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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. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
doubles
75-OC
Arctic Atmosphere
Monthly maximums and minimums
2. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
More rain means no drought
Why Water Vapor is not a climate forcing
Sea Ice Extent is Changing in Antarctica as well
Why the Arctic climate is special
3. 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%
Active Layer
Albedos of Snow and Ice
Dynamic thinning
Strong
4. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Some parts of the planet are dry because of their location
US and precipitation
Precipitation and High Latitudes
Radiative Forcing
5. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
How the cryosphere is affected by climate change
Positive
.7O Celsius over the past century.
Mass Balance
6. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
% of Greenhouse Gases
Grounding Lines
Depth v Surface
El Nio is in the coasts of...
7. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Depth v Surface
Ice in the Arctic
Melt
Sea Ice
8. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
doubles
Heat Source and Pressure
Negative Ice-Albedo Feedback
1 m/yr; 10x
9. Where do greenhouse gases warm up the Earth?
Climate Change in the Arctic
Through talik
In the troposphere that we live in.
Mass Budget
10. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Shortwave Length
Sea-Ice Albedo
Ice in the Arctic
25%
11. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Arctic Atmosphere
Global warming and hot nights?
Time Variable Gravity
Ice in the Arctic
12. 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.
Methane
.7O Celsius over the past century.
Closed talik
Climate Change in the Arctic
13. 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
Affect Floods and Droughts
Ice Shelf
Permafrost
winter
14. 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.
How talik forms under lakes
Dry
Open talik
Depth v Surface
15. Number of days that exceed a given temperature
Sea Ice Extent is Changing in Antarctica as well
Some regions of the Earth have warmed faster than other regions.
Agricultural Drought
Absolute thresholds
16. High cloud has a _____ effect and cool cloud has a ____ effect
Permafrost Degradation
Grounding Lines
Warming; cooling
Precipitation and High Latitudes
17. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Effect of Deforestation on CO-2
Sea Ice Extent is Changing in Antarctica as well
Stronger
How to define a heatwave
18. 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
Snow and snow covered ice absorb
Meteorological Drought
Mass Change
Reduction in sea-ice extent
19. The past climate...for this reason - both keep good records of climate change.
La Nia
Permafrost
Thickness of the active layer and the permafrost depend on this
Radiative Flux
20. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Hydrological Drought
Ice absorbs
Thermokarst
Radiative Flux
21. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
The Ozone Hole
Inversion Layer Winter
Thermokarst
Grounding Lines
22. 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
70%
Ice Sheets
Ice Motion
El Nino
23. South polar vortex - Temperatures drop below 80O Celsius in the lower stratosphere - At these temperatures the chemicals in the stratosphere freeze and form Polar Stratospheric Clouds (PSCS) - These increase the concentration of CFCs in turn destroyi
What happens with the Ozone Hole
Change in vegetation generates a further feedback
Today melting ice
winter
24. Precipitation intensity will rise ___ for every 1 OC of warming.
Where rise in OC is greatest
7%
Why the Arctic climate is special
Infrared radiation
25. Frozen +2 years - Few centimeters to 1500 m
Grounding Lines
Sea-Ice Albedo
Permafrost
La Nia
26. 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
Ice Motion
Indirect heat wave effect
Methane
Questions to think about
27. The Earth emits this.
Questions to think about
Longwave Radiation
Troposphere
Ice Discharge
28. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Greenland
Where rise in OC is greatest
.7O Celsius over the past century.
Accumulation
29. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Thermokarst
Methane
Why the Arctic climate is special
Air pollution
30. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
How to define a heatwave
Stratospheric Ozone Depletion
El Nio is in the coasts of...
Carbon Dioxide
31. 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
Stratospheric Ozone Depletion
Why ice-albedo feedback is a big deal in the Arctic
Ice Sheets
Altimetry
32. 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
How the cryosphere is affected by climate change
Once every 4 years.
Major distinction between Kyoto Protocol and Convention
Percentile departures
33. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Permafrost Degradation
1 m/yr; 10x
Through talik
34. Permafrost- A frozen soil
Frozen Soil
45%
Atmospheric Composition
1 m/yr; 10x
35. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Thermohaline Circulation
Strong
Open talik
Cloud Feedbacks
36. 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.
In the stratosphere.
Altimetry
Changes in Arctic sea-ice Extent
Ice-Albedo
37. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
How we measure Mass Balance
Through talik
El Nio is in the coasts of...
Energy Budget
38. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
El Nino
Heat wave
Calving
Thermohaline Circulation Effect
39. The amount of light reflected by an object.
Archimedes' Principle
Affect Floods and Droughts
Albedo
7%
40. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Black Carbon
Thermokarst
Some parts of the planet are dry because of their location
Why Water Vapor is not a climate forcing
41. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Agricultural Drought
Atmospheric Circulation
Ice shelf
Precipitation and High Latitudes
42. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Albedo
Carbon Dioxide
Thermokarst Lake
Mass Change
43. 240 w/m squared
Amount of light actually reaching the Earth
Today melting ice
Ice-Ocean Interactions
Antarctica
44. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Frozen Soil
US and precipitation
Importance of ice sheets
Affect Floods and Droughts
45. Extent 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.
Air pollution
reduction in sea-ice
Percentile departures
Negative Ice-Albedo Feedback
46. 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
Ocean water
Sea Ice Extent is Changing in Antarctica as well
Altimetry Pros
30%
47. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Mass Budget
Hydrological Drought
The cryosphere
Accumulation
48. Betts et al found that: if CO-2 __________ this has a physiological effect on plant transpiration increased simulated runoff by 6% b. How? i. More CO2 1. Plants pores open less 2. This reduces transpiration 3. More water in the land surface
Ocean water
Warm
doubles
Very small portion
49. Melting Point decreases
Mass Budget
Some regions of the Earth have warmed faster than other regions.
.75OC/km-1
Methane
50. Really measures volume.
Discontinuous Permafrosrt
Ice Cap
Affect Floods and Droughts
Altimetry