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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. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
IN the last 2 decades what we've seen
The cryosphere
Natural Causes of Warming
Melt
2. LW - SW - 55% absorbed by surface
Energy Budget
Frozen Soil
Meteorological Drought
Grounding v Surface Melting
3. Total absorbed solar radiation
Permafrost Degradation
70%
Atmospheric Structure
Greenland
4. 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%
Ocean-Ice-Atmosphere Interaction
Precipitation and High Latitudes
Atmospheric Circulation
Albedos of Snow and Ice
5. The Earth emits this.
Longwave Radiation
Heat wave
Ice Motion
Thermokarst Lake
6. Really measures volume.
Open talik
Altimetry
Inversion Layer Summer
Inversion Layer (feedback)
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.
Ice Sheets
Severe coastal erosion
70%
Ice loss
8. 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
Ice Shelf
Reduction in sea-ice extent
Atmospheric Composition
air can warm dramatically
9. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Why the Arctic climate is special
Accumulation
Change in vegetation generates a further feedback
Mass Budget
10. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Heat Source and Pressure
Global warming and hot nights?
reduction in sea-ice
Grounding Lines
11. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Antarctica
Climate Change in the Arctic
Is precipitation around the world increasing?
Negative
12. How much is the planet really warming?
Effect of Deforestation on CO-2
Methane
Ozone Hole
.7O Celsius over the past century.
13. In ________- inversion layer is more common in the Arctic
Altimetry Cons
Thickness of the active layer and the permafrost depend on this
winter
Air pollution
14. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Ice Shelf
Atlantic Thermohaline Circulation
Permafrost
Natural Causes of Warming
15. 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
Mass Change
Radiative Flux
Natural Causes of Warming
Ocean-Ice-Atmosphere Interaction
16. 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
Active Layer
The Ozone Hole
How the cryosphere is affected by climate change
Radiative Forcing
17. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Climate Change in the Arctic
Ocean-Ice-Atmosphere Interaction
Thickness of the active layer and the permafrost depend on this
Cloud Feedbacks
18. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Discontinuous
Importance of ice sheets
Energy Budget
Positive
19. Laser radar - H V - Long time series - high accuracy - Density
Surface Mass Balance
The Ozone Hole
Severe coastal erosion
Altimetry (height)
20. US is responsible for ___ of the total CO2
Radiative Flux
30%
Strong
Normal condition for air
21. The air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
La Nia
Frozen Soil
7%
In the Arctic where the air is cooler
22. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Dry
Ice Motion
Permafrost
Permafrost Degradation
23. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Thermohaline Circulation Effect
Thermohaline Circulation
Increases - decreases
Grounding Lines
24. Is not an externally imposed perturbation to the climate system.
Threshold departures
Natural Causes of Warming
Why Water Vapor is not a climate forcing
Radiative Flux
25. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Thermokarst
Through talik
Hydrological Drought
reduction in sea-ice
26. Warming- positive feedback - Cooling- negative feedback.
Ice-Albedo
Troposphere
Importance of ice sheets
How the cryosphere is affected by climate change
27. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Ice in the Arctic
Ocean water
Questions to think about
75-OC
28. 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
30%
Ice Shelf
Talik
29. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Black Carbon
Dry
Altimetry Cons
Types of Albedo
30. Industrial product - 300 ppb (parts per billion)
Reduction in sea-ice extent
Nitrous Oxide (N2O)
Altimetry Cons
doubles
31. 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
Deep tropics between 15O N and 15 O S are quite
Atlantic Thermohaline Circulation
El Nino
Mass Change
32. 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.
Melt
Inversion Layer (feedback)
Stratospheric Ozone Depletion
Sea-Ice Albedo
33. 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.
Threshold departures
Hydrological Drought
1 m/yr; 10x
Change in vegetation generates a further feedback
34. 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
Greenhouse Gases
Importance of ice sheets
.75OC/km-1
Ice Sheets
35. Antarctica - stratosphere - Sep-Oct
In the stratosphere.
Ozone Hole
Infrared radiation
Sublimation
36. Greenhouse gases are a ___ portion of the atmosphere
Grounding Lines
Surface Mass Balance
Very small portion
air can warm dramatically
37. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Frozen Soil
Precipitation and High Latitudes
7%
Positive feedbacks both found in...
38. 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) -
Ice-Albedo
Ocean water
Normal condition for air
Ice loss
39. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
Ice-Ocean Interactions
Active Layer
Frozen Soil
40. Like weighing oneself on the scale.
Sea-Ice Albedo
Time Variable Gravity
Thermohaline Circulation Effect
Layers of Earth
41. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Contributions to CO2 from different activities
Sea Ice
Depth v Surface
Ozone
42. Greenhouse gases are mixed in the ____
Where rise in OC is greatest
Monthly maximums and minimums
The Ozone Hole
Troposphere
43. Massive cooldown has allowed colder conditions to persist leading to cfcs stabilizing leading to ozone depletion. Later - more warming will lead to more moisture in the air which will lead to more snowfall!
Ice absorbs
Altimetry Cons
Antarctica
Permafrost
44. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Time Variable Gravity
Thermokarst
30%
Contributions to CO2 from different activities
45. Over the Northern Hemisphere than the tropics.
Ice Sheets
7%
Time Variable Gravity
Where rise in OC is greatest
46. Water vapor means more water up in the clouds and less in the ground!
Thermohaline Circulation
Depth v Surface
winter
More rain means no drought
47. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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48. Atmosphere retains ____ CO2
Global warming and hot nights?
Severe coastal erosion
45%
Percentile departures
49. Clouds 40~90% - Vegetation 10~15%
Permafrost Degradation
Types of Albedo
summer
45%
50. Radiation absorbed by atmospheric greenhouse gases?
GHG
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Agricultural Drought
Cloud Feedbacks