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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. How often does El Nio occur?
All Greenhouse gases
25%
Active Layer
Once every 4 years.
2. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Albedo
Grounding Lines
Radiative Forcing
Once every 4 years.
3. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Positive
Surface Mass Balance
Is precipitation around the world increasing?
In the Arctic where the air is cooler
4. Antarctica - stratosphere - Sep-Oct
What happens with the Ozone Hole
Heat wave
Ozone Hole
Some regions of the Earth have warmed faster than other regions.
5. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
Global warming and hot nights?
Sea Ice
Ice loss
70%
6. he increase of ozone concentration in the atmosphere helps ____ our planet
70%
Warm
Ice Motion
Negative Ice-Albedo Feedback
7. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Sublimation
air can warm dramatically
Sunspots
Surface Mass Balance
8. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Troposphere
Methane
Surface Mass Balance
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
9. Rainy on yearly average. In these regions - rising air predominates.
Sea ice melt does not change sea level
Thermokarst
Deep tropics between 15O N and 15 O S are quite
Grounding Lines
10. What can cause a change in the Earth's climate balance?
Mass Budget
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Ocean-Ice-Atmosphere Interaction
The cryosphere
11. Melting Point decreases
Amount of light actually reaching the Earth
.75OC/km-1
Hydrological Drought
Changes in Arctic sea-ice Extent
12. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Positive feedbacks both found in...
Methane
Layers of Earth
Ice in the Arctic
13. Poor resolution (200-400 km) does not allow us to distinguish glaciers and basins.
Warming; cooling
Frozen Soil
Altimetry Cons
Contributions to CO2 from different activities
14. Arctic warms faster than other parts of the globe in response to a given increase in greenhouse gasses - More direct route to warming - In the Arctic a greater fraction of any increase in radiation absorbed by the surface goes directly into warming t
Cloud Feedbacks
reduction in sea-ice
Why the Arctic climate is special
Sea ice melt does not change sea level
15. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
Thermohaline Circulation
air can warm dramatically
Permafrost
Percentile departures
16. 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
Average radiative flux reaching the atmosphere
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Frozen Soil
Wetter; drier
17. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Surface Mass Balance
25%
How the cryosphere is affected by climate change
Ice/snow
18. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Energy Budget
Reduction in sea-ice extent
Types of Albedo
Average radiative flux reaching the atmosphere
19. 20% human produced CO2 emissions. Tropical forests hold around 50% of the carbon present in vegetation on Earth.
Grounding Lines
Effect of Deforestation on CO-2
Methane
What happens with the Ozone Hole
20. Number of days when temperatures climb above average by a fixed amount.
How to define a heatwave
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
What effects the density
Threshold departures
21. 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.
Wetter; drier
Active Layer
Change in vegetation generates a further feedback
Time Variable Gravity
22. How much is the planet really warming?
.7O Celsius over the past century.
45%
Ice in the Arctic
Some regions of the Earth have warmed faster than other regions.
23. Where does the ozone protect us?
Altimetry
Albedos of Snow and Ice
Thermokarst
In the stratosphere.
24. 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
Where rise in OC is greatest
Ice Sheets
Why ice-albedo feedback is a big deal in the Arctic
Changes in Arctic sea-ice Extent
25. Radiation that comes from the Sun - Visible light - 'near infrared' - ultraviolet radiation.
Frozen Soil
Shortwave Length
IPCC
doubles
26. In ________- inversion layer is more common in the Arctic
Melt
Why the Arctic climate is special
Ice/snow
winter
27. 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
Methane
Absolute thresholds
Active Layer
28. Over the Northern Hemisphere than the tropics.
More rain means no drought
Where rise in OC is greatest
Stronger
Grounding v Surface Melting
29. High cloud has a _____ effect and cool cloud has a ____ effect
Discontinuous
air can warm dramatically
Warming; cooling
Accumulation
30. Grace - Tells us how much mass change we have - M - This is the measure of gravity (gives us the mass) - Directly measure mass change - Poor resolution
Dry
Increases - decreases
Mass Change
Active Layer
31. 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
Antarctica
Severe coastal erosion
Rainy
Permafrost
32. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Inversion Layer Summer
Altimetry (height)
Ice Motion
Ice Cap
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
Thinner atmosphere
Monthly maximums and minimums
Dry
Absolute thresholds
34. Forms in a mosaic of favoured locations.
Inversion Layer Summer
Energy Budget
Discontinuous Permafrosrt
Atmospheric Composition
35. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
% of Greenhouse Gases
Atmospheric Composition
El Nio is in the coasts of...
IN the last 2 decades what we've seen
36. Volcanic eruptions - Sunspots - Wobbly Earth
The cryosphere
Natural Causes of Warming
Questions to think about
Grounding Lines
37. Laser radar - H V - Long time series - high accuracy - Density
IN the last 2 decades what we've seen
Altimetry (height)
30%
Meteorological Drought
38. 1. Altimetry survey 2. Time-variable gravity 3. Ice motion + Regional Climate Modeling
Atmospheric Circulation
How we measure Mass Balance
Ozone Hole
Monthly maximums and minimums
39. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Active Layer
% of Greenhouse Gases
Time Variable Gravity
Earth's tilt
40. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Rainy
Absolute thresholds
Precipitation and High Latitudes
La Nia
41. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Atmospheric Composition?
Thermokarst
Global warming and hot nights?
Atlantic Thermohaline Circulation
42. 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
.7O Celsius over the past century.
doubles
La Nia
How to define a heatwave
43. 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
Longwave Radiation
How we measure Mass Balance
Permafrost Degradation
Radiative Flux
44. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
reduction in sea-ice
Meteorological Drought
IPCC
Once every 4 years.
45. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
summer
Thinner atmosphere
Archimedes' Principle
Mass Balance
46. Total absorbed solar radiation
70%
What effects the density
Why ice-albedo feedback is a big deal in the Arctic
Grounding Lines
47. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Thermokarst
Layers of Earth
30%
Ocean water
48. 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
Wetter; drier
Thinner atmosphere
In the Arctic where the air is cooler
Heat Source and Pressure
49. Absolute thresholds - Monthly maximums and minimums - Threshold departures - Percentile departure - Atmospheric Water Vapor: More water vapor in the air - warmer nights!
Warm
How to define a heatwave
Sea Ice Extent is Changing in Antarctica as well
How the cryosphere is affected by climate change
50. Greenhouse gases are a ___ portion of the atmosphere
Why Water Vapor is not a climate forcing
Through talik
Very small portion
Archimedes' Principle