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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. 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
Climate Change in the Arctic
45%
Radiative Flux
Melt
2. LW - SW - 55% absorbed by surface
summer
Energy Budget
Ice in the Arctic
Thermohaline Circulation Effect
3. Is best viewed as a combination of...- Natural Variability - Associated with atmospheric circulation patterns - Growing Radiative Forcing - Associated with rising concentrations of atmospheric greenhouse gases - Strongly suggests a human influence.
Types of Albedo
Sunspots
Thickness of the active layer and the permafrost depend on this
Ice loss
4. Number of days that exceed a given temperature
Carbon Dioxide
Absolute thresholds
Depth v Surface
Energy Budget
5. 10 : 1 - grounding ; surface
Ice Motion
Antarctica
Atlantic Thermohaline Circulation
Grounding v Surface Melting
6. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Average radiative flux reaching the atmosphere
Sea-Ice Albedo
Sublimation
Is precipitation around the world increasing?
7. High cloud has a _____ effect and cool cloud has a ____ effect
IN the last 2 decades what we've seen
Thermohaline Circulation
El Nino
Warming; cooling
8. Rainy on yearly average. In these regions - rising air predominates.
25%
Deep tropics between 15O N and 15 O S are quite
Where rise in OC is greatest
.7O Celsius over the past century.
9. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Ice Cap
US and precipitation
Ice shelf
Absolute thresholds
10. Melting Point decreases
.75OC/km-1
Inversion Layer Summer
Atlantic Thermohaline Circulation
Absolute thresholds
11. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Ice/snow
Antarctica
Greenhouse Gases
air can warm dramatically
12. Precipitation intensity will rise ___ for every 1 OC of warming.
Ice-Albedo
7%
30%
Radiative Flux
13. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
In the troposphere that we live in.
Meteorological Drought
Normal condition for air
Altimetry Pros
14. A thick - floating slab of freshwater ice extending from coast to coast.
Layers of Earth
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ice shelf
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
15. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Surface Mass Balance
Ocean water
Rainy
Radiative Forcing
16. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
30%
Air pollution
Positive
Ice Sheets
17. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Active Layer
Affect Floods and Droughts
Sea-Ice Albedo
Altimetry (height)
18. A dome shaped cover of perennial ice and snow.
Antarctica
How to define a heatwave
Ice Cap
Archimedes' Principle
19. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
La Nia
Some regions of the Earth have warmed faster than other regions.
Mass Balance
75-OC
20. Where do greenhouse gases warm up the Earth?
Ozone Hole
In the troposphere that we live in.
Sea-Ice Albedo
Inversion Layer Summer
21. Land Based Ecosystems retain ____ CO2.
Greenhouse Gases
Very small portion
How the cryosphere is affected by climate change
30%
22. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Dynamic thinning
Albedos of Snow and Ice
summer
Discontinuous
23. Amount of light absorbed by surface
50%
Snow and snow covered ice absorb
Meteorological Drought
Antarctica
24. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Change in vegetation generates a further feedback
Dry
Heat Source and Pressure
30%
25. 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
Closed talik
Thermokarst
Ozone
Ice Sheets
26. 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
.7O Celsius over the past century.
Greenhouse Gases
Grounding v Surface Melting
27. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Methane
Shortwave Length
Greenland
doubles
28. The air can hold less water vapor - Consequently - less water can be evaporated in the air - and only a small portion of energy is used in this process - Most of the energy that reaches the Arctic goes directly into warming the air
Ozone Hole
What happens with the Ozone Hole
Inversion Layer Winter
In the Arctic where the air is cooler
29. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Grounding Lines
30%
The cryosphere
Inversion Layer Summer
30. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Thermokarst Lake
Sea Ice Extent is Changing in Antarctica as well
IPCC
Precipitation and High Latitudes
31. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
Positive feedbacks both found in...
The Ozone Hole
Positive
Atmospheric Circulation
32. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
45%
Why ice-albedo feedback is a big deal in the Arctic
Through talik
reduction in sea-ice
33. 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
Ice in the Arctic
Thinner atmosphere
Threshold departures
Albedos of Snow and Ice
34. Amount of light absorbed by atmosphere
Sunspots
20%
Today melting ice
Indirect heat wave effect
35. 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
Energy Budget
What effects the density
Some regions of the Earth have warmed faster than other regions.
36. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Negative
Sea Ice
Permafrost Degradation
Hydrological Drought
37. 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
Why ice-albedo feedback is a big deal in the Arctic
Air pollution
El Nino
.7O Celsius over the past century.
38. Industrial product - 300 ppb (parts per billion)
Snow and snow covered ice absorb
Talik
Antarctica
Nitrous Oxide (N2O)
39. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
45%
Ice Shelf
Surface Mass Balance
All Greenhouse gases
40. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Atmospheric Composition?
Grounding v Surface Melting
Is precipitation around the world increasing?
Active Layer
41. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Ozone
More rain means no drought
Air pollution
Atmospheric Composition
42. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Depth v Surface
Surface Mass Balance
25%
Increases - decreases
43. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Surface Mass Balance
Altimetry Cons
Snow and snow covered ice absorb
Black Carbon
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.
Why ice-albedo feedback is a big deal in the Arctic
Inversion Layer Winter
Ice in the Arctic
Ice Shelf
45. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Where rise in OC is greatest
Mass Balance
Accumulation
Altimetry Cons
46. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Open talik
Ice loss
Atlantic Thermohaline Circulation
How we measure Mass Balance
47. The amount of light reflected by an object.
Sea Ice
Layers of Earth
Amount of light actually reaching the Earth
Albedo
48. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Meteorological Drought
Open talik
In the Arctic where the air is cooler
Average radiative flux reaching the atmosphere
49. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
The cryosphere
Agricultural Drought
Ozone Hole
Ocean water
50. Number of days when temperatures climb above average by a fixed amount.
Deep tropics between 15O N and 15 O S are quite
How a closed talik forms
Threshold departures
Inversion Layer (feedback)