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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. ~15% of incident solar energy (albedo 85)
Carbon Dioxide
Depth v Surface
Closed talik
Snow and snow covered ice absorb
2. 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) -
Normal condition for air
The cryosphere
Meteorological Drought
Amount of light actually reaching the Earth
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%
Ocean water
Global warming and hot nights?
Ice Shelf
Albedos of Snow and Ice
4. Less frequent and weaker
Amount of light actually reaching the Earth
Air pollution
Inversion Layer Summer
In the stratosphere.
5. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
doubles
Ozone
Altimetry Pros
Meteorological Drought
6. 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.
Dynamic thinning
Ice loss
La Nia
In the troposphere that we live in.
7. 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
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Threshold departures
Why ice-albedo feedback is a big deal in the Arctic
In the troposphere that we live in.
8. Permafrost- A frozen soil
Open talik
Sublimation
Frozen Soil
Why the Arctic climate is special
9. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Closed talik
Atmospheric Composition?
Ice Motion
Altimetry
10. 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
Strong
Why the Arctic climate is special
Ozone
doubles
11. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
doubles
Time Variable Gravity
Grounding v Surface Melting
Sea Ice
12. 240 w/m squared
How talik forms under lakes
Amount of light actually reaching the Earth
Inversion Layer Winter
Talik
13. Number of days when temperatures climb above average by a fixed amount.
Threshold departures
Greenland
7%
70%
14. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Ocean-Ice-Atmosphere Interaction
Albedo
Agricultural Drought
Thinner atmosphere
15. 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.
Warm
Greenhouse Gases
Methane
How talik forms under lakes
16. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Melt
Surface Mass Balance
Meteorological Drought
air can warm dramatically
17. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
doubles
Dry
Negative Ice-Albedo Feedback
Effect of Deforestation on CO-2
18. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Closed talik
Grounding Lines
Altimetry Pros
Sea Ice Extent is Changing in Antarctica as well
19. 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
Sea Ice
How we measure Mass Balance
Permafrost Degradation
Ice Sheets
20. In ________- inversion layer is more common in the Arctic
reduction in sea-ice
winter
Ice Shelf
Inversion Layer Winter
21. 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
Ice/snow
Inversion Layer Winter
Ozone Hole
What happens with the Ozone Hole
22. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Sublimation
Sea-Ice Albedo
Change in vegetation generates a further feedback
Surface Mass Balance
23. Measures input and output.
Mass Budget
Shortwave Length
Effect of Deforestation on CO-2
Cloud Feedbacks
24. Amount of light absorbed by surface
50%
.7O Celsius over the past century.
Wetter; drier
Grounding Lines
25. Unfrozen ground that is found within a mass of permafrost
Discontinuous
air can warm dramatically
Closed talik
Antarctica
26. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Absolute thresholds
Ice in the Arctic
Sunspots
More rain means no drought
27. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Precipitation and High Latitudes
Thermohaline Circulatoin
Ice-Albedo
Increases - decreases
28. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Accumulation
Closed talik
30%
How to define a heatwave
29. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Natural Causes of Warming
Why the Arctic climate is special
Active Layer
summer
30. 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
Inversion Layer Winter
Permafrost Degradation
Ozone
31. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Atmospheric Composition
Active Layer
Precipitation and High Latitudes
Greenland
32. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
20%
Inversion Layer Winter
Methane
7%
33. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
All Greenhouse gases
doubles
75-OC
IN the last 2 decades what we've seen
34. Industrial product - 300 ppb (parts per billion)
Grounding v Surface Melting
Nitrous Oxide (N2O)
Altimetry
Amount of light actually reaching the Earth
35. Rainy on yearly average. In these regions - rising air predominates.
Change in vegetation generates a further feedback
Deep tropics between 15O N and 15 O S are quite
Air pollution
Effect of Deforestation on CO-2
36. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Absolute thresholds
.75OC/km-1
Sea ice melt does not change sea level
Atlantic Thermohaline Circulation
37. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Wetter; drier
Open talik
The cryosphere
Air pollution
38. Really measures volume.
Snow and snow covered ice absorb
Dynamic thinning
All Greenhouse gases
Altimetry
39. 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.
Permafrost Degradation
Cause of break of inversion layers or decrease in frequency
Indirect heat wave effect
Where rise in OC is greatest
40. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Grounding Lines
Ocean water
Monthly maximums and minimums
45%
41. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Agricultural Drought
Absolute thresholds
Ocean-Ice-Atmosphere Interaction
Ocean water
42. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Calving
Thermokarst Lake
More rain means no drought
Severe coastal erosion
43. Warming- positive feedback - Cooling- negative feedback.
Warm
Troposphere
Ice-Albedo
Global warming and hot nights?
44. 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.
Carbon Dioxide
Ice Sheets
Air pollution
Warming; cooling
45. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
45%
Affect Floods and Droughts
Carbon Dioxide
Mass Change
46. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
% of Greenhouse Gases
Talik
El Nino
Climate Change in the Arctic
47. 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 Shelf
Altimetry
Inversion Layer (feedback)
.7O Celsius over the past century.
48. x7 smaller - 7m total sea level equivalent.
Greenland
Heat wave
Radiative Forcing
US and precipitation
49. Total absorbed solar radiation
Sea Ice
Sublimation
Stratospheric Ozone Depletion
70%
50. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Changes in Arctic sea-ice Extent
75-OC
Negative
Discontinuous