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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. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
Ice Shelf
Longwave Radiation
In the stratosphere.
2. 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
Dry
Permafrost
Methane
Some regions of the Earth have warmed faster than other regions.
3. 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.
Agricultural Drought
Thermohaline Circulation Effect
Rainy
Why ice-albedo feedback is a big deal in the Arctic
4. Permafrost- A frozen soil
Normal condition for air
Frozen Soil
Atlantic Thermohaline Circulation
Stratospheric Ozone Depletion
5. 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
Albedos of Snow and Ice
Thermohaline Circulation
Active Layer
6. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
El Nio is in the coasts of...
Climate Change in the Arctic
Thickness of the active layer and the permafrost depend on this
Thermokarst Lake
7. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
% of Greenhouse Gases
winter
Indirect heat wave effect
Altimetry Cons
8. 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.
Permafrost
Sea Ice
Ice-Albedo
Ice Sheets
9. Where do greenhouse gases warm up the Earth?
In the troposphere that we live in.
Atmospheric Structure
50%
Positive
10. Industrial product - 300 ppb (parts per billion)
Nitrous Oxide (N2O)
Effect of Deforestation on CO-2
Monthly maximums and minimums
Grounding v Surface Melting
11. 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
Altimetry Cons
.7O Celsius over the past century.
How talik forms under lakes
12. 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
Dry
Affect Floods and Droughts
Ocean water
Major distinction between Kyoto Protocol and Convention
13. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Mass Balance
Surface Mass Balance
How we measure Mass Balance
Snow and snow covered ice absorb
14. 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
What effects the density
Affect Floods and Droughts
Radiative Flux
The Ozone Hole
15. 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.
Questions to think about
Indirect heat wave effect
The Ozone Hole
US and precipitation
16. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Negative Ice-Albedo Feedback
Methane
Affect Floods and Droughts
Arctic Atmosphere
17. Warming- positive feedback - Cooling- negative feedback.
Active Layer
Some regions of the Earth have warmed faster than other regions.
Ice-Albedo
45%
18. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Greenland
Severe coastal erosion
Active Layer
Reduction in sea-ice extent
19. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Inversion Layer (feedback)
75-OC
Thermokarst
Ocean-Ice-Atmosphere Interaction
20. Much of the Arctic is overlain by snow and sea ice (land ice and sea ice) - It makes warming a much bigger deal in the Arctic
Why ice-albedo feedback is a big deal in the Arctic
Questions to think about
Sea-Ice Albedo
Active Layer
21. Clouds 40~90% - Vegetation 10~15%
reduction in sea-ice
Meteorological Drought
Types of Albedo
Radiative Forcing
22. Reduction of snow and ice cover - Changes in atmospheric circulation.
Why ice-albedo feedback is a big deal in the Arctic
Sea ice melt does not change sea level
Cause of break of inversion layers or decrease in frequency
Surface Mass Balance
23. 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
Antarctica
Air pollution
Mass Change
Closed talik
24. Antarctica - stratosphere - Sep-Oct
Absolute thresholds
Ozone Hole
Accumulation
Cloud Feedbacks
25. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Warming; cooling
Negative
Effect of Deforestation on CO-2
Air pollution
26. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Rainy
Atmospheric Composition?
Grounding Lines
Thermohaline Circulation
27. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Accumulation
Severe coastal erosion
Ocean-Ice-Atmosphere Interaction
Sea Ice Extent is Changing in Antarctica as well
28. 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.
Why the Arctic climate is special
Layers of Earth
Greenhouse Gases
Ocean water
29. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice in the Arctic
Ocean water
Stratospheric Ozone Depletion
Ozone Hole
30. 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
Thermohaline Circulation
Albedos of Snow and Ice
Why the Arctic climate is special
Agricultural Drought
31. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Why Water Vapor is not a climate forcing
Global warming and hot nights?
Indirect heat wave effect
Albedo
32. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Changes in Arctic sea-ice Extent
Hydrological Drought
Precipitation and High Latitudes
Grounding v Surface Melting
33. Measures input and output.
Mass Budget
30%
20%
Ocean-Ice-Atmosphere Interaction
34. Fresh snow and snow-covered sea ice may have an albedo higher than 80% - even when melting in the summer. Sea ice has a higher albedo and can absorb as little as 10% of the solar energy. On average - sea ice albedo is around 85%
Absolute thresholds
Permafrost
Albedos of Snow and Ice
Melt
35. Over the Northern Hemisphere than the tropics.
In the troposphere that we live in.
Change in vegetation generates a further feedback
Where rise in OC is greatest
GHG
36. Precipitation intensity will rise ___ for every 1 OC of warming.
Longwave Radiation
Stratospheric Ozone Depletion
Atmospheric Structure
7%
37. 1. Keeps the ocean and the earth cooler 2. Coastal impacts of ice: prevents waves from eroding coastlines and protects from storms. 3. Ecological importance of ice: a. Most visibly for the many fish - birds - and mammal species that live in - on - or
Thermohaline Circulation Effect
7%
How the cryosphere is affected by climate change
Strong
38. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Troposphere
Through talik
Black Carbon
Deep tropics between 15O N and 15 O S are quite
39. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
.75OC/km-1
In the troposphere that we live in.
Atmospheric Composition?
Frozen Soil
40. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Cause of break of inversion layers or decrease in frequency
Discontinuous
Today melting ice
Thermokarst
41. 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) -
Rainy
Major distinction between Kyoto Protocol and Convention
1 m/yr; 10x
Normal condition for air
42. In average: +1% in respect to 100 years ago.
Is precipitation around the world increasing?
Indirect heat wave effect
Negative
Ice-Albedo
43. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Why Water Vapor is not a climate forcing
El Nio is in the coasts of...
Ice/snow
30%
44. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Sublimation
Inversion Layer Winter
Discontinuous
Methane
45. 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
Thermohaline Circulation
Altimetry Pros
What effects the density
Open talik
46. Greenhouse gases are a ___ portion of the atmosphere
Very small portion
doubles
Mass Balance
Wetter; drier
47. A dome shaped cover of perennial ice and snow.
In the stratosphere.
Some regions of the Earth have warmed faster than other regions.
Longwave Radiation
Ice Cap
48. 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
Major distinction between Kyoto Protocol and Convention
Sublimation
Why ice-albedo feedback is a big deal in the Arctic
Reduction in sea-ice extent
49. Number of days that land among the hottest of all days in that month's long-term record.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Percentile departures
Reduction in sea-ice extent
Black Carbon
50. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
In the Arctic where the air is cooler
Black Carbon
Radiative Forcing
Dry