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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. Unfrozen ground that is found within a mass of permafrost
Altimetry
Inversion Layer Winter
Change in vegetation generates a further feedback
Closed talik
2. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
Altimetry Pros
US and precipitation
What effects the density
What happens with the Ozone Hole
3. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Carbon Dioxide
El Nino
Positive
Ozone Hole
4. 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) -
Greenhouse Gases
Normal condition for air
Ice Sheets
Active Layer
5. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Surface Mass Balance
Ice Shelf
Meteorological Drought
El Nio is in the coasts of...
6. Volcanic eruptions - Sunspots - Wobbly Earth
Today melting ice
Melt
Thermohaline Circulation Effect
Natural Causes of Warming
7. 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.
Dynamic thinning
Black Carbon
Altimetry Pros
Indirect heat wave effect
8. What can cause a change in the Earth's climate balance?
Amount of light actually reaching the Earth
Thermokarst Lake
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
summer
9. 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?
30%
Reduction in sea-ice extent
Atmospheric Circulation
10. 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
Infrared radiation
How talik forms under lakes
Melt
Threshold departures
11. Most of the deserts are around 30 N and 30 S - where sinking air predominates
Some parts of the planet are dry because of their location
Thermohaline Circulation
The cryosphere
Positive
12. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Rainy
GHG
Average radiative flux reaching the atmosphere
doubles
13. ~15% of incident solar energy (albedo 85)
Arctic Atmosphere
Active Layer
Warming; cooling
Snow and snow covered ice absorb
14. 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
Importance of ice sheets
Once every 4 years.
Ice-Albedo
Why the Arctic climate is special
15. 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
Heat wave
Heat Source and Pressure
Absolute thresholds
What happens with the Ozone Hole
16. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Atlantic Thermohaline Circulation
Heat Source and Pressure
Ozone
Grounding Lines
17. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Albedos of Snow and Ice
Increases - decreases
Earth's tilt
Atmospheric Composition
18. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Severe coastal erosion
Negative Ice-Albedo Feedback
Arctic Atmosphere
.7O Celsius over the past century.
19. Amount of light absorbed by atmosphere
20%
% of Greenhouse Gases
Altimetry Pros
Frozen Soil
20. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
How talik forms under lakes
Warming; cooling
Stronger
Sea Ice
21. Land Based Ecosystems retain ____ CO2.
How a closed talik forms
30%
Thinner atmosphere
air can warm dramatically
22. 10 : 1 - grounding ; surface
How we measure Mass Balance
Grounding v Surface Melting
Thickness of the active layer and the permafrost depend on this
Energy Budget
23. Industry 40% - Buildings 31% - Transportations 22% - Agriculture 4%
Ice shelf
Greenhouse Gases
Contributions to CO2 from different activities
How we measure Mass Balance
24. 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.
In the stratosphere.
Ice Cap
Climate Change in the Arctic
Time Variable Gravity
25. 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.
In the stratosphere.
Change in vegetation generates a further feedback
Climate Change in the Arctic
Stronger
26. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Severe coastal erosion
Air pollution
US and precipitation
Stratospheric Ozone Depletion
27. 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
Permafrost Degradation
Radiative Forcing
Stratospheric Ozone Depletion
Why the Arctic climate is special
28. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Depth v Surface
75-OC
Sea Ice
% of Greenhouse Gases
29. 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.
Climate Change in the Arctic
Antarctica
Cause of break of inversion layers or decrease in frequency
How talik forms under lakes
30. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Absolute thresholds
Sea Ice
Energy Budget
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
31. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Through talik
Hydrological Drought
Atlantic Thermohaline Circulation
Questions to think about
32. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
45%
Ocean-Ice-Atmosphere Interaction
Radiative Forcing
Permafrost
33. The order of 1 m/year. Melting is ten times more.
Stronger
Heat wave
Surface Mass Balance
winter
34. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
How to define a heatwave
Affect Floods and Droughts
In the Arctic where the air is cooler
summer
35. 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
doubles
Calving
Inversion Layer Summer
Permafrost
36. A mass of land ice - continental or sub-continental in extent - and thick enough to cover most of the underlying bedrock topography - If you have a warm ocean - it will melt the ice sheet. Its shape is mainly determined by the dynamics of its outward
7%
Carbon Dioxide
Ice Sheets
Ice Discharge
37. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Longwave Radiation
Meteorological Drought
Ice/snow
Methane
38. 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 Discharge
Ice in the Arctic
Questions to think about
Wetter; drier
39. How often does El Nio occur?
Once every 4 years.
Threshold departures
Ice Discharge
In the stratosphere.
40. A naturally or artificially caused decrease in the thickness and/or areal extent of permafrost - It is caused by the deepening fo the active layer and the thawing of the adjacent permafrost.
Discontinuous Permafrosrt
Ice-Ocean Interactions
How talik forms under lakes
Permafrost Degradation
41. Is not an externally imposed perturbation to the climate system.
Reduction in sea-ice extent
Altimetry
Altimetry (height)
Why Water Vapor is not a climate forcing
42. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Effect of Deforestation on CO-2
Methane
Meteorological Drought
Discontinuous
43. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
30%
Monthly maximums and minimums
Surface Mass Balance
% of Greenhouse Gases
44. The Earth emits this.
Earth's tilt
Atlantic Thermohaline Circulation
.75OC/km-1
Longwave Radiation
45. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Earth's tilt
Grounding Lines
Hydrological Drought
Surface Mass Balance
46. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
How we measure Mass Balance
Accumulation
Surface Mass Balance
Ice Discharge
47. Amount of light absorbed by surface
50%
Severe coastal erosion
Normal condition for air
Atmospheric Structure
48. 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.
Indirect heat wave effect
Inversion Layer (feedback)
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Open talik
49. 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
Mass Change
Contributions to CO2 from different activities
Wetter; drier
Melt
50. Surface Mass Balance is of the order of _____ melting is ____ times more.
1 m/yr; 10x
reduction in sea-ice
Some regions of the Earth have warmed faster than other regions.
IN the last 2 decades what we've seen