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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. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Percentile departures
Open talik
Methane
Permafrost Degradation
2. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Greenland
Ocean water
20%
Stratospheric Ozone Depletion
3. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Sublimation
Ice-Ocean Interactions
Contributions to CO2 from different activities
Ozone
4. Melting Point decreases
.75OC/km-1
Why Water Vapor is not a climate forcing
Types of Albedo
How we measure Mass Balance
5. 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
Grounding Lines
Why the Arctic climate is special
Ice-Albedo
Depth v Surface
6. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Dynamic thinning
Calving
Positive
Time Variable Gravity
7. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Grounding Lines
summer
El Nio is in the coasts of...
Sea Ice Extent is Changing in Antarctica as well
8. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ozone
winter
Radiative Flux
Calving
9. Number of days when temperatures climb above average by a fixed amount.
Some parts of the planet are dry because of their location
Absolute thresholds
Ice Sheets
Threshold departures
10. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Heat Source and Pressure
Open talik
Ice in the Arctic
Ozone Hole
11. 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
Global warming and hot nights?
Troposphere
Wetter; drier
12. 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.
Surface Mass Balance
All Greenhouse gases
reduction in sea-ice
Ocean-Ice-Atmosphere Interaction
13. The past climate...for this reason - both keep good records of climate change.
Thermohaline Circulatoin
Today melting ice
Thickness of the active layer and the permafrost depend on this
% of Greenhouse Gases
14. 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.
Change in vegetation generates a further feedback
30%
Sea ice melt does not change sea level
Inversion Layer (feedback)
15. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
Ice in the Arctic
Sea-Ice Albedo
La Nia
16. The high pressure decreases the melting point and favors melting - Melt water being less dense rises along the water column along the ice shelf bottom and may either escape the cavity or refreeze at some intermediate depth. Melting point decreases:
Altimetry Cons
Dynamic thinning
Thermohaline Circulation
Mass Change
17. 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.
Talik
Negative Ice-Albedo Feedback
More rain means no drought
doubles
18. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
In the troposphere that we live in.
Altimetry Cons
How a closed talik forms
Active Layer
19. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
How to define a heatwave
Global warming and hot nights?
Sea-Ice Albedo
How we measure Mass Balance
20. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Thermokarst Lake
The cryosphere
Wetter; drier
Air pollution
21. Surface Mass Balance is of the order of _____ melting is ____ times more.
Ice absorbs
1 m/yr; 10x
Natural Causes of Warming
Agricultural Drought
22. Set up in 1988 by WMO and UNEP.
Change in vegetation generates a further feedback
Monthly maximums and minimums
IPCC
Natural Causes of Warming
23. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Indirect heat wave effect
Stratospheric Ozone Depletion
Effect of Deforestation on CO-2
air can warm dramatically
24. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Why ice-albedo feedback is a big deal in the Arctic
GHG
Time Variable Gravity
Heat Source and Pressure
25. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Agricultural Drought
Atmospheric Composition
Increases - decreases
Ice Motion
26. 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
Open talik
How the cryosphere is affected by climate change
Positive feedbacks both found in...
Ice Motion
27. Where do greenhouse gases warm up the Earth?
Discontinuous Permafrosrt
In the troposphere that we live in.
Why the Arctic climate is special
Dry
28. 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
Types of Albedo
Mass Budget
Permafrost
Altimetry
29. 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
Archimedes' Principle
Why ice-albedo feedback is a big deal in the Arctic
Hydrological Drought
30. Atmosphere retains ____ CO2
45%
Mass Change
winter
Importance of ice sheets
31. O Climate change in the Arctic is occurring now - Changes have been huge already
Archimedes' Principle
Today melting ice
All Greenhouse gases
Ice Shelf
32. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Surface Mass Balance
Antarctica
Grounding Lines
Shortwave Length
33. Clouds 40~90% - Vegetation 10~15%
How we measure Mass Balance
Types of Albedo
Active Layer
Meteorological Drought
34. Radiation absorbed by atmospheric greenhouse gases?
Mass Balance
Affect Floods and Droughts
El Nino
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
35. Where does the ozone protect us?
30%
Talik
In the stratosphere.
Thermokarst Lake
36. The large-scale ocean circulation that moves water between the deep and surface ocean which effects salinity and temperature change - Supplies heat to the polar-regions.
Is precipitation around the world increasing?
Thermohaline Circulation Effect
Ice Cap
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
37. 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
Questions to think about
Why ice-albedo feedback is a big deal in the Arctic
Through talik
Dry
38. 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
Dry
Ice-Ocean Interactions
Warm
Permafrost
39. Number of days that exceed a given temperature
Reduction in sea-ice extent
Time Variable Gravity
Severe coastal erosion
Absolute thresholds
40. Industrial product - 300 ppb (parts per billion)
Nitrous Oxide (N2O)
Ozone Hole
Arctic Atmosphere
Longwave Radiation
41. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Ice absorbs
Why Water Vapor is not a climate forcing
Rainy
Indirect heat wave effect
42. 1.4 USA - 57 m total sea level equivalent
Antarctica
70%
Precipitation and High Latitudes
Grounding Lines
43. South polar vortex - Temperatures drop below 80O Celsius in the lower stratosphere - At these temperatures the chemicals in the stratosphere freeze and form Polar Stratospheric Clouds (PSCS) - These increase the concentration of CFCs in turn destroyi
In the stratosphere.
What happens with the Ozone Hole
Sublimation
20%
44. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Ice/snow
Ocean water
Surface Mass Balance
IN the last 2 decades what we've seen
45. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Nitrous Oxide (N2O)
Grounding Lines
Stronger
Layers of Earth
46. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Importance of ice sheets
Average radiative flux reaching the atmosphere
summer
Permafrost Degradation
47. How often does El Nio occur?
Once every 4 years.
Grounding Lines
Percentile departures
Ozone Hole
48. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Through talik
Negative
Surface Mass Balance
Thinner atmosphere
49. Greenhouse gases are a ___ portion of the atmosphere
Questions to think about
Very small portion
Ice-Ocean Interactions
Where rise in OC is greatest
50. 10 : 1 - grounding ; surface
Is precipitation around the world increasing?
45%
Surface Mass Balance
Grounding v Surface Melting