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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
Surface Mass Balance
Ice Sheets
Closed talik
Methane
2. 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
Questions to think about
Albedos of Snow and Ice
Altimetry Pros
Open talik
3. Less frequent and weaker
Inversion Layer Summer
20%
Changes in Arctic sea-ice Extent
Ice shelf
4. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Positive feedbacks both found in...
Inversion Layer (feedback)
Permafrost
How a closed talik forms
5. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Melt
Ice in the Arctic
Heat wave
6. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Surface Mass Balance
Severe coastal erosion
Through talik
7. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Ice loss
.7O Celsius over the past century.
Shortwave Length
Grounding Lines
8. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
La Nia
Ocean water
Why ice-albedo feedback is a big deal in the Arctic
Ice/snow
9. LW - SW - 55% absorbed by surface
Why the Arctic climate is special
% of Greenhouse Gases
What effects the density
Energy Budget
10. Cooler water and drought conditions.
Changes in Arctic sea-ice Extent
La Nia
summer
Arctic Atmosphere
11. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Wetter; drier
Climate Change in the Arctic
Ice Sheets
Ice in the Arctic
12. ~15% of incident solar energy (albedo 85)
Greenland
Changes in Arctic sea-ice Extent
Snow and snow covered ice absorb
Mass Balance
13. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Discontinuous
Air pollution
Climate Change in the Arctic
Altimetry Cons
14. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Some parts of the planet are dry because of their location
All Greenhouse gases
Melt
15. Where does the ozone protect us?
GHG
Importance of ice sheets
Very small portion
In the stratosphere.
16. Really measures volume.
Altimetry
Antarctica
Longwave Radiation
Effect of Deforestation on CO-2
17. Measures input and output.
Mass Budget
Active Layer
Calving
Sea ice melt does not change sea level
18. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Troposphere
20%
Sea Ice
Mass Budget
19. 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.
Inversion Layer (feedback)
Atmospheric Structure
Antarctica
Greenhouse Gases
20. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Wetter; drier
Sublimation
50%
Shortwave Length
21. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Strong
Today melting ice
Rainy
50%
22. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Severe coastal erosion
Atmospheric Composition?
Albedo
More rain means no drought
23. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
GHG
Average radiative flux reaching the atmosphere
20%
Deep tropics between 15O N and 15 O S are quite
24. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Dynamic thinning
All Greenhouse gases
Layers of Earth
air can warm dramatically
25. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Longwave Radiation
The cryosphere
Natural Causes of Warming
26. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Negative
Discontinuous
What effects the density
Ocean water
27. 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
Carbon Dioxide
Global warming and hot nights?
Changes in Arctic sea-ice Extent
28. High cloud has a _____ effect and cool cloud has a ____ effect
Ocean water
Radiative Forcing
Warming; cooling
Once every 4 years.
29. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Global warming and hot nights?
Dynamic thinning
Why Water Vapor is not a climate forcing
In the troposphere that we live in.
30. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Grounding Lines
Why ice-albedo feedback is a big deal in the Arctic
doubles
31. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Hydrological Drought
The cryosphere
How a closed talik forms
Surface Mass Balance
32. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
How a closed talik forms
75-OC
Frozen Soil
Active Layer
33. Ice sheets have a very ____ Albedo
Radiative Flux
Methane
Archimedes' Principle
Strong
34. Summer increase in cloud cover - Winter decrease in cloud cover.
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35. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Sunspots
What effects the density
Through talik
Methane
36. High vs low
Cloud Feedbacks
All Greenhouse gases
Altimetry (height)
Ozone
37. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Thermohaline Circulation Effect
Methane
Heat Source and Pressure
Thickness of the active layer and the permafrost depend on this
38. The buoyant force is equal to the weight of the displaced water.
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39. Arctic warms faster than other parts of the globe in response to a given increase in greenhouse gasses - More direct route to warming - In the Arctic a greater fraction of any increase in radiation absorbed by the surface goes directly into warming t
Why the Arctic climate is special
Energy Budget
Global warming and hot nights?
Change in vegetation generates a further feedback
40. Greenhouse gases are a ___ portion of the atmosphere
Very small portion
Discontinuous Permafrosrt
Why Water Vapor is not a climate forcing
Radiative Flux
41. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Change in vegetation generates a further feedback
45%
Stratospheric Ozone Depletion
Melt
42. O Climate change in the Arctic is occurring now - Changes have been huge already
Infrared radiation
7%
Today melting ice
Threshold departures
43. Atmosphere retains ____ CO2
7%
30%
Thermohaline Circulatoin
45%
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.
GHG
Troposphere
Thermokarst
Permafrost Degradation
45. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Rainy
Grounding Lines
Very small portion
Calving
46. The amount of light reflected by an object.
Atlantic Thermohaline Circulation
Albedo
Ocean water
Depth v Surface
47. Greenhouse gases are mixed in the ____
Heat wave
Troposphere
Thinner atmosphere
La Nia
48. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Amount of light actually reaching the Earth
Radiative Forcing
Through talik
Positive
49. Wet gets _____ - dry gets ____ - Wet - 50ON (sub polar) Canada - N Europe - Russia - Tropical area- monsoon (rainforest) - Drier - Subtropics - Australia - S. Africa - Mediterranean - Caribbean - Mexico - SW US
Atmospheric Structure
US and precipitation
Wetter; drier
Greenhouse Gases
50. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Threshold departures
Methane
Cloud Feedbacks
% of Greenhouse Gases