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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. Is not an externally imposed perturbation to the climate system.
Importance of ice sheets
Why Water Vapor is not a climate forcing
Normal condition for air
How to define a heatwave
2. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Sea Ice
Threshold departures
Atlantic Thermohaline Circulation
Albedos of Snow and Ice
3. Number of days that land among the hottest of all days in that month's long-term record.
Once every 4 years.
Percentile departures
Talik
Surface Mass Balance
4. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Greenland
Methane
Talik
Severe coastal erosion
5. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Ice absorbs
Albedo
Sea Ice Extent is Changing in Antarctica as well
Percentile departures
6. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Atmospheric Composition?
Sublimation
Ice Motion
Stronger
7. 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.
30%
Meteorological Drought
Contributions to CO2 from different activities
Changes in Arctic sea-ice Extent
8. 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
Snow and snow covered ice absorb
Sea Ice Extent is Changing in Antarctica as well
Ice/snow
Permafrost
9. What can cause a change in the Earth's climate balance?
% of Greenhouse Gases
Inversion Layer (feedback)
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Importance of ice sheets
10. In _______ - the inversions are less frequent and weaker in the Arctic.
summer
Surface Mass Balance
Ocean water
Rainy
11. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Thinner atmosphere
Calving
Meteorological Drought
Air pollution
12. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
La Nia
75-OC
Thermokarst Lake
Heat Source and Pressure
13. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
Hydrological Drought
Albedos of Snow and Ice
Melt
Longwave Radiation
14. 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) -
Carbon Dioxide
70%
Atmospheric Structure
Normal condition for air
15. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Precipitation and High Latitudes
Ocean water
Permafrost
Average radiative flux reaching the atmosphere
16. Ocean retains ____ CO2
25%
Percentile departures
Stratospheric Ozone Depletion
Frozen Soil
17. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Mass Balance
Negative Ice-Albedo Feedback
In the Arctic where the air is cooler
Closed talik
18. 1.4 USA - 57 m total sea level equivalent
Why the Arctic climate is special
Antarctica
.7O Celsius over the past century.
Precipitation and High Latitudes
19. Changes over time in the highest and lowest single temperature observed during a given month of the year.
Some regions of the Earth have warmed faster than other regions.
Atmospheric Structure
Active Layer
Monthly maximums and minimums
20. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
How the cryosphere is affected by climate change
Thermohaline Circulation
Ice in the Arctic
Layers of Earth
21. 85%
Open talik
Heat wave
Sea-Ice Albedo
Altimetry Pros
22. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Cause of break of inversion layers or decrease in frequency
Surface Mass Balance
winter
Thermohaline Circulation
23. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Mass Budget
Indirect heat wave effect
US and precipitation
Heat wave
24. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Sea ice melt does not change sea level
Earth's tilt
Time Variable Gravity
air can warm dramatically
25. Some parts of the planet are dry because of their location: most of the deserts are around 30 N and 30 S - where sinking air predominates
Questions to think about
Dry
Dynamic thinning
All Greenhouse gases
26. Frozen +2 years - Few centimeters to 1500 m
Where rise in OC is greatest
Permafrost
Greenhouse Gases
Antarctica
27. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Sea ice melt does not change sea level
Arctic Atmosphere
Positive
Depth v Surface
28. 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.
How we measure Mass Balance
Permafrost Degradation
Ice Motion
Is precipitation around the world increasing?
29. 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
Ice-Ocean Interactions
Ozone
El Nino
Ice loss
30. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
25%
Heat Source and Pressure
Permafrost
How we measure Mass Balance
31. 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.
Greenhouse Gases
Cloud Feedbacks
Grounding v Surface Melting
Positive
32. Descending Air dry - Convection cells are wet.
Atmospheric Circulation
Thermokarst
Thermohaline Circulatoin
Troposphere
33. 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.
Thinner atmosphere
Major distinction between Kyoto Protocol and Convention
reduction in sea-ice
Active Layer
34. Where does the ozone protect us?
Methane
Permafrost
In the stratosphere.
How we measure Mass Balance
35. CO2 GHG forcing - H2O - dominant/major GHG
Severe coastal erosion
GHG
Troposphere
Heat Source and Pressure
36. 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
Agricultural Drought
Air pollution
IN the last 2 decades what we've seen
Discontinuous Permafrosrt
37. Amount of light absorbed by atmosphere
Effect of Deforestation on CO-2
20%
Antarctica
Grounding Lines
38. Over the past century what has happened to the Earth's temperature?
Climate Change in the Arctic
Some regions of the Earth have warmed faster than other regions.
Discontinuous Permafrosrt
In the stratosphere.
39. More common
Inversion Layer Winter
Monthly maximums and minimums
Talik
Layers of Earth
40. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Warm
Shortwave Length
Reduction in sea-ice extent
Climate Change in the Arctic
41. The amount of light reflected by an object.
Albedo
El Nino
Absolute thresholds
Why the Arctic climate is special
42. 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
Effect of Deforestation on CO-2
Shortwave Length
Importance of ice sheets
Why ice-albedo feedback is a big deal in the Arctic
43. 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.
Average radiative flux reaching the atmosphere
Mass Change
Calving
Ice-Ocean Interactions
44. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
More rain means no drought
Dry
Meteorological Drought
How talik forms under lakes
45. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
reduction in sea-ice
Atmospheric Composition
Thermokarst
Permafrost Degradation
46. The order of 1 m/year. Melting is ten times more.
Questions to think about
Longwave Radiation
Atmospheric Composition
Surface Mass Balance
47. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Altimetry (height)
70%
Inversion Layer Summer
48. 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.
How a closed talik forms
Ice loss
Longwave Radiation
Dry
49. 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
summer
Depth v Surface
Why the Arctic climate is special
Thinner atmosphere
50. 10 : 1 - grounding ; surface
Percentile departures
Agricultural Drought
Grounding v Surface Melting
Active Layer