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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. The major distinction between the Protocol and the Convention is that while the Convention encouraged industrialized countries to stabilize GHG emissions - the Protocol commits them to do so.
1 m/yr; 10x
Why the Arctic climate is special
Major distinction between Kyoto Protocol and Convention
Severe coastal erosion
2. The last portion of a glacier grounded to bedrock - after this line there are ice shelves.
Cloud Feedbacks
Radiative Forcing
Grounding Lines
Severe coastal erosion
3. Nitrogen (N2 78%) and Oxygen (O2 21%) - Their linear 2 atom molecular structure
Ozone Hole
Longwave Radiation
Atmospheric Composition
Active Layer
4. Some parts of the planet are dry because of their location: most of the deserts are around 30 N and 30 S - where sinking air predominates
Sea-Ice Albedo
Dry
Antarctica
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
5. CO2 - CH4 - O3 - H2O - N2O - CFCs
Ice/snow
Ocean-Ice-Atmosphere Interaction
Heat wave
All Greenhouse gases
6. Atmosphere retains ____ CO2
45%
Layers of Earth
Ocean-Ice-Atmosphere Interaction
Permafrost
7. Number of days that exceed a given temperature
Percentile departures
Absolute thresholds
Rainy
Active Layer
8. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Through talik
Heat wave
How to define a heatwave
Ocean-Ice-Atmosphere Interaction
9. 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
30%
Atmospheric Circulation
El Nino
Archimedes' Principle
10. A dome shaped cover of perennial ice and snow.
Ice Cap
Stronger
Ocean water
30%
11. 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%
Average radiative flux reaching the atmosphere
Ocean water
Albedos of Snow and Ice
Ice-Albedo
12. Is defined usually on the basis of the degree of dryness (in comparison to some 'normal' or average amount
45%
Hydrological Drought
Wetter; drier
Meteorological Drought
13. Amount of light absorbed by surface
Antarctica
What effects the density
Ocean water
50%
14. 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
Radiative Flux
Positive feedbacks both found in...
Earth's tilt
15. 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.
Ozone
More rain means no drought
50%
Permafrost Degradation
16. 1.4 USA - 57 m total sea level equivalent
IN the last 2 decades what we've seen
Heat wave
Antarctica
Positive
17. The high pressure decreases the melting point and favors melting - Melt water being less dense rises along the water column along the ice shelf bottom and may either escape the cavity or refreeze at some intermediate depth. Melting point decreases:
Cloud Feedbacks
Thermohaline Circulation
Once every 4 years.
How we measure Mass Balance
18. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
How to define a heatwave
Ice loss
Positive
The cryosphere
19. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
Thermokarst
Radiative Flux
Methane
Antarctica
20. 1. Land usage changes 2. Seasonal timing 3. Rising CO2 levels may be a factor
Affect Floods and Droughts
Average radiative flux reaching the atmosphere
75-OC
Indirect heat wave effect
21. High vs low
Grounding Lines
Closed talik
Cloud Feedbacks
In the Arctic where the air is cooler
22. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Methane
Why Water Vapor is not a climate forcing
Open talik
Active Layer
23. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
What happens with the Ozone Hole
The Ozone Hole
Talik
Nitrous Oxide (N2O)
24. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Ocean water
Climate Change in the Arctic
Sublimation
Natural Causes of Warming
25. Forms from frozen ocean water - Floats on the ocean surface - Grows over the winter - melts in the summer
reduction in sea-ice
Sea Ice
Ozone Hole
Indirect heat wave effect
26. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Albedos of Snow and Ice
Sea Ice Extent is Changing in Antarctica as well
Thermohaline Circulatoin
Accumulation
27. Melting Point decreases
.75OC/km-1
Stratospheric Ozone Depletion
IPCC
Threshold departures
28. Warming- positive feedback - Cooling- negative feedback.
Ice-Albedo
Agricultural Drought
Altimetry
What effects the density
29. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
75-OC
Inversion Layer (feedback)
Positive feedbacks both found in...
Ice Shelf
30. The past climate...for this reason - both keep good records of climate change.
Frozen Soil
doubles
Thickness of the active layer and the permafrost depend on this
Albedo
31. Is unfrozen ground that is exposed to the ground surface and to a larger mass of unfrozen ground beneath it.
Through talik
Today melting ice
In the stratosphere.
Active Layer
32. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
Thermokarst
US and precipitation
Layers of Earth
Surface Mass Balance
33. O Climate change in the Arctic is occurring now - Changes have been huge already
Increases - decreases
Calving
Today melting ice
Atlantic Thermohaline Circulation
34. 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
Black Carbon
Layers of Earth
Atmospheric Structure
35. 240 w/m squared
Ice Motion
Why ice-albedo feedback is a big deal in the Arctic
Amount of light actually reaching the Earth
How to define a heatwave
36. Like weighing oneself on the scale.
Mass Balance
Time Variable Gravity
Very small portion
30%
37. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
Black Carbon
Troposphere
Ocean water
Thinner atmosphere
38. Ice melting rapidly? What type causes sea level to rise? What have been the main contributors to sea level rise so far? What are the impacts of melting ice? - On nature - On humans
Questions to think about
Melt
Agricultural Drought
Stronger
39. Ozone layer in high stratosphere (25-40 km altitude) absorbs about 95-99% of ultraviolet radiation.
Sea-Ice Albedo
Accumulation
Mass Budget
Stratospheric Ozone Depletion
40. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Sea-Ice Albedo
Active Layer
Altimetry Cons
air can warm dramatically
41. Same amount of H2O - Mass does not change - Density of ice < density of water - Volume of ice > volume of water
Thermokarst
Altimetry
Dynamic thinning
Sea ice melt does not change sea level
42. How often does El Nio occur?
Once every 4 years.
US and precipitation
Talik
Importance of ice sheets
43. Greenhouse gases are mixed in the ____
Increases - decreases
Sea ice melt does not change sea level
How to define a heatwave
Troposphere
44. The buoyant force is equal to the weight of the displaced water.
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45. 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
Carbon Dioxide
What happens with the Ozone Hole
25%
Sea ice melt does not change sea level
46. ~15% of incident solar energy (albedo 85)
Methane
Snow and snow covered ice absorb
Sunspots
Climate Change in the Arctic
47. In average: +1% in respect to 100 years ago.
Ozone Hole
air can warm dramatically
Is precipitation around the world increasing?
Melt
48. The amount of light reflected by an object.
Very small portion
Albedo
Ice loss
Cause of break of inversion layers or decrease in frequency
49. 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
Agricultural Drought
What happens with the Ozone Hole
Stronger
Atmospheric Composition?
50. The Earth emits this.
Ice absorbs
Ice loss
Longwave Radiation
winter