layers of Earth
25. Radiation absorbed by atmospheric greenhouse gases?
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Inversion Layer Winter
Ice-Albedo
Thermohaline Circulation Effect
26. 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.
Sea-Ice Albedo
Antarctica
Thermokarst
Ice loss
27. Fresh snow and snow-covered sea ice may have an albedo higher than 80% - even when melting in the summer. Sea ice has a higher albedo and can absorb as little as 10% of the solar energy. On average - sea ice albedo is around 85%
Albedos of Snow and Ice
.75OC/km-1
Today melting ice
Grounding Lines
28. 1. Keeps the ocean and the earth cooler 2. Coastal impacts of ice: prevents waves from eroding coastlines and protects from storms. 3. Ecological importance of ice: a. Most visibly for the many fish - birds - and mammal species that live in - on - or
What effects the density
Grounding Lines
Stratospheric Ozone Depletion
How the cryosphere is affected by climate change
29. Descending Air dry - Convection cells are wet.
Effect of Deforestation on CO-2
Ocean-Ice-Atmosphere Interaction
Discontinuous Permafrosrt
Atmospheric Circulation
30. High vs low
Black Carbon
air can warm dramatically
Cloud Feedbacks
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
31. Total absorbed solar radiation
Why the Arctic climate is special
Antarctica
70%
Thermohaline Circulatoin
32. Number of days when temperatures climb above average by a fixed amount.
Permafrost
Threshold departures
How a closed talik forms
45%
33. The amount of light reflected by an object.
Albedo
How to define a heatwave
30%
Grounding Lines
34. 10 : 1 - grounding ; surface
Is precipitation around the world increasing?
Grounding v Surface Melting
Thermohaline Circulation
In the stratosphere.
35. 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.
Layers of Earth
Ice loss
Ozone Hole
Major distinction between Kyoto Protocol and Convention
36. Ocean retains ____ CO2
winter
Ice-Ocean Interactions
Precipitation and High Latitudes
25%
37. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Ocean water
Sea ice melt does not change sea level
Effect of Deforestation on CO-2
reduction in sea-ice
38. Refers to the irregular warming in the Sea Surface Temperatures (SST) from the coasts of Peru and Ecuador to the equatorial central Pacific - the Southern Oscillation
Percentile departures
Indirect heat wave effect
Surface Mass Balance
El Nino
39. Ice sheets have a very ____ Albedo
Inversion Layer Winter
Strong
Thickness of the active layer and the permafrost depend on this
Altimetry
40. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
Thermohaline Circulatoin
Absolute thresholds
Cloud Feedbacks
41. Taliks are found under lakes because of the ability of water to store and vertically transfer heat energy - Vertical extent of the taliks found under lakes is related to the depth and volume of the overlying water body.
How talik forms under lakes
Atmospheric Composition
Albedos of Snow and Ice
Surface Mass Balance
42. Is not an externally imposed perturbation to the climate system.
Inversion Layer Summer
Why Water Vapor is not a climate forcing
25%
Nitrous Oxide (N2O)
43. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
El Nio is in the coasts of...
Grounding v Surface Melting
75-OC
Methane
44. 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
Talik
Why ice-albedo feedback is a big deal in the Arctic
Thinner atmosphere
75-OC
45. Laser radar - H V - Long time series - high accuracy - Density
doubles
Agricultural Drought
Altimetry (height)
Sea ice melt does not change sea level
46. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Stratospheric Ozone Depletion
winter
% of Greenhouse Gases
Indirect heat wave effect
47. 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.
Mass Budget
Thermohaline Circulation Effect
Ice Sheets
Monthly maximums and minimums
48. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Atmospheric Circulation
Dynamic thinning
Melt
Altimetry Pros
49. 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
Mass Balance
Ozone
Infrared radiation
Thinner atmosphere
50. Permafrost- A frozen soil
Layers of Earth
Frozen Soil
Natural Causes of Warming
Indirect heat wave effect