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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. A dome shaped cover of perennial ice and snow.
% of Greenhouse Gases
Ice/snow
Ice Motion
Ice Cap
2. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
The cryosphere
Stronger
Surface Mass Balance
Methane
3. Number of days that exceed a given temperature
Open talik
Shortwave Length
Absolute thresholds
30%
4. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Active Layer
Heat wave
Ice in the Arctic
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
5. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Negative
Mass Balance
Albedo
In the Arctic where the air is cooler
6. 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.
Frozen Soil
Atmospheric Composition
reduction in sea-ice
doubles
7. Longwave radiation - any radiation with a long wave will heat up quickly.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Methane
Why ice-albedo feedback is a big deal in the Arctic
Infrared radiation
8. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
El Nino
Infrared radiation
Ozone Hole
9. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Albedos of Snow and Ice
45%
Ice Sheets
Negative
10. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Talik
Radiative Forcing
Permafrost
20%
11. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
.7O Celsius over the past century.
Permafrost
Increases - decreases
Atmospheric Composition
12. Unfrozen ground that is found within a mass of permafrost
Closed talik
Sea-Ice Albedo
reduction in sea-ice
Monthly maximums and minimums
13. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Altimetry Cons
Sunspots
25%
Ozone Hole
14. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Thermohaline Circulation Effect
Permafrost Degradation
.75OC/km-1
Active Layer
15. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Radiative Forcing
Depth v Surface
How the cryosphere is affected by climate change
Thermokarst
16. 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
Ozone Hole
Reduction in sea-ice extent
Questions to think about
Positive feedbacks both found in...
17. Just remember the general direction of the circulation - Rising northern pacific. You start in between Greenland and Europe (youngest water) - Oldest water is in the Pacific Ocean - Salty water> fresh water - Cold Water > Warm Water
Ocean-Ice-Atmosphere Interaction
Ice-Albedo
Ozone Hole
Thermohaline Circulation
18. 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
Sea Ice
Types of Albedo
Normal condition for air
19. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Amount of light actually reaching the Earth
Ozone Hole
75-OC
GHG
20. Over the Northern Hemisphere than the tropics.
Affect Floods and Droughts
Questions to think about
Surface Mass Balance
Where rise in OC is greatest
21. 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
Melt
Altimetry
Talik
22. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
In the troposphere that we live in.
Sublimation
Heat Source and Pressure
70%
23. Amount of light absorbed by atmosphere
Threshold departures
Inversion Layer Summer
Atmospheric Circulation
20%
24. 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
Thermohaline Circulation
Atlantic Thermohaline Circulation
doubles
What effects the density
25. 85%
Sea-Ice Albedo
Rainy
The Ozone Hole
Ice Sheets
26. Volcanic eruptions - Sunspots - Wobbly Earth
Ozone Hole
La Nia
Where rise in OC is greatest
Natural Causes of Warming
27. 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%
Albedos of Snow and Ice
Methane
Effect of Deforestation on CO-2
70%
28. ~15% of incident solar energy (albedo 85)
Longwave Radiation
Snow and snow covered ice absorb
Major distinction between Kyoto Protocol and Convention
Open talik
29. Ocean retains ____ CO2
25%
Active Layer
Closed talik
GHG
30. Summer increase in cloud cover - Winter decrease in cloud cover.
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31. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Contributions to CO2 from different activities
Mass Balance
Thermohaline Circulatoin
Threshold departures
32. 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!
Ice Motion
Cloud Feedbacks
Antarctica
Ice/snow
33. 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
Atmospheric Composition
Positive feedbacks both found in...
Why the Arctic climate is special
30%
34. Set up in 1988 by WMO and UNEP.
All Greenhouse gases
IPCC
What happens with the Ozone Hole
.7O Celsius over the past century.
35. 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
Troposphere
Major distinction between Kyoto Protocol and Convention
IPCC
Why ice-albedo feedback is a big deal in the Arctic
36. The Earth emits this.
Changes in Arctic sea-ice Extent
Thermokarst Lake
Longwave Radiation
How a closed talik forms
37. Soil at or below the freezing point of water for two or more years - Can be: Terrestrial - Subsea - Can be: Continuous: exists across a landscape as an unbroken layer. More than 90% is frozen - Discontinuous
How talik forms under lakes
Sunspots
Permafrost
What happens with the Ozone Hole
38. The large-scale ocean circulation that moves water between the deep and surface ocean which effects salinity and temperature change - Supplies heat to the polar-regions.
Methane
Altimetry Cons
30%
Thermohaline Circulation Effect
39. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Antarctica
Deep tropics between 15O N and 15 O S are quite
Altimetry Pros
% of Greenhouse Gases
40. Cooler water and drought conditions.
La Nia
Ice-Ocean Interactions
Natural Causes of Warming
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
41. 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.
Amount of light actually reaching the Earth
Heat Source and Pressure
What effects the density
Questions to think about
42. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Surface Mass Balance
Positive
Normal condition for air
Change in vegetation generates a further feedback
43. LW - SW - 55% absorbed by surface
Sea Ice Extent is Changing in Antarctica as well
Heat wave
Energy Budget
Altimetry (height)
44. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Meteorological Drought
.75OC/km-1
Warming; cooling
Thermokarst
45. High cloud has a _____ effect and cool cloud has a ____ effect
Where rise in OC is greatest
Warming; cooling
Longwave Radiation
Warm
46. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Accumulation
Cause of break of inversion layers or decrease in frequency
Altimetry Pros
Ice Motion
47. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Indirect heat wave effect
Ocean water
Antarctica
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
48. Land Based Ecosystems retain ____ CO2.
Air pollution
30%
Radiative Forcing
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
49. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Heat wave
Increases - decreases
Ice shelf
El Nio is in the coasts of...
50. In average: +1% in respect to 100 years ago.
In the troposphere that we live in.
Precipitation and High Latitudes
Is precipitation around the world increasing?
Earth's tilt