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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. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
45%
Ice in the Arctic
20%
Albedo
2. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
Accumulation
Amount of light actually reaching the Earth
Strong
3. 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
Changes in Arctic sea-ice Extent
Thinner atmosphere
Precipitation and High Latitudes
Active Layer
4. The amount of light reflected by an object.
Albedo
Longwave Radiation
Severe coastal erosion
doubles
5. Some parts of the planet are dry because of their location: most of the deserts are around 30 N and 30 S - where sinking air predominates
Radiative Forcing
How we measure Mass Balance
Thermohaline Circulation Effect
Dry
6. Just remember the general direction of the circulation - Rising northern pacific. You start in between Greenland and Europe (youngest water) - Oldest water is in the Pacific Ocean - Salty water> fresh water - Cold Water > Warm Water
Once every 4 years.
The Ozone Hole
Thermohaline Circulation
Calving
7. More common
doubles
Inversion Layer Winter
Threshold departures
Severe coastal erosion
8. Set up in 1988 by WMO and UNEP.
Positive feedbacks both found in...
IPCC
Normal condition for air
The cryosphere
9. Frozen +2 years - Few centimeters to 1500 m
Ice in the Arctic
Threshold departures
doubles
Permafrost
10. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Thickness of the active layer and the permafrost depend on this
Threshold departures
75-OC
Precipitation and High Latitudes
11. 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
Agricultural Drought
Antarctica
Questions to think about
Stronger
12. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Nitrous Oxide (N2O)
Ice-Ocean Interactions
Normal condition for air
Arctic Atmosphere
13. Amount of light absorbed by surface
Ocean water
Warming; cooling
50%
Ice-Ocean Interactions
14. 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
Melt
Natural Causes of Warming
Why ice-albedo feedback is a big deal in the Arctic
70%
15. Radiation absorbed by atmospheric greenhouse gases?
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Permafrost Degradation
Ice-Ocean Interactions
Ice Sheets
16. In average: +1% in respect to 100 years ago.
Importance of ice sheets
GHG
Is precipitation around the world increasing?
How talik forms under lakes
17. Ocean retains ____ CO2
The Ozone Hole
Melt
25%
Thinner atmosphere
18. 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
Normal condition for air
Time Variable Gravity
doubles
Precipitation and High Latitudes
19. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Ocean water
Why ice-albedo feedback is a big deal in the Arctic
El Nino
Atmospheric Structure
20. 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.
What happens with the Ozone Hole
Black Carbon
Negative Ice-Albedo Feedback
Indirect heat wave effect
21. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Heat Source and Pressure
Why Water Vapor is not a climate forcing
Meteorological Drought
Atmospheric Composition
22. Surface Mass Balance is of the order of _____ melting is ____ times more.
1 m/yr; 10x
The cryosphere
Greenland
Antarctica
23. Laser radar - H V - Long time series - high accuracy - Density
Inversion Layer Winter
Greenland
All Greenhouse gases
Altimetry (height)
24. Descending Air dry - Convection cells are wet.
How to define a heatwave
Albedo
Warming; cooling
Atmospheric Circulation
25. 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%
Thinner atmosphere
Climate Change in the Arctic
Albedos of Snow and Ice
Changes in Arctic sea-ice Extent
26. ~10% of incident solar energy (albedo 90)
Stronger
Ice absorbs
Is precipitation around the world increasing?
Atmospheric Composition
27. 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.
Very small portion
Sunspots
How talik forms under lakes
Time Variable Gravity
28. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Positive feedbacks both found in...
Contributions to CO2 from different activities
What happens with the Ozone Hole
Inversion Layer Winter
29. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Ice Cap
Calving
Altimetry Cons
Energy Budget
30. Is not an externally imposed perturbation to the climate system.
Why Water Vapor is not a climate forcing
Ozone Hole
Greenland
Thermohaline Circulatoin
31. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Greenhouse Gases
Radiative Forcing
Ice loss
Shortwave Length
32. Cooler water and drought conditions.
Snow and snow covered ice absorb
La Nia
Energy Budget
Through talik
33. The past climate...for this reason - both keep good records of climate change.
Wetter; drier
Thickness of the active layer and the permafrost depend on this
Very small portion
Types of Albedo
34. 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
Altimetry Pros
Air pollution
How the cryosphere is affected by climate change
The cryosphere
35. 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 Sheets
Ice-Ocean Interactions
Permafrost Degradation
36. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
30%
Severe coastal erosion
Sublimation
Ice Discharge
37. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Ocean water
Sublimation
Permafrost Degradation
Effect of Deforestation on CO-2
38. ~15% of incident solar energy (albedo 85)
Snow and snow covered ice absorb
Where rise in OC is greatest
Permafrost
Arctic Atmosphere
39. 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
Antarctica
30%
Radiative Flux
40. Precipitation intensity will rise ___ for every 1 OC of warming.
Grounding Lines
7%
Altimetry (height)
Ice loss
41. Rainy on yearly average. In these regions - rising air predominates.
US and precipitation
Deep tropics between 15O N and 15 O S are quite
Ocean water
IPCC
42. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Thermokarst
Stronger
winter
Ice Motion
43. Where does the ozone protect us?
Warm
Atmospheric Composition?
Negative Ice-Albedo Feedback
In the stratosphere.
44. 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.
Sea Ice
Agricultural Drought
Greenhouse Gases
% of Greenhouse Gases
45. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
summer
Thermohaline Circulation
Thickness of the active layer and the permafrost depend on this
46. 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
Reduction in sea-ice extent
Thermokarst
Inversion Layer (feedback)
45%
47. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
In the Arctic where the air is cooler
Air pollution
Ozone
Active Layer
48. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Amount of light actually reaching the Earth
Black Carbon
1 m/yr; 10x
Ocean water
49. 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.
Global warming and hot nights?
air can warm dramatically
What effects the density
Rainy
50. The Earth emits this.
Longwave Radiation
How to define a heatwave
Surface Mass Balance
Heat wave
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