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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
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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. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
The cryosphere
Warming; cooling
Surface Mass Balance
50%
2. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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3. How often does El Nio occur?
Once every 4 years.
Frozen Soil
Thermokarst
Sublimation
4. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Shortwave Length
Inversion Layer Winter
Surface Mass Balance
5. 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!
Closed talik
Antarctica
Ice loss
75-OC
6. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Grounding Lines
Ice in the Arctic
Sea Ice Extent is Changing in Antarctica as well
Antarctica
7. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
75-OC
Heat wave
70%
Deep tropics between 15O N and 15 O S are quite
8. CO2 - CH4 - O3 - H2O - N2O - CFCs
All Greenhouse gases
Mass Change
Major distinction between Kyoto Protocol and Convention
winter
9. Laser radar - H V - Long time series - high accuracy - Density
50%
Surface Mass Balance
Altimetry (height)
Ice-Ocean Interactions
10. 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.
Climate Change in the Arctic
Questions to think about
Mass Budget
Greenland
11. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Active Layer
Longwave Radiation
.7O Celsius over the past century.
How talik forms under lakes
12. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Black Carbon
Greenhouse Gases
summer
How to define a heatwave
13. Most of the deserts are around 30 N and 30 S - where sinking air predominates
1 m/yr; 10x
Infrared radiation
Thinner atmosphere
Some parts of the planet are dry because of their location
14. 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
Natural Causes of Warming
Shortwave Length
Altimetry (height)
15. 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
Grounding Lines
Methane
Surface Mass Balance
Agricultural Drought
16. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Greenhouse Gases
Rainy
Arctic Atmosphere
La Nia
17. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Amount of light actually reaching the Earth
7%
75-OC
Ice Discharge
18. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Greenhouse Gases
Antarctica
Atmospheric Circulation
Grounding Lines
19. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Archimedes' Principle
air can warm dramatically
Cloud Feedbacks
Sea-Ice Albedo
20. CO2 GHG forcing - H2O - dominant/major GHG
GHG
air can warm dramatically
Permafrost Degradation
Positive feedbacks both found in...
21. In average: +1% in respect to 100 years ago.
Radiative Flux
30%
Is precipitation around the world increasing?
Calving
22. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Permafrost
Types of Albedo
Natural Causes of Warming
Sea ice melt does not change sea level
23. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
In the stratosphere.
Atmospheric Structure
GHG
Global warming and hot nights?
24. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Ocean water
Ice Sheets
Grounding Lines
25. 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.
Altimetry Cons
IPCC
Negative Ice-Albedo Feedback
Open talik
26. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Deep tropics between 15O N and 15 O S are quite
Sea-Ice Albedo
In the Arctic where the air is cooler
Atmospheric Structure
27. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
air can warm dramatically
Ozone Hole
The Ozone Hole
Average radiative flux reaching the atmosphere
28. 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.
Calving
Ice Motion
70%
Permafrost Degradation
29. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ocean-Ice-Atmosphere Interaction
Atmospheric Structure
Ice/snow
Rainy
30. 10 : 1 - grounding ; surface
Today melting ice
How to define a heatwave
Grounding v Surface Melting
Ozone Hole
31. Greenhouse gases are mixed in the ____
Mass Balance
The cryosphere
Troposphere
Meteorological Drought
32. 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.
Changes in Arctic sea-ice Extent
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Snow and snow covered ice absorb
Accumulation
33. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Percentile departures
How a closed talik forms
30%
Indirect heat wave effect
34. 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
Where rise in OC is greatest
25%
More rain means no drought
Why ice-albedo feedback is a big deal in the Arctic
35. Ocean retains ____ CO2
25%
Sea ice melt does not change sea level
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice Discharge
36. Clouds 40~90% - Vegetation 10~15%
Indirect heat wave effect
Types of Albedo
.7O Celsius over the past century.
Ozone
37. 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
Cause of break of inversion layers or decrease in frequency
Today melting ice
Sea Ice Extent is Changing in Antarctica as well
How the cryosphere is affected by climate change
38. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Ice-Albedo
Change in vegetation generates a further feedback
Calving
Atmospheric Structure
39. x7 smaller - 7m total sea level equivalent.
Ice Discharge
Greenland
Infrared radiation
Ice-Ocean Interactions
40. High vs low
Why ice-albedo feedback is a big deal in the Arctic
Types of Albedo
Thermokarst
Cloud Feedbacks
41. In _______ - the inversions are less frequent and weaker in the Arctic.
Major distinction between Kyoto Protocol and Convention
Inversion Layer Winter
Permafrost
summer
42. US is responsible for ___ of the total CO2
Once every 4 years.
30%
Mass Budget
What happens with the Ozone Hole
43. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
IN the last 2 decades what we've seen
Closed talik
Antarctica
44. ~10% of incident solar energy (albedo 90)
Negative
Permafrost
Time Variable Gravity
Ice absorbs
45. LW - SW - 55% absorbed by surface
Thinner atmosphere
Is precipitation around the world increasing?
Sea ice melt does not change sea level
Energy Budget
46. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Active Layer
1 m/yr; 10x
Altimetry (height)
The cryosphere
47. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Active Layer
Grounding Lines
Warm
Mass Balance
48. Unfrozen ground that is found within a mass of permafrost
Atmospheric Structure
Sea-Ice Albedo
Closed talik
Archimedes' Principle
49. Set up in 1988 by WMO and UNEP.
Open talik
How the cryosphere is affected by climate change
Ocean water
IPCC
50. 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.
How we measure Mass Balance
Cause of break of inversion layers or decrease in frequency
doubles
Thermohaline Circulation Effect
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