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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 last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Stronger
Negative Ice-Albedo Feedback
Grounding Lines
Inversion Layer (feedback)
2. 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.
What effects the density
Antarctica
Threshold departures
Inversion Layer (feedback)
3. 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
Positive feedbacks both found in...
What happens with the Ozone Hole
45%
Questions to think about
4. Unfrozen ground that is found within a mass of permafrost
Closed talik
Thermokarst
US and precipitation
Stratospheric Ozone Depletion
5. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Mass Balance
Layers of Earth
Inversion Layer (feedback)
Severe coastal erosion
6. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
The Ozone Hole
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Positive
Greenhouse Gases
7. Is not an externally imposed perturbation to the climate system.
Some regions of the Earth have warmed faster than other regions.
Why Water Vapor is not a climate forcing
Dynamic thinning
Altimetry
8. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Permafrost
Affect Floods and Droughts
Stratospheric Ozone Depletion
Grounding Lines
9. Holds unique and key information - Are highly interconnected - Respond and drive climate change - Are the largest freshwater reservoirs of the planet - Ice cores tell us that in climate records - nothing is regular and ice sheet plays major role.
Ice Sheets
doubles
Ozone Hole
Thinner atmosphere
10. 85%
Increases - decreases
Surface Mass Balance
Melt
Sea-Ice Albedo
11. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Contributions to CO2 from different activities
Climate Change in the Arctic
Sunspots
La Nia
12. The order of 1 m/year. Melting is ten times more.
Stratospheric Ozone Depletion
Surface Mass Balance
.7O Celsius over the past century.
Percentile departures
13. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
50%
Heat Source and Pressure
More rain means no drought
Stronger
14. 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.
Today melting ice
Natural Causes of Warming
Ice-Ocean Interactions
What happens with the Ozone Hole
15. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Ice Discharge
Cloud Feedbacks
Agricultural Drought
Melt
16. Trade winds blow from East to West - Pool of warm water in the west - Meanwhile deep colder water rises up in the Eastern Pacific - The sea level is ~ 50-60 cm higher in Western Pacific (Indonesia) than in the Eastern Pacific (South America/Peru) -
Natural Causes of Warming
Once every 4 years.
Normal condition for air
Thermokarst Lake
17. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Layers of Earth
What happens with the Ozone Hole
Negative Ice-Albedo Feedback
% of Greenhouse Gases
18. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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19. 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!
Grounding v Surface Melting
Antarctica
How we measure Mass Balance
Amount of light actually reaching the Earth
20. Over the Northern Hemisphere than the tropics.
Greenland
Where rise in OC is greatest
Frozen Soil
Rainy
21. Greenhouse gases are mixed in the ____
air can warm dramatically
Percentile departures
Natural Causes of Warming
Troposphere
22. Number of days that exceed a given temperature
Thermokarst
Sea Ice Extent is Changing in Antarctica as well
Absolute thresholds
Albedo
23. Melting Point decreases
Negative
.75OC/km-1
Absolute thresholds
Inversion Layer (feedback)
24. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Melt
How a closed talik forms
Change in vegetation generates a further feedback
Monthly maximums and minimums
25. 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.
Major distinction between Kyoto Protocol and Convention
25%
75-OC
Radiative Flux
26. 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
Earth's tilt
Altimetry Pros
70%
Stronger
27. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
1 m/yr; 10x
Thermokarst
Depth v Surface
Importance of ice sheets
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
Strong
Inversion Layer Winter
Greenland
29. 1. They are the largest contributor to sea level rise 2. Can affect the thermohaline circulation (mainly in Greenland) 3. Are directly connected to climate change
Sea ice melt does not change sea level
In the stratosphere.
Importance of ice sheets
Heat wave
30. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Greenhouse Gases
Thermokarst Lake
Accumulation
.7O Celsius over the past century.
31. he increase of ozone concentration in the atmosphere helps ____ our planet
Greenhouse Gases
Warm
Reduction in sea-ice extent
Mass Change
32. In _______ - the inversions are less frequent and weaker in the Arctic.
Radiative Forcing
Active Layer
summer
Negative Ice-Albedo Feedback
33. A thick - floating slab of freshwater ice extending from coast to coast.
Ice shelf
Reduction in sea-ice extent
Arctic Atmosphere
La Nia
34. Grace - Tells us how much mass change we have - M - This is the measure of gravity (gives us the mass) - Directly measure mass change - Poor resolution
Mass Change
Altimetry Cons
Heat wave
20%
35. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
70%
Black Carbon
Frozen Soil
Inversion Layer Summer
36. Number of days that land among the hottest of all days in that month's long-term record.
Sea Ice
Agricultural Drought
Percentile departures
Time Variable Gravity
37. How often does El Nio occur?
Once every 4 years.
Ice/snow
Ice Sheets
Surface Mass Balance
38. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Why Water Vapor is not a climate forcing
Permafrost
air can warm dramatically
Antarctica
39. Forms in a mosaic of favoured locations.
Discontinuous Permafrosrt
Sea-Ice Albedo
How a closed talik forms
Sunspots
40. A dome shaped cover of perennial ice and snow.
Ice Cap
Arctic Atmosphere
Nitrous Oxide (N2O)
Grounding Lines
41. Climate models suggest once the sea ice cover is thinned sufficiently - a strong kick from natural variability could initiate a rapid slide towards ice-free conditions in the summer.
Ocean-Ice-Atmosphere Interaction
Threshold departures
Changes in Arctic sea-ice Extent
Precipitation and High Latitudes
42. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Altimetry (height)
Meteorological Drought
50%
Greenhouse Gases
43. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Some parts of the planet are dry because of their location
Sea Ice Extent is Changing in Antarctica as well
Accumulation
Open talik
44. In ________- inversion layer is more common in the Arctic
winter
Ice Motion
Permafrost
Ocean water
45. Like weighing oneself on the scale.
Heat wave
Time Variable Gravity
Strong
Negative
46. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Once every 4 years.
Atlantic Thermohaline Circulation
Archimedes' Principle
winter
47. Number of days when temperatures climb above average by a fixed amount.
Methane
Heat wave
Average radiative flux reaching the atmosphere
Threshold departures
48. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Ice loss
Open talik
Surface Mass Balance
Ice Cap
49. 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.
Mass Change
Negative Ice-Albedo Feedback
Dynamic thinning
Greenland
50. The Earth emits this.
75-OC
Atmospheric Structure
Longwave Radiation
Warming; cooling