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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. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Percentile departures
Why the Arctic climate is special
Methane
Shortwave Length
2. 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.
What effects the density
Climate Change in the Arctic
Mass Budget
Some parts of the planet are dry because of their location
3. Over the Northern Hemisphere than the tropics.
Heat Source and Pressure
Where rise in OC is greatest
Atmospheric Circulation
Grounding Lines
4. Unfrozen ground that is found within a mass of permafrost
Closed talik
Ozone
Altimetry Pros
El Nino
5. South polar vortex - Temperatures drop below 80O Celsius in the lower stratosphere - At these temperatures the chemicals in the stratosphere freeze and form Polar Stratospheric Clouds (PSCS) - These increase the concentration of CFCs in turn destroyi
Grounding Lines
What happens with the Ozone Hole
Albedos of Snow and Ice
The cryosphere
6. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Precipitation and High Latitudes
Reduction in sea-ice extent
Antarctica
Ocean water
7. Holds unique and key information - Are highly interconnected - Respond and drive climate change - Are the largest freshwater reservoirs of the planet - Ice cores tell us that in climate records - nothing is regular and ice sheet plays major role.
Ozone Hole
Effect of Deforestation on CO-2
Ice Sheets
Radiative Forcing
8. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Mass Budget
Surface Mass Balance
Hydrological Drought
Active Layer
9. How much is the planet really warming?
Albedo
Ozone Hole
The cryosphere
.7O Celsius over the past century.
10. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Melt
Ozone Hole
Major distinction between Kyoto Protocol and Convention
Ocean water
11. ~15% of incident solar energy (albedo 85)
air can warm dramatically
Snow and snow covered ice absorb
Affect Floods and Droughts
Shortwave Length
12. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Through talik
The Ozone Hole
Warming; cooling
Dry
13. ~10% of incident solar energy (albedo 90)
.7O Celsius over the past century.
How the cryosphere is affected by climate change
Ice absorbs
Contributions to CO2 from different activities
14. Really measures volume.
Negative Ice-Albedo Feedback
Accumulation
Altimetry
Ice Motion
15. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Closed talik
Warming; cooling
Rainy
Strong
16. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Thermokarst
doubles
Discontinuous
Archimedes' Principle
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
Ozone Hole
Thermohaline Circulation
Inversion Layer Winter
Negative Ice-Albedo Feedback
18. The amount of light reflected by an object.
1 m/yr; 10x
IN the last 2 decades what we've seen
Albedo
Longwave Radiation
19. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Melt
Ozone
Ice-Albedo
Surface Mass Balance
20. Number of days when temperatures climb above average by a fixed amount.
Threshold departures
In the stratosphere.
Heat wave
Sublimation
21. 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)
Open talik
Monthly maximums and minimums
Types of Albedo
22. Cooler water and drought conditions.
Grounding v Surface Melting
Ocean water
Altimetry Pros
La Nia
23. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Atmospheric Structure
Increases - decreases
.75OC/km-1
Importance of ice sheets
24. The buoyant force is equal to the weight of the displaced water.
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25. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
45%
In the Arctic where the air is cooler
20%
26. x7 smaller - 7m total sea level equivalent.
Average radiative flux reaching the atmosphere
Positive feedbacks both found in...
Greenland
Hydrological Drought
27. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Dry
Depth v Surface
Thermohaline Circulatoin
Ice/snow
28. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Positive feedbacks both found in...
Ice Sheets
Is precipitation around the world increasing?
Thermohaline Circulation Effect
29. 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.
Thickness of the active layer and the permafrost depend on this
Thermohaline Circulation Effect
El Nio is in the coasts of...
Normal condition for air
30. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Ice Cap
Ocean-Ice-Atmosphere Interaction
Ice Motion
Ice Discharge
31. Where does the ozone protect us?
In the stratosphere.
Longwave Radiation
Heat wave
Mass Change
32. O Climate change in the Arctic is occurring now - Changes have been huge already
Amount of light actually reaching the Earth
Heat Source and Pressure
Today melting ice
Inversion Layer (feedback)
33. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Natural Causes of Warming
Types of Albedo
Monthly maximums and minimums
Ocean-Ice-Atmosphere Interaction
34. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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35. 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.
air can warm dramatically
Ice-Ocean Interactions
Atmospheric Structure
Grounding v Surface Melting
36. 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:
Sea ice melt does not change sea level
Thermohaline Circulation
Ozone Hole
.7O Celsius over the past century.
37. A dome shaped cover of perennial ice and snow.
20%
Surface Mass Balance
30%
Ice Cap
38. Permafrost- A frozen soil
Frozen Soil
Is precipitation around the world increasing?
Mass Balance
Permafrost
39. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
25%
Thermokarst
Calving
Ice Motion
40. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Methane
Hydrological Drought
Inversion Layer Winter
How to define a heatwave
41. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
El Nino
Permafrost
Altimetry Pros
Mass Balance
42. Like weighing oneself on the scale.
Normal condition for air
Frozen Soil
Time Variable Gravity
Ocean water
43. 10 : 1 - grounding ; surface
Grounding v Surface Melting
Positive feedbacks both found in...
Contributions to CO2 from different activities
Through talik
44. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
Sunspots
GHG
Thermohaline Circulatoin
45. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Open talik
IPCC
Thermokarst
Archimedes' Principle
46. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Stratospheric Ozone Depletion
Importance of ice sheets
Stronger
Earth's tilt
47. What can cause a change in the Earth's climate balance?
IN the last 2 decades what we've seen
Major distinction between Kyoto Protocol and Convention
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
.7O Celsius over the past century.
48. 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
Melt
Why the Arctic climate is special
Open talik
Carbon Dioxide
49. Total absorbed solar radiation
70%
Altimetry Pros
Some parts of the planet are dry because of their location
Ocean-Ice-Atmosphere Interaction
50. High cloud has a _____ effect and cool cloud has a ____ effect
Warming; cooling
Ice Sheets
Positive feedbacks both found in...
Permafrost
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