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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. 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
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Troposphere
30%
2. Forms in a mosaic of favoured locations.
Discontinuous Permafrosrt
winter
Ice Sheets
reduction in sea-ice
3. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Amount of light actually reaching the Earth
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Some parts of the planet are dry because of their location
The cryosphere
4. Greenhouse gases are mixed in the ____
Thinner atmosphere
El Nio is in the coasts of...
Troposphere
Mass Balance
5. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Surface Mass Balance
Atlantic Thermohaline Circulation
30%
Heat wave
6. 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
Thermohaline Circulation
Radiative Flux
Ice Shelf
Open talik
7. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Stratospheric Ozone Depletion
Ice-Albedo
Ice in the Arctic
Calving
8. More common
20%
Heat wave
Inversion Layer Winter
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
9. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Antarctica
Ice-Albedo
Wetter; drier
Sea Ice Extent is Changing in Antarctica as well
10. Melting Point decreases
.75OC/km-1
Once every 4 years.
Altimetry (height)
Thinner atmosphere
11. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Ice Sheets
summer
Ice in the Arctic
Warm
12. 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%
More rain means no drought
Methane
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Albedos of Snow and Ice
13. Is not an externally imposed perturbation to the climate system.
Precipitation and High Latitudes
Albedo
Albedos of Snow and Ice
Why Water Vapor is not a climate forcing
14. Water vapor means more water up in the clouds and less in the ground!
Through talik
The Ozone Hole
More rain means no drought
Positive
15. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Ice shelf
Ocean-Ice-Atmosphere Interaction
.75OC/km-1
% of Greenhouse Gases
16. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Hydrological Drought
Changes in Arctic sea-ice Extent
Strong
More rain means no drought
17. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Thermokarst Lake
Negative
Precipitation and High Latitudes
Antarctica
18. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Today melting ice
30%
Antarctica
Layers of Earth
19. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Snow and snow covered ice absorb
75-OC
Accumulation
Ice-Albedo
20. The buoyant force is equal to the weight of the displaced water.
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21. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Mass Budget
Sea-Ice Albedo
Thermohaline Circulation
22. The amount of light reflected by an object.
Surface Mass Balance
Atmospheric Composition
Albedo
Inversion Layer (feedback)
23. Cooler water and drought conditions.
Longwave Radiation
La Nia
Positive
Ozone Hole
24. The major distinction between the Protocol and the Convention is that while the Convention encouraged industrialized countries to stabilize GHG emissions - the Protocol commits them to do so.
Affect Floods and Droughts
Ice shelf
Major distinction between Kyoto Protocol and Convention
Thermohaline Circulation
25. High vs low
Hydrological Drought
Cloud Feedbacks
Stronger
Positive feedbacks both found in...
26. LW - SW - 55% absorbed by surface
% of Greenhouse Gases
Energy Budget
Why ice-albedo feedback is a big deal in the Arctic
Calving
27. 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
Wetter; drier
Radiative Forcing
What effects the density
Thermokarst
28. O Unfrozen soil that stays within the permafrost.
Discontinuous Permafrosrt
Ice shelf
Talik
Ice loss
29. Amount of light absorbed by atmosphere
20%
How talik forms under lakes
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
IN the last 2 decades what we've seen
30. Set up in 1988 by WMO and UNEP.
IPCC
Atmospheric Structure
Radiative Flux
Once every 4 years.
31. 1.4 USA - 57 m total sea level equivalent
Sea Ice
Antarctica
Thinner atmosphere
summer
32. 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
Sea ice melt does not change sea level
Thermohaline Circulation
Today melting ice
Dry
33. 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
Greenland
El Nino
Importance of ice sheets
Negative Ice-Albedo Feedback
34. Ocean retains ____ CO2
Sea-Ice Albedo
25%
Ice in the Arctic
30%
35. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Increases - decreases
Cloud Feedbacks
Positive
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
36. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
Affect Floods and Droughts
Why ice-albedo feedback is a big deal in the Arctic
Arctic Atmosphere
Meteorological Drought
37. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Air pollution
Thermokarst
summer
Hydrological Drought
38. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Inversion Layer Summer
Increases - decreases
Calving
Percentile departures
39. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Thermokarst
Mass Balance
Where rise in OC is greatest
How we measure Mass Balance
40. Total absorbed solar radiation
El Nino
70%
Inversion Layer Summer
Accumulation
41. ~15% of incident solar energy (albedo 85)
Melt
Affect Floods and Droughts
Nitrous Oxide (N2O)
Snow and snow covered ice absorb
42. 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.
Time Variable Gravity
Altimetry
Change in vegetation generates a further feedback
Sunspots
43. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
What effects the density
Sea Ice
Albedos of Snow and Ice
Ice absorbs
44. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Dry
Indirect heat wave effect
Shortwave Length
45. A dome shaped cover of perennial ice and snow.
Sunspots
IN the last 2 decades what we've seen
Ozone Hole
Ice Cap
46. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Sea Ice Extent is Changing in Antarctica as well
Depth v Surface
Nitrous Oxide (N2O)
summer
47. Amount of light absorbed by surface
25%
Energy Budget
50%
Strong
48. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
% of Greenhouse Gases
summer
Reduction in sea-ice extent
Dry
49. Unfrozen ground that is found within a mass of permafrost
Questions to think about
Closed talik
1 m/yr; 10x
Time Variable Gravity
50. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
25%
Heat Source and Pressure
Inversion Layer Winter
More rain means no drought
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