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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. he increase of ozone concentration in the atmosphere helps ____ our planet
Grounding Lines
summer
Warm
Dynamic thinning
2. Less frequent and weaker
Ice Sheets
Inversion Layer Summer
Atlantic Thermohaline Circulation
20%
3. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Importance of ice sheets
% of Greenhouse Gases
Active Layer
IN the last 2 decades what we've seen
4. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
The Ozone Hole
Closed talik
air can warm dramatically
Ice Motion
5. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Changes in Arctic sea-ice Extent
Accumulation
1 m/yr; 10x
Ice Discharge
6. Laser radar - H V - Long time series - high accuracy - Density
Ice absorbs
Altimetry (height)
Ice Cap
Amount of light actually reaching the Earth
7. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Atmospheric Composition
Strong
Calving
Through talik
8. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Sunspots
summer
Nitrous Oxide (N2O)
Sublimation
9. Measures input and output.
Talik
Mass Budget
Greenhouse Gases
70%
10. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Sea ice melt does not change sea level
Antarctica
Earth's tilt
doubles
11. 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
Thermokarst Lake
Why ice-albedo feedback is a big deal in the Arctic
Sea Ice Extent is Changing in Antarctica as well
Radiative Flux
12. 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.
Sea Ice Extent is Changing in Antarctica as well
Absolute thresholds
Negative Ice-Albedo Feedback
El Nino
13. CO2 GHG forcing - H2O - dominant/major GHG
Today melting ice
GHG
Ozone
Warm
14. 10 : 1 - grounding ; surface
Grounding v Surface Melting
Frozen Soil
Altimetry
Thermokarst Lake
15. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Ice absorbs
Black Carbon
Positive
Heat Source and Pressure
16. In _______ - the inversions are less frequent and weaker in the Arctic.
Cloud Feedbacks
Ice Motion
summer
Thermohaline Circulation Effect
17. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Negative Ice-Albedo Feedback
Ozone Hole
Sunspots
Mass Budget
18. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Thermohaline Circulatoin
Ice-Ocean Interactions
Percentile departures
Rainy
19. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Radiative Flux
Monthly maximums and minimums
Hydrological Drought
Infrared radiation
20. The buoyant force is equal to the weight of the displaced water.
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21. 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
In the Arctic where the air is cooler
Arctic Atmosphere
Methane
El Nio is in the coasts of...
22. Number of days that exceed a given temperature
Antarctica
Melt
Absolute thresholds
Wetter; drier
23. 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.
Climate Change in the Arctic
Calving
Layers of Earth
Greenhouse Gases
24. 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%
Greenland
Wetter; drier
In the stratosphere.
Albedos of Snow and Ice
25. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Warm
75-OC
Talik
Depth v Surface
26. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Major distinction between Kyoto Protocol and Convention
Average radiative flux reaching the atmosphere
Albedo
Mass Balance
27. Where do greenhouse gases warm up the Earth?
Atmospheric Composition
How a closed talik forms
In the troposphere that we live in.
In the Arctic where the air is cooler
28. Total absorbed solar radiation
Heat wave
Normal condition for air
70%
Contributions to CO2 from different activities
29. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
El Nio is in the coasts of...
Amount of light actually reaching the Earth
Carbon Dioxide
30. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Ocean-Ice-Atmosphere Interaction
Altimetry
Layers of Earth
Severe coastal erosion
31. LW - SW - 55% absorbed by surface
Some parts of the planet are dry because of their location
Absolute thresholds
Cloud Feedbacks
Energy Budget
32. US is responsible for ___ of the total CO2
Thinner atmosphere
Questions to think about
30%
Ice Sheets
33. Frozen +2 years - Few centimeters to 1500 m
Ice Motion
Permafrost
Warming; cooling
What effects the density
34. High vs low
Cloud Feedbacks
What happens with the Ozone Hole
Permafrost Degradation
Where rise in OC is greatest
35. A dome shaped cover of perennial ice and snow.
Surface Mass Balance
Active Layer
Ice Cap
The Ozone Hole
36. 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.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Climate Change in the Arctic
Open talik
Ocean water
37. The amount of light reflected by an object.
Albedo
Major distinction between Kyoto Protocol and Convention
Wetter; drier
Active Layer
38. In ________- inversion layer is more common in the Arctic
Strong
Thermohaline Circulation Effect
What effects the density
winter
39. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Shortwave Length
Energy Budget
Accumulation
GHG
40. 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
Why ice-albedo feedback is a big deal in the Arctic
Normal condition for air
Ice Cap
Dry
41. 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
Indirect heat wave effect
Radiative Forcing
Importance of ice sheets
Change in vegetation generates a further feedback
42. Land Based Ecosystems retain ____ CO2.
Dry
30%
Mass Budget
Albedo
43. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Grounding Lines
How to define a heatwave
winter
Reduction in sea-ice extent
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.
Ozone Hole
Permafrost Degradation
.7O Celsius over the past century.
Atmospheric Composition?
45. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Thermohaline Circulation
Agricultural Drought
Heat wave
Thermokarst
46. Clouds 40~90% - Vegetation 10~15%
Radiative Flux
Types of Albedo
Stronger
.7O Celsius over the past century.
47. Number of days that land among the hottest of all days in that month's long-term record.
Ice shelf
Effect of Deforestation on CO-2
Percentile departures
Ice absorbs
48. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Sunspots
Contributions to CO2 from different activities
Percentile departures
Permafrost Degradation
49. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Albedos of Snow and Ice
Global warming and hot nights?
Severe coastal erosion
Snow and snow covered ice absorb
50. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Carbon Dioxide
Permafrost
Thermokarst
Dry