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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. Ice sheets have a very ____ Albedo
Shortwave Length
Thermohaline Circulatoin
Atmospheric Structure
Strong
2. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Methane
More rain means no drought
Atmospheric Structure
doubles
3. 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
25%
Indirect heat wave effect
Sunspots
4. The buoyant force is equal to the weight of the displaced water.
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5. Warming- positive feedback - Cooling- negative feedback.
Altimetry Pros
Active Layer
Ice-Albedo
Ice Discharge
6. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
7%
Stronger
Earth's tilt
Amount of light actually reaching the Earth
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
Radiative Flux
Atlantic Thermohaline Circulation
IPCC
50%
8. 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
Ocean water
Dynamic thinning
Infrared radiation
Dry
9. Permafrost- A frozen soil
Layers of Earth
Frozen Soil
75-OC
winter
10. CO2 - CH4 - O3 - H2O - N2O - CFCs
Amount of light actually reaching the Earth
Deep tropics between 15O N and 15 O S are quite
All Greenhouse gases
Strong
11. Is not an externally imposed perturbation to the climate system.
Why Water Vapor is not a climate forcing
Inversion Layer Winter
Earth's tilt
In the troposphere that we live in.
12. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
% of Greenhouse Gases
The cryosphere
Carbon Dioxide
Snow and snow covered ice absorb
13. 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.
Thermohaline Circulation
Once every 4 years.
Thickness of the active layer and the permafrost depend on this
Ice-Ocean Interactions
14. 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
Contributions to CO2 from different activities
Questions to think about
Normal condition for air
Why ice-albedo feedback is a big deal in the Arctic
15. The past climate...for this reason - both keep good records of climate change.
How a closed talik forms
Sublimation
Heat wave
Thickness of the active layer and the permafrost depend on this
16. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Precipitation and High Latitudes
Discontinuous
Time Variable Gravity
Thinner atmosphere
17. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Agricultural Drought
Atmospheric Composition?
Hydrological Drought
.75OC/km-1
18. Industrial product - 300 ppb (parts per billion)
Surface Mass Balance
Permafrost
How the cryosphere is affected by climate change
Nitrous Oxide (N2O)
19. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Frozen Soil
Sunspots
75-OC
Active Layer
20. 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
La Nia
Inversion Layer Summer
All Greenhouse gases
21. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Accumulation
% of Greenhouse Gases
Discontinuous Permafrosrt
doubles
22. 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.
All Greenhouse gases
Earth's tilt
Ocean-Ice-Atmosphere Interaction
How talik forms under lakes
23. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Change in vegetation generates a further feedback
% of Greenhouse Gases
Agricultural Drought
Surface Mass Balance
24. Rainy on yearly average. In these regions - rising air predominates.
IN the last 2 decades what we've seen
US and precipitation
La Nia
Deep tropics between 15O N and 15 O S are quite
25. 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.
Ozone Hole
Sea Ice
The Ozone Hole
Thermohaline Circulatoin
26. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
Global warming and hot nights?
Heat Source and Pressure
Atlantic Thermohaline Circulation
27. Cooler water and drought conditions.
Thermohaline Circulation
Mass Budget
La Nia
Average radiative flux reaching the atmosphere
28. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Atlantic Thermohaline Circulation
Accumulation
Ice absorbs
Ice shelf
29. 85%
Sea-Ice Albedo
Surface Mass Balance
La Nia
Ice Shelf
30. How often does El Nio occur?
Once every 4 years.
Ice in the Arctic
1 m/yr; 10x
Stratospheric Ozone Depletion
31. ~15% of incident solar energy (albedo 85)
% of Greenhouse Gases
Ice/snow
Snow and snow covered ice absorb
Climate Change in the Arctic
32. Ocean retains ____ CO2
Greenhouse Gases
25%
Questions to think about
IN the last 2 decades what we've seen
33. Frozen +2 years - Few centimeters to 1500 m
Ice shelf
Sunspots
What effects the density
Permafrost
34. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
75-OC
.7O Celsius over the past century.
Agricultural Drought
Rainy
35. 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:
Thermohaline Circulation
Thickness of the active layer and the permafrost depend on this
Ice absorbs
Ocean water
36. O Unfrozen soil that stays within the permafrost.
Troposphere
Archimedes' Principle
La Nia
Talik
37. 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
GHG
Energy Budget
More rain means no drought
38. 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!
70%
Absolute thresholds
Antarctica
Earth's tilt
39. 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
Active Layer
El Nino
Ice shelf
El Nio is in the coasts of...
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.
Contributions to CO2 from different activities
Ice Shelf
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Cloud Feedbacks
41. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Permafrost Degradation
Severe coastal erosion
Sea Ice Extent is Changing in Antarctica as well
Sublimation
42. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
doubles
El Nio is in the coasts of...
Heat Source and Pressure
Methane
43. 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.
Frozen Soil
Greenhouse Gases
Arctic Atmosphere
Inversion Layer Winter
44. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Severe coastal erosion
Some parts of the planet are dry because of their location
Atmospheric Composition
Black Carbon
45. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Radiative Forcing
Normal condition for air
Average radiative flux reaching the atmosphere
Warm
46. Where does the ozone protect us?
Once every 4 years.
Antarctica
.75OC/km-1
In the stratosphere.
47. Volcanic eruptions - Sunspots - Wobbly Earth
Infrared radiation
Natural Causes of Warming
% of Greenhouse Gases
Surface Mass Balance
48. A thick - floating slab of freshwater ice extending from coast to coast.
Changes in Arctic sea-ice Extent
Greenland
Sunspots
Ice shelf
49. Where do greenhouse gases warm up the Earth?
Ice shelf
In the troposphere that we live in.
Calving
Heat Source and Pressure
50. Over the past century what has happened to the Earth's temperature?
Some regions of the Earth have warmed faster than other regions.
Closed talik
Major distinction between Kyoto Protocol and Convention
20%
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