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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. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
50%
Troposphere
Mass Budget
2. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
75-OC
Active Layer
Methane
Sea-Ice Albedo
3. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Altimetry Pros
Grounding Lines
Greenhouse Gases
Positive
4. 240 w/m squared
La Nia
How we measure Mass Balance
Increases - decreases
Amount of light actually reaching the Earth
5. Average molecular life span is less than 10 years - Major sources: Wetlands and oceans - Raising cattle and landfills.
Methane
Ice Shelf
20%
Ocean water
6. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Ocean-Ice-Atmosphere Interaction
Changes in Arctic sea-ice Extent
Atmospheric Composition?
Permafrost Degradation
7. 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
Radiative Flux
Permafrost
Air pollution
summer
8. 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%
Deep tropics between 15O N and 15 O S are quite
Why Water Vapor is not a climate forcing
Albedos of Snow and Ice
In the troposphere that we live in.
9. At the bottom of the ice sheets the temperature doesn't necessarily have to be above 0... it could _____ more easily because of the water
Melt
Sea-Ice Albedo
Ice in the Arctic
Ice absorbs
10. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Mass Change
Calving
Average radiative flux reaching the atmosphere
All Greenhouse gases
11. 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
Indirect heat wave effect
air can warm dramatically
Snow and snow covered ice absorb
12. Warming- positive feedback - Cooling- negative feedback.
Ice-Albedo
Sea ice melt does not change sea level
Sea Ice
Average radiative flux reaching the atmosphere
13. Over the past century what has happened to the Earth's temperature?
Ice Discharge
Some regions of the Earth have warmed faster than other regions.
Thickness of the active layer and the permafrost depend on this
IPCC
14. 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.
Grounding Lines
More rain means no drought
Agricultural Drought
Greenhouse Gases
15. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Albedo
Arctic Atmosphere
Mass Balance
Severe coastal erosion
16. 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.
Albedos of Snow and Ice
Discontinuous
Ice Shelf
Ice Discharge
17. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
IPCC
Effect of Deforestation on CO-2
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
US and precipitation
18. 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
Ozone Hole
Black Carbon
Permafrost
Ocean water
19. 85%
Ice/snow
What effects the density
Sea-Ice Albedo
Atlantic Thermohaline Circulation
20. 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
doubles
In the stratosphere.
Heat wave
Hydrological Drought
21. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
All Greenhouse gases
Affect Floods and Droughts
Sea Ice Extent is Changing in Antarctica as well
Permafrost Degradation
22. Pollution: heat and sunlight cook the air and the chemical compounds which are in it. This combines with the nitrogen oxide and creates 'smog'. This makes breathing difficult for those with respiratory ailments.
Indirect heat wave effect
Thinner atmosphere
Ice shelf
Mass Change
23. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Ice Sheets
Infrared radiation
Sunspots
Stratospheric Ozone Depletion
24. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Dry
Arctic Atmosphere
Altimetry Pros
Thermokarst
25. LW - SW - 55% absorbed by surface
Energy Budget
Climate Change in the Arctic
Troposphere
What effects the density
26. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
% of Greenhouse Gases
30%
Surface Mass Balance
27. More common
winter
Black Carbon
Positive feedbacks both found in...
Inversion Layer Winter
28. 1.4 USA - 57 m total sea level equivalent
Antarctica
Stratospheric Ozone Depletion
Ice Sheets
75-OC
29. Most of the deserts are around 30 N and 30 S - where sinking air predominates
air can warm dramatically
Ice Cap
Some parts of the planet are dry because of their location
Altimetry
30. Low clouds are a ____ feedback; they will reflect more sunlight. Clouds reflect shortwave radiation but also absorb longwave radiation
30%
Agricultural Drought
Melt
Negative
31. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Ice loss
Ice Shelf
Heat wave
Accumulation
32. 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
Snow and snow covered ice absorb
Ice Sheets
Ice Discharge
Grounding Lines
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
Importance of ice sheets
Monthly maximums and minimums
Depth v Surface
50%
34. Frozen +2 years - Few centimeters to 1500 m
How we measure Mass Balance
Ice Shelf
Permafrost
Importance of ice sheets
35. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Inversion Layer (feedback)
IN the last 2 decades what we've seen
Shortwave Length
Atmospheric Composition
36. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Accumulation
Black Carbon
Sublimation
Sea ice melt does not change sea level
37. Laser radar - H V - Long time series - high accuracy - Density
Altimetry (height)
Ice Shelf
Wetter; drier
Discontinuous Permafrosrt
38. Where does the ozone protect us?
Carbon Dioxide
La Nia
In the stratosphere.
% of Greenhouse Gases
39. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Ozone Hole
Open talik
Thermokarst
30%
40. Total absorbed solar radiation
Permafrost
70%
Natural Causes of Warming
Accumulation
41. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Agricultural Drought
Contributions to CO2 from different activities
Thermokarst
Atmospheric Structure
42. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Hydrological Drought
Active Layer
Ice Cap
Atlantic Thermohaline Circulation
43. 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.
Mass Budget
Ice Shelf
Negative Ice-Albedo Feedback
Hydrological Drought
44. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Carbon Dioxide
Atmospheric Composition
The cryosphere
Ice in the Arctic
45. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Some parts of the planet are dry because of their location
Grounding Lines
Antarctica
Radiative Forcing
46. Volcanic eruptions - Sunspots - Wobbly Earth
Positive
Natural Causes of Warming
Antarctica
Is precipitation around the world increasing?
47. When meltwater seeps through a flowing glacier - it can lubricate the base and hasten the glacier's seaward flow.
Thermohaline Circulation
Sea-Ice Albedo
Dynamic thinning
Time Variable Gravity
48. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Melt
How a closed talik forms
Black Carbon
Rainy
49. The amount of light reflected by an object.
Surface Mass Balance
Melt
Albedo
Precipitation and High Latitudes
50. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Ocean-Ice-Atmosphere Interaction
Antarctica
Warm
Methane