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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. 78% nitrogen - 28% oxygen - Greenhouse gases: Have a more complex molecular structure and can absorb and re:radiate heat in all directions.
Absolute thresholds
Atmospheric Composition?
Changes in Arctic sea-ice Extent
Indirect heat wave effect
2. How much is the planet really warming?
Atmospheric Structure
.7O Celsius over the past century.
Sea-Ice Albedo
Some parts of the planet are dry because of their location
3. Cooler water and drought conditions.
All Greenhouse gases
Natural Causes of Warming
Is precipitation around the world increasing?
La Nia
4. South polar vortex - Temperatures drop below 80O Celsius in the lower stratosphere - At these temperatures the chemicals in the stratosphere freeze and form Polar Stratospheric Clouds (PSCS) - These increase the concentration of CFCs in turn destroyi
What happens with the Ozone Hole
Where rise in OC is greatest
Ice in the Arctic
Dynamic thinning
5. Changes over time in the highest and lowest single temperature observed during a given month of the year.
.75OC/km-1
Ozone Hole
Monthly maximums and minimums
Effect of Deforestation on CO-2
6. Land Based Ecosystems retain ____ CO2.
Deep tropics between 15O N and 15 O S are quite
30%
Wetter; drier
Some regions of the Earth have warmed faster than other regions.
7. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Sea ice melt does not change sea level
25%
Ice Discharge
El Nino
8. In _______ - the inversions are less frequent and weaker in the Arctic.
Ozone Hole
El Nio is in the coasts of...
summer
50%
9. In ________- inversion layer is more common in the Arctic
air can warm dramatically
Hydrological Drought
winter
Thermohaline Circulation
10. 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.
Some regions of the Earth have warmed faster than other regions.
Grounding Lines
Greenhouse Gases
Inversion Layer (feedback)
11. 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
45%
Surface Mass Balance
Shortwave Length
Ice Sheets
12. When inversion breaks up _______________. - Consequently - anything that breaks inversions or makes them form less often could produce major ground level warming.
IPCC
% of Greenhouse Gases
Threshold departures
air can warm dramatically
13. 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
Importance of ice sheets
Ozone Hole
US and precipitation
14. Help darkens the snow and ice surface - increasing the amount of energy that is absorbed.
Ozone Hole
30%
La Nia
Air pollution
15. Water vapor means more water up in the clouds and less in the ground!
Energy Budget
El Nio is in the coasts of...
Talik
More rain means no drought
16. 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.
Altimetry
Thermokarst Lake
Greenhouse Gases
winter
17. Longwave radiation - any radiation with a long wave will heat up quickly.
Albedos of Snow and Ice
Infrared radiation
Earth's tilt
Discontinuous Permafrosrt
18. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Ocean-Ice-Atmosphere Interaction
Stronger
winter
Average radiative flux reaching the atmosphere
19. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Infrared radiation
How talik forms under lakes
Atlantic Thermohaline Circulation
Carbon Dioxide
20. Precipitation extremes appear to generally increase across the planet at especially high latitudes.
Ocean water
Precipitation and High Latitudes
Discontinuous Permafrosrt
Ice-Ocean Interactions
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.
Is precipitation around the world increasing?
Some parts of the planet are dry because of their location
How to define a heatwave
Change in vegetation generates a further feedback
22. Summer increase in cloud cover - Winter decrease in cloud cover.
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183
23. 342 W/m squared - DWEC - These things reflect sunlight (30%): water vapor - clouds - dust particles - earth's surface
Average radiative flux reaching the atmosphere
Surface Mass Balance
IPCC
Radiative Flux
24. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Why Water Vapor is not a climate forcing
Severe coastal erosion
Precipitation and High Latitudes
Reduction in sea-ice extent
25. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Surface Mass Balance
How a closed talik forms
Thinner atmosphere
Albedos of Snow and Ice
26. 23 -45 degrees. The Larger the tilt the larger the variability of the seasons.
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27. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Active Layer
Monthly maximums and minimums
Heat Source and Pressure
Severe coastal erosion
28. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
Grounding Lines
Arctic Atmosphere
Mass Balance
Hydrological Drought
29. Pockets of ice in the topmost permafrost caused by thawing which create an underground lake.
Some regions of the Earth have warmed faster than other regions.
Grounding Lines
Threshold departures
Thermokarst
30. The buoyant force is equal to the weight of the displaced water.
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31. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
summer
Atlantic Thermohaline Circulation
Through talik
Thermokarst
32. Hydrological drought is associated with the effect of low rainfall on water levels in rivers -!reservoirs -!lakes and aquifers.
Sublimation
Hydrological Drought
Ice in the Arctic
Talik
33. The Earth emits this.
Longwave Radiation
Ice loss
Ozone
Ice in the Arctic
34. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Ocean water
Antarctica
30%
Rainy
35. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
Dry
Albedos of Snow and Ice
Hydrological Drought
36. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Reduction in sea-ice extent
Atmospheric Composition
Black Carbon
Ice Motion
37. The amount of light reflected by an object.
reduction in sea-ice
20%
Ozone Hole
Albedo
38. Floating extensions are ice shelves - rivers of ice are ice streams or outlet glaciers - the junctions with the ocean are called the grounding line.
Inversion Layer (feedback)
Mass Budget
Ocean-Ice-Atmosphere Interaction
Ice Discharge
39. Volcanic eruptions - Sunspots - Wobbly Earth
Heat wave
Antarctica
Sea Ice Extent is Changing in Antarctica as well
Natural Causes of Warming
40. Number of days that exceed a given temperature
Absolute thresholds
Warming; cooling
All Greenhouse gases
Atmospheric Structure
41. Due to a set of mutually reinforcing processes - climate change appears to be progressing in the arctic more quickly than in any other region on Earth.
Carbon Dioxide
Climate Change in the Arctic
Antarctica
Inversion Layer Winter
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
Thermohaline Circulation
Depth v Surface
doubles
Thermohaline Circulation Effect
43. All processes that add snow or ice to a glacier or to flowing ice or snow cover.
Accumulation
Atmospheric Composition
Permafrost
Atlantic Thermohaline Circulation
44. Reduction of snow and ice cover - Changes in atmospheric circulation.
Positive feedbacks both found in...
Cause of break of inversion layers or decrease in frequency
Antarctica
Grounding Lines
45. LW - SW - 55% absorbed by surface
Energy Budget
Surface Mass Balance
Shortwave Length
Mass Change
46. In troposphere = greenhouse warming gas - However - most of it is in the stratosphere.
Ozone
Snow and snow covered ice absorb
Ice/snow
Sunspots
47. CO2 GHG forcing - H2O - dominant/major GHG
winter
Through talik
Methane
GHG
48. CO2 ____ in winter in the NH and ____ decreases during the 'greening season'
Infrared radiation
Active Layer
Once every 4 years.
Increases - decreases
49. Closed talik can develop when lakes fill in with sediment and become deposits of dead plant material (bog).
Altimetry Pros
How a closed talik forms
Positive
Ozone Hole
50. What can cause a change in the Earth's climate balance?
Wetter; drier
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Some parts of the planet are dry because of their location
The Ozone Hole