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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. High vs low
Troposphere
Sublimation
Cloud Feedbacks
Time Variable Gravity
2. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
All Greenhouse gases
Cause of break of inversion layers or decrease in frequency
Black Carbon
Negative
3. The buoyant force is equal to the weight of the displaced water.
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4. Really measures volume.
Active Layer
Ozone Hole
% of Greenhouse Gases
Altimetry
5. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Natural Causes of Warming
Stronger
Ocean water
The cryosphere
6. 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!
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Thickness of the active layer and the permafrost depend on this
Stronger
Antarctica
7. 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
Ice-Ocean Interactions
How talik forms under lakes
Ice shelf
8. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Dry
Ozone Hole
doubles
Active Layer
9. Water vapor means more water up in the clouds and less in the ground!
20%
More rain means no drought
Hydrological Drought
Radiative Flux
10. 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.
Sunspots
All Greenhouse gases
What effects the density
Sea Ice Extent is Changing in Antarctica as well
11. More common
Inversion Layer Winter
30%
Ice Sheets
How we measure Mass Balance
12. The amount of light reflected by an object.
All Greenhouse gases
Hydrological Drought
Albedo
Increases - decreases
13. Radiation absorbed by atmospheric greenhouse gases?
Natural Causes of Warming
Ice loss
Grounding Lines
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
14. 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
Reduction in sea-ice extent
Permafrost
Precipitation and High Latitudes
Agricultural Drought
15. Summer increase in cloud cover - Winter decrease in cloud cover.
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16. 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
Stratospheric Ozone Depletion
Heat wave
More rain means no drought
Ice Sheets
17. 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
Thermokarst
Wetter; drier
Thermokarst
Some regions of the Earth have warmed faster than other regions.
18. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Monthly maximums and minimums
Ice in the Arctic
Positive feedbacks both found in...
Importance of ice sheets
19. Arctic troposphere is thinner (8-10 km) than the tropics...The depth of the atmospheric layer is much shallower in the Arctic - It takes less energy to warm the Arctic rather than the Tropics - Same as heating an apartment vs. a house
70%
Average radiative flux reaching the atmosphere
Greenhouse Gases
Thinner atmosphere
20. High cloud has a _____ effect and cool cloud has a ____ effect
Thermohaline Circulatoin
The cryosphere
Warming; cooling
Where rise in OC is greatest
21. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Permafrost Degradation
Average radiative flux reaching the atmosphere
Ice Cap
Atmospheric Structure
22. O Unfrozen soil that stays within the permafrost.
US and precipitation
Albedo
Talik
Negative
23. 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 the cryosphere is affected by climate change
Methane
Thinner atmosphere
How talik forms under lakes
24. Ice sheets have a very ____ Albedo
Monthly maximums and minimums
Average radiative flux reaching the atmosphere
.75OC/km-1
Strong
25. Industrial product - 300 ppb (parts per billion)
Nitrous Oxide (N2O)
What happens with the Ozone Hole
Heat wave
Today melting ice
26. In average: +1% in respect to 100 years ago.
Contributions to CO2 from different activities
What happens with the Ozone Hole
Is precipitation around the world increasing?
Altimetry Cons
27. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
How the cryosphere is affected by climate change
Grounding Lines
Mass Balance
Open talik
28. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
25%
Hydrological Drought
The Ozone Hole
29. They saw a massive thinning of the ice where it enters into the ocean - This is due to the pronounced melting of the ice once it is in contact with the ocean. Melt rates of 25 m/year near the grounding lines and more than 10 m/year on average.
70%
How the cryosphere is affected by climate change
Ice-Ocean Interactions
Inversion Layer Winter
30. Greenhouse gases are mixed in the ____
Thermohaline Circulation
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Troposphere
Ozone Hole
31. LW - SW - 55% absorbed by surface
Permafrost
All Greenhouse gases
Energy Budget
Inversion Layer Summer
32. In _______ - the inversions are less frequent and weaker in the Arctic.
Severe coastal erosion
The cryosphere
summer
More rain means no drought
33. 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
Methane
Ocean water
El Nino
The cryosphere
34. 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
Thermohaline Circulation Effect
Warm
Thermohaline Circulation
35. Laser radar - H V - Long time series - high accuracy - Density
Altimetry (height)
Thermokarst Lake
Radiative Forcing
Antarctica
36. Less frequent and weaker
How a closed talik forms
Heat wave
Amount of light actually reaching the Earth
Inversion Layer Summer
37. ~10% of incident solar energy (albedo 90)
Permafrost Degradation
Increases - decreases
Ice absorbs
Why ice-albedo feedback is a big deal in the Arctic
38. 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
More rain means no drought
Dynamic thinning
Thermokarst
39. Precipitation intensity will rise ___ for every 1 OC of warming.
Albedo
7%
Mass Change
Today melting ice
40. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
7%
The cryosphere
Atmospheric Composition
Ice in the Arctic
41. 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
Melt
Earth's tilt
Importance of ice sheets
Shortwave Length
42. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Atmospheric Composition?
Antarctica
Absolute thresholds
Agricultural Drought
43. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
What effects the density
Normal condition for air
winter
44. 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.
Talik
Ice Shelf
Methane
Hydrological Drought
45. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Radiative Forcing
75-OC
45%
Methane
46. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
Cause of break of inversion layers or decrease in frequency
Surface Mass Balance
Arctic Atmosphere
47. Volcanic eruptions - Sunspots - Wobbly Earth
Climate Change in the Arctic
Inversion Layer (feedback)
Changes in Arctic sea-ice Extent
Natural Causes of Warming
48. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Thermokarst
Grounding Lines
Altimetry Cons
49. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Severe coastal erosion
GHG
Thermohaline Circulation Effect
Why the Arctic climate is special
50. How often does El Nio occur?
Once every 4 years.
Thinner atmosphere
How we measure Mass Balance
Deep tropics between 15O N and 15 O S are quite
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