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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
Average radiative flux reaching the atmosphere
How we measure Mass Balance
Altimetry (height)
2. What can cause a change in the Earth's climate balance?
70%
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Sea-Ice Albedo
Sea ice melt does not change sea level
3. Antarctica - stratosphere - Sep-Oct
Atmospheric Circulation
Surface Mass Balance
Closed talik
Ozone Hole
4. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Grounding Lines
Snow and snow covered ice absorb
doubles
5. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Active Layer
Thermohaline Circulatoin
El Nino
Longwave Radiation
6. Surface Mass Balance is of the order of _____ melting is ____ times more.
Atmospheric Circulation
How to define a heatwave
1 m/yr; 10x
Stronger
7. O The amount of energy moving in the form of photons or other elementary particles at a certain distance from the source per unit of area per second. Area/second
Radiative Flux
Through talik
Dry
Carbon Dioxide
8. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Thermokarst Lake
Atlantic Thermohaline Circulation
Grounding Lines
Calving
9. 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
How we measure Mass Balance
Grounding Lines
The cryosphere
10. Industrial product - 300 ppb (parts per billion)
Importance of ice sheets
Severe coastal erosion
Nitrous Oxide (N2O)
Strong
11. 10 : 1 - grounding ; surface
Mass Change
Negative
Positive feedbacks both found in...
Grounding v Surface Melting
12. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
How the cryosphere is affected by climate change
Amount of light actually reaching the Earth
Mass Budget
Severe coastal erosion
13. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
More rain means no drought
Sea-Ice Albedo
Permafrost
14. Unfrozen ground that is found within a mass of permafrost
Ice Sheets
Closed talik
Discontinuous Permafrosrt
Ice Shelf
15. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Ice Discharge
25%
air can warm dramatically
Surface Mass Balance
16. 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.
Wetter; drier
Permafrost Degradation
Greenland
Amount of light actually reaching the Earth
17. Ocean retains ____ CO2
Active Layer
25%
GHG
The cryosphere
18. The amount of light reflected by an object.
Ice in the Arctic
In the stratosphere.
Albedo
Permafrost
19. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Greenland
Negative
Ice Motion
Positive feedbacks both found in...
20. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Sea Ice
What happens with the Ozone Hole
Ice Cap
Ice-Albedo
21. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Thermohaline Circulatoin
Positive
Shortwave Length
Agricultural Drought
22. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Global warming and hot nights?
air can warm dramatically
Talik
Mass Balance
23. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
Threshold departures
Meteorological Drought
Surface Mass Balance
24. US is responsible for ___ of the total CO2
Thermohaline Circulatoin
30%
Thickness of the active layer and the permafrost depend on this
How talik forms under lakes
25. Less frequent and weaker
Atmospheric Composition
Inversion Layer Summer
Mass Budget
Thermohaline Circulation
26. CO2 GHG forcing - H2O - dominant/major GHG
Heat wave
Inversion Layer (feedback)
GHG
Ice in the Arctic
27. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Mass Budget
Arctic Atmosphere
How we measure Mass Balance
air can warm dramatically
28. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Thermokarst
Albedos of Snow and Ice
Methane
Meteorological Drought
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
Ocean water
Talik
El Nino
1 m/yr; 10x
30. Clouds 40~90% - Vegetation 10~15%
El Nino
Types of Albedo
Global warming and hot nights?
Arctic Atmosphere
31. 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
Climate Change in the Arctic
Frozen Soil
Importance of ice sheets
Energy Budget
32. 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
Monthly maximums and minimums
Dry
Surface Mass Balance
Hydrological Drought
33. ~10% of incident solar energy (albedo 90)
How to define a heatwave
Earth's tilt
Ice absorbs
Open talik
34. Warming- positive feedback - Cooling- negative feedback.
Ice-Albedo
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Where rise in OC is greatest
Archimedes' Principle
35. Frozen +2 years - Few centimeters to 1500 m
Effect of Deforestation on CO-2
Discontinuous Permafrosrt
Antarctica
Permafrost
36. Radiation absorbed by atmospheric greenhouse gases?
Why Water Vapor is not a climate forcing
Ice Cap
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Rainy
37. Atmosphere retains ____ CO2
The cryosphere
Carbon Dioxide
45%
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
38. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
Heat Source and Pressure
Ice-Albedo
75-OC
Indirect heat wave effect
39. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Mass Balance
Grounding Lines
Greenhouse Gases
Depth v Surface
40. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Arctic Atmosphere
Agricultural Drought
Surface Mass Balance
Why ice-albedo feedback is a big deal in the Arctic
41. 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.
Ice-Ocean Interactions
30%
Earth's tilt
Thinner atmosphere
42. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Troposphere
Ice Sheets
Depth v Surface
Through talik
43. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
El Nio is in the coasts of...
Through talik
Indirect heat wave effect
The Ozone Hole
44. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
winter
What happens with the Ozone Hole
Arctic Atmosphere
Climate Change in the Arctic
45. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Ice absorbs
GHG
Sea ice melt does not change sea level
Warm
46. 85%
Inversion Layer (feedback)
Sea-Ice Albedo
air can warm dramatically
IN the last 2 decades what we've seen
47. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Changes in Arctic sea-ice Extent
Longwave Radiation
Why Water Vapor is not a climate forcing
48. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Thermokarst
Indirect heat wave effect
Stronger
Black Carbon
49. 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.
Thermohaline Circulation Effect
Reduction in sea-ice extent
Longwave Radiation
.75OC/km-1
50. 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.
Antarctica
Negative Ice-Albedo Feedback
Active Layer
Wetter; drier
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