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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 buoyant force is equal to the weight of the displaced water.
2. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Today melting ice
Greenhouse Gases
Arctic Atmosphere
Layers of Earth
3. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
Ice absorbs
Heat Source and Pressure
How talik forms under lakes
4. Laser radar - H V - Long time series - high accuracy - Density
Open talik
Altimetry (height)
Sea-Ice Albedo
.7O Celsius over the past century.
5. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
How the cryosphere is affected by climate change
What happens with the Ozone Hole
Negative Ice-Albedo Feedback
Sea Ice
6. Precipitation intensity will rise ___ for every 1 OC of warming.
7%
Heat wave
Importance of ice sheets
Ice Shelf
7. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Why ice-albedo feedback is a big deal in the Arctic
Active Layer
Ice Cap
Talik
8. LW - SW - 55% absorbed by surface
Air pollution
Why the Arctic climate is special
Permafrost
Energy Budget
9. Number of days that exceed a given temperature
Atmospheric Structure
Methane
Major distinction between Kyoto Protocol and Convention
Absolute thresholds
10. 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
Grounding v Surface Melting
Altimetry (height)
Positive feedbacks both found in...
Mass Change
11. Really measures volume.
Longwave Radiation
Ozone Hole
Change in vegetation generates a further feedback
Altimetry
12. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Indirect heat wave effect
How we measure Mass Balance
Average radiative flux reaching the atmosphere
Open talik
13. The Earth emits this.
Ozone Hole
Increases - decreases
Longwave Radiation
El Nio is in the coasts of...
14. he increase of ozone concentration in the atmosphere helps ____ our planet
45%
Monthly maximums and minimums
Deep tropics between 15O N and 15 O S are quite
Warm
15. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
Some regions of the Earth have warmed faster than other regions.
How to define a heatwave
How a closed talik forms
16. A thick - floating slab of freshwater ice extending from coast to coast.
20%
summer
Strong
Ice shelf
17. 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
In the troposphere that we live in.
Frozen Soil
Ice Discharge
18. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Melt
Ice Cap
Atmospheric Composition
Cloud Feedbacks
19. The amount of light reflected by an object.
Permafrost
Infrared radiation
Albedo
Once every 4 years.
20. Melting Point decreases
Mass Budget
Surface Mass Balance
Why Water Vapor is not a climate forcing
.75OC/km-1
21. Over the past century what has happened to the Earth's temperature?
Global warming and hot nights?
Sublimation
The Ozone Hole
Some regions of the Earth have warmed faster than other regions.
22. 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.
70%
summer
Negative Ice-Albedo Feedback
In the stratosphere.
23. Frozen +2 years - Few centimeters to 1500 m
Permafrost
20%
Energy Budget
Severe coastal erosion
24. Forms in a mosaic of favoured locations.
Natural Causes of Warming
Discontinuous Permafrosrt
.7O Celsius over the past century.
El Nio is in the coasts of...
25. Industrial product - 300 ppb (parts per billion)
Heat Source and Pressure
Global warming and hot nights?
Nitrous Oxide (N2O)
Altimetry Pros
26. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Global warming and hot nights?
Active Layer
Ice-Albedo
El Nio is in the coasts of...
27. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Effect of Deforestation on CO-2
Sea-Ice Albedo
Thermokarst
Why the Arctic climate is special
28. 1.4 USA - 57 m total sea level equivalent
Shortwave Length
Antarctica
Dry
Ice in the Arctic
29. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Active Layer
Ice Motion
Sublimation
How a closed talik forms
30. Greenhouse gases are a ___ portion of the atmosphere
Sea Ice
Thermohaline Circulatoin
Discontinuous
Very small portion
31. 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
Hydrological Drought
What effects the density
Why the Arctic climate is special
How talik forms under lakes
32. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Positive
Carbon Dioxide
Indirect heat wave effect
Ice-Ocean Interactions
33. 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.
Snow and snow covered ice absorb
Ice loss
Inversion Layer Winter
Warming; cooling
34. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Atmospheric Composition
Monthly maximums and minimums
In the troposphere that we live in.
% of Greenhouse Gases
35. A mass of land ice - continental or sub-continental in extent - and thick enough to cover most of the underlying bedrock topography - If you have a warm ocean - it will melt the ice sheet. Its shape is mainly determined by the dynamics of its outward
Ozone Hole
Ocean water
Absolute thresholds
Ice Sheets
36. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Meteorological Drought
Depth v Surface
Contributions to CO2 from different activities
How talik forms under lakes
37. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Some parts of the planet are dry because of their location
Deep tropics between 15O N and 15 O S are quite
Atmospheric Circulation
Warming; cooling
38. CO2 GHG forcing - H2O - dominant/major GHG
Some regions of the Earth have warmed faster than other regions.
GHG
Greenland
Positive feedbacks both found in...
39. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Inversion Layer (feedback)
Archimedes' Principle
Ocean water
Is precipitation around the world increasing?
40. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
25%
Ozone
Negative
41. 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
Discontinuous
Inversion Layer Winter
What happens with the Ozone Hole
Thinner atmosphere
42. 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
Sea-Ice Albedo
Antarctica
Why ice-albedo feedback is a big deal in the Arctic
43. 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
Once every 4 years.
Atmospheric Composition?
Accumulation
El Nino
44. 240 w/m squared
Amount of light actually reaching the Earth
El Nino
Sunspots
Ice Motion
45. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Atmospheric Composition?
Permafrost
Altimetry Cons
Time Variable Gravity
46. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Carbon Dioxide
Ozone Hole
Negative
.7O Celsius over the past century.
47. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
How we measure Mass Balance
Why Water Vapor is not a climate forcing
Albedos of Snow and Ice
Surface Mass Balance
48. In ________- inversion layer is more common in the Arctic
More rain means no drought
Wetter; drier
winter
GHG
49. 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
Ocean water
Sea-Ice Albedo
45%
50. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Talik
Atmospheric Composition?
Thermohaline Circulation
Greenhouse Gases