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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. CO2 GHG forcing - H2O - dominant/major GHG
Carbon Dioxide
Monthly maximums and minimums
GHG
Greenland
2. Ocean retains ____ CO2
Greenhouse Gases
Arctic Atmosphere
25%
50%
3. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
La Nia
Rainy
Wetter; drier
Thermohaline Circulation Effect
4. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Altimetry
Sea ice melt does not change sea level
Surface Mass Balance
US and precipitation
5. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
Depth v Surface
Active Layer
Meteorological Drought
Questions to think about
6. 240 w/m squared
Sublimation
Amount of light actually reaching the Earth
Open talik
Some parts of the planet are dry because of their location
7. 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
reduction in sea-ice
Permafrost
In the Arctic where the air is cooler
Positive feedbacks both found in...
8. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
Arctic Atmosphere
Sea Ice Extent is Changing in Antarctica as well
Accumulation
9. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
Discontinuous Permafrosrt
Ozone
25%
10. 85%
Natural Causes of Warming
Sea-Ice Albedo
Snow and snow covered ice absorb
How talik forms under lakes
11. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Thermohaline Circulation
Rainy
Sea Ice
12. Total absorbed solar radiation
70%
Ice Sheets
Strong
Melt
13. The Earth emits this.
Absolute thresholds
Closed talik
Cloud Feedbacks
Longwave Radiation
14. How much is the planet really warming?
.7O Celsius over the past century.
25%
Cloud Feedbacks
30%
15. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Sea Ice Extent is Changing in Antarctica as well
Sea ice melt does not change sea level
Dry
In the Arctic where the air is cooler
16. Where does the ozone protect us?
In the stratosphere.
Altimetry Cons
Global warming and hot nights?
More rain means no drought
17. 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.
Climate Change in the Arctic
45%
Greenland
Today melting ice
18. 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
Infrared radiation
Dry
summer
1 m/yr; 10x
19. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Heat wave
Questions to think about
The Ozone Hole
Ocean water
20. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
reduction in sea-ice
Surface Mass Balance
El Nio is in the coasts of...
Heat Source and Pressure
21. Warming- positive feedback - Cooling- negative feedback.
Some parts of the planet are dry because of their location
Snow and snow covered ice absorb
Ice-Albedo
Thermohaline Circulatoin
22. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Altimetry Cons
Surface Mass Balance
Some parts of the planet are dry because of their location
Mass Balance
23. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Ocean water
Radiative Forcing
45%
Where rise in OC is greatest
24. 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.
La Nia
Sea-Ice Albedo
Major distinction between Kyoto Protocol and Convention
Climate Change in the Arctic
25. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Thinner atmosphere
Severe coastal erosion
Why the Arctic climate is special
Agricultural Drought
26. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Where rise in OC is greatest
Negative Ice-Albedo Feedback
Percentile departures
Sublimation
27. Volcanic eruptions - Sunspots - Wobbly Earth
Energy Budget
Radiative Forcing
Natural Causes of Warming
Climate Change in the Arctic
28. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Once every 4 years.
Natural Causes of Warming
The Ozone Hole
Heat wave
29. Descending Air dry - Convection cells are wet.
45%
Greenhouse Gases
Inversion Layer (feedback)
Atmospheric Circulation
30. Less frequent and weaker
Ice-Ocean Interactions
In the troposphere that we live in.
How we measure Mass Balance
Inversion Layer Summer
31. Measures input and output.
Mass Budget
Warming; cooling
Accumulation
Dynamic thinning
32. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Shortwave Length
Depth v Surface
Once every 4 years.
Global warming and hot nights?
33. Like weighing oneself on the scale.
Today melting ice
Time Variable Gravity
Atmospheric Composition
Altimetry (height)
34. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
75-OC
Sea Ice Extent is Changing in Antarctica as well
45%
.75OC/km-1
35. 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
Major distinction between Kyoto Protocol and Convention
How a closed talik forms
How the cryosphere is affected by climate change
Surface Mass Balance
36. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Infrared radiation
Hydrological Drought
Ocean-Ice-Atmosphere Interaction
air can warm dramatically
37. 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
Some parts of the planet are dry because of their location
Thinner atmosphere
Importance of ice sheets
Radiative Forcing
38. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Altimetry Pros
How to define a heatwave
Rainy
Methane
39. Occurs when there is not enough water available for a particular crop to grow at a particular time.Typically seen after!meteorological drought (when rainfall decreases) but before a hydrological drought
Questions to think about
Methane
Cloud Feedbacks
Agricultural Drought
40. Melting Point decreases
.75OC/km-1
Agricultural Drought
Permafrost
Ice/snow
41. Greenhouse gases are a ___ portion of the atmosphere
Grounding Lines
Very small portion
Ice in the Arctic
Ocean water
42. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Ice Sheets
What happens with the Ozone Hole
Open talik
25%
43. Soil at or below the freezing point of water for two or more years - Can be: Terrestrial - Subsea - Can be: Continuous: exists across a landscape as an unbroken layer. More than 90% is frozen - Discontinuous
Permafrost
Ice shelf
Inversion Layer Summer
Today melting ice
44. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Mass Balance
Monthly maximums and minimums
Thermokarst Lake
Troposphere
45. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Dynamic thinning
Ice shelf
Permafrost Degradation
Ocean water
46. Is best viewed as a combination of...- Natural Variability - Associated with atmospheric circulation patterns - Growing Radiative Forcing - Associated with rising concentrations of atmospheric greenhouse gases - Strongly suggests a human influence.
Absolute thresholds
Major distinction between Kyoto Protocol and Convention
Altimetry Cons
Ice loss
47. 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
20%
Longwave Radiation
48. 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
Heat wave
Atmospheric Composition?
Affect Floods and Droughts
Mass Change
49. The amount of light reflected by an object.
Atmospheric Composition?
Natural Causes of Warming
Albedo
Negative
50. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Meteorological Drought
Permafrost Degradation
Atmospheric Structure
Stratospheric Ozone Depletion