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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. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Closed talik
Climate Change in the Arctic
Open talik
Antarctica
2. 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
30%
Monthly maximums and minimums
El Nino
Amount of light actually reaching the Earth
3. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
The cryosphere
Thermokarst Lake
Questions to think about
Longwave Radiation
4. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Permafrost
Active Layer
Black Carbon
Ice/snow
5. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Why the Arctic climate is special
Atmospheric Structure
Mass Balance
Methane
6. The amount of light reflected by an object.
Altimetry Pros
Radiative Flux
Albedo
Amount of light actually reaching the Earth
7. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Surface Mass Balance
Active Layer
Calving
Thermokarst
8. 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
Ice-Ocean Interactions
Amount of light actually reaching the Earth
Sea ice melt does not change sea level
Mass Change
9. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Positive feedbacks both found in...
Radiative Forcing
El Nio is in the coasts of...
El Nino
10. 1. Keeps the ocean and the earth cooler 2. Coastal impacts of ice: prevents waves from eroding coastlines and protects from storms. 3. Ecological importance of ice: a. Most visibly for the many fish - birds - and mammal species that live in - on - or
How the cryosphere is affected by climate change
Ice/snow
Positive feedbacks both found in...
Mass Budget
11. More common
Depth v Surface
Effect of Deforestation on CO-2
What happens with the Ozone Hole
Inversion Layer Winter
12. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Sunspots
1 m/yr; 10x
In the Arctic where the air is cooler
Ice Discharge
13. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Rainy
Albedos of Snow and Ice
Ice Shelf
Snow and snow covered ice absorb
14. LW - SW - 55% absorbed by surface
Permafrost Degradation
Where rise in OC is greatest
Energy Budget
Accumulation
15. 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:
Questions to think about
Ozone Hole
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Thermohaline Circulation
16. Number of days that exceed a given temperature
Altimetry Cons
Where rise in OC is greatest
Absolute thresholds
Reduction in sea-ice extent
17. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Ice Motion
In the Arctic where the air is cooler
50%
Mass Balance
18. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
IN the last 2 decades what we've seen
Deep tropics between 15O N and 15 O S are quite
Ozone Hole
19. CO2 - CH4 - O3 - H2O - N2O - CFCs
Threshold departures
Atmospheric Circulation
Sea Ice Extent is Changing in Antarctica as well
All Greenhouse gases
20. 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
Ice Sheets
What effects the density
Heat wave
Dynamic thinning
21. Summer increase in cloud cover - Winter decrease in cloud cover.
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22. x7 smaller - 7m total sea level equivalent.
Greenland
Types of Albedo
Grounding Lines
Ice Motion
23. 240 w/m squared
Thermohaline Circulation
Increases - decreases
Ice-Albedo
Amount of light actually reaching the Earth
24. 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
What effects the density
Importance of ice sheets
Talik
More rain means no drought
25. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Longwave Radiation
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Stratospheric Ozone Depletion
Frozen Soil
26. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
How we measure Mass Balance
air can warm dramatically
Heat wave
In the troposphere that we live in.
27. The buoyant force is equal to the weight of the displaced water.
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28. ~10% of incident solar energy (albedo 90)
Deep tropics between 15O N and 15 O S are quite
Ice absorbs
Ocean-Ice-Atmosphere Interaction
Amount of light actually reaching the Earth
29. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Changes in Arctic sea-ice Extent
Positive feedbacks both found in...
Heat wave
30. 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.
Stronger
Ice loss
Sea-Ice Albedo
What happens with the Ozone Hole
31. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Shortwave Length
Monthly maximums and minimums
Earth's tilt
What effects the density
32. Heat is provided by outside sources that flow down the continental slope to reach the deepest part of the glacier. High pressure decreases the melting point and favors melting.
Ozone Hole
Grounding Lines
Thermohaline Circulatoin
How the cryosphere is affected by climate change
33. A dome shaped cover of perennial ice and snow.
Ice Cap
air can warm dramatically
Thermokarst
Sea ice melt does not change sea level
34. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Dynamic thinning
Ice loss
Methane
Positive feedbacks both found in...
35. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Shortwave Length
75-OC
Severe coastal erosion
All Greenhouse gases
36. 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
Longwave Radiation
Is precipitation around the world increasing?
doubles
Ozone
37. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Increases - decreases
Thermohaline Circulation
Deep tropics between 15O N and 15 O S are quite
Sea Ice Extent is Changing in Antarctica as well
38. Occurs when there is not enough water available for a particular crop to grow at a particular time.Typically seen after!meteorological drought (when rainfall decreases) but before a hydrological drought
Contributions to CO2 from different activities
Layers of Earth
Reduction in sea-ice extent
Agricultural Drought
39. High cloud has a _____ effect and cool cloud has a ____ effect
Ice Sheets
Effect of Deforestation on CO-2
Warming; cooling
Discontinuous
40. In _______ - the inversions are less frequent and weaker in the Arctic.
7%
Mass Balance
Thinner atmosphere
summer
41. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Mass Balance
Some parts of the planet are dry because of their location
Greenhouse Gases
Reduction in sea-ice extent
42. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Negative
Radiative Forcing
7%
Ozone Hole
43. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Cloud Feedbacks
Closed talik
How to define a heatwave
45%
44. 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
Inversion Layer Winter
Grounding Lines
Black Carbon
45. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
Ice Sheets
Mass Budget
Permafrost
Questions to think about
46. 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.
Ocean water
Climate Change in the Arctic
How a closed talik forms
Contributions to CO2 from different activities
47. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Closed talik
Atlantic Thermohaline Circulation
Dry
Inversion Layer (feedback)
48. Greenhouse gases are mixed in the ____
reduction in sea-ice
winter
Talik
Troposphere
49. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Negative Ice-Albedo Feedback
.75OC/km-1
Atmospheric Composition?
Thermokarst
50. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Longwave Radiation
air can warm dramatically
Sea Ice Extent is Changing in Antarctica as well
Thickness of the active layer and the permafrost depend on this
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