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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. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
Why ice-albedo feedback is a big deal in the Arctic
Methane
In the stratosphere.
2. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Carbon Dioxide
25%
Thermokarst
3. 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.
Heat wave
reduction in sea-ice
More rain means no drought
Through talik
4. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
Radiative Forcing
Why Water Vapor is not a climate forcing
Shortwave Length
5. The amount of light reflected by an object.
Threshold departures
Positive feedbacks both found in...
Atmospheric Circulation
Albedo
6. Measures input and output.
Strong
Reduction in sea-ice extent
Mass Budget
Absolute thresholds
7. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
El Nino
Positive
In the Arctic where the air is cooler
Ocean-Ice-Atmosphere Interaction
8. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Amount of light actually reaching the Earth
Ice-Ocean Interactions
Depth v Surface
IPCC
9. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Antarctica
75-OC
Negative Ice-Albedo Feedback
Ice in the Arctic
10. he increase of ozone concentration in the atmosphere helps ____ our planet
Air pollution
Warm
Active Layer
Major distinction between Kyoto Protocol and Convention
11. 1.4 USA - 57 m total sea level equivalent
Antarctica
Mass Change
Infrared radiation
Depth v Surface
12. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
30%
Ice/snow
Surface Mass Balance
Arctic Atmosphere
13. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Air pollution
Longwave Radiation
How to define a heatwave
Closed talik
14. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Infrared radiation
GHG
Sea Ice Extent is Changing in Antarctica as well
Types of Albedo
15. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Sea Ice
Climate Change in the Arctic
The cryosphere
Some parts of the planet are dry because of their location
16. 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.
Greenhouse Gases
Negative
reduction in sea-ice
Thermokarst
17. 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.
Thermokarst Lake
Indirect heat wave effect
Strong
Ice/snow
18. Cooler water and drought conditions.
Positive
summer
Ice in the Arctic
La Nia
19. The Earth emits this.
Warm
Longwave Radiation
The Ozone Hole
Ice Sheets
20. Volcanic eruptions - Sunspots - Wobbly Earth
Natural Causes of Warming
Grounding v Surface Melting
Thickness of the active layer and the permafrost depend on this
Affect Floods and Droughts
21. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Ocean water
Normal condition for air
Grounding Lines
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
22. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Ice absorbs
Surface Mass Balance
Sunspots
reduction in sea-ice
23. Melting Point decreases
Air pollution
.75OC/km-1
75-OC
In the Arctic where the air is cooler
24. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Ice in the Arctic
Types of Albedo
Ocean water
25. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Sublimation
Carbon Dioxide
Atmospheric Structure
Ocean water
26. The past climate...for this reason - both keep good records of climate change.
Permafrost Degradation
Ice-Ocean Interactions
Thickness of the active layer and the permafrost depend on this
Archimedes' Principle
27. 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
Through talik
Discontinuous
Once every 4 years.
In the Arctic where the air is cooler
28. How much is the planet really warming?
.7O Celsius over the past century.
Very small portion
Ice/snow
Longwave Radiation
29. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Indirect heat wave effect
Ocean water
Atmospheric Composition?
Sea Ice Extent is Changing in Antarctica as well
30. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stronger
El Nino
air can warm dramatically
IPCC
31. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Why the Arctic climate is special
Permafrost Degradation
Melt
32. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Nitrous Oxide (N2O)
Sublimation
Warm
Permafrost
33. CO2 - CH4 - O3 - H2O - N2O - CFCs
Ice Cap
Earth's tilt
All Greenhouse gases
75-OC
34. 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.
Permafrost
Climate Change in the Arctic
25%
Some regions of the Earth have warmed faster than other regions.
35. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Nitrous Oxide (N2O)
Ice/snow
Hydrological Drought
Ice Discharge
36. What can cause a change in the Earth's climate balance?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Shortwave Length
Grounding Lines
Ice Shelf
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
How the cryosphere is affected by climate change
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Greenland
All Greenhouse gases
38. 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
In the stratosphere.
Cloud Feedbacks
Warm
Reduction in sea-ice extent
39. Where does the ozone protect us?
In the stratosphere.
In the Arctic where the air is cooler
Atmospheric Circulation
Altimetry Pros
40. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
All Greenhouse gases
Ocean water
doubles
41. 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
Ice loss
Talik
Why ice-albedo feedback is a big deal in the Arctic
Altimetry (height)
42. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Contributions to CO2 from different activities
Positive feedbacks both found in...
Discontinuous
Permafrost
43. Radiation absorbed by atmospheric greenhouse gases?
Surface Mass Balance
Very small portion
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Hydrological Drought
44. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Cause of break of inversion layers or decrease in frequency
In the stratosphere.
Importance of ice sheets
Calving
45. Permafrost- A frozen soil
Discontinuous Permafrosrt
Accumulation
Affect Floods and Droughts
Frozen Soil
46. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Heat wave
Atmospheric Composition
Talik
Dynamic thinning
47. A mass of land ice - continental or sub-continental in extent - and thick enough to cover most of the underlying bedrock topography - If you have a warm ocean - it will melt the ice sheet. Its shape is mainly determined by the dynamics of its outward
Thermokarst Lake
Active Layer
Ice Sheets
Agricultural Drought
48. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Greenland
Discontinuous
% of Greenhouse Gases
Arctic Atmosphere
49. x7 smaller - 7m total sea level equivalent.
Troposphere
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Sea-Ice Albedo
Greenland
50. Number of days that exceed a given temperature
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Absolute thresholds
Layers of Earth
Ice Discharge