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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. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
reduction in sea-ice
Thermohaline Circulation Effect
Cloud Feedbacks
How a closed talik forms
2. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Increases - decreases
Calving
Ice Motion
doubles
3. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
Climate Change in the Arctic
The Ozone Hole
Absolute thresholds
4. Over the past century what has happened to the Earth's temperature?
Altimetry (height)
Dry
Some regions of the Earth have warmed faster than other regions.
Effect of Deforestation on CO-2
5. Greenhouse gases are mixed in the ____
Depth v Surface
Negative Ice-Albedo Feedback
reduction in sea-ice
Troposphere
6. Rainy on yearly average. In these regions - rising air predominates.
Monthly maximums and minimums
Ocean-Ice-Atmosphere Interaction
Deep tropics between 15O N and 15 O S are quite
Inversion Layer Winter
7. Over the Northern Hemisphere than the tropics.
Surface Mass Balance
Atmospheric Structure
Where rise in OC is greatest
Closed talik
8. Greenhouse gases are a ___ portion of the atmosphere
Negative
50%
Very small portion
Some parts of the planet are dry because of their location
9. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Altimetry (height)
Thinner atmosphere
Radiative Forcing
Natural Causes of Warming
10. 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
Importance of ice sheets
Ice Shelf
Altimetry
25%
11. Industrial product - 300 ppb (parts per billion)
Cloud Feedbacks
Thermohaline Circulation
All Greenhouse gases
Nitrous Oxide (N2O)
12. High cloud has a _____ effect and cool cloud has a ____ effect
Infrared radiation
Warming; cooling
Mass Budget
Through talik
13. Unfrozen ground that is found within a mass of permafrost
Closed talik
Some parts of the planet are dry because of their location
Deep tropics between 15O N and 15 O S are quite
Meteorological Drought
14. The order of 1 m/year. Melting is ten times more.
Thinner atmosphere
Altimetry
Altimetry Cons
Surface Mass Balance
15. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Ice Discharge
Grounding Lines
Indirect heat wave effect
Cause of break of inversion layers or decrease in frequency
16. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Ice/snow
winter
Thinner atmosphere
% of Greenhouse Gases
17. 240 w/m squared
Percentile departures
Depth v Surface
Amount of light actually reaching the Earth
The Ozone Hole
18. Reduction of snow and ice cover - Changes in atmospheric circulation.
Altimetry (height)
What effects the density
Cause of break of inversion layers or decrease in frequency
In the troposphere that we live in.
19. High vs low
Cloud Feedbacks
Melt
Once every 4 years.
US and precipitation
20. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Ozone Hole
US and precipitation
Dynamic thinning
How the cryosphere is affected by climate change
21. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
What happens with the Ozone Hole
20%
Ozone Hole
Active Layer
22. O Unfrozen soil that stays within the permafrost.
Talik
Natural Causes of Warming
air can warm dramatically
Inversion Layer (feedback)
23. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Carbon Dioxide
Thermokarst
Inversion Layer Winter
Surface Mass Balance
24. O Climate change in the Arctic is occurring now - Changes have been huge already
Permafrost
Today melting ice
Discontinuous
Methane
25. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Time Variable Gravity
Cause of break of inversion layers or decrease in frequency
Shortwave Length
Percentile departures
26. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
How the cryosphere is affected by climate change
Altimetry
Greenhouse Gases
Heat Source and Pressure
27. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
Dynamic thinning
.75OC/km-1
25%
28. 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
All Greenhouse gases
How to define a heatwave
Deep tropics between 15O N and 15 O S are quite
29. 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) -
Thermohaline Circulation
Normal condition for air
Ice shelf
Sunspots
30. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Albedo
Mass Budget
GHG
Thermokarst Lake
31. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Snow and snow covered ice absorb
Antarctica
air can warm dramatically
winter
32. Total absorbed solar radiation
Heat Source and Pressure
Surface Mass Balance
70%
Stratospheric Ozone Depletion
33. 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.
Ice-Ocean Interactions
Altimetry Pros
% of Greenhouse Gases
Thermokarst
34. 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
How a closed talik forms
What happens with the Ozone Hole
Thinner atmosphere
Thermokarst Lake
35. A dome shaped cover of perennial ice and snow.
Ocean-Ice-Atmosphere Interaction
Cause of break of inversion layers or decrease in frequency
Ice Cap
Meteorological Drought
36. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Why ice-albedo feedback is a big deal in the Arctic
In the Arctic where the air is cooler
Atmospheric Composition?
Ice Cap
37. Land Based Ecosystems retain ____ CO2.
30%
Grounding v Surface Melting
Sunspots
Cause of break of inversion layers or decrease in frequency
38. 85%
Sea-Ice Albedo
45%
Why ice-albedo feedback is a big deal in the Arctic
What effects the density
39. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Black Carbon
Dynamic thinning
Normal condition for air
Very small portion
40. Set up in 1988 by WMO and UNEP.
El Nio is in the coasts of...
Mass Budget
IPCC
La Nia
41. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Sea Ice
What happens with the Ozone Hole
More rain means no drought
Average radiative flux reaching the atmosphere
42. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
Atmospheric Composition
Climate Change in the Arctic
Surface Mass Balance
Absolute thresholds
43. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Troposphere
Reduction in sea-ice extent
Positive feedbacks both found in...
The cryosphere
44. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
25%
Greenland
Indirect heat wave effect
Negative Ice-Albedo Feedback
45. In _______ - the inversions are less frequent and weaker in the Arctic.
Strong
summer
Warm
Ozone Hole
46. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Permafrost
El Nino
Grounding Lines
Indirect heat wave effect
47. Is not an externally imposed perturbation to the climate system.
Is precipitation around the world increasing?
US and precipitation
Why Water Vapor is not a climate forcing
Ocean-Ice-Atmosphere Interaction
48. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Stronger
Sea Ice Extent is Changing in Antarctica as well
Heat Source and Pressure
Altimetry Cons
49. 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%
Indirect heat wave effect
Albedos of Snow and Ice
Importance of ice sheets
Melt
50. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Greenland
Once every 4 years.
Ozone