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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 air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
Sea-Ice Albedo
In the Arctic where the air is cooler
Dry
Ice Discharge
2. The Earth emits this.
Longwave Radiation
Percentile departures
Positive
Average radiative flux reaching the atmosphere
3. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Thickness of the active layer and the permafrost depend on this
Questions to think about
Ice in the Arctic
Grounding Lines
4. Industrial product - 300 ppb (parts per billion)
Ice/snow
Archimedes' Principle
Nitrous Oxide (N2O)
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
5. 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
Time Variable Gravity
Longwave Radiation
Mass Balance
6. 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
Thinner atmosphere
Absolute thresholds
Cause of break of inversion layers or decrease in frequency
Mass Change
7. Greenhouse gases are mixed in the ____
Sea-Ice Albedo
Climate Change in the Arctic
US and precipitation
Troposphere
8. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Rainy
Calving
How to define a heatwave
7%
9. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Methane
Thermokarst
Surface Mass Balance
Changes in Arctic sea-ice Extent
10. In ________- inversion layer is more common in the Arctic
Normal condition for air
Antarctica
Sea Ice Extent is Changing in Antarctica as well
winter
11. Forms in a mosaic of favoured locations.
45%
Agricultural Drought
Discontinuous Permafrosrt
Thermohaline Circulation Effect
12. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Sea Ice
Albedos of Snow and Ice
Active Layer
Monthly maximums and minimums
13. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Cause of break of inversion layers or decrease in frequency
Ice-Albedo
Stronger
Positive feedbacks both found in...
14. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Today melting ice
Positive feedbacks both found in...
Thermohaline Circulation Effect
15. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Albedos of Snow and Ice
Stratospheric Ozone Depletion
Ice/snow
Troposphere
16. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Reduction in sea-ice extent
Time Variable Gravity
Through talik
Thickness of the active layer and the permafrost depend on this
17. Rainy on yearly average. In these regions - rising air predominates.
Where rise in OC is greatest
Atmospheric Composition?
Surface Mass Balance
Deep tropics between 15O N and 15 O S are quite
18. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ozone Hole
Ocean water
Sea ice melt does not change sea level
Dry
19. 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
Ocean-Ice-Atmosphere Interaction
Open talik
Albedos of Snow and Ice
20. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Surface Mass Balance
How we measure Mass Balance
air can warm dramatically
Ice/snow
21. Taliks are found under lakes because of the ability of water to store and vertically transfer heat energy - Vertical extent of the taliks found under lakes is related to the depth and volume of the overlying water body.
Time Variable Gravity
Cause of break of inversion layers or decrease in frequency
.75OC/km-1
How talik forms under lakes
22. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
El Nio is in the coasts of...
Sublimation
Ice Discharge
Altimetry (height)
23. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stratospheric Ozone Depletion
Thermohaline Circulatoin
Cloud Feedbacks
Stronger
24. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Ocean water
Energy Budget
Ocean-Ice-Atmosphere Interaction
Methane
25. What can cause a change in the Earth's climate balance?
Thermohaline Circulatoin
Sublimation
Inversion Layer (feedback)
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
26. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Shortwave Length
Mass Change
Active Layer
IPCC
27. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Types of Albedo
Talik
% of Greenhouse Gases
Antarctica
28. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Accumulation
Radiative Flux
air can warm dramatically
Dynamic thinning
29. 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.
Today melting ice
Ocean-Ice-Atmosphere Interaction
Surface Mass Balance
Climate Change in the Arctic
30. 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
El Nino
Thermohaline Circulation
.75OC/km-1
Ozone Hole
31. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
In the Arctic where the air is cooler
Once every 4 years.
Thermohaline Circulation Effect
Heat Source and Pressure
32. O Climate change in the Arctic is occurring now - Changes have been huge already
Mass Balance
Today melting ice
Cloud Feedbacks
Methane
33. 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.
Inversion Layer (feedback)
Meteorological Drought
Affect Floods and Droughts
Ozone Hole
34. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
What happens with the Ozone Hole
Radiative Forcing
Sea-Ice Albedo
Ice Motion
35. 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
Sea ice melt does not change sea level
Ice-Albedo
How the cryosphere is affected by climate change
36. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Thermohaline Circulation
Accumulation
Is precipitation around the world increasing?
Calving
37. 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.
Indirect heat wave effect
7%
Radiative Forcing
Importance of ice sheets
38. Number of days when temperatures climb above average by a fixed amount.
Threshold departures
Atmospheric Composition
Frozen Soil
Mass Budget
39. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Atmospheric Composition
Black Carbon
winter
Thinner atmosphere
40. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
30%
Troposphere
Albedos of Snow and Ice
41. 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
Why ice-albedo feedback is a big deal in the Arctic
7%
In the troposphere that we live in.
Dynamic thinning
42. Reduction of Summer Sea- 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 - Snow and snow covered ice absorb 15% of incident solar energy - Ice absorbs 10% of inc
Reduction in sea-ice extent
Active Layer
Altimetry (height)
air can warm dramatically
43. Summer increase in cloud cover - Winter decrease in cloud cover.
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44. 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
Indirect heat wave effect
Amount of light actually reaching the Earth
Is precipitation around the world increasing?
45. Over the past century what has happened to the Earth's temperature?
Some regions of the Earth have warmed faster than other regions.
Negative
Average radiative flux reaching the atmosphere
50%
46. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Atlantic Thermohaline Circulation
Thermokarst Lake
How to define a heatwave
Grounding Lines
47. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Inversion Layer (feedback)
Heat Source and Pressure
Heat wave
Discontinuous
48. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Air pollution
reduction in sea-ice
Increases - decreases
Hydrological Drought
49. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
In the Arctic where the air is cooler
75-OC
Strong
50. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Precipitation and High Latitudes
Questions to think about
Change in vegetation generates a further feedback
Climate Change in the Arctic