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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. If the Earth is warmer - are we going to have the Hadley cell stronger or weaker? Hotter = heat rises which increases the circulation.
Ice shelf
Stronger
Infrared radiation
Climate Change in the Arctic
2. The past climate...for this reason - both keep good records of climate change.
In the Arctic where the air is cooler
Longwave Radiation
Thickness of the active layer and the permafrost depend on this
Climate Change in the Arctic
3. The depletion of stratospheric ozone layer in Antarctica in Springtime (august through October)
The Ozone Hole
Earth's tilt
In the stratosphere.
La Nia
4. 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.
Atmospheric Structure
Greenhouse Gases
Talik
Heat wave
5. The land-surface configuration that results from the melting of ground ice in a region where permafrost degrades is called Thermokarst.
Thinner atmosphere
Altimetry Cons
Thermohaline Circulation Effect
Thermokarst
6. Greenhouse gases are mixed in the ____
Dynamic thinning
Positive feedbacks both found in...
Thermokarst Lake
Troposphere
7. 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
The Ozone Hole
What effects the density
Some regions of the Earth have warmed faster than other regions.
In the Arctic where the air is cooler
8. 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
Archimedes' Principle
How a closed talik forms
Ice Sheets
Calving
9. Changes in the Earth's solar radiation levels can impact the climate. Shortterm warming cycles on Earth.
Shortwave Length
GHG
Sunspots
El Nio is in the coasts of...
10. Prolonged period of excessively hot weather - Which may be accompanied by high humidity.
Atlantic Thermohaline Circulation
Ice Sheets
Ocean water
Heat wave
11. 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
Thermohaline Circulation
El Nino
Thickness of the active layer and the permafrost depend on this
IN the last 2 decades what we've seen
12. Is not an externally imposed perturbation to the climate system.
Global warming and hot nights?
Why Water Vapor is not a climate forcing
Ice Shelf
What effects the density
13. Atmospheric Cooling - Both negative (stabilizing) feedbacks - It is not happening now - but it has happened in the past - Ice-albedo feedback was the dominant feedback during the ice ages.
Energy Budget
Inversion Layer Summer
Precipitation and High Latitudes
Negative Ice-Albedo Feedback
14. Refers to a body of freshwater - usually shallow - formed in a depression by melt water from thawing permafrost.
Atmospheric Circulation
Inversion Layer Summer
Thermokarst Lake
Through talik
15. Extent 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.
reduction in sea-ice
Cause of break of inversion layers or decrease in frequency
Mass Balance
Sea-Ice Albedo
16. Melting Point decreases
.75OC/km-1
Stronger
Layers of Earth
Effect of Deforestation on CO-2
17. Taliks are found under lakes because of the ability of water to store and vertically transfer heat energy - Vertical extent of the taliks found under lakes is related to the depth and volume of the overlying water body.
Today melting ice
doubles
GHG
How talik forms under lakes
18. Thawing permafrost weakens coastal lands. Risk of flooding in coastal wetlands. Pollution and toxins locked in the snow and ice will be released.
Global warming and hot nights?
GHG
Ice in the Arctic
Severe coastal erosion
19. x7 smaller - 7m total sea level equivalent.
Energy Budget
Carbon Dioxide
Greenland
Normal condition for air
20. 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.
IPCC
Global warming and hot nights?
Inversion Layer (feedback)
Inversion Layer Summer
21. Ocean retains ____ CO2
45%
Ice-Albedo
How we measure Mass Balance
25%
22. Sea ice and continental ice. This is caused by Atmospheric warming triggers.
Positive feedbacks both found in...
Grounding Lines
25%
Open talik
23. Peru and Ecuador to the equatorial central pacific - Causes irregular warming in sea surface
El Nio is in the coasts of...
Thickness of the active layer and the permafrost depend on this
Greenland
Black Carbon
24. Number of days when temperatures climb above average by a fixed amount.
Threshold departures
El Nino
Positive
Amount of light actually reaching the Earth
25. 10 : 1 - grounding ; surface
Altimetry Pros
Why the Arctic climate is special
Ice in the Arctic
Grounding v Surface Melting
26. Number of days that land among the hottest of all days in that month's long-term record.
What effects the density
Percentile departures
Carbon Dioxide
Inversion Layer Summer
27. Water vapor - 36-70% - carbon dioxide - 9-26% - methane - 4-9% - ozone - 3-7%
Thermokarst
Increases - decreases
Surface Mass Balance
% of Greenhouse Gases
28. This is the total mass change - difference between input and outputs—snow accumulation-ablation.
.7O Celsius over the past century.
What happens with the Ozone Hole
Mass Balance
25%
29. 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.
Dynamic thinning
Change in vegetation generates a further feedback
Antarctica
Melt
30. The large-scale ocean circulation that moves water between the deep and surface ocean which effects salinity and temperature change - Supplies heat to the polar-regions.
Energy Budget
Precipitation and High Latitudes
Thermohaline Circulation Effect
Reduction in sea-ice extent
31. 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
Positive
Inversion Layer (feedback)
32. Really measures volume.
Sea Ice
Troposphere
Ozone Hole
Altimetry
33. 1. They are the largest contributor to sea level rise 2. Can affect the thermohaline circulation (mainly in Greenland) 3. Are directly connected to climate change
Importance of ice sheets
1 m/yr; 10x
Inversion Layer Summer
Calving
34. Clouds 40~90% - Vegetation 10~15%
Stronger
More rain means no drought
Types of Albedo
Ice shelf
35. Mass balance due to processes that affect the surface of the ice sheet. Precipitation-evapotranspiration-runoff-blowing snow etc...
Carbon Dioxide
Surface Mass Balance
Ocean-Ice-Atmosphere Interaction
Depth v Surface
36. 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
Heat wave
Mass Change
1 m/yr; 10x
Thinner atmosphere
37. High cloud has a _____ effect and cool cloud has a ____ effect
30%
Warming; cooling
Contributions to CO2 from different activities
Thermohaline Circulation Effect
38. The heat input is either driven by the 1- thermohaline circulation associated with sea ice formation. The direct influx of intermediate warmth water.
Air pollution
Heat Source and Pressure
Thermohaline Circulation
Once every 4 years.
39. 1.4 USA - 57 m total sea level equivalent
Warming; cooling
Increase in the amount of water vapor or cloud vapor - Volcanic eruptions
Warm
Antarctica
40. How often does El Nio occur?
Major distinction between Kyoto Protocol and Convention
Ozone
Troposphere
Once every 4 years.
41. he increase of ozone concentration in the atmosphere helps ____ our planet
Warm
Monthly maximums and minimums
1 m/yr; 10x
In the stratosphere.
42. Measures input and output.
Mass Budget
Altimetry
Altimetry Cons
Dynamic thinning
43. Longwave radiation - any radiation with a long wave will heat up quickly.
Infrared radiation
Permafrost Degradation
Amount of light actually reaching the Earth
El Nino
44. 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.
Effect of Deforestation on CO-2
Ice Sheets
GHG
Thermokarst
45. Radiation absorbed by atmospheric greenhouse gases?
Atmospheric Composition?
15 percent (70% is not reflected but radiated to space from clouds - atmosphere - and Earth.)
Ice in the Arctic
20%
46. 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.
Negative Ice-Albedo Feedback
Through talik
Ice-Ocean Interactions
Discontinuous
47. Sea ice - Continental ice sheets - Permafrost (frozen soil) - Mountain glaciers - Snow cover
The cryosphere
Mass Change
Hydrological Drought
Reduction in sea-ice extent
48. ~15% of incident solar energy (albedo 85)
air can warm dramatically
Once every 4 years.
75-OC
Snow and snow covered ice absorb
49. If the mean annual air temperature is only slightly below 0 degrees C - permafrost will form only in spots that are sheltered.
Ice-Albedo
Indirect heat wave effect
Discontinuous
Thermohaline Circulation
50. CO2 - CH4 - O3 - H2O - N2O - CFCs
Very small portion
All Greenhouse gases
Inversion Layer Winter
GHG