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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. Radiation absorbed by atmospheric greenhouse gases?
Reduction in sea-ice extent
Thermohaline Circulation
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice Sheets
2. Antarctica - stratosphere - Sep-Oct
Ozone Hole
La Nia
Thermohaline Circulatoin
Ocean water
3. 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
Time Variable Gravity
Stratospheric Ozone Depletion
Once every 4 years.
4. Where do greenhouse gases warm up the Earth?
In the troposphere that we live in.
Negative Ice-Albedo Feedback
El Nio is in the coasts of...
Altimetry Cons
5. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Time Variable Gravity
Ocean water
Surface Mass Balance
Change in vegetation generates a further feedback
6. 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.
Why ice-albedo feedback is a big deal in the Arctic
Greenhouse Gases
Change in vegetation generates a further feedback
The cryosphere
7. Frozen +2 years - Few centimeters to 1500 m
Precipitation and High Latitudes
Permafrost
Methane
Archimedes' Principle
8. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Methane
In the stratosphere.
Sea-Ice Albedo
Thermokarst
9. Where does the ozone protect us?
Permafrost Degradation
Indirect heat wave effect
reduction in sea-ice
In the stratosphere.
10. Melting Point decreases
Greenland
Methane
.75OC/km-1
50%
11. Amount of light absorbed by surface
Mass Change
70%
All Greenhouse gases
50%
12. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
30%
Stratospheric Ozone Depletion
Positive
Atlantic Thermohaline Circulation
13. The past climate...for this reason - both keep good records of climate change.
Thickness of the active layer and the permafrost depend on this
Grounding Lines
Antarctica
Shortwave Length
14. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Strong
Altimetry Cons
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Air pollution
15. 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
Energy Budget
70%
Inversion Layer Summer
16. Atmosphere retains ____ CO2
Thermokarst
Dry
Amount of light actually reaching the Earth
45%
17. The buoyant force is equal to the weight of the displaced water.
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18. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Sunspots
Why the Arctic climate is special
The cryosphere
Greenhouse Gases
19. How much is the planet really warming?
Importance of ice sheets
.7O Celsius over the past century.
Amount of light actually reaching the Earth
Reduction in sea-ice extent
20. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Antarctica
Ice Discharge
Through talik
Permafrost
21. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Surface Mass Balance
Ice shelf
Thinner atmosphere
Thermokarst
22. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Hydrological Drought
Types of Albedo
Methane
Mass Balance
23. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Dynamic thinning
How we measure Mass Balance
Ozone
Once every 4 years.
24. Really measures volume.
Thickness of the active layer and the permafrost depend on this
How a closed talik forms
Altimetry
Effect of Deforestation on CO-2
25. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Inversion Layer Winter
Surface Mass Balance
Ocean water
doubles
26. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Cause of break of inversion layers or decrease in frequency
50%
Albedo
27. Total absorbed solar radiation
.7O Celsius over the past century.
70%
Active Layer
Longwave Radiation
28. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Grounding Lines
Depth v Surface
Sea ice melt does not change sea level
Albedo
29. Cooler water and drought conditions.
La Nia
Why Water Vapor is not a climate forcing
Thermohaline Circulation Effect
Discontinuous Permafrosrt
30. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
% of Greenhouse Gases
La Nia
75-OC
Negative
31. 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.
reduction in sea-ice
Altimetry (height)
Surface Mass Balance
Ozone Hole
32. 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
In the troposphere that we live in.
Importance of ice sheets
Threshold departures
Altimetry Pros
33. 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
Melt
Ocean water
20%
Natural Causes of Warming
34. 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.
Atmospheric Circulation
Negative Ice-Albedo Feedback
Ozone Hole
70%
35. 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
Altimetry
El Nino
Active Layer
In the troposphere that we live in.
36. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Methane
Thermokarst
El Nio is in the coasts of...
Indirect heat wave effect
37. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Permafrost
Albedo
Black Carbon
Change in vegetation generates a further feedback
38. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Ice Shelf
Some regions of the Earth have warmed faster than other regions.
Thinner atmosphere
Methane
39. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Questions to think about
Precipitation and High Latitudes
Ozone Hole
US and precipitation
40. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
How a closed talik forms
Surface Mass Balance
Through talik
Antarctica
41. High cloud has a _____ effect and cool cloud has a ____ effect
Negative
Climate Change in the Arctic
Surface Mass Balance
Warming; cooling
42. High vs low
Altimetry (height)
In the troposphere that we live in.
Cloud Feedbacks
Types of Albedo
43. Ocean retains ____ CO2
Mass Balance
1 m/yr; 10x
25%
The cryosphere
44. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
Dynamic thinning
1 m/yr; 10x
Normal condition for air
45. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Ice shelf
Deep tropics between 15O N and 15 O S are quite
7%
Monthly maximums and minimums
46. 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.
Methane
Importance of ice sheets
Layers of Earth
Inversion Layer (feedback)
47. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
How we measure Mass Balance
Methane
summer
Increases - decreases
48. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Ice in the Arctic
30%
Depth v Surface
Ocean water
49. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Altimetry (height)
Thermokarst
Precipitation and High Latitudes
50. ~15% of incident solar energy (albedo 85)
Permafrost Degradation
20%
Increases - decreases
Snow and snow covered ice absorb