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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. Where does the ozone protect us?
Greenhouse Gases
In the stratosphere.
Negative Ice-Albedo Feedback
winter
2. 10 : 1 - grounding ; surface
Grounding v Surface Melting
Increases - decreases
Layers of Earth
What happens with the Ozone Hole
3. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Contributions to CO2 from different activities
Thermohaline Circulation
Air pollution
How the cryosphere is affected by climate change
4. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Where rise in OC is greatest
Ice Discharge
Is precipitation around the world increasing?
Greenhouse Gases
5. 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.
Surface Mass Balance
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
reduction in sea-ice
Troposphere
6. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Strong
Threshold departures
How a closed talik forms
Global warming and hot nights?
7. The Earth emits this.
Longwave Radiation
Percentile departures
Normal condition for air
70%
8. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ice Motion
Ocean water
Grounding Lines
How to define a heatwave
9. 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
Methane
Permafrost
Grounding Lines
Thinner atmosphere
10. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Layers of Earth
Ice in the Arctic
Changes in Arctic sea-ice Extent
How talik forms under lakes
11. Greenhouse gases are mixed in the ____
Ice in the Arctic
Altimetry
Negative
Troposphere
12. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Antarctica
Infrared radiation
Longwave Radiation
Altimetry Cons
13. Ice sheets have a very ____ Albedo
Monthly maximums and minimums
Surface Mass Balance
Negative
Strong
14. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stronger
Deep tropics between 15O N and 15 O S are quite
Negative
Talik
15. 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
All Greenhouse gases
Melt
Greenhouse Gases
Thermohaline Circulation Effect
16. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
How to define a heatwave
Ocean water
Ice Cap
17. 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.
Arctic Atmosphere
How talik forms under lakes
Altimetry Pros
30%
18. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Positive
The Ozone Hole
Thermokarst Lake
air can warm dramatically
19. Total absorbed solar radiation
70%
20%
Indirect heat wave effect
How talik forms under lakes
20. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Hydrological Drought
Deep tropics between 15O N and 15 O S are quite
Mass Balance
Closed talik
21. Surface Mass Balance is of the order of _____ melting is ____ times more.
1 m/yr; 10x
Through talik
Ice loss
Sea ice melt does not change sea level
22. How much is the planet really warming?
Depth v Surface
.7O Celsius over the past century.
Inversion Layer Summer
Monthly maximums and minimums
23. 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.
Major distinction between Kyoto Protocol and Convention
Melt
air can warm dramatically
Why Water Vapor is not a climate forcing
24. Set up in 1988 by WMO and UNEP.
30%
Warm
IPCC
Why ice-albedo feedback is a big deal in the Arctic
25. CO2 GHG forcing - H2O - dominant/major GHG
Questions to think about
Global warming and hot nights?
Thickness of the active layer and the permafrost depend on this
GHG
26. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
Altimetry Pros
Permafrost
Talik
30%
27. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Discontinuous Permafrosrt
IPCC
Increases - decreases
Carbon Dioxide
28. 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
Reduction in sea-ice extent
Very small portion
Ice in the Arctic
Discontinuous Permafrosrt
29. O Unfrozen soil that stays within the permafrost.
70%
In the stratosphere.
Is precipitation around the world increasing?
Talik
30. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Ocean water
Radiative Forcing
Greenhouse Gases
Atmospheric Composition?
31. Tundra absorbs more energy than ice and snow but less than scrubs and forest - and with those plants migrating towards the north - they will further contribute ot absorb more energy.
Active Layer
Change in vegetation generates a further feedback
Altimetry (height)
Atmospheric Composition
32. Rainy on yearly average. In these regions - rising air predominates.
Thickness of the active layer and the permafrost depend on this
Deep tropics between 15O N and 15 O S are quite
Types of Albedo
Very small portion
33. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
air can warm dramatically
Discontinuous Permafrosrt
Albedos of Snow and Ice
Carbon Dioxide
34. Less frequent and weaker
Threshold departures
Ice-Albedo
Inversion Layer Summer
reduction in sea-ice
35. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Types of Albedo
Indirect heat wave effect
In the troposphere that we live in.
Ozone Hole
36. 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.
Arctic Atmosphere
Ice-Ocean Interactions
El Nio is in the coasts of...
Indirect heat wave effect
37. O The amount of energy moving in the form of photons or other elementary particles at a certain distance from the source per unit of area per second. Area/second
Today melting ice
Accumulation
Radiative Flux
45%
38. Permafrost- A frozen soil
Frozen Soil
50%
Ice Discharge
20%
39. 1.4 USA - 57 m total sea level equivalent
Surface Mass Balance
Open talik
Antarctica
Global warming and hot nights?
40. How often does El Nio occur?
Nitrous Oxide (N2O)
Once every 4 years.
Stratospheric Ozone Depletion
Atmospheric Circulation
41. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
US and precipitation
75-OC
Positive
Types of Albedo
42. Grace - Tells us how much mass change we have - M - This is the measure of gravity (gives us the mass) - Directly measure mass change - Poor resolution
Antarctica
Negative
Mass Change
Altimetry (height)
43. What can cause a change in the Earth's climate balance?
summer
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Wetter; drier
Grounding Lines
44. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Cloud Feedbacks
Why Water Vapor is not a climate forcing
Antarctica
45. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Cause of break of inversion layers or decrease in frequency
Air pollution
Effect of Deforestation on CO-2
Thermokarst Lake
46. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Affect Floods and Droughts
All Greenhouse gases
Types of Albedo
Monthly maximums and minimums
47. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
70%
7%
Atmospheric Structure
Hydrological Drought
48. he increase of ozone concentration in the atmosphere helps ____ our planet
Thermokarst Lake
Warm
Stratospheric Ozone Depletion
Antarctica
49. 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
Archimedes' Principle
El Nino
Atlantic Thermohaline Circulation
Inversion Layer Summer
50. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Meteorological Drought
Sunspots
Positive feedbacks both found in...
Stratospheric Ozone Depletion