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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. 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
Thermokarst Lake
45%
Global warming and hot nights?
Permafrost
2. The buoyant force is equal to the weight of the displaced water.
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3. The amount of light reflected by an object.
Albedo
Normal condition for air
Ozone Hole
Permafrost Degradation
4. 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!
Antarctica
Closed talik
Why the Arctic climate is special
Grounding v Surface Melting
5. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Cloud Feedbacks
Ocean water
Through talik
Radiative Forcing
6. 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
Why Water Vapor is not a climate forcing
Ice Sheets
The Ozone Hole
25%
7. Descending Air dry - Convection cells are wet.
Atmospheric Circulation
Reduction in sea-ice extent
The cryosphere
Positive feedbacks both found in...
8. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Sea Ice
Hydrological Drought
Today melting ice
Altimetry
9. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
Monthly maximums and minimums
What happens with the Ozone Hole
Active Layer
10. 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
Inversion Layer Summer
Ice-Ocean Interactions
Reduction in sea-ice extent
Heat Source and Pressure
11. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
winter
Why Water Vapor is not a climate forcing
Amount of light actually reaching the Earth
US and precipitation
12. High vs low
Hydrological Drought
Ice Sheets
How the cryosphere is affected by climate change
Cloud Feedbacks
13. Atmospheric Cooling - Both negative (stabilizing) feedbacks - It is not happening now - but it has happened in the past - Ice-albedo feedback was the dominant feedback during the ice ages.
Negative Ice-Albedo Feedback
Mass Budget
In the stratosphere.
% of Greenhouse Gases
14. Reduction of snow and ice cover - Changes in atmospheric circulation.
Cause of break of inversion layers or decrease in frequency
Ice Shelf
Carbon Dioxide
Ice-Albedo
15. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Altimetry
Altimetry (height)
Carbon Dioxide
Stronger
16. 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
Radiative Forcing
Melt
In the Arctic where the air is cooler
17. 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.
Negative Ice-Albedo Feedback
Depth v Surface
Longwave Radiation
Thermohaline Circulation Effect
18. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
Sea ice melt does not change sea level
Black Carbon
Ozone
19. 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.
Atmospheric Structure
Ice loss
Permafrost Degradation
Thermohaline Circulation
20. 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.
Arctic Atmosphere
Ice-Ocean Interactions
50%
Ocean-Ice-Atmosphere Interaction
21. Melting Point decreases
Greenhouse Gases
.75OC/km-1
Atlantic Thermohaline Circulation
Thermohaline Circulation Effect
22. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Black Carbon
What effects the density
Troposphere
In the stratosphere.
23. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
All Greenhouse gases
Sublimation
Altimetry Pros
Negative Ice-Albedo Feedback
24. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Is precipitation around the world increasing?
Why ice-albedo feedback is a big deal in the Arctic
Ice Motion
More rain means no drought
25. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Thermohaline Circulation Effect
Cause of break of inversion layers or decrease in frequency
Increases - decreases
Atmospheric Composition
26. 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
Meteorological Drought
1 m/yr; 10x
Melt
Where rise in OC is greatest
27. Frozen +2 years - Few centimeters to 1500 m
Very small portion
Ozone
IPCC
Permafrost
28. Laser radar - H V - Long time series - high accuracy - Density
Ocean water
How we measure Mass Balance
Altimetry (height)
Air pollution
29. A dome shaped cover of perennial ice and snow.
20%
% of Greenhouse Gases
Ice Cap
Ice loss
30. Like weighing oneself on the scale.
Longwave Radiation
Time Variable Gravity
Affect Floods and Droughts
Increases - decreases
31. Extent 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.
reduction in sea-ice
Questions to think about
Hydrological Drought
Atmospheric Composition
32. Really measures volume.
Ocean water
Natural Causes of Warming
Altimetry
summer
33. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Carbon Dioxide
Ice loss
Ice in the Arctic
Absolute thresholds
34. Number of days when temperatures climb above average by a fixed amount.
Once every 4 years.
reduction in sea-ice
Threshold departures
7%
35. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Severe coastal erosion
Ice Sheets
Ice loss
36. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Inversion Layer (feedback)
Active Layer
Today melting ice
Agricultural Drought
37. Carbon dioxide - Methane - Ozone - Water Vapor - Few others - Most ___________________ are mixed in the troposphere (Except water vapor) - Water vapor is concentrated closer to the ground.
Black Carbon
Methane
Greenhouse Gases
Permafrost Degradation
38. Rainy on yearly average. In these regions - rising air predominates.
Today melting ice
Black Carbon
Deep tropics between 15O N and 15 O S are quite
Stronger
39. CO2 - CH4 - O3 - H2O - N2O - CFCs
Where rise in OC is greatest
All Greenhouse gases
Major distinction between Kyoto Protocol and Convention
Ice Sheets
40. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Rainy
Active Layer
Positive feedbacks both found in...
Wetter; drier
41. 85%
Ice Sheets
air can warm dramatically
Archimedes' Principle
Sea-Ice Albedo
42. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Closed talik
Stronger
70%
% of Greenhouse Gases
43. In average: +1% in respect to 100 years ago.
Ocean water
Why the Arctic climate is special
Is precipitation around the world increasing?
Ice Sheets
44. 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.
Thermokarst Lake
Mass Balance
Why Water Vapor is not a climate forcing
Permafrost Degradation
45. Ocean retains ____ CO2
Ice/snow
25%
Heat wave
Ice Motion
46. 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
Nitrous Oxide (N2O)
Where rise in OC is greatest
Agricultural Drought
Importance of ice sheets
47. Warming- positive feedback - Cooling- negative feedback.
The cryosphere
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice-Albedo
Why Water Vapor is not a climate forcing
48. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Thinner atmosphere
Altimetry Pros
Mass Change
49. Measures input and output.
Nitrous Oxide (N2O)
Mass Change
Mass Budget
Earth's tilt
50. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Rainy
Thermokarst
Melt
Surface Mass Balance
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