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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. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Reduction in sea-ice extent
Greenhouse Gases
How to define a heatwave
Methane
2. x7 smaller - 7m total sea level equivalent.
Ocean water
Greenland
Thermokarst
Thermokarst
3. 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
Once every 4 years.
20%
Altimetry Pros
4. 1.4 USA - 57 m total sea level equivalent
Air pollution
Antarctica
Snow and snow covered ice absorb
Percentile departures
5. Industrial product - 300 ppb (parts per billion)
The cryosphere
Warming; cooling
Nitrous Oxide (N2O)
Methane
6. 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
Albedos of Snow and Ice
Melt
Sea Ice
1 m/yr; 10x
7. Antarctica - stratosphere - Sep-Oct
Energy Budget
Ozone Hole
Calving
Major distinction between Kyoto Protocol and Convention
8. Amount of light absorbed by atmosphere
Global warming and hot nights?
Discontinuous Permafrosrt
Ice in the Arctic
20%
9. The buoyant force is equal to the weight of the displaced water.
10. Clouds 40~90% - Vegetation 10~15%
Ice Discharge
Ozone Hole
Types of Albedo
Heat Source and Pressure
11. O Unfrozen soil that stays within the permafrost.
How a closed talik forms
Importance of ice sheets
Talik
air can warm dramatically
12. In ________- inversion layer is more common in the Arctic
winter
Global warming and hot nights?
Heat wave
Earth's tilt
13. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Thermokarst
20%
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Discontinuous Permafrosrt
14. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Altimetry
Warming; cooling
Indirect heat wave effect
15. 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
Thermokarst
Altimetry Cons
Cloud Feedbacks
16. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Time Variable Gravity
Frozen Soil
Altimetry Cons
Active Layer
17. 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
30%
doubles
Dry
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
18. Unfrozen ground that is found within a mass of permafrost
Mass Budget
Air pollution
Closed talik
Longwave Radiation
19. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Energy Budget
summer
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Contributions to CO2 from different activities
20. ~10% of incident solar energy (albedo 90)
Ice absorbs
Severe coastal erosion
45%
Why Water Vapor is not a climate forcing
21. In _______ - the inversions are less frequent and weaker in the Arctic.
Amount of light actually reaching the Earth
summer
1 m/yr; 10x
Permafrost
22. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
The Ozone Hole
Positive feedbacks both found in...
Thickness of the active layer and the permafrost depend on this
Methane
23. 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
Atmospheric Circulation
Heat wave
What happens with the Ozone Hole
24. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Atlantic Thermohaline Circulation
Threshold departures
Amount of light actually reaching the Earth
25. Greenhouse gases are mixed in the ____
Natural Causes of Warming
Today melting ice
Troposphere
winter
26. 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.
Thermohaline Circulation Effect
Surface Mass Balance
Positive
Ice Shelf
27. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Monthly maximums and minimums
Percentile departures
El Nino
How a closed talik forms
28. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Archimedes' Principle
Ice Discharge
Atmospheric Composition?
Frozen Soil
29. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Types of Albedo
Why the Arctic climate is special
Ice Motion
Air pollution
30. 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
Arctic Atmosphere
Thermohaline Circulation Effect
Antarctica
Thinner atmosphere
31. 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
Mass Change
Thinner atmosphere
Types of Albedo
Atmospheric Composition
32. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Questions to think about
Heat wave
Ice Discharge
Meteorological Drought
33. How often does El Nio occur?
Longwave Radiation
Once every 4 years.
How the cryosphere is affected by climate change
Thermokarst
34. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Rainy
Thinner atmosphere
Negative
Hydrological Drought
35. The past climate...for this reason - both keep good records of climate change.
Thermohaline Circulation
Thickness of the active layer and the permafrost depend on this
Thermohaline Circulation
Infrared radiation
36. 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:
Talik
Thermohaline Circulation
Earth's tilt
Ice Discharge
37. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Ice Cap
Ocean-Ice-Atmosphere Interaction
Permafrost
What happens with the Ozone Hole
38. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
The cryosphere
Precipitation and High Latitudes
Antarctica
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
39. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Very small portion
Types of Albedo
Precipitation and High Latitudes
40. Summer increase in cloud cover - Winter decrease in cloud cover.
41. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Methane
Permafrost
Ice Motion
42. More common
Thermokarst Lake
Mass Change
Methane
Inversion Layer Winter
43. 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.
Inversion Layer Summer
Cloud Feedbacks
Negative Ice-Albedo Feedback
Ice Cap
44. 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
Ice Shelf
Stronger
In the Arctic where the air is cooler
All Greenhouse gases
45. Greenhouse gases are a ___ portion of the atmosphere
Through talik
Why Water Vapor is not a climate forcing
Very small portion
Atmospheric Composition?
46. Permafrost- A frozen soil
Some regions of the Earth have warmed faster than other regions.
Grounding v Surface Melting
Precipitation and High Latitudes
Frozen Soil
47. Surface Mass Balance is of the order of _____ melting is ____ times more.
Thinner atmosphere
Amount of light actually reaching the Earth
Stronger
1 m/yr; 10x
48. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
The cryosphere
Sublimation
IPCC
Major distinction between Kyoto Protocol and Convention
49. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Dynamic thinning
Ozone Hole
Mass Balance
Affect Floods and Droughts
50. 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
Thermohaline Circulation
% of Greenhouse Gases
Ice-Ocean Interactions