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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. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Monthly maximums and minimums
How a closed talik forms
Altimetry Cons
Average radiative flux reaching the atmosphere
2. High vs low
Cloud Feedbacks
Permafrost
IPCC
Calving
3. Like weighing oneself on the scale.
Sea Ice
The Ozone Hole
The cryosphere
Time Variable Gravity
4. In _______ - the inversions are less frequent and weaker in the Arctic.
Percentile departures
summer
Ice Sheets
Inversion Layer (feedback)
5. 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
Monthly maximums and minimums
Ozone Hole
Dry
Ocean water
6. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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7. Melting Point decreases
Greenland
Ozone
.75OC/km-1
Discontinuous
8. How much is the planet really warming?
Very small portion
75-OC
.7O Celsius over the past century.
IN the last 2 decades what we've seen
9. Greenhouse gases are mixed in the ____
Shortwave Length
Troposphere
Wetter; drier
Talik
10. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Thermokarst
Heat Source and Pressure
reduction in sea-ice
Why Water Vapor is not a climate forcing
11. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Ice Shelf
Questions to think about
Severe coastal erosion
Shortwave Length
12. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Agricultural Drought
Major distinction between Kyoto Protocol and Convention
Precipitation and High Latitudes
Troposphere
13. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Heat Source and Pressure
Grounding v Surface Melting
Depth v Surface
Thermohaline Circulation
14. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
El Nio is in the coasts of...
Atlantic Thermohaline Circulation
Cloud Feedbacks
Thermokarst Lake
15. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Through talik
Some parts of the planet are dry because of their location
Sea Ice Extent is Changing in Antarctica as well
summer
16. 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.
Sea Ice Extent is Changing in Antarctica as well
Today melting ice
Permafrost Degradation
Archimedes' Principle
17. Water vapor means more water up in the clouds and less in the ground!
Antarctica
70%
Longwave Radiation
More rain means no drought
18. Ocean retains ____ CO2
Thermohaline Circulation
doubles
Atmospheric Circulation
25%
19. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Today melting ice
Sea Ice Extent is Changing in Antarctica as well
Change in vegetation generates a further feedback
Sublimation
20. Heat is provided by outside sources that flow down the continental slope to reach the deepest part of the glacier. High pressure decreases the melting point and favors melting.
Thermohaline Circulatoin
Agricultural Drought
In the troposphere that we live in.
30%
21. Carbon dioxide - Methane - Ozone - Water Vapor - Few others - Most ___________________ are mixed in the troposphere (Except water vapor) - Water vapor is concentrated closer to the ground.
Archimedes' Principle
Positive
Once every 4 years.
Greenhouse Gases
22. Set up in 1988 by WMO and UNEP.
IPCC
Sea Ice Extent is Changing in Antarctica as well
75-OC
Energy Budget
23. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Melt
Surface Mass Balance
Grounding Lines
Increases - decreases
24. US is responsible for ___ of the total CO2
30%
Sea Ice Extent is Changing in Antarctica as well
Archimedes' Principle
Ice absorbs
25. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Frozen Soil
Sunspots
Ice Motion
Time Variable Gravity
26. The air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
Types of Albedo
Cause of break of inversion layers or decrease in frequency
Altimetry (height)
In the Arctic where the air is cooler
27. How often does El Nio occur?
air can warm dramatically
Strong
Once every 4 years.
IN the last 2 decades what we've seen
28. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
75-OC
Sea ice melt does not change sea level
30%
29. More common
Layers of Earth
Discontinuous
Ozone Hole
Inversion Layer Winter
30. Forms in a mosaic of favoured locations.
Discontinuous Permafrosrt
Ice/snow
Ocean-Ice-Atmosphere Interaction
Archimedes' Principle
31. In ________- inversion layer is more common in the Arctic
winter
Global warming and hot nights?
US and precipitation
Stronger
32. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
More rain means no drought
70%
El Nino
Climate Change in the Arctic
33. Cooler water and drought conditions.
Ice-Albedo
Surface Mass Balance
La Nia
Mass Budget
34. 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.
Through talik
Stratospheric Ozone Depletion
Heat Source and Pressure
reduction in sea-ice
35. 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
Altimetry
Carbon Dioxide
Sea ice melt does not change sea level
Why the Arctic climate is special
36. 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!
Thermokarst
Shortwave Length
Ice Discharge
Antarctica
37. 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
Atmospheric Structure
Carbon Dioxide
Why ice-albedo feedback is a big deal in the Arctic
20%
38. Fresh snow and snow-covered sea ice may have an albedo higher than 80% - even when melting in the summer. Sea ice has a higher albedo and can absorb as little as 10% of the solar energy. On average - sea ice albedo is around 85%
Albedos of Snow and Ice
Ice shelf
Ocean-Ice-Atmosphere Interaction
Ice-Albedo
39. 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
Sublimation
Thinner atmosphere
Percentile departures
Atmospheric Circulation
40. Grounding line is the last portion of a glacier grounded to bedrock - after this line there are ice shelves - Glaciers contribute to sea level rise after passing the grounding line - Maximum thinning at grounding line.
Ice-Ocean Interactions
Ice-Albedo
Strong
Ice Shelf
41. Total absorbed solar radiation
Major distinction between Kyoto Protocol and Convention
Amount of light actually reaching the Earth
70%
30%
42. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Sea ice melt does not change sea level
Radiative Flux
Inversion Layer Winter
Change in vegetation generates a further feedback
43. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Greenland
Affect Floods and Droughts
Mass Balance
Permafrost
44. CO2 GHG forcing - H2O - dominant/major GHG
Altimetry Pros
75-OC
GHG
Sea Ice Extent is Changing in Antarctica as well
45. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Agricultural Drought
Today melting ice
70%
Atmospheric Composition
46. x7 smaller - 7m total sea level equivalent.
Amount of light actually reaching the Earth
Greenland
Accumulation
Energy Budget
47. Radiation absorbed by atmospheric greenhouse gases?
Contributions to CO2 from different activities
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice in the Arctic
La Nia
48. 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
Is precipitation around the world increasing?
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Black Carbon
49. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Altimetry (height)
Monthly maximums and minimums
70%
Questions to think about
50. Where does the ozone protect us?
In the stratosphere.
Ozone
Why Water Vapor is not a climate forcing
Very small portion