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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. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Atmospheric Composition?
Some regions of the Earth have warmed faster than other regions.
Negative
Calving
2. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Radiative Forcing
Why ice-albedo feedback is a big deal in the Arctic
Depth v Surface
US and precipitation
3. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Grounding Lines
Cloud Feedbacks
Ice Discharge
Some parts of the planet are dry because of their location
4. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Meteorological Drought
Atmospheric Circulation
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Sublimation
5. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Grounding Lines
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Arctic Atmosphere
6. Tundra absorbs more energy than ice and snow but less than scrubs and forest - and with those plants migrating towards the north - they will further contribute ot absorb more energy.
What effects the density
Change in vegetation generates a further feedback
Thermohaline Circulation Effect
Frozen Soil
7. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Grounding Lines
Frozen Soil
Surface Mass Balance
Sublimation
8. What can cause a change in the Earth's climate balance?
.7O Celsius over the past century.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ice loss
Ice Motion
9. Amount of light absorbed by atmosphere
20%
Black Carbon
Ice Motion
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
10. 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.
How talik forms under lakes
Thickness of the active layer and the permafrost depend on this
Greenhouse Gases
Albedo
11. Where does the ozone protect us?
How to define a heatwave
Albedo
Ocean water
In the stratosphere.
12. Warming- positive feedback - Cooling- negative feedback.
Ice-Albedo
Ozone Hole
Percentile departures
summer
13. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Thermokarst
Talik
How the cryosphere is affected by climate change
Carbon Dioxide
14. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Some regions of the Earth have warmed faster than other regions.
7%
Arctic Atmosphere
How talik forms under lakes
15. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Talik
Ice Motion
Depth v Surface
Methane
16. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Dynamic thinning
Ice/snow
30%
Rainy
17. How often does El Nio occur?
Ice shelf
Atmospheric Circulation
Once every 4 years.
Sunspots
18. Atmosphere retains ____ CO2
45%
Dynamic thinning
Ozone Hole
Ice Sheets
19. 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
Surface Mass Balance
Indirect heat wave effect
Ice Sheets
20. Measures input and output.
Mass Budget
Greenland
Increases - decreases
Warming; cooling
21. 85%
Contributions to CO2 from different activities
All Greenhouse gases
Sea-Ice Albedo
The Ozone Hole
22. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Accumulation
Amount of light actually reaching the Earth
Effect of Deforestation on CO-2
Sea Ice Extent is Changing in Antarctica as well
23. Laser radar - H V - Long time series - high accuracy - Density
Altimetry (height)
75-OC
Atmospheric Composition
All Greenhouse gases
24. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Methane
Stronger
Grounding Lines
Ice-Ocean Interactions
25. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Snow and snow covered ice absorb
Mass Change
Wetter; drier
Black Carbon
26. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Troposphere
Methane
Some regions of the Earth have warmed faster than other regions.
Stratospheric Ozone Depletion
27. US is responsible for ___ of the total CO2
Permafrost
Absolute thresholds
30%
All Greenhouse gases
28. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
How a closed talik forms
Greenland
La Nia
Thermohaline Circulatoin
29. Over the past century what has happened to the Earth's temperature?
Archimedes' Principle
Ice-Albedo
Nitrous Oxide (N2O)
Some regions of the Earth have warmed faster than other regions.
30. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Meteorological Drought
Ice-Ocean Interactions
How talik forms under lakes
The Ozone Hole
31. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Closed talik
Percentile departures
Archimedes' Principle
Active Layer
32. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Very small portion
Affect Floods and Droughts
Once every 4 years.
Infrared radiation
33. CO2 - CH4 - O3 - H2O - N2O - CFCs
All Greenhouse gases
30%
Ocean water
Thermokarst
34. 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
Sea ice melt does not change sea level
Altimetry
Importance of ice sheets
Cause of break of inversion layers or decrease in frequency
35. Descending Air dry - Convection cells are wet.
Greenhouse Gases
Thermokarst Lake
Atmospheric Circulation
Ice Cap
36. Number of days that land among the hottest of all days in that month's long-term record.
Infrared radiation
Air pollution
Percentile departures
Ice/snow
37. 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.
Ice loss
Altimetry Cons
Positive feedbacks both found in...
Agricultural Drought
38. Amount of light absorbed by surface
45%
Increases - decreases
50%
La Nia
39. 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.
25%
Questions to think about
Antarctica
Thermohaline Circulatoin
40. Changes over time in the highest and lowest single temperature observed during a given month of the year.
.7O Celsius over the past century.
30%
US and precipitation
Monthly maximums and minimums
41. 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
Thermokarst
Sublimation
Hydrological Drought
Thermohaline Circulation
42. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Ice Motion
Accumulation
Thermohaline Circulation
Thermokarst
43. 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
Depth v Surface
Some regions of the Earth have warmed faster than other regions.
Thermokarst
44. 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.
Natural Causes of Warming
30%
Changes in Arctic sea-ice Extent
Mass Budget
45. Water vapor means more water up in the clouds and less in the ground!
Thermohaline Circulatoin
Ozone Hole
More rain means no drought
Surface Mass Balance
46. 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.
Amount of light actually reaching the Earth
Precipitation and High Latitudes
Altimetry
How talik forms under lakes
47. 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
Percentile departures
El Nio is in the coasts of...
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Agricultural Drought
48. he increase of ozone concentration in the atmosphere helps ____ our planet
Dry
How the cryosphere is affected by climate change
winter
Warm
49. The amount of light reflected by an object.
Albedo
Amount of light actually reaching the Earth
Ice Sheets
Ice Shelf
50. A thick - floating slab of freshwater ice extending from coast to coast.
30%
Sea ice melt does not change sea level
Ice shelf
50%