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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. Number of days when temperatures climb above average by a fixed amount.
Threshold departures
Stratospheric Ozone Depletion
What happens with the Ozone Hole
Major distinction between Kyoto Protocol and Convention
2. Less frequent and weaker
Discontinuous Permafrosrt
IN the last 2 decades what we've seen
Inversion Layer Summer
Accumulation
3. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
.75OC/km-1
Discontinuous
Radiative Flux
Negative
4. Amount of light absorbed by surface
Longwave Radiation
1 m/yr; 10x
El Nio is in the coasts of...
50%
5. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
Some parts of the planet are dry because of their location
Greenhouse Gases
Mass Balance
6. Radiation absorbed by atmospheric greenhouse gases?
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
45%
Absolute thresholds
Infrared radiation
7. ~10% of incident solar energy (albedo 90)
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
75-OC
El Nio is in the coasts of...
Ice absorbs
8. Refers to the irregular warming in the Sea Surface Temperatures (SST) from the coasts of Peru and Ecuador to the equatorial central Pacific - the Southern Oscillation
Change in vegetation generates a further feedback
El Nino
reduction in sea-ice
The Ozone Hole
9. 240 w/m squared
Amount of light actually reaching the Earth
Snow and snow covered ice absorb
Mass Change
Positive
10. Industrial product - 300 ppb (parts per billion)
45%
Through talik
Ocean water
Nitrous Oxide (N2O)
11. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Methane
Grounding Lines
Altimetry (height)
Troposphere
12. x7 smaller - 7m total sea level equivalent.
Mass Balance
Warm
Changes in Arctic sea-ice Extent
Greenland
13. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Grounding Lines
Layers of Earth
Sea ice melt does not change sea level
Some parts of the planet are dry because of their location
14. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Sea Ice Extent is Changing in Antarctica as well
Thermokarst
Greenland
Radiative Forcing
15. Where do greenhouse gases warm up the Earth?
Ice Motion
Heat wave
In the troposphere that we live in.
Hydrological Drought
16. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
How the cryosphere is affected by climate change
Snow and snow covered ice absorb
Discontinuous
Surface Mass Balance
17. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Arctic Atmosphere
Dynamic thinning
Longwave Radiation
Closed talik
18. The Earth emits this.
Thinner atmosphere
Surface Mass Balance
Ice shelf
Longwave Radiation
19. Forms in a mosaic of favoured locations.
Discontinuous Permafrosrt
Increases - decreases
Importance of ice sheets
Why ice-albedo feedback is a big deal in the Arctic
20. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
air can warm dramatically
Monthly maximums and minimums
Discontinuous
Active Layer
21. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
Some parts of the planet are dry because of their location
Thermohaline Circulation Effect
Melt
Atmospheric Structure
22. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Atmospheric Structure
Carbon Dioxide
Discontinuous Permafrosrt
23. 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
Percentile departures
Atmospheric Structure
Reduction in sea-ice extent
Heat wave
24. Precipitation intensity will rise ___ for every 1 OC of warming.
Heat wave
7%
Inversion Layer Winter
Atmospheric Circulation
25. Total absorbed solar radiation
Accumulation
Normal condition for air
70%
Surface Mass Balance
26. 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.
In the troposphere that we live in.
Thermohaline Circulation
Nitrous Oxide (N2O)
Inversion Layer (feedback)
27. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Altimetry Cons
US and precipitation
Is precipitation around the world increasing?
La Nia
28. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Mass Change
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
7%
29. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
In the Arctic where the air is cooler
Stratospheric Ozone Depletion
Change in vegetation generates a further feedback
30. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
IN the last 2 decades what we've seen
Positive feedbacks both found in...
Earth's tilt
Atmospheric Composition?
31. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Atlantic Thermohaline Circulation
Indirect heat wave effect
Energy Budget
32. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Thermohaline Circulation
El Nio is in the coasts of...
Deep tropics between 15O N and 15 O S are quite
33. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Radiative Flux
30%
air can warm dramatically
Changes in Arctic sea-ice Extent
34. LW - SW - 55% absorbed by surface
Ozone Hole
Ocean water
Energy Budget
Open talik
35. 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
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Wetter; drier
Energy Budget
Precipitation and High Latitudes
36. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Discontinuous
Open talik
Grounding Lines
Albedos of Snow and Ice
37. Really measures volume.
Frozen Soil
30%
Altimetry
.75OC/km-1
38. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Atmospheric Composition
Greenhouse Gases
Ice-Ocean Interactions
Effect of Deforestation on CO-2
39. Clouds 40~90% - Vegetation 10~15%
Types of Albedo
Methane
Grounding Lines
air can warm dramatically
40. 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!
30%
Time Variable Gravity
Antarctica
Surface Mass Balance
41. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Monthly maximums and minimums
Ozone Hole
Today melting ice
Surface Mass Balance
42. The buoyant force is equal to the weight of the displaced water.
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43. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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44. Is not an externally imposed perturbation to the climate system.
Agricultural Drought
Altimetry
Why Water Vapor is not a climate forcing
Very small portion
45. The order of 1 m/year. Melting is ten times more.
Inversion Layer Summer
Hydrological Drought
Sunspots
Surface Mass Balance
46. Warming- positive feedback - Cooling- negative feedback.
Dry
Greenland
Ice-Albedo
Frozen Soil
47. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
Ice in the Arctic
Atmospheric Composition?
Active Layer
Indirect heat wave effect
48. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Severe coastal erosion
Ice Sheets
Monthly maximums and minimums
Inversion Layer (feedback)
49. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
How we measure Mass Balance
25%
Average radiative flux reaching the atmosphere
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
50. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Percentile departures
Altimetry Pros
7%
Methane