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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. A dome shaped cover of perennial ice and snow.
Cloud Feedbacks
La Nia
summer
Ice Cap
2. 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
El Nino
Why the Arctic climate is special
Grounding Lines
Permafrost
3. Precipitation intensity will rise ___ for every 1 OC of warming.
Severe coastal erosion
Increases - decreases
Ice shelf
7%
4. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Sea Ice Extent is Changing in Antarctica as well
air can warm dramatically
% of Greenhouse Gases
Methane
5. 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.
Indirect heat wave effect
How a closed talik forms
Greenhouse Gases
Ice shelf
6. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Nitrous Oxide (N2O)
Altimetry Pros
Albedos of Snow and Ice
Shortwave Length
7. How much is the planet really warming?
Albedo
20%
.7O Celsius over the past century.
Grounding v Surface Melting
8. In ________- inversion layer is more common in the Arctic
La Nia
Reduction in sea-ice extent
winter
Surface Mass Balance
9. 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%
Indirect heat wave effect
Absolute thresholds
Albedos of Snow and Ice
Negative Ice-Albedo Feedback
10. Greenhouse gases are a ___ portion of the atmosphere
Ice/snow
Types of Albedo
Very small portion
Ice Cap
11. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Why the Arctic climate is special
Some parts of the planet are dry because of their location
What effects the density
12. Like weighing oneself on the scale.
Sunspots
30%
Time Variable Gravity
What effects the density
13. 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
% of Greenhouse Gases
Normal condition for air
Ocean-Ice-Atmosphere Interaction
14. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Altimetry Cons
Ice absorbs
summer
Ice/snow
15. 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.
How to define a heatwave
reduction in sea-ice
Thermohaline Circulation Effect
Climate Change in the Arctic
16. The amount of light reflected by an object.
Sea ice melt does not change sea level
Antarctica
Albedo
Major distinction between Kyoto Protocol and Convention
17. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Melt
Through talik
Sublimation
Greenland
18. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Effect of Deforestation on CO-2
Methane
El Nio is in the coasts of...
30%
19. CO2 - CH4 - O3 - H2O - N2O - CFCs
Ice/snow
All Greenhouse gases
Open talik
Positive
20. Ocean retains ____ CO2
Sublimation
Altimetry Cons
Why the Arctic climate is special
25%
21. ~15% of incident solar energy (albedo 85)
Inversion Layer Summer
Altimetry
Monthly maximums and minimums
Snow and snow covered ice absorb
22. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Inversion Layer Summer
Grounding Lines
Sea ice melt does not change sea level
What happens with the Ozone Hole
23. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Atmospheric Composition?
Ice shelf
Very small portion
Precipitation and High Latitudes
24. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Nitrous Oxide (N2O)
Greenhouse Gases
Dynamic thinning
Grounding Lines
25. Rainy on yearly average. In these regions - rising air predominates.
Depth v Surface
Antarctica
50%
Deep tropics between 15O N and 15 O S are quite
26. 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
US and precipitation
Thickness of the active layer and the permafrost depend on this
Why ice-albedo feedback is a big deal in the Arctic
How to define a heatwave
27. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Change in vegetation generates a further feedback
Atmospheric Composition
% of Greenhouse Gases
Ice-Ocean Interactions
28. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
How a closed talik forms
Cause of break of inversion layers or decrease in frequency
Meteorological Drought
reduction in sea-ice
29. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
Time Variable Gravity
Thermohaline Circulatoin
Wetter; drier
30. The past climate...for this reason - both keep good records of climate change.
In the stratosphere.
Thickness of the active layer and the permafrost depend on this
IN the last 2 decades what we've seen
Ocean water
31. A thick - floating slab of freshwater ice extending from coast to coast.
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Dry
Ice shelf
Shortwave Length
32. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Permafrost
Discontinuous
Increases - decreases
What happens with the Ozone Hole
33. In _______ - the inversions are less frequent and weaker in the Arctic.
Surface Mass Balance
La Nia
Atmospheric Circulation
summer
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
Heat Source and Pressure
Ice Sheets
Positive feedbacks both found in...
Importance of ice sheets
35. 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.
Negative Ice-Albedo Feedback
Once every 4 years.
Ocean water
reduction in sea-ice
36. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Sea Ice
Closed talik
Ice-Albedo
Active Layer
37. 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
Antarctica
Reduction in sea-ice extent
Infrared radiation
38. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Amount of light actually reaching the Earth
Thermohaline Circulation Effect
Active Layer
Positive
39. 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.
Ozone
Changes in Arctic sea-ice Extent
Energy Budget
What effects the density
40. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ice Sheets
45%
Is precipitation around the world increasing?
Ocean water
41. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
US and precipitation
Altimetry
Air pollution
Mass Balance
42. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
Dry
75-OC
.7O Celsius over the past century.
Some parts of the planet are dry because of their location
43. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Negative Ice-Albedo Feedback
Thermohaline Circulation Effect
The Ozone Hole
Earth's tilt
44. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
Warming; cooling
Cloud Feedbacks
30%
45. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Altimetry Cons
Wetter; drier
Greenland
46. Where do greenhouse gases warm up the Earth?
Frozen Soil
In the troposphere that we live in.
Ice Sheets
Heat Source and Pressure
47. Longwave radiation - any radiation with a long wave will heat up quickly.
Positive
Altimetry Pros
In the troposphere that we live in.
Infrared radiation
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
US and precipitation
How we measure Mass Balance
doubles
Thermokarst
49. 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.
Agricultural Drought
How talik forms under lakes
Inversion Layer Winter
Warm
50. 10 : 1 - grounding ; surface
Grounding v Surface Melting
Discontinuous Permafrosrt
Permafrost
70%