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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. Greenhouse gases are mixed in the ____
air can warm dramatically
Heat wave
75-OC
Troposphere
2. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Methane
Open talik
All Greenhouse gases
How a closed talik forms
3. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Sea ice melt does not change sea level
70%
Radiative Forcing
Time Variable Gravity
4. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Where rise in OC is greatest
Increases - decreases
Atmospheric Structure
Ice-Ocean Interactions
5. 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
Where rise in OC is greatest
Thinner atmosphere
Methane
Carbon Dioxide
6. Where does the ozone protect us?
Inversion Layer (feedback)
Thermokarst
50%
In the stratosphere.
7. 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.
Negative Ice-Albedo Feedback
Thickness of the active layer and the permafrost depend on this
Heat Source and Pressure
Atmospheric Structure
8. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Black Carbon
Atmospheric Structure
GHG
Ice Shelf
9. They saw a massive thinning of the ice where it enters into the ocean - This is due to the pronounced melting of the ice once it is in contact with the ocean. Melt rates of 25 m/year near the grounding lines and more than 10 m/year on average.
Antarctica
Ice-Ocean Interactions
Accumulation
The cryosphere
10. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Surface Mass Balance
air can warm dramatically
Effect of Deforestation on CO-2
Black Carbon
11. Summer increase in cloud cover - Winter decrease in cloud cover.
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12. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Longwave Radiation
IPCC
How to define a heatwave
Thermokarst Lake
13. Unfrozen ground that is found within a mass of permafrost
Thermohaline Circulation
Closed talik
Sea-Ice Albedo
Percentile departures
14. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Depth v Surface
Stronger
Time Variable Gravity
Stratospheric Ozone Depletion
15. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Nitrous Oxide (N2O)
winter
GHG
Global warming and hot nights?
16. Forms in a mosaic of favoured locations.
Radiative Forcing
Stronger
Discontinuous Permafrosrt
Surface Mass Balance
17. Surface Mass Balance is of the order of _____ melting is ____ times more.
IN the last 2 decades what we've seen
1 m/yr; 10x
Mass Change
Why the Arctic climate is special
18. 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
How talik forms under lakes
Altimetry Pros
50%
Questions to think about
19. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
All Greenhouse gases
Time Variable Gravity
Global warming and hot nights?
Stratospheric Ozone Depletion
20. Number of days that exceed a given temperature
US and precipitation
Change in vegetation generates a further feedback
GHG
Absolute thresholds
21. Amount of light absorbed by surface
doubles
50%
Why the Arctic climate is special
Wetter; drier
22. 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
Grounding Lines
The cryosphere
What happens with the Ozone Hole
Thermokarst Lake
23. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Sublimation
% of Greenhouse Gases
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Once every 4 years.
24. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Radiative Flux
Open talik
US and precipitation
Hydrological Drought
25. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Archimedes' Principle
Absolute thresholds
Greenhouse Gases
The cryosphere
26. LW - SW - 55% absorbed by surface
Mass Change
Energy Budget
doubles
Dynamic thinning
27. Rainy on yearly average. In these regions - rising air predominates.
Cloud Feedbacks
Inversion Layer Summer
Deep tropics between 15O N and 15 O S are quite
La Nia
28. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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29. 85%
.75OC/km-1
Thermokarst
Stronger
Sea-Ice Albedo
30. 240 w/m squared
1 m/yr; 10x
Amount of light actually reaching the Earth
Thermohaline Circulation
Thinner atmosphere
31. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Ice Sheets
Methane
Thermohaline Circulation Effect
Today melting ice
32. Really measures volume.
Active Layer
Accumulation
Rainy
Altimetry
33. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Negative
Ice shelf
Ice Sheets
34. 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.
Ice shelf
Thermohaline Circulation Effect
Altimetry (height)
Surface Mass Balance
35. 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.
Affect Floods and Droughts
What effects the density
Nitrous Oxide (N2O)
Ice Discharge
36. 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
Reduction in sea-ice extent
doubles
Ice Sheets
Average radiative flux reaching the atmosphere
37. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Importance of ice sheets
Monthly maximums and minimums
Hydrological Drought
Albedo
38. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Carbon Dioxide
Hydrological Drought
Thermohaline Circulation
Mass Budget
39. The buoyant force is equal to the weight of the displaced water.
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40. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Atmospheric Circulation
Hydrological Drought
Ice-Albedo
Sea ice melt does not change sea level
41. Industrial product - 300 ppb (parts per billion)
Grounding v Surface Melting
Sea Ice Extent is Changing in Antarctica as well
Nitrous Oxide (N2O)
Natural Causes of Warming
42. Set up in 1988 by WMO and UNEP.
Ice/snow
Energy Budget
IPCC
Atmospheric Composition?
43. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
More rain means no drought
Ocean water
Absolute thresholds
Ice absorbs
44. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Dynamic thinning
More rain means no drought
Thermokarst
reduction in sea-ice
45. 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
Importance of ice sheets
Rainy
Global warming and hot nights?
46. Laser radar - H V - Long time series - high accuracy - Density
Altimetry (height)
What happens with the Ozone Hole
Black Carbon
Ice in the Arctic
47. Taliks are found under lakes because of the ability of water to store and vertically transfer heat energy - Vertical extent of the taliks found under lakes is related to the depth and volume of the overlying water body.
7%
How talik forms under lakes
Heat wave
doubles
48. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Amount of light actually reaching the Earth
Heat wave
Infrared radiation
Average radiative flux reaching the atmosphere
49. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Sea ice melt does not change sea level
Energy Budget
Depth v Surface
50. In average: +1% in respect to 100 years ago.
What effects the density
Is precipitation around the world increasing?
El Nio is in the coasts of...
Sunspots