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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. Holds unique and key information - Are highly interconnected - Respond and drive climate change - Are the largest freshwater reservoirs of the planet - Ice cores tell us that in climate records - nothing is regular and ice sheet plays major role.
Ice Sheets
Dynamic thinning
Ice-Ocean Interactions
Ozone Hole
2. 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
Reduction in sea-ice extent
Permafrost
Thermokarst
Ocean water
3. An area of unfrozen ground that is open to the ground surface but otherwise enclosed in permafrost.
Open talik
Infrared radiation
How to define a heatwave
Atmospheric Composition?
4. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Greenhouse Gases
Severe coastal erosion
Ocean water
Deep tropics between 15O N and 15 O S are quite
5. Top layer of soil that thaws during the summer and freezes again during autumn. - Between 1 and 3 m thick.
Sea ice melt does not change sea level
Stratospheric Ozone Depletion
Active Layer
Altimetry Pros
6. Over the Northern Hemisphere than the tropics.
Where rise in OC is greatest
Threshold departures
Major distinction between Kyoto Protocol and Convention
Calving
7. Same as heating an apartment v home - Thinner atmosphere than tropics; warms faster.
Once every 4 years.
Ice Cap
.75OC/km-1
Arctic Atmosphere
8. x7 smaller - 7m total sea level equivalent.
Open talik
El Nino
Greenland
Absolute thresholds
9. 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
Discontinuous
Effect of Deforestation on CO-2
Thermohaline Circulation
20%
10. 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
1 m/yr; 10x
In the troposphere that we live in.
El Nino
Reduction in sea-ice extent
11. Where does the ozone protect us?
Hydrological Drought
Why ice-albedo feedback is a big deal in the Arctic
In the stratosphere.
Ice Sheets
12. ~10% of incident solar energy (albedo 90)
El Nio is in the coasts of...
Ice absorbs
What happens with the Ozone Hole
Dynamic thinning
13. Sea ice extent in Antarctica is rapidly reducing. Seasonal variability. People - Animals and Ice
Sea Ice Extent is Changing in Antarctica as well
45%
Troposphere
Discontinuous
14. In ________- inversion layer is more common in the Arctic
winter
Thickness of the active layer and the permafrost depend on this
Ice shelf
Discontinuous
15. Laser radar - H V - Long time series - high accuracy - Density
Carbon Dioxide
Precipitation and High Latitudes
Ocean water
Altimetry (height)
16. Clouds 40~90% - Vegetation 10~15%
Today melting ice
Thermohaline Circulatoin
Permafrost Degradation
Types of Albedo
17. CO2 GHG forcing - H2O - dominant/major GHG
How we measure Mass Balance
GHG
Rainy
Snow and snow covered ice absorb
18. Troposphere - Stratosphere (Ozone Layer) - Mesosphere - Ionosphere
Methane
Atmospheric Structure
US and precipitation
Sea ice melt does not change sea level
19. 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:
Thermohaline Circulation
Dry
Ice Sheets
Agricultural Drought
20. 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
Where rise in OC is greatest
What happens with the Ozone Hole
Open talik
Severe coastal erosion
21. Is not an externally imposed perturbation to the climate system.
Why Water Vapor is not a climate forcing
Thermokarst
What happens with the Ozone Hole
Sunspots
22. Greenhouse gases are a ___ portion of the atmosphere
Very small portion
Climate Change in the Arctic
Rainy
Greenhouse Gases
23. 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
Natural Causes of Warming
30%
Inversion Layer Winter
24. Radiation absorbed by atmospheric greenhouse gases?
Thinner atmosphere
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Deep tropics between 15O N and 15 O S are quite
summer
25. 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
Percentile departures
Why the Arctic climate is special
Air pollution
Ice loss
26. 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
1 m/yr; 10x
Hydrological Drought
Change in vegetation generates a further feedback
27. 240 w/m squared
Questions to think about
Amount of light actually reaching the Earth
30%
Grounding v Surface Melting
28. 2ppm of the atmosphere - less than 20% of greenhouse gases - 1/3 greenhouse gases effect of CO2
GHG
Methane
Surface Mass Balance
How a closed talik forms
29. Number of days that exceed a given temperature
Hydrological Drought
Absolute thresholds
Radiative Forcing
Monthly maximums and minimums
30. Less frequent and weaker
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Inversion Layer Summer
Sea ice melt does not change sea level
Talik
31. A process whereby slabs of ice at the glacier margin mechanically fracture and detach from the main ice mass -
Greenhouse Gases
Ice shelf
Calving
50%
32. High clouds are a ____ feedback; larger greenhouse warming - Clouds reflect shortwave radiation but also absorb longwave radiation
Ice-Albedo
Positive
How a closed talik forms
1 m/yr; 10x
33. 1. We live in troposphere. Greenhouse gases here warm up the Earth 2. Above stratosphere. The ozone in this layer protects us.
Layers of Earth
Ice absorbs
Snow and snow covered ice absorb
Accumulation
34. 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
Ice Sheets
Ozone Hole
Questions to think about
35. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Sunspots
How we measure Mass Balance
Ice Sheets
Amount of light actually reaching the Earth
36. In _______ - the inversions are less frequent and weaker in the Arctic.
Permafrost Degradation
Inversion Layer Summer
In the Arctic where the air is cooler
summer
37. 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.
Natural Causes of Warming
Deep tropics between 15O N and 15 O S are quite
Ice Shelf
Hydrological Drought
38. 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
Atmospheric Circulation
Thinner atmosphere
Natural Causes of Warming
Closed talik
39. O Unfrozen soil that stays within the permafrost.
Surface Mass Balance
Today melting ice
Inversion Layer (feedback)
Talik
40. The Day After Tomorrow - Circulation will slow by 10% to 50% in the next century
Atlantic Thermohaline Circulation
Calving
Mass Budget
What effects the density
41. SMB- mass balance due to processes that affect the surface of the ice sheet. Precipitation- evapotranspiration-runoff-blowing snow etc.
Surface Mass Balance
50%
Positive feedbacks both found in...
Ocean water
42. 1.4 USA - 57 m total sea level equivalent
Antarctica
Heat wave
Major distinction between Kyoto Protocol and Convention
winter
43. Industrial product - 300 ppb (parts per billion)
Altimetry
Thinner atmosphere
Indirect heat wave effect
Nitrous Oxide (N2O)
44. Cooler water and drought conditions.
Global warming and hot nights?
Ice-Ocean Interactions
La Nia
1 m/yr; 10x
45. The difference between the incoming radiation energy and the outgoing radiation energy - A measure of the net energy.
Arctic Atmosphere
The cryosphere
Radiative Forcing
Time Variable Gravity
46. Rainy on yearly average. In these regions - rising air predominates.
Negative
Closed talik
Deep tropics between 15O N and 15 O S are quite
Thermokarst
47. Positive Albedo Feedback - increase in temperature melts ice and snow reduces albedo increases temperature melts ice and snow reduces albedo... ETC
Ice/snow
Ice Motion
IPCC
Why the Arctic climate is special
48. They saw a massive thinning of the ice where it enters into the ocean - This is due to the pronounced melting of the ice once it is in contact with the ocean. Melt rates of 25 m/year near the grounding lines and more than 10 m/year on average.
Ice-Ocean Interactions
Layers of Earth
.75OC/km-1
Wetter; drier
49. Summer increase in cloud cover - Winter decrease in cloud cover.
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50. he increase of ozone concentration in the atmosphere helps ____ our planet
Sea-Ice Albedo
winter
Inversion Layer Winter
Warm