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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. Amount of light absorbed by atmosphere
Heat Source and Pressure
20%
Dynamic thinning
Arctic Atmosphere
2. Where do greenhouse gases warm up the Earth?
In the troposphere that we live in.
Mass Balance
Absolute thresholds
Frozen Soil
3. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
% of Greenhouse Gases
Active Layer
winter
Albedos of Snow and Ice
4. 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:
Through talik
Thermohaline Circulation
How the cryosphere is affected by climate change
Carbon Dioxide
5. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
Carbon Dioxide
Questions to think about
Talik
Active Layer
6. 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
How talik forms under lakes
Amount of light actually reaching the Earth
Energy Budget
El Nino
7. he increase of ozone concentration in the atmosphere helps ____ our planet
Deep tropics between 15O N and 15 O S are quite
Warm
Inversion Layer (feedback)
Earth's tilt
8. 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
Permafrost
Thinner atmosphere
Black Carbon
Dry
9. 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.
Ice/snow
Ice loss
Ice shelf
Thermokarst
10. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
Climate Change in the Arctic
Heat Source and Pressure
Inversion Layer (feedback)
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
11. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Greenland
Ice in the Arctic
45%
Dynamic thinning
12. 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%
All Greenhouse gases
Atmospheric Circulation
Heat wave
Albedos of Snow and Ice
13. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
The Ozone Hole
Greenland
Infrared radiation
14. Climate models suggest once the sea ice cover is thinned sufficiently - a strong kick from natural variability could initiate a rapid slide towards ice-free conditions in the summer.
Very small portion
Sea Ice Extent is Changing in Antarctica as well
Ice Discharge
Changes in Arctic sea-ice Extent
15. 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
Negative Ice-Albedo Feedback
Discontinuous Permafrosrt
Ozone Hole
In the Arctic where the air is cooler
16. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Wetter; drier
Dry
Dynamic thinning
Heat Source and Pressure
17. O Climate change in the Arctic is occurring now - Changes have been huge already
Today melting ice
Mass Change
Change in vegetation generates a further feedback
Radiative Flux
18. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Thermokarst
Atmospheric Composition
Natural Causes of Warming
Heat wave
19. 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
Sea ice melt does not change sea level
The cryosphere
Ice-Ocean Interactions
Thinner atmosphere
20. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Positive feedbacks both found in...
25%
Black Carbon
The Ozone Hole
21. 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.
Indirect heat wave effect
Stratospheric Ozone Depletion
Ice-Ocean Interactions
The cryosphere
22. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Surface Mass Balance
Warm
Stronger
23. Reduction of snow and ice cover - Changes in atmospheric circulation.
Precipitation and High Latitudes
Surface Mass Balance
Ozone
Cause of break of inversion layers or decrease in frequency
24. Descending Air dry - Convection cells are wet.
Ocean water
Atmospheric Circulation
Atmospheric Composition
Atlantic Thermohaline Circulation
25. 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!
Ice Cap
How we measure Mass Balance
Depth v Surface
Antarctica
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
IPCC
Melt
Atlantic Thermohaline Circulation
.75OC/km-1
27. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Atmospheric Composition?
Sublimation
Thermohaline Circulation
28. 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.
.75OC/km-1
Methane
Ice Cap
Indirect heat wave effect
29. Number of days when temperatures climb above average by a fixed amount.
Mass Budget
Heat Source and Pressure
Threshold departures
Altimetry Pros
30. Ocean retains ____ CO2
Negative Ice-Albedo Feedback
Air pollution
25%
Thickness of the active layer and the permafrost depend on this
31. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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32. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
summer
Mass Balance
Atmospheric Composition
Thermokarst Lake
33. 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
45%
Reduction in sea-ice extent
Albedo
Sea Ice
34. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
air can warm dramatically
Atmospheric Circulation
In the troposphere that we live in.
Antarctica
35. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
How to define a heatwave
25%
Atmospheric Composition
Accumulation
36. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
% of Greenhouse Gases
Discontinuous Permafrosrt
Through talik
Troposphere
37. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Energy Budget
Meteorological Drought
What effects the density
Global warming and hot nights?
38. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
El Nino
Atmospheric Composition
Ice Discharge
Sublimation
39. 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
Altimetry
Layers of Earth
Agricultural Drought
Inversion Layer (feedback)
40. The order of 1 m/year. Melting is ten times more.
Surface Mass Balance
Radiative Forcing
Major distinction between Kyoto Protocol and Convention
30%
41. Ice sheets have a very ____ Albedo
US and precipitation
Strong
Radiative Forcing
Atmospheric Structure
42. 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
Antarctica
Sunspots
Importance of ice sheets
Hydrological Drought
43. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Carbon Dioxide
70%
Monthly maximums and minimums
Global warming and hot nights?
44. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Mass Change
Ozone Hole
Ozone
In the Arctic where the air is cooler
45. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Ice Sheets
reduction in sea-ice
Grounding Lines
Thermokarst
46. Summer increase in cloud cover - Winter decrease in cloud cover.
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47. O Unfrozen soil that stays within the permafrost.
Percentile departures
How the cryosphere is affected by climate change
Talik
Albedos of Snow and Ice
48. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Heat Source and Pressure
Wetter; drier
Mass Change
Ice Discharge
49. Industrial product - 300 ppb (parts per billion)
Nitrous Oxide (N2O)
Carbon Dioxide
Active Layer
Discontinuous Permafrosrt
50. Number of days that land among the hottest of all days in that month's long-term record.
Ocean water
Percentile departures
Arctic Atmosphere
Warm