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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. The Earth emits this.
Longwave Radiation
Arctic Atmosphere
Radiative Forcing
Mass Balance
2. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Active Layer
Warm
More rain means no drought
70%
3. Summer increase in cloud cover - Winter decrease in cloud cover.
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4. 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.
Some regions of the Earth have warmed faster than other regions.
Change in vegetation generates a further feedback
IPCC
Greenland
5. CO2 - CH4 - O3 - H2O - N2O - CFCs
Ice-Albedo
Ocean water
Precipitation and High Latitudes
All Greenhouse gases
6. 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.
Ice-Ocean Interactions
Thermohaline Circulation
Energy Budget
Ice in the Arctic
7. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Shortwave Length
Hydrological Drought
Albedo
.75OC/km-1
8. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Warm
Monthly maximums and minimums
What effects the density
Ozone Hole
9. Where does the ozone protect us?
Negative
In the stratosphere.
Positive feedbacks both found in...
Albedo
10. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Greenhouse Gases
Energy Budget
Climate Change in the Arctic
Sublimation
11. 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.
Changes in Arctic sea-ice Extent
Inversion Layer (feedback)
7%
Ozone
12. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Thermohaline Circulation
Atmospheric Structure
Affect Floods and Droughts
Ice loss
13. Frozen +2 years - Few centimeters to 1500 m
Permafrost
Ice Cap
7%
Albedo
14. 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
Inversion Layer Winter
Thermohaline Circulatoin
Some regions of the Earth have warmed faster than other regions.
Thinner atmosphere
15. A thick - floating slab of freshwater ice extending from coast to coast.
Permafrost
Ice-Albedo
Ice shelf
Strong
16. O The amount of energy moving in the form of photons or other elementary particles at a certain distance from the source per unit of area per second. Area/second
45%
In the stratosphere.
Radiative Flux
Affect Floods and Droughts
17. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
Heat Source and Pressure
Negative
Permafrost
Questions to think about
18. 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
Agricultural Drought
Types of Albedo
Atmospheric Composition?
Altimetry Pros
19. ~15% of incident solar energy (albedo 85)
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Snow and snow covered ice absorb
Thermokarst
Surface Mass Balance
20. In ________- inversion layer is more common in the Arctic
Rainy
winter
Stronger
Sunspots
21. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Global warming and hot nights?
Atmospheric Composition
Methane
US and precipitation
22. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Indirect heat wave effect
Today melting ice
Active Layer
% of Greenhouse Gases
23. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Positive
Questions to think about
Ice in the Arctic
Why the Arctic climate is special
24. Greenhouse gases are a ___ portion of the atmosphere
Stronger
Greenland
Very small portion
Calving
25. Less frequent and weaker
How talik forms under lakes
Carbon Dioxide
Dynamic thinning
Inversion Layer Summer
26. Is not an externally imposed perturbation to the climate system.
Why Water Vapor is not a climate forcing
Snow and snow covered ice absorb
Earth's tilt
Thermokarst Lake
27. 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
Albedos of Snow and Ice
Earth's tilt
Ice in the Arctic
28. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Depth v Surface
Greenland
Stronger
Sea Ice
29. How often does El Nio occur?
Melt
Once every 4 years.
air can warm dramatically
Reduction in sea-ice extent
30. 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.
US and precipitation
How talik forms under lakes
Normal condition for air
Ozone Hole
31. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Time Variable Gravity
Ice Shelf
Contributions to CO2 from different activities
Accumulation
32. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Talik
30%
Reduction in sea-ice extent
Ice/snow
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
Thermohaline Circulation
Percentile departures
Ice Sheets
El Nino
34. The order of 1 m/year. Melting is ten times more.
La Nia
Troposphere
Dynamic thinning
Surface Mass Balance
35. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Methane
Ice Sheets
La Nia
Through talik
36. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Changes in Arctic sea-ice Extent
Albedo
Ice Motion
How the cryosphere is affected by climate change
37. Where do greenhouse gases warm up the Earth?
Mass Balance
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Threshold departures
In the troposphere that we live in.
38. Atmosphere retains ____ CO2
How we measure Mass Balance
Surface Mass Balance
Very small portion
45%
39. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
Troposphere
IPCC
Types of Albedo
El Nio is in the coasts of...
40. 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) -
How we measure Mass Balance
% of Greenhouse Gases
Energy Budget
Normal condition for air
41. Amount of light absorbed by atmosphere
Stronger
20%
Sea-Ice Albedo
How talik forms under lakes
42. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Stratospheric Ozone Depletion
Radiative Forcing
50%
Ozone Hole
43. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Permafrost
How we measure Mass Balance
Stronger
Radiative Flux
44. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
Severe coastal erosion
US and precipitation
Ice Cap
45. Amount of light absorbed by surface
50%
doubles
Accumulation
Atmospheric Composition
46. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Positive feedbacks both found in...
How to define a heatwave
50%
Surface Mass Balance
47. 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%
Albedos of Snow and Ice
Once every 4 years.
Archimedes' Principle
Stratospheric Ozone Depletion
48. The past climate...for this reason - both keep good records of climate change.
Ice Motion
Methane
Ozone Hole
Thickness of the active layer and the permafrost depend on this
49. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Positive
Average radiative flux reaching the atmosphere
Ozone
Warm
50. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Heat Source and Pressure
Greenhouse Gases
summer
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