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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. CO2 GHG forcing - H2O - dominant/major GHG
Ice Sheets
Frozen Soil
GHG
Ice-Ocean Interactions
2. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Average radiative flux reaching the atmosphere
In the troposphere that we live in.
Atmospheric Composition
All Greenhouse gases
3. Over the past century what has happened to the Earth's temperature?
Snow and snow covered ice absorb
Depth v Surface
Some regions of the Earth have warmed faster than other regions.
Very small portion
4. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Change in vegetation generates a further feedback
Sea Ice
Importance of ice sheets
In the troposphere that we live in.
5. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Arctic Atmosphere
Atlantic Thermohaline Circulation
Carbon Dioxide
Ice Shelf
6. Total absorbed solar radiation
Sublimation
70%
Methane
Hydrological Drought
7. Atmosphere retains ____ CO2
45%
Accumulation
Surface Mass Balance
Carbon Dioxide
8. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Active Layer
Surface Mass Balance
How a closed talik forms
Depth v Surface
9. Set up in 1988 by WMO and UNEP.
.7O Celsius over the past century.
IPCC
Troposphere
Major distinction between Kyoto Protocol and Convention
10. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Dynamic thinning
Stratospheric Ozone Depletion
Average radiative flux reaching the atmosphere
How we measure Mass Balance
11. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
How we measure Mass Balance
Layers of Earth
Ozone
El Nio is in the coasts of...
12. The amount of light reflected by an object.
Open talik
Albedo
Where rise in OC is greatest
Ozone Hole
13. 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.
Arctic Atmosphere
Inversion Layer (feedback)
Ice loss
Thermokarst
14. Under higher pressure the melting point decreases ____ - The pressure comes from the weight of the ice shelf.
75-OC
Permafrost
Talik
How talik forms under lakes
15. 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
GHG
El Nino
Thermohaline Circulation
Ocean water
16. 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.
Permafrost Degradation
Warming; cooling
Reduction in sea-ice extent
Agricultural Drought
17. Forms in a mosaic of favoured locations.
Carbon Dioxide
Discontinuous Permafrosrt
Where rise in OC is greatest
Altimetry Cons
18. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Ozone Hole
Monthly maximums and minimums
Atmospheric Composition?
Threshold departures
19. Number of days that land among the hottest of all days in that month's long-term record.
70%
Percentile departures
doubles
Ice in the Arctic
20. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Negative
Positive feedbacks both found in...
50%
Why the Arctic climate is special
21. The order of 1 m/year. Melting is ten times more.
doubles
Surface Mass Balance
Absolute thresholds
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
22. Descending Air dry - Convection cells are wet.
Percentile departures
Sea ice melt does not change sea level
Atmospheric Circulation
What effects the density
23. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Meteorological Drought
Through talik
Atlantic Thermohaline Circulation
Mass Change
24. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
Grounding v Surface Melting
All Greenhouse gases
La Nia
25. Radiation absorbed by atmospheric greenhouse gases?
In the troposphere that we live in.
Ozone Hole
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Thinner atmosphere
26. Sea ice - Glaciers and Ice sheets - Alaska- ice glaciers - Greenland- ice sheets
Altimetry Cons
.75OC/km-1
Ice in the Arctic
El Nino
27. Warming- positive feedback - Cooling- negative feedback.
Shortwave Length
Thermohaline Circulation
Ocean water
Ice-Albedo
28. A thick - floating slab of freshwater ice extending from coast to coast.
winter
Thermokarst Lake
Ice shelf
Frozen Soil
29. Longwave radiation - any radiation with a long wave will heat up quickly.
How we measure Mass Balance
Ice in the Arctic
Greenland
Infrared radiation
30. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Sublimation
IN the last 2 decades what we've seen
Earth's tilt
Precipitation and High Latitudes
31. 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) -
Normal condition for air
Radiative Flux
Inversion Layer Winter
20%
32. Land Based Ecosystems retain ____ CO2.
Archimedes' Principle
30%
Ocean water
Shortwave Length
33. Melting Point decreases
Longwave Radiation
.75OC/km-1
45%
Meteorological Drought
34. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
30%
IPCC
Types of Albedo
Depth v Surface
35. 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
Antarctica
IN the last 2 decades what we've seen
Why ice-albedo feedback is a big deal in the Arctic
Discontinuous Permafrosrt
36. O Unfrozen soil that stays within the permafrost.
Ice in the Arctic
La Nia
Talik
Ocean-Ice-Atmosphere Interaction
37. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Surface Mass Balance
Global warming and hot nights?
Indirect heat wave effect
Altimetry (height)
38. Soil at or below the freezing point of water for two or more years - Can be: Terrestrial - Subsea - Can be: Continuous: exists across a landscape as an unbroken layer. More than 90% is frozen - Discontinuous
45%
Permafrost
Atmospheric Composition
Amount of light actually reaching the Earth
39. 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
Nitrous Oxide (N2O)
Ice Sheets
Inversion Layer Summer
40. 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
Ice loss
Wetter; drier
Infrared radiation
Mass Balance
41. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Effect of Deforestation on CO-2
Monthly maximums and minimums
Questions to think about
% of Greenhouse Gases
42. 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
Is precipitation around the world increasing?
30%
Sea-Ice Albedo
43. US is responsible for ___ of the total CO2
7%
Longwave Radiation
30%
Heat Source and Pressure
44. 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
.7O Celsius over the past century.
Once every 4 years.
Ice in the Arctic
Agricultural Drought
45. 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
Sea ice melt does not change sea level
Atmospheric Structure
Radiative Flux
US and precipitation
46. O Climate change in the Arctic is occurring now - Changes have been huge already
% of Greenhouse Gases
Today melting ice
Thermokarst
Changes in Arctic sea-ice Extent
47. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
30%
Hydrological Drought
Average radiative flux reaching the atmosphere
Sunspots
48. Where do greenhouse gases warm up the Earth?
Sea Ice
Dynamic thinning
In the troposphere that we live in.
Ice Shelf
49. Number of days that exceed a given temperature
Absolute thresholds
Threshold departures
How we measure Mass Balance
More rain means no drought
50. Deep tropics between 15O N and 15 O S are quite rainy on yearly average. In these regions - rising air predominates.
Grounding Lines
Rainy
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
winter