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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 heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Positive
Heat Source and Pressure
.7O Celsius over the past century.
Ozone Hole
2. How much is the planet really warming?
Increases - decreases
Ozone Hole
.7O Celsius over the past century.
Where rise in OC is greatest
3. Summer increase in cloud cover - Winter decrease in cloud cover.
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4. he increase of ozone concentration in the atmosphere helps ____ our planet
Climate Change in the Arctic
Warm
Thermohaline Circulation Effect
How a closed talik forms
5. 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
20%
Melt
.7O Celsius over the past century.
Increases - decreases
6. ~10% of incident solar energy (albedo 90)
Global warming and hot nights?
Ice absorbs
Sea Ice Extent is Changing in Antarctica as well
IN the last 2 decades what we've seen
7. LW - SW - 55% absorbed by surface
Energy Budget
Accumulation
1 m/yr; 10x
Affect Floods and Droughts
8. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Radiative Forcing
Depth v Surface
Ocean-Ice-Atmosphere Interaction
Ozone Hole
9. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Ice Motion
Depth v Surface
In the Arctic where the air is cooler
10. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Indirect heat wave effect
Infrared radiation
US and precipitation
Ice absorbs
11. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
Radiative Flux
Longwave Radiation
Black Carbon
12. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Some regions of the Earth have warmed faster than other regions.
GHG
Normal condition for air
13. What can cause a change in the Earth's climate balance?
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Increases - decreases
Thermokarst Lake
Permafrost
14. The order of 1 m/year. Melting is ten times more.
Changes in Arctic sea-ice Extent
Talik
Inversion Layer Summer
Surface Mass Balance
15. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
How talik forms under lakes
Rainy
Ice Sheets
Percentile departures
16. 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
Active Layer
Climate Change in the Arctic
Carbon Dioxide
Why ice-albedo feedback is a big deal in the Arctic
17. Changes over time in the highest and lowest single temperature observed during a given month of the year.
50%
Monthly maximums and minimums
Heat wave
Greenland
18. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Why Water Vapor is not a climate forcing
Sea ice melt does not change sea level
Dynamic thinning
The cryosphere
19. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Inversion Layer Summer
Ocean water
Cloud Feedbacks
Increases - decreases
20. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Methane
Affect Floods and Droughts
Ozone Hole
30%
21. Over the past century what has happened to the Earth's temperature?
Indirect heat wave effect
Thermohaline Circulation
Mass Balance
Some regions of the Earth have warmed faster than other regions.
22. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Why the Arctic climate is special
Where rise in OC is greatest
Some parts of the planet are dry because of their location
Dry
23. Volcanic eruptions - Sunspots - Wobbly Earth
Natural Causes of Warming
Discontinuous Permafrosrt
Radiative Forcing
Atmospheric Structure
24. 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
Surface Mass Balance
Atmospheric Structure
Antarctica
25. 10 : 1 - grounding ; surface
Negative Ice-Albedo Feedback
Grounding v Surface Melting
Time Variable Gravity
Thermohaline Circulation
26. 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.
Greenhouse Gases
Negative
Why Water Vapor is not a climate forcing
% of Greenhouse Gases
27. Climate models suggest once the sea ice cover is thinned sufficiently - a strong kick from natural variability could initiate a rapid slide towards ice-free conditions in the summer.
Thermokarst Lake
Changes in Arctic sea-ice Extent
Thermohaline Circulation
Sunspots
28. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Altimetry Pros
Snow and snow covered ice absorb
Stratospheric Ozone Depletion
Inversion Layer (feedback)
29. The major distinction between the Protocol and the Convention is that while the Convention encouraged industrialized countries to stabilize GHG emissions - the Protocol commits them to do so.
Threshold departures
Major distinction between Kyoto Protocol and Convention
Atmospheric Structure
Ozone Hole
30. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
Positive
Warm
Ice-Ocean Interactions
31. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Thermokarst
Importance of ice sheets
Where rise in OC is greatest
Altimetry Cons
32. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Discontinuous
Ice in the Arctic
Atlantic Thermohaline Circulation
Thermokarst Lake
33. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
Altimetry Pros
Atmospheric Structure
Affect Floods and Droughts
US and precipitation
34. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Layers of Earth
Once every 4 years.
Permafrost
Meteorological Drought
35. 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
How talik forms under lakes
Altimetry Pros
Importance of ice sheets
More rain means no drought
36. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
Sea ice melt does not change sea level
What effects the density
Change in vegetation generates a further feedback
75-OC
37. Where do greenhouse gases warm up the Earth?
In the troposphere that we live in.
Climate Change in the Arctic
.75OC/km-1
Antarctica
38. 85%
Sea-Ice Albedo
Reduction in sea-ice extent
Changes in Arctic sea-ice Extent
Layers of Earth
39. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Thermokarst Lake
air can warm dramatically
Thermohaline Circulation
Altimetry Pros
40. In _______ - the inversions are less frequent and weaker in the Arctic.
Inversion Layer Winter
How we measure Mass Balance
Percentile departures
summer
41. A dome shaped cover of perennial ice and snow.
Grounding Lines
Ice Cap
25%
Major distinction between Kyoto Protocol and Convention
42. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Sea Ice
Negative Ice-Albedo Feedback
Ice-Ocean Interactions
Methane
43. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Talik
Sea-Ice Albedo
Discontinuous Permafrosrt
Black Carbon
44. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Heat Source and Pressure
Thermokarst
% of Greenhouse Gases
Thickness of the active layer and the permafrost depend on this
45. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Indirect heat wave effect
Mass Balance
Arctic Atmosphere
Ice absorbs
46. CO2 GHG forcing - H2O - dominant/major GHG
GHG
Increases - decreases
Permafrost Degradation
Troposphere
47. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Radiative Flux
Sunspots
Absolute thresholds
Dynamic thinning
48. 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%
Surface Mass Balance
Albedos of Snow and Ice
Ice Sheets
Surface Mass Balance
49. 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
Today melting ice
Ice Motion
Talik
50. Measures input and output.
Active Layer
Heat Source and Pressure
Mass Budget
25%