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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. Over the Northern Hemisphere than the tropics.
Albedo
Heat wave
Where rise in OC is greatest
Troposphere
2. 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
Ice Shelf
Methane
Sea Ice
3. Set up in 1988 by WMO and UNEP.
Ocean water
50%
Snow and snow covered ice absorb
IPCC
4. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
winter
Negative Ice-Albedo Feedback
Thermohaline Circulation Effect
Severe coastal erosion
5. Number of days when temperatures climb above average by a fixed amount.
Threshold departures
Reduction in sea-ice extent
45%
30%
6. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Frozen Soil
Discontinuous
Ice/snow
Major distinction between Kyoto Protocol and Convention
7. Higher temperature increases atmospheric water vapor @ global scale more water vapor in the air that causes nights to stay warmer.
More rain means no drought
How we measure Mass Balance
Is precipitation around the world increasing?
Global warming and hot nights?
8. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Average radiative flux reaching the atmosphere
Global warming and hot nights?
Thermohaline Circulatoin
Active Layer
9. 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.
Change in vegetation generates a further feedback
Today melting ice
Positive feedbacks both found in...
Meteorological Drought
10. 240 w/m squared
Layers of Earth
Amount of light actually reaching the Earth
Altimetry Cons
El Nio is in the coasts of...
11. Ice sheets have a very ____ Albedo
Very small portion
Strong
Calving
Thermohaline Circulation
12. The warmer the temperature - the deeper the active layer - thaws and refreezes every year - Permafrost below freezing for two or more years.
Active Layer
Importance of ice sheets
Radiative Flux
Atmospheric Composition?
13. Water vapor means more water up in the clouds and less in the ground!
More rain means no drought
Dynamic thinning
Thermohaline Circulatoin
Ozone Hole
14. Heat is provided by outside sources that flow down the continental slope to reach the deepest part of the glacier. High pressure decreases the melting point and favors melting.
Thermohaline Circulatoin
Ice Sheets
Negative Ice-Albedo Feedback
Hydrological Drought
15. Reduction of Summer Sea- will increase the warming because less energy will be reflected back to the atmosphere by the ice and more will be absorbed by the ocean - Snow and snow covered ice absorb 15% of incident solar energy - Ice absorbs 10% of inc
Reduction in sea-ice extent
Longwave Radiation
20%
Thinner atmosphere
16. Permafrost- A frozen soil
Frozen Soil
Grounding Lines
Inversion Layer (feedback)
Depth v Surface
17. Slow steady decline of about 4% per decade in the total volume of Earth's stratospheric ozone.
Sea Ice Extent is Changing in Antarctica as well
Ozone Hole
Permafrost
Sunspots
18. 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.
Depth v Surface
Ice loss
How to define a heatwave
Closed talik
19. The past climate...for this reason - both keep good records of climate change.
Thickness of the active layer and the permafrost depend on this
Methane
Positive feedbacks both found in...
Grounding Lines
20. InSAR - +snow/-ice loss - ice dynamics - requires a lot of data.
Ice Motion
Methane
Thickness of the active layer and the permafrost depend on this
Severe coastal erosion
21. Cooler water and drought conditions.
Talik
El Nio is in the coasts of...
Active Layer
La Nia
22. Unfrozen ground that is found within a mass of permafrost
Ocean-Ice-Atmosphere Interaction
Antarctica
Closed talik
Negative Ice-Albedo Feedback
23. Concentration of 380 ppmv - Have risen about 40% - Preindustrial~ 270~280 ppmv
Absolute thresholds
Carbon Dioxide
Closed talik
Changes in Arctic sea-ice Extent
24. Measures input and output.
IN the last 2 decades what we've seen
What effects the density
Talik
Mass Budget
25. 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
Increases - decreases
More rain means no drought
Permafrost
Strong
26. Just remember the general direction of the circulation - Rising northern pacific. You start in between Greenland and Europe (youngest water) - Oldest water is in the Pacific Ocean - Salty water> fresh water - Cold Water > Warm Water
Melt
Strong
Once every 4 years.
Thermohaline Circulation
27. The transition of a substance from the solid phase directly to the vapor phase - or vice versa - without passing through an intermediate liquid phase.
Methane
Ocean water
Grounding Lines
Sublimation
28. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Global warming and hot nights?
Carbon Dioxide
Sunspots
Albedo
29. Temperature needed to melt at depth is much lower than that needed to melt at the surface.
Active Layer
Climate Change in the Arctic
Depth v Surface
Contributions to CO2 from different activities
30. 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
Ice Sheets
In the stratosphere.
Mass Budget
50%
31. A climate forcing agent formed through the incomplete combustion of fossil fuels - biofuel - and biomass; emitted both anthropogenic:ally and naturally.
Earth's tilt
Monthly maximums and minimums
Black Carbon
Surface Mass Balance
32. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
Sea-Ice Albedo
Inversion Layer (feedback)
Indirect heat wave effect
The cryosphere
33. By contrast reflects only about 7% of solar radiation (Albedo~7%) - absorbing 93%.
All Greenhouse gases
Surface Mass Balance
Ocean water
Ice/snow
34. SALTY WATER = MORE DENSE - Maximum density at 4OC - This is why ice melting is a big deal; if the whole circle slows down - Ice bergs are fresh water higher sea level rise.
Carbon Dioxide
70%
What effects the density
Contributions to CO2 from different activities
35. Rain is getting harder and the rain is lasting longer since the past couple of decades and will continue for that amount.
US and precipitation
Stratospheric Ozone Depletion
GHG
Time Variable Gravity
36. The buoyant force is equal to the weight of the displaced water.
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37. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Contributions to CO2 from different activities
Ocean water
Stronger
Atmospheric Composition?
38. High cloud has a _____ effect and cool cloud has a ____ effect
air can warm dramatically
Warming; cooling
Effect of Deforestation on CO-2
GHG
39. Descending Air dry - Convection cells are wet.
Atmospheric Circulation
Air pollution
Greenland
Why the Arctic climate is special
40. Total absorbed solar radiation
Depth v Surface
Permafrost Degradation
Layers of Earth
70%
41. Number of days that land among the hottest of all days in that month's long-term record.
Some regions of the Earth have warmed faster than other regions.
Strong
Percentile departures
What happens with the Ozone Hole
42. Greenhouse gases are a ___ portion of the atmosphere
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Carbon Dioxide
Mass Balance
Very small portion
43. Rainy on yearly average. In these regions - rising air predominates.
Frozen Soil
Heat Source and Pressure
Ice loss
Deep tropics between 15O N and 15 O S are quite
44. Ice flowing from the middle of Greenland to the edges and melting. 90 feet a day- speed that ice is moving.
Negative Ice-Albedo Feedback
Hydrological Drought
How to define a heatwave
Ice Discharge
45. ~10% of incident solar energy (albedo 90)
Altimetry
Natural Causes of Warming
Ice absorbs
Grounding Lines
46. 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
Why ice-albedo feedback is a big deal in the Arctic
Thermohaline Circulation Effect
Major distinction between Kyoto Protocol and Convention
Ozone Hole
47. A thick - floating slab of freshwater ice extending from coast to coast.
Some parts of the planet are dry because of their location
Questions to think about
Thermokarst
Ice shelf
48. he increase of ozone concentration in the atmosphere helps ____ our planet
Greenland
Strong
Warm
Positive feedbacks both found in...
49. Is not an externally imposed perturbation to the climate system.
What effects the density
winter
Accumulation
Why Water Vapor is not a climate forcing
50. 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.
Rainy
Permafrost Degradation
Atmospheric Composition?
Strong