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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. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Layers of Earth
Atmospheric Circulation
Accumulation
Stronger
2. 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
Active Layer
Energy Budget
45%
3. CO2 - CH4 - O3 - H2O - N2O - CFCs
Arctic Atmosphere
% of Greenhouse Gases
All Greenhouse gases
Warm
4. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Warm
Ice in the Arctic
Importance of ice sheets
5. 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:
Ozone
Ocean water
Thermohaline Circulation
Change in vegetation generates a further feedback
6. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Atlantic Thermohaline Circulation
Melt
Grounding Lines
Arctic Atmosphere
7. 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
Cloud Feedbacks
Greenland
Radiative Flux
Why ice-albedo feedback is a big deal in the Arctic
8. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
20%
Altimetry Pros
summer
Surface Mass Balance
9. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Wetter; drier
Ozone
Accumulation
Thermokarst
10. 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.
Thermohaline Circulatoin
Inversion Layer (feedback)
Agricultural Drought
Infrared radiation
11. 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.
Ocean water
Change in vegetation generates a further feedback
Permafrost Degradation
Warming; cooling
12. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
75-OC
summer
Wetter; drier
Effect of Deforestation on CO-2
13. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Precipitation and High Latitudes
How a closed talik forms
Carbon Dioxide
Permafrost
14. 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.
How we measure Mass Balance
.75OC/km-1
Severe coastal erosion
reduction in sea-ice
15. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Very small portion
Cloud Feedbacks
reduction in sea-ice
16. 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
Talik
Through talik
Mass Budget
Why the Arctic climate is special
17. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
50%
Ice/snow
Cloud Feedbacks
Average radiative flux reaching the atmosphere
18. Ocean retains ____ CO2
25%
Atmospheric Circulation
Albedo
Altimetry (height)
19. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Ice in the Arctic
Stronger
Thermokarst
El Nio is in the coasts of...
20. Number of days that exceed a given temperature
reduction in sea-ice
Ozone Hole
Absolute thresholds
summer
21. Over the Northern Hemisphere than the tropics.
All Greenhouse gases
Ice Discharge
Where rise in OC is greatest
Ice Cap
22. Melting Point decreases
Albedos of Snow and Ice
Cloud Feedbacks
.75OC/km-1
Ice Discharge
23. 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
Sublimation
Ice Discharge
Dry
Major distinction between Kyoto Protocol and Convention
24. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Today melting ice
air can warm dramatically
How a closed talik forms
Accumulation
25. What can cause a change in the Earth's climate balance?
Accumulation
Cause of break of inversion layers or decrease in frequency
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Albedo
26. A naturally or artificially caused decrease in the thickness and/or areal extent of permafrost - It is caused by the deepening fo the active layer and the thawing of the adjacent permafrost.
Rainy
Wetter; drier
Permafrost Degradation
Change in vegetation generates a further feedback
27. Where do greenhouse gases warm up the Earth?
Positive feedbacks both found in...
Infrared radiation
In the troposphere that we live in.
Ocean water
28. 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
How a closed talik forms
75-OC
Permafrost Degradation
29. 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.
How talik forms under lakes
Meteorological Drought
Albedos of Snow and Ice
Active Layer
30. ~15% of incident solar energy (albedo 85)
30%
Ice Shelf
Dynamic thinning
Snow and snow covered ice absorb
31. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Closed talik
Heat wave
Atmospheric Composition
Melt
32. Changes over time in the highest and lowest single temperature observed during a given month of the year.
What happens with the Ozone Hole
Earth's tilt
Mass Budget
Monthly maximums and minimums
33. Set up in 1988 by WMO and UNEP.
Archimedes' Principle
IPCC
Negative Ice-Albedo Feedback
reduction in sea-ice
34. 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.
Altimetry (height)
Ice-Ocean Interactions
Reduction in sea-ice extent
Percentile departures
35. Ice sheets have a very ____ Albedo
Strong
Grounding v Surface Melting
Sea Ice Extent is Changing in Antarctica as well
Normal condition for air
36. In average: +1% in respect to 100 years ago.
Increases - decreases
Ice Cap
Is precipitation around the world increasing?
20%
37. 1.4 USA - 57 m total sea level equivalent
Energy Budget
Ice shelf
Ice loss
Antarctica
38. Atmosphere retains ____ CO2
Thermohaline Circulation Effect
Accumulation
In the troposphere that we live in.
45%
39. Amount of light absorbed by surface
Thermohaline Circulation
50%
Atmospheric Composition
Wetter; drier
40. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
air can warm dramatically
Hydrological Drought
Ice-Ocean Interactions
41. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
In the troposphere that we live in.
Open talik
Shortwave Length
Negative Ice-Albedo Feedback
42. 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
Why Water Vapor is not a climate forcing
What effects the density
Atlantic Thermohaline Circulation
Agricultural Drought
43. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Atmospheric Circulation
Thermohaline Circulatoin
Thermohaline Circulation
44. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Rainy
Ice Discharge
Thermohaline Circulatoin
30%
45. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
30%
Inversion Layer Summer
Snow and snow covered ice absorb
46. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
IN the last 2 decades what we've seen
Air pollution
Radiative Flux
Ocean-Ice-Atmosphere Interaction
47. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
IN the last 2 decades what we've seen
Sea Ice Extent is Changing in Antarctica as well
How a closed talik forms
Ocean-Ice-Atmosphere Interaction
48. 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.
Methane
Surface Mass Balance
Ice loss
Radiative Flux
49. 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
Thermokarst
Ocean water
Questions to think about
Effect of Deforestation on CO-2
50. A dome shaped cover of perennial ice and snow.
Ice Sheets
Troposphere
Ice Cap
Global warming and hot nights?