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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 warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Calving
Active Layer
Sea-Ice Albedo
reduction in sea-ice
2. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Altimetry Pros
Atlantic Thermohaline Circulation
Thermokarst
Why Water Vapor is not a climate forcing
3. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
How to define a heatwave
Radiative Flux
Dynamic thinning
Sea-Ice Albedo
4. Descending Air dry - Convection cells are wet.
Change in vegetation generates a further feedback
Atmospheric Circulation
Ice Motion
Grounding v Surface Melting
5. Is not an externally imposed perturbation to the climate system.
doubles
Ice in the Arctic
Permafrost Degradation
Why Water Vapor is not a climate forcing
6. Set up in 1988 by WMO and UNEP.
Types of Albedo
Open talik
IPCC
Agricultural Drought
7. Surface Mass Balance is of the order of _____ melting is ____ times more.
Amount of light actually reaching the Earth
30%
Ice Sheets
1 m/yr; 10x
8. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Cause of break of inversion layers or decrease in frequency
Arctic Atmosphere
Questions to think about
How a closed talik forms
9. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
How we measure Mass Balance
reduction in sea-ice
Surface Mass Balance
What effects the density
10. Greenhouse gases are mixed in the ____
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ice shelf
30%
Troposphere
11. Frozen +2 years - Few centimeters to 1500 m
Sea ice melt does not change sea level
Contributions to CO2 from different activities
Ocean-Ice-Atmosphere Interaction
Permafrost
12. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Active Layer
Greenhouse Gases
Rainy
Ice Motion
13. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Radiative Forcing
Ice/snow
Surface Mass Balance
In the troposphere that we live in.
14. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Sublimation
Severe coastal erosion
US and precipitation
Thermohaline Circulation Effect
15. On a clear cold day - the thin layer of air hugging the ground is called inversion. This layer is much cooler than the air a few hundred meters above it.
Earth's tilt
Inversion Layer (feedback)
Stronger
Greenland
16. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Atmospheric Composition?
Active Layer
Sea ice melt does not change sea level
Warming; cooling
17. 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.
Change in vegetation generates a further feedback
How we measure Mass Balance
Major distinction between Kyoto Protocol and Convention
Thermokarst
18. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Changes in Arctic sea-ice Extent
Inversion Layer Summer
reduction in sea-ice
Sea Ice Extent is Changing in Antarctica as well
19. 1.4 USA - 57 m total sea level equivalent
Thermokarst
Amount of light actually reaching the Earth
Ice/snow
Antarctica
20. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Through talik
Greenhouse Gases
Heat Source and Pressure
Earth's tilt
21. How often does El Nio occur?
Radiative Forcing
Once every 4 years.
Monthly maximums and minimums
Negative
22. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Greenhouse Gases
Grounding Lines
Climate Change in the Arctic
Methane
23. 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
Indirect heat wave effect
doubles
.75OC/km-1
Ice Sheets
24. Volcanic eruptions - Sunspots - Wobbly Earth
Increases - decreases
Natural Causes of Warming
Ice loss
Sea-Ice Albedo
25. Precipitation intensity will rise ___ for every 1 OC of warming.
Severe coastal erosion
What happens with the Ozone Hole
7%
Altimetry (height)
26. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Contributions to CO2 from different activities
Thermokarst Lake
Natural Causes of Warming
Energy Budget
27. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
How we measure Mass Balance
Ice-Ocean Interactions
Depth v Surface
Ocean water
28. 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
Meteorological Drought
30%
Questions to think about
Once every 4 years.
29. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Time Variable Gravity
Severe coastal erosion
Talik
Normal condition for air
30. Laser radar - H V - Long time series - high accuracy - Density
Inversion Layer (feedback)
Sea ice melt does not change sea level
Altimetry (height)
Melt
31. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Grounding Lines
IPCC
Sea Ice
Altimetry Cons
32. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Longwave Radiation
Global warming and hot nights?
Ice absorbs
Effect of Deforestation on CO-2
33. Clouds 40~90% - Vegetation 10~15%
Types of Albedo
Greenhouse Gases
Ice Sheets
In the troposphere that we live in.
34. 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
Discontinuous
Mass Budget
Methane
35. High vs low
Cloud Feedbacks
Talik
Once every 4 years.
Inversion Layer (feedback)
36. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Wetter; drier
Ozone
Threshold departures
Ice/snow
37. CO2 GHG forcing - H2O - dominant/major GHG
Where rise in OC is greatest
GHG
Why ice-albedo feedback is a big deal in the Arctic
Heat wave
38. Rainy on yearly average. In these regions - rising air predominates.
Deep tropics between 15O N and 15 O S are quite
Atmospheric Circulation
Types of Albedo
Ice Sheets
39. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Greenland
Thickness of the active layer and the permafrost depend on this
Change in vegetation generates a further feedback
Surface Mass Balance
40. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
doubles
Layers of Earth
Questions to think about
Active Layer
41. More common
Snow and snow covered ice absorb
Percentile departures
Inversion Layer Winter
Active Layer
42. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Melt
Precipitation and High Latitudes
air can warm dramatically
Agricultural Drought
43. Cooler water and drought conditions.
Stratospheric Ozone Depletion
La Nia
How we measure Mass Balance
Ice Sheets
44. O The amount of energy moving in the form of photons or other elementary particles at a certain distance from the source per unit of area per second. Area/second
Radiative Flux
Heat wave
Deep tropics between 15O N and 15 O S are quite
Types of Albedo
45. Really measures volume.
Ice Shelf
Altimetry
Precipitation and High Latitudes
Sea Ice
46. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Ozone Hole
Major distinction between Kyoto Protocol and Convention
Dynamic thinning
Dry
47. ~15% of incident solar energy (albedo 85)
Ocean water
Methane
Snow and snow covered ice absorb
7%
48. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Negative
Ice Discharge
Ice shelf
How the cryosphere is affected by climate change
49. Land Based Ecosystems retain ____ CO2.
Troposphere
Heat Source and Pressure
30%
Heat wave
50. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Sea Ice Extent is Changing in Antarctica as well
Affect Floods and Droughts
% of Greenhouse Gases
Atlantic Thermohaline Circulation