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Test your basic knowledge |
Global Warming
Start Test
Study First
Subjects
:
literacy
,
science
Instructions:
Answer 50 questions in 15 minutes.
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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 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
Ice-Albedo
Altimetry
Why the Arctic climate is special
In the Arctic where the air is cooler
2. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
% of Greenhouse Gases
30%
Dynamic thinning
Change in vegetation generates a further feedback
3. Clouds 40~90% - Vegetation 10~15%
Earth's tilt
Altimetry (height)
Sunspots
Types of Albedo
4. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
US and precipitation
Strong
air can warm dramatically
20%
5. 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
Precipitation and High Latitudes
Warm
.7O Celsius over the past century.
6. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Active Layer
The cryosphere
Indirect heat wave effect
In the stratosphere.
7. 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
Hydrological Drought
Wetter; drier
Reduction in sea-ice extent
Ice absorbs
8. 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
.7O Celsius over the past century.
Troposphere
Surface Mass Balance
9. Climate models suggest once the sea ice cover is thinned sufficiently - a strong kick from natural variability could initiate a rapid slide towards ice-free conditions in the summer.
What effects the density
Accumulation
Changes in Arctic sea-ice Extent
Climate Change in the Arctic
10. Melting Point decreases
Amount of light actually reaching the Earth
Meteorological Drought
Altimetry (height)
.75OC/km-1
11. 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
Shortwave Length
Closed talik
Through talik
Why ice-albedo feedback is a big deal in the Arctic
12. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
How talik forms under lakes
Air pollution
Arctic Atmosphere
Sea Ice
13. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Contributions to CO2 from different activities
Ozone Hole
Ozone Hole
Deep tropics between 15O N and 15 O S are quite
14. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
Global warming and hot nights?
Air pollution
La Nia
Energy Budget
15. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Thermokarst
Arctic Atmosphere
Some regions of the Earth have warmed faster than other regions.
Thermohaline Circulatoin
16. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
The Ozone Hole
IPCC
Surface Mass Balance
17. 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.
30%
Increases - decreases
doubles
Inversion Layer (feedback)
18. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Thermokarst
Ocean water
Ice in the Arctic
Arctic Atmosphere
19. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Ice Sheets
Ocean-Ice-Atmosphere Interaction
Ice Discharge
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
20. Antarctica - stratosphere - Sep-Oct
Thinner atmosphere
Earth's tilt
Ozone Hole
Affect Floods and Droughts
21. Cooler water and drought conditions.
Melt
La Nia
Reduction in sea-ice extent
Closed talik
22. Summer increase in cloud cover - Winter decrease in cloud cover.
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23. Radiation absorbed by atmospheric greenhouse gases?
Arctic Atmosphere
Permafrost Degradation
Indirect heat wave effect
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
24. Total absorbed solar radiation
El Nino
Calving
70%
Thermokarst
25. Number of days that land among the hottest of all days in that month's long-term record.
Percentile departures
The cryosphere
Some parts of the planet are dry because of their location
Energy Budget
26. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Calving
Cloud Feedbacks
Thermohaline Circulatoin
Radiative Forcing
27. Measures input and output.
Mass Budget
The cryosphere
Amount of light actually reaching the Earth
How talik forms under lakes
28. Laser radar - H V - Long time series - high accuracy - Density
Calving
Altimetry (height)
summer
Archimedes' Principle
29. 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:
Thermohaline Circulation
In the troposphere that we live in.
Active Layer
Radiative Flux
30. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Rainy
Global warming and hot nights?
La Nia
25%
31. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Grounding Lines
Ocean water
Mass Balance
Natural Causes of Warming
32. 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%
Permafrost
70%
Time Variable Gravity
Albedos of Snow and Ice
33. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Atlantic Thermohaline Circulation
In the stratosphere.
Stratospheric Ozone Depletion
Time Variable Gravity
34. 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.
Closed talik
Ice Shelf
Why ice-albedo feedback is a big deal in the Arctic
Ocean-Ice-Atmosphere Interaction
35. Long time series started in the '70s and yielding good data in the '90s - Detects elevation with high accuracy: 10 cm precision (laser) to 1 m (radar) - 2/3 Gravity Surveys (GRACE) - Weighing the total mass every 30 days - Direct monthly estimate
7%
Heat wave
Altimetry Pros
The Ozone Hole
36. 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) -
Radiative Forcing
El Nino
Normal condition for air
Atmospheric Circulation
37. The past climate...for this reason - both keep good records of climate change.
Surface Mass Balance
Contributions to CO2 from different activities
Atmospheric Composition?
Thickness of the active layer and the permafrost depend on this
38. Is not an externally imposed perturbation to the climate system.
Mass Change
Positive feedbacks both found in...
Today melting ice
Why Water Vapor is not a climate forcing
39. Wet gets _____ - dry gets ____ - Wet - 50ON (sub polar) Canada - N Europe - Russia - Tropical area- monsoon (rainforest) - Drier - Subtropics - Australia - S. Africa - Mediterranean - Caribbean - Mexico - SW US
Infrared radiation
Ice Sheets
Wetter; drier
Ice Shelf
40. 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.
Increases - decreases
Atmospheric Circulation
Altimetry
Indirect heat wave effect
41. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
% of Greenhouse Gases
How to define a heatwave
Altimetry
How talik forms under lakes
42. Is best viewed as a combination of...- Natural Variability - Associated with atmospheric circulation patterns - Growing Radiative Forcing - Associated with rising concentrations of atmospheric greenhouse gases - Strongly suggests a human influence.
Ice loss
Very small portion
IPCC
Ice Shelf
43. How often does El Nio occur?
Calving
Some parts of the planet are dry because of their location
Ozone
Once every 4 years.
44. 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
Why the Arctic climate is special
Warming; cooling
Active Layer
Talik
45. 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
Negative
How the cryosphere is affected by climate change
Ice Sheets
Warming; cooling
46. Precipitation intensity will rise ___ for every 1 OC of warming.
US and precipitation
Thermokarst Lake
7%
Inversion Layer Summer
47. 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
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Some regions of the Earth have warmed faster than other regions.
Where rise in OC is greatest
Melt
48. High vs low
summer
Earth's tilt
Cloud Feedbacks
Melt
49. Number of days when temperatures climb above average by a fixed amount.
Monthly maximums and minimums
Inversion Layer Winter
Discontinuous Permafrosrt
Threshold departures
50. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
Thickness of the active layer and the permafrost depend on this
Grounding Lines
Climate Change in the Arctic
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