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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. The major distinction between the Protocol and the Convention is that while the Convention encouraged industrialized countries to stabilize GHG emissions - the Protocol commits them to do so.
Major distinction between Kyoto Protocol and Convention
45%
Importance of ice sheets
Infrared radiation
2. he increase of ozone concentration in the atmosphere helps ____ our planet
In the stratosphere.
Heat Source and Pressure
Warm
All Greenhouse gases
3. Reduction of snow and ice cover - Changes in atmospheric circulation.
Cause of break of inversion layers or decrease in frequency
Effect of Deforestation on CO-2
IN the last 2 decades what we've seen
Discontinuous
4. In _______ - the inversions are less frequent and weaker in the Arctic.
summer
winter
Thermokarst
Ice Motion
5. Land Based Ecosystems retain ____ CO2.
Discontinuous
Stronger
30%
Nitrous Oxide (N2O)
6. Volcanic eruptions - Sunspots - Wobbly Earth
Natural Causes of Warming
Antarctica
Inversion Layer (feedback)
.7O Celsius over the past century.
7. Permafrost- A frozen soil
Albedos of Snow and Ice
Frozen Soil
Ice Cap
Very small portion
8. Grounding line is the last portion of a glacier grounded to bedrock - after this line there are ice shelves - Glaciers contribute to sea level rise after passing the grounding line - Maximum thinning at grounding line.
Atmospheric Composition
IPCC
Stratospheric Ozone Depletion
Ice Shelf
9. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Warm
In the Arctic where the air is cooler
Sublimation
Ice in the Arctic
10. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Ice-Ocean Interactions
Deep tropics between 15O N and 15 O S are quite
Radiative Forcing
Severe coastal erosion
11. In average: +1% in respect to 100 years ago.
Ice Sheets
Melt
Is precipitation around the world increasing?
Why Water Vapor is not a climate forcing
12. Amount of light absorbed by surface
Inversion Layer Winter
Ice absorbs
Percentile departures
50%
13. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Stronger
Ice absorbs
El Nino
Atmospheric Circulation
14. Radiation absorbed by atmospheric greenhouse gases?
Natural Causes of Warming
Warm
Major distinction between Kyoto Protocol and Convention
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
15. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Layers of Earth
Precipitation and High Latitudes
Ice/snow
Hydrological Drought
16. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Surface Mass Balance
GHG
20%
Ocean water
17. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Positive feedbacks both found in...
Atmospheric Composition?
Hydrological Drought
Ocean-Ice-Atmosphere Interaction
18. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Infrared radiation
US and precipitation
How the cryosphere is affected by climate change
Percentile departures
19. Atmosphere retains ____ CO2
45%
Very small portion
Heat Source and Pressure
Discontinuous
20. Where do greenhouse gases warm up the Earth?
air can warm dramatically
Albedos of Snow and Ice
1 m/yr; 10x
In the troposphere that we live in.
21. 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.
Change in vegetation generates a further feedback
Greenhouse Gases
How a closed talik forms
1 m/yr; 10x
22. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Is precipitation around the world increasing?
Carbon Dioxide
Grounding Lines
Ice absorbs
23. The Earth emits this.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Longwave Radiation
Deep tropics between 15O N and 15 O S are quite
Earth's tilt
24. How often does El Nio occur?
Indirect heat wave effect
Once every 4 years.
Altimetry
Why Water Vapor is not a climate forcing
25. 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
The Ozone Hole
Heat Source and Pressure
Wetter; drier
Reduction in sea-ice extent
26. Cooler water and drought conditions.
Mass Balance
Why ice-albedo feedback is a big deal in the Arctic
La Nia
How the cryosphere is affected by climate change
27. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Average radiative flux reaching the atmosphere
Percentile departures
Some parts of the planet are dry because of their location
Mass Balance
28. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
In the troposphere that we live in.
Calving
Carbon Dioxide
Thermokarst
29. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
The cryosphere
Increases - decreases
Air pollution
How talik forms under lakes
30. 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
What happens with the Ozone Hole
Is precipitation around the world increasing?
30%
El Nino
31. Ice sheets have a very ____ Albedo
Climate Change in the Arctic
US and precipitation
Strong
doubles
32. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
20%
Altimetry
Amount of light actually reaching the Earth
Contributions to CO2 from different activities
33. Atmospheric Cooling - Both negative (stabilizing) feedbacks - It is not happening now - but it has happened in the past - Ice-albedo feedback was the dominant feedback during the ice ages.
Infrared radiation
Mass Change
Negative Ice-Albedo Feedback
Severe coastal erosion
34. 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.
Ice Sheets
Warm
Ozone Hole
Is precipitation around the world increasing?
35. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Depth v Surface
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Greenhouse Gases
Albedo
36. 1.4 USA - 57 m total sea level equivalent
Earth's tilt
% of Greenhouse Gases
Antarctica
Heat wave
37. High vs low
Permafrost Degradation
Permafrost
Cloud Feedbacks
Surface Mass Balance
38. 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
Questions to think about
Earth's tilt
In the stratosphere.
Melt
39. The buoyant force is equal to the weight of the displaced water.
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40. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Why the Arctic climate is special
Cloud Feedbacks
Inversion Layer Summer
Sea Ice Extent is Changing in Antarctica as well
41. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Atmospheric Circulation
Mass Balance
How we measure Mass Balance
42. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
75-OC
In the Arctic where the air is cooler
Ice Cap
Thinner atmosphere
43. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Ocean-Ice-Atmosphere Interaction
Atmospheric Composition
Types of Albedo
Black Carbon
44. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Longwave Radiation
Ozone Hole
Archimedes' Principle
air can warm dramatically
45. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Greenhouse Gases
Natural Causes of Warming
Discontinuous
Active Layer
46. 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
Permafrost Degradation
Mass Change
7%
Is precipitation around the world increasing?
47. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Warming; cooling
Atmospheric Structure
Greenhouse Gases
Infrared radiation
48. Surface Mass Balance is of the order of _____ melting is ____ times more.
20%
Albedo
1 m/yr; 10x
Sea Ice
49. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Heat wave
Sunspots
Is precipitation around the world increasing?
Some parts of the planet are dry because of their location
50. Rainy on yearly average. In these regions - rising air predominates.
reduction in sea-ice
Black Carbon
Deep tropics between 15O N and 15 O S are quite
75-OC